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I<br />

,~<br />

I<br />

AMSC WA<br />

MILITARY HANDBOOK<br />

GIOSSary of hlapp~wj,<br />

Chatiing, and Geodetic Terms<br />

ruSTRIBuTlo~ STAT-T k<br />

distribution Ie unllmlted.<br />

NOT MEASUREMENT<br />

I GI?m,~lrlVE<br />

aGm- . . . . —<br />

I<br />

\<br />

MIL -HDBK-850<br />

~<br />

--- _. ._.<br />

m---------- nsYuCGTtiFtMS —- —-<br />

Approved for public release;<br />

FOURTH EDITION 1981<br />

AREA MCGT<br />

-4


MIL-HDBK-850<br />

FOREWORD<br />

i. This military hsndbock is apprwad for use by afl De~rfmanfs and Agancrns of the Departmanl<br />

of Defanaa.<br />

2. Benefnial commank (mcammandstkms, additkms, deletions) and any pertinent data wh~h<br />

my bS of u= in imPW@ Ihh d0CIJm4Mi 6houid bsI sddrassad 10 DMA~lJ), Stop A-10, S913<br />

Las Highway, Fairfax, Virginia, 22031-2137, by using Ihe Sfsndardization Document Prop@al (DD<br />

Form 1426) appearing al ths and d this daoumanl or by latter.<br />

3. The purpose of this glossary ie to provide a c~ahsnshfe and sufhofitelfve aouma of cument<br />

usage of mapping, charting, and gsodel”k terms for sII Iavafs of users 10 help them oommunksta<br />

effacthrefy. TWs adffian of the gba6ary In addiiion to the main gbasary of terms, includes a fiit of<br />

MC&G misted abbreviatbns, acronyms, end inifiifs commonfy used wtihin DoD. If alw includes a<br />

section on Mapping, Charting 6 Geodesy qfsn”KsfLens.<br />

4. The terms and definitions in lhis pubfiialion ware salectad from authoritative glossaries and<br />

dcliancwies. and from technical pubkstions end papers concerned with the many disciplines<br />

associated with mapping, charting, end gaedasy. Numerous changes, additions, and dalelions<br />

were made effer a Itmmugh review by Defense Mapping Agenoy components and by the<br />

Depmlmants of the Army, Navy, and Ah Force.<br />

5. This publbatlon b not a substitute for the Department of Defense Dictionary of hWlary<br />

and Asaaciatsd Terms (JOINT PUB 1-02), formatly JCS PUB 1, which the Secretary 04 Defanse has<br />

directed to be used throughout the Deparfmanl of Defense. Terms included herein wfrkh are<br />

deaignatd “(JCS)” ware extractsd from and defined as stated in JOINT PUB 1-02. In mms<br />

inetancea, the JCS definition has been expended 10 includs mare detailed or supplementary<br />

informrnkrn. This sddflionel matter is set df trj braokete and is not to be wnstrued es changing or<br />

conflicting with fhe JCS definition. JCS terms whbh have been acceptsd by NATO end by the<br />

lnler-Amerium Defense Board ere se designated in JOINT PUB 1-02. Only thoss NATO terms<br />

whiih do not sppasr in JOINT PUB 1-o2 are aa inrkakt in ths gbaaery,<br />

6. The daaignafion “(USPLS)” indicstas U.S. PuMc Land Suwey ferms similsrty defined by the<br />

Bumou of Land Msnagemenf, U.S. Dapsrtmsnt of Interior.<br />

7. Alphabeliz.alicm of terms in this glaaaaIY folbws the rdandard A through Z order, except fhat<br />

mulfiward ferms are alphsbatizad according to the inifiil word.<br />

& Muffiile definitions for e single term are numbered and, wherever apptkble, are identified wilh<br />

the appmpriafe science, discipline, or function in parentheses. Al the end of some definitions the<br />

uss~s affenfian is directed to related terms by tha expression ‘Sss ebo.”<br />

S. When two or more terms have Identical maaning, ths definition has been appfiad orrfy to the<br />

preferred term, followed by the expmsaion “Also celled” and a Iii d the aynonyma. The synarryms<br />

are shown in alphabetical order in the glossary, and ere referenced to fhe prefemd ferrn.<br />

Anfonyrns are fisted after the expression “Opposite of.”<br />

Any mention herein of a commercial product does nOt<br />

constitute endorsement by the United Slates Government.<br />

ii


I<br />

MIL-HDBK-B50<br />

CONTENTS<br />

2. APPLICABLE DOCUMENTS ............................................................... ...<br />

2.1 Govsrmmenl Documents .................... ...................................... ........<br />

2.1.1 Spadfk.aliena, elanderds , and hendbooks ......................................<br />

2.1.2 Other govemmenl documenls, drawings, and publications ...............<br />

2.2 Non-Govemmen! publications ..................... ...... ........................... .....<br />

2.3 Order of precedence .........................................................................<br />

3. TERMS AND DEFINITIONS ..........\ ..........................................................<br />

4. LIST OF ABBREVIATIONS, ACRONYMS, AND INITIALS .................... ....<br />

5. MC&G 0RGANKA?70NS ........................... .............................................<br />

INDEx .............................................................. ............................. ....... ..<br />

CONCLUDING MATERIAL ...................... ..............................................<br />

- ‘ii<br />

3<br />

285<br />

26’2<br />

294<br />

295


,,<br />

I<br />

1<br />

I<br />

I<br />

I<br />

I<br />

‘1<br />

MIL-HDBK-850<br />

1. SCOPE<br />

1.1 =. This handbook provides a comprehensive gfossary of Mspping, Chsrting, and<br />

(kcufesy (MC&G) terms cxwnrnonly used within the Ds$eIrlmerd of Defenam<br />

1.2 ~. This Gfoaeq epphs uniformfy 10 designers, pducem, and ussrs of MC&G<br />

producfs.<br />

1.3 Th=e terms apply to troth inlernd and sonlrecturd development dforls by<br />

the Mifiiry Departments, Cffiie of the Secretwy of Dafenae, Orgsnizalicm of the pint Chiefs of<br />

slaff, and the Defense Agencks of the Dapwtment of Defensa (DoD), colktivefy knmvn as D@<br />

Components, end to all levels involved in the prepsrat”m end rminmnsnce of MC&G preducfs.<br />

1.4 ~, This handbook is UNCLASSIFIED.<br />

1


I<br />

I<br />

2.1 ~<br />

MIL-HDBK-850<br />

2. APPLICABLE DOCUMENTS<br />

2.1.1 ~ This section is not eppfiible to Ihm<br />

handbook.<br />

2.1.2 ~<br />

~<br />

. .<br />

The folbwing dher<br />

government documents, drawings, snd ptblitione form a psrf of this doourmnf 10 Ihe exfenf<br />

spaoifii herein. Unless otherwise specified, he issues ere hose cited in the solicktetbn.<br />

JOINT PUB 1-02 Depsrtnrent d Defense Dktiirrery d Mililery end AesorSeted Terms.<br />

(Copies of !Ks ptddiilicm em evaileble frem the SIenderdiia!ion Dcx.wnent Otdef Desk, 703<br />

Robbins Avenue, Bfdg. 4D, Phifedelphii, PA 19111 -501M.)<br />

2.2 ~.<br />

. .<br />

Thii section is ml eppfiiable to this hendtmok.<br />

2.3 ~ In the event of e conflii fmlween the texl of this document and<br />

the rehwensas cited herein (except for refsled essocieled detail specificelione, specilisetien sheets,<br />

or MS standards) the text c4 this decument takes presedeme. Nothing in this dosurnent, however,<br />

supereedee e#iisble laws end regulations unless e specifii exemption hes been obteined.<br />

2


I<br />

I<br />

1,<br />

I<br />

f<br />

i<br />

!<br />

1<br />

,<br />

Al time-A particular atomic MIS scale,<br />

aatabfiahed by the U.S. Naval Observatory, wHh<br />

the o~in on 1 Jaruary 1958, at zaro hours UT2<br />

and with the unif (sewxf) equal Io<br />

9,192,621 ,nO cycles of cesium at zero field.<br />

see also UT2 time.<br />

ABAC—A nomogram for obtaining Ihe<br />

Corwamion angle to apply when pbtting graatsircle<br />

bSarings on a Marcafor pmjectbn.<br />

abnormal magnatlc varlatlon-Any<br />

anomabus deflecliin, whosa cause is unknown,<br />

of the compass needle Irom the magnetic<br />

meridian.<br />

MIL-HDBK-850<br />

3. TERMS AND DEFINITIONS<br />

abaclsea—The horizontal coordinate of a sat ot<br />

rectangular smordirrates, Also used in a similar<br />

sense in connection with oblique coordinates.<br />

Also called total daparfuras: X-COOrdlflate.<br />

absolute accuracy--The evaluation of all<br />

errors in determining a posil’bn with respect to an<br />

absotufe reference frame, such as the DoD<br />

World Gaodelic System,<br />

absolute errOr—AbSolute deviation, the value<br />

taken without regard to sign, from tfte<br />

corresponding true value.<br />

abaoluta gravity atatlon—A marked poinf,<br />

usually in a laboratory, where the value of<br />

absolute gravity has been detenrrined. See also<br />

abaolute gravity.<br />

I abaoluta grevlty-The acceleration of gravity<br />

diracfly determined by a device that measures<br />

time and length. See also gravity.<br />

I abeolute orlerrtatlorr-The acalirrg arid<br />

feveling to ground control (in a phofogrammetric<br />

instrument) 01 a relatively ortentad stereosmpic<br />

model or group of models. See also refathra<br />

orlontatlon.<br />

abaolute parallax—See absoluta<br />

atereoscoplc parallax.<br />

abaoluta po81tlonlng—Determhration of the<br />

posffirnn of a point with respect to the cenler of<br />

mass of fhe Earth as deffrred in fhe DoD World<br />

Geodetic System.<br />

abaoluta stereoacoplc parallax—<br />

Considering a pair of aatial photographs of e~al<br />

prircipaf dlslance, the absolute sfereomoplo<br />

parallax of a poinf k lha algabrak diffararca of<br />

Ihe distances of the two Imagas trom their<br />

raapacffva photograph nadirs, measured in a<br />

horfzonfal pfana and paralkrl to the air base.<br />

Afao caliad abaolutst parallax; trorfzonta?<br />

parallax; Ihrear parallax; parallax;<br />

●tareoacoplc parallax; x+araltax.<br />

ebeolufe tetm-A term (ueualfy only one) In an<br />

eqmfbn, which represents a known numerical<br />

value and does not contain any unknown or<br />

variabla elamanfs.<br />

abaolufa unit—Any unit in a system that is<br />

based directly upon associated fundamental<br />

units of length, mass, and time. See also<br />

dynamic number.<br />

absofute vatua-A mathematical quantity<br />

taken without regard !0 hs associated plus or<br />

minus sign. Used often with res”duals.<br />

abaoluie vector—A directad line segmenl<br />

whose end points are measured in absolute rttThS<br />

from a pcint designated as the origin.<br />

abaorptlon-Conversion of radianf energy Into<br />

other forms by passage through or reflacrion<br />

from maner.<br />

accelaratlon of gravity—The accaleratlon of<br />

a traefy tallirq body, approximately 9.8mJsac2.<br />

accalaratlon-1. Tha rafe of change of<br />

vebcify. 2. The acl or prcrceas of accafarating, or<br />

the state of being accelerated.<br />

accelarometar-1. A device that meaaures<br />

the rafe of change of spaed ot an object. 2. An<br />

Inatrumenl, spaclally designed for carrying In<br />

aircrafi or mk4eS, which measures the rate of<br />

change in velocity, dhatilorr, ars%or affltuda.<br />

accldenfal arror—See random arror.<br />

accommodation—l. The ability of the human<br />

eye to adjust ifsetf to give sharp images of<br />

objects 01 dtiferarsf distances. fn ateraoampy, the<br />

abilily of Ihe human eyes to bring two imagee<br />

hfO superimposition !or steraosoopic viewing. 2.<br />

3


I<br />

The Ilmifs or range wnhin which a stereopfoffing<br />

instrument is capable of operating. For example,<br />

the rnuttii)ax can adjust (or accommodate] for<br />

smell fibs in the projectors ranging fmm<br />

approximately 10° about the x-axis to 20” ebout<br />

the yexis.<br />

MIL-HDBK-850<br />

accumsslatod dlscropmrcy-The algebreic<br />

sum of the aarparssfediiepenciee which occur in<br />

the various sleps 01 Maklnc! a survey or of the<br />

computa!kxr of a survey.<br />

accumulated dhrergenca-(leveling) The<br />

algebraic sum of the rtiva~nces for the sactiirse<br />

of a MIS of levels, tmm me ba@nning of the tine<br />

to any section end a! which If Is deslmsf to<br />

@mPWe the total divergence.<br />

accumulative error—Sae ayatematlc<br />

error.<br />

eccurecy checkln@—The procurement of<br />

presumpfiwe evidence of a map’s wrnpliance<br />

with specified accuracy sfanderds. Accuracy<br />

cheddng generally indicates fhe relative (rather<br />

than the absolula) accuracy 01 map Iaatures.<br />

accuracy evaluation—The comparison of the<br />

quaihy of an MC&G producl with meintenake<br />

criteria to ascertain ifs adequacy with respecl to<br />

its intendad use.<br />

accuracy mathod-The method used in<br />

determining the staled aocuracy ot s produci.<br />

The melhod can range from a system empfoying<br />

highly sophisticated tachnlquea to a highly<br />

subjective )udgment, and IS essential for proper<br />

use of the stated accuracy.<br />

accuracy revlow-The comparison of an<br />

exlstlng MC&G preducl against source material<br />

or data more accurate lhan that from which H<br />

was produced, for the purpose of determining<br />

the accuracy of its horizontal and verfiial values.<br />

accuracy teatlng—The procurement of<br />

corrflnmad evidence, on a sarnpting basis, of a<br />

map’s Co@lance wifh specified accuracy<br />

srandards Accvrecy tasfing Is designed to<br />

indkate both the relafive and absolute accuracy<br />

of map feeturas.<br />

accuracy—1. The degree of conforrnit y with a<br />

standard, or tha degree of parlecfion atfalnad In<br />

a maasuramam. Afxuracy ralafee to the quallty<br />

“@a KEJdt, Srnd IS tLSW’I@Sht3d lrOM precisbn,<br />

which relates to the quelily of tha Op.SratlOn by<br />

which tha resuil k obtained end can be<br />

repeatti. 2. The ctoseness of the besf<br />

eefimeled value obtainad by fhe rnaaeuremente<br />

to Ihe %ue- value of the quamity meaeured.<br />

accurate contour—A contour line, the<br />

accuracy of which ties within one-half of the basic<br />

vertical inlewal. Atao called normal contour.<br />

ecetata-A nonflammable plaatic ahaeli~<br />

uaad as a besa for photograph!! films or as e<br />

drafting base for overlays where Crnlcal<br />

registration Is not required.<br />

achromatic color-Cobr that does not etiiif<br />

hue.<br />

achromatic larta-A lens that has been parfly<br />

corrected for chromatic aberration. Such a Iana is<br />

usually of a mutli-elemem design to bring green<br />

and red Iighl rays to approximately the same<br />

polm of focus.<br />

acoua!lc navigation-blavlgation by means of<br />

sound waves whether or not they are wiihin the<br />

audible range. Also called aonlc navigation.<br />

See also Dopplar sonar navigation.<br />

acthrlc Ilght+ighl which is capabla of causing<br />

pholochemical cha~es in a sensitized emuision.<br />

acflve $atalllt-A saleltite which transmits an<br />

electromagnetic signal. A satelliie with the<br />

capability to transmit, repeat, or retransmit<br />

electromagnetic information, Sae also pasahra<br />

aatalitta.<br />

actlva tracklno ayatem—A satellite tracking<br />

system which operates by transmission of signals<br />

to and receipt of responses from fhe safelfite.<br />

actual error—The dMerence between !he true<br />

value and the measured value of a physical<br />

quanf ity.<br />

acutanca-An Oblecfive measure of [ha ablfiiy<br />

of e photographic system to show a sharp edge<br />

between comiguous areas of low and hiih<br />

illuminance.<br />

acfap!atlon-The facufry of fhe human eye to<br />

adjust its sensitivity to varying Immensitiesof<br />

illumination.<br />

aedftlve color mixture- Super- Impoafflon or<br />

other nondestructive cortrbhation of Iiiht of<br />

dHferant chromaticlfies.<br />

4


I<br />

I<br />

add ftlva color Wewer-Projecfor tor positive<br />

trarrsparenclas obtained through muttibsnd<br />

photography. Each image IS Superimposed by<br />

use of a d~erem colored tight.<br />

addltlvfty of lumlnence-Lumhtance<br />

produced w(th a mLxture of fight from several<br />

sources ts the sum of the Iuminarrces produced<br />

by the fight from la of IIte acwrces acting<br />

separately.<br />

●doquaW-A !arm usad to descrfba s product<br />

which meats all ot the accamacy and curren~<br />

standards established by ifs moat stringent use,<br />

and thus, is suftabte for all ifs intended uses.<br />

adjacency-A topolo~ical property which<br />

pmv~es relalbrships between objects which<br />

abut or are beefed In ctose proximity. Alao<br />

known as contigutfy.<br />

ast]olnlng sheets—Adjacent maps to one or<br />

all sktes and corners ot a particular map aheel.<br />

adjustad mepplng support data<br />

(AMSD)-The pest-mission relined version ot<br />

those paramstars used to posil”on collaaor<br />

plaftomta, sensors, arm sensor pointing anglas.<br />

adiuatad va[ue—A vafue of a auantitv derived<br />

froin observed data by some oid~rly pticess<br />

which eliminates cikcrepancias arising trom errors<br />

in those qata.<br />

MIL-HDBK-850<br />

adjustment; balanclng ● survay;<br />

dlrocllon molhod of sd)us?nrent; flsure<br />

●djustment; Instrument sd)ustment;<br />

Iand-ltna ●djustment; Iaaat ●quarea; map<br />

adjustment.<br />

●dmlnlewatlva map-(JCS) A map on which is<br />

graphically recorded Information perfattkig to<br />

administrative matters, such aa supply and<br />

evacuation inataliationa, personnel installations,<br />

medical facilities, cullecflng points for stragglers<br />

and pdaonara of war, train bivou-, aervka and<br />

maintenance areas, rnaln supply mists, traffic<br />

circulafbn, boundaries, and other details<br />

necessary 10 show the administrative siiuatkrn.<br />

See also map.<br />

Advanced Very High Resoluslon<br />

Radiometer (AWIRR)-A five to six channel<br />

sensor with a retmlu!ion of 11 km. Applcatbna<br />

inctude cJoud Iemparatum, aea swlaca<br />

Temperature, iand Iemparalure, and vegetation<br />

Indces.<br />

Advancad Weapona and Syatama Data<br />

Base (A WSDB )-A DMA relational data base<br />

used to assess and consolidate the MC&G<br />

praduct requirements for fielded, new, and<br />

emerging DoD weapons ad systems.<br />

aerial camera-A camera specifically designed<br />

Ior uae from an airborne stalkm.<br />

aerial cartooraptdc photography—See<br />

mapping photography.<br />

adjustment of obaarvatlona-The<br />

detenninatbn and aoDlicalbn of corrections aerial film epead (AFS)-A measure of<br />

corraaponding to etiis affecting the<br />

Wfred for aerial film which replacas the formerly<br />

obaervatlona, maklrrg fhe obsarv~lons<br />

arrwng themselves, and ccadhating<br />

consistent<br />

and<br />

u~ed aer@l exWsure i~ex. (I is *fined as 3@-E,<br />

where E is fhe exposure in metar+andle-secorrds<br />

correlating the derived data. at the fmint on the characlerislk curve where Ihe<br />

densitv is 0.3 above base DIUS Ioa denaitv on<br />

I ●djustment—1. (general) The determination bbck~;nd-white film. r - .<br />

ati application of Eor7ecfi6ns to observations, for<br />

the puroose of raductno armra or ramovlno<br />

inteinai inconsistencies-in derived results. _The<br />

tafm may reter either to mathematical<br />

procedures or to correctkrne applied 10<br />

instnmlants used In making observatbns. 2.<br />

(Iavaling) The detenssination and application of<br />

CW?eCSiOnSto orshometric differences of elevalbn<br />

or to o?thotrWIrfC elavatbns, fo make the<br />

efwatbn of ali bench marks tmnsisterst and<br />

Indeparrderrf of the circuit closures, 3.<br />

@logrsphy) Placing delafl or comrol stations in<br />

their positbne ralatiie to other detail or cantrol<br />

slalbns. See also adjuatmant of<br />

obaervatlona: engle method of<br />

aarial Illm-specially designed roii film<br />

supphed in many lengths and widths, with various<br />

emulsbn types for use in aerial cameras.<br />

aarlal imagary-Any remotaly-sensed<br />

nonphotographic image taken fmm the air (as<br />

opposed to space).<br />

aarlal mosaic-see moaalc, defintiion 1.<br />

aerial photogrammetry—The use of aerial<br />

phonographs in the science ot photogrammetry.<br />

5


1<br />

aerlsil ptrotogrcphlc reconrsaissance-<br />

The otxa”ming of information by aerial<br />

photogrephy4Nidad into three types: (1)<br />

efralegic phofographii reconnaisaanca; (2)<br />

Iacfiml photographic remrmak3sarq3; and (3)<br />

eurveyhwfographic photography, whti is aerial<br />

photography taken for eurveykerfograpfsic<br />

purposas and to aurveyksrrtogrephic standards<br />

cd acaracy.<br />

aertel photography-The art, science, or<br />

process 01 Iaklng sarlal photographs. See also<br />

mapplrtg pftotography; raconnalssanca<br />

photography.<br />

aarlal photograph-Any phonograph taken<br />

from the air. Also celled alr phonograph.<br />

aerial plalform-A term referring to the<br />

supporf of an aerial camera at the air statbn.<br />

MIL-HDBK-850<br />

rserlal reconnalaeance-lha collaclion of<br />

information by visual, elearonk, photographic, or<br />

other means from fhe ah.<br />

aerial survey-A survey utilizing photographic,<br />

electronic, or other data obtained from an<br />

airbc.rne station,<br />

aeriaf trlengufatlon—See photo.<br />

triangulation.<br />

aerodetlc—(JCS) Of or pertaining 10, or<br />

determined by aerodesy.<br />

eeroleve llng-As applied to model orientation<br />

during phofotriangulafion, barometric height<br />

measurements of the camera air stations which<br />

have been recorded during fhe photographic<br />

missbn are used to present the Bz values durin~<br />

fhe orfentatbn of the successive models on the<br />

sfereoploning instrument. Only ti(fferences In<br />

attitude are required and these are provided by<br />

the aratoecope. See also orlentatlon, definition<br />

7.<br />

aaromataorograph—An Inslrumem lhal<br />

remrds the pressure and temperature of the air,<br />

the armum of mofstura in the air, and the rate of<br />

metbn of the wind,<br />

Aeronautical Datm Malnlanence (ADM)-<br />

A production element of DMA’s DPS which<br />

hwelves the prmaases of mllectirsg, compiling,<br />

and updating. See also Dlgltal Production<br />

System.<br />

aaroneutlcal chart-(JCS) A specialized<br />

raprese~ation of mapped features o! the Earth,<br />

or some part of it, produced to show selected<br />

terrain, cultural, and hydrogrephic features, and<br />

eupplemenlal kfformetbn requlrad for air<br />

navigation, Pilotaw, or for planning air<br />

operations. Also Caffed naW9St10n chart.<br />

aeronautical Information overprint— (JCS)<br />

Additkmat lnfOMIaIiOn which is primed or<br />

stamped on a map or chart for tha spcftlc<br />

purpose ot air navigefkrn.<br />

aaronaulical pllotage chart-An<br />

aeronautical chart designed prfmarlly tor air<br />

navigation.<br />

aeronautical planning charf-An<br />

aeronaut”bsl charl of small scale designed to<br />

satisly brig-range air navigation and missien<br />

planning requirements.<br />

eeropau8a-(JCS) Region in which functional<br />

effects of the atmosphere on man and aircraft<br />

cease to exist.<br />

aerospace-(JCS] Of, or pertaining to, the<br />

Eanh’s envelope of atrrusphere and the space<br />

above If; two separate entities mnaidered as s<br />

single realm for activiiy in launching, guidance,<br />

and mntrol of vehcles wtilch will travel in bofh<br />

entities.<br />

aerotriengulatlon — See phototrlartgulatlon.<br />

afflne deformation-One In which fhe scale<br />

abng one axis or referance plane is diierent<br />

from fhe scale along fhe other axis or plane.<br />

a?flne traneformatfon-A transformation in<br />

which sfraighl finas remain straight and parallel<br />

lines parallel. Angles may undergo changes and<br />

differential ecafe changee may be Introduced.<br />

age of dlurrrel lnequaflty—The flma Interval<br />

between the maximum semimonthly norlh or<br />

south declination of the Mmn and the flme thaf<br />

Ihe maximum effect of the declination upon tha<br />

range of fide or speed of the tidal rwrrant ormrs.<br />

Also called ags of diurnal Ilds; dlurnaf<br />

sga.<br />

age of diurnal tld+See age of diurnal<br />

Inequaflty.<br />

6


I<br />

aQglomeratlon—A generallxallcm process that<br />

groups nvo or more proxknete features to form a<br />

single feature.<br />

a99r09at10n opemtlonrJ-The process of<br />

bringing together many distinct parts or<br />

categories of data Imo one grouping, usually as<br />

a composite dlaptay.<br />

uggmgnt)on-The combtning 01 data collected<br />

et point kxations or smaller statistical units info<br />

Iatyrer units.<br />

agonb llne-(JCS) A line drawn on a map or<br />

charl joining polnfs of zero ma~netic declination<br />

for a spdfied year dale. In nautical and<br />

aemmautkal navfgaf’bn, the term magnetic<br />

varlatlon Is used ln!Xead of Magnatlc<br />

dacllnatlon.<br />

almlng llne-See Ilne of alght, definition 2;<br />

Ilna of collimation.<br />

Alr Afman8c—A joint publication of fhe Unfred<br />

States Naval Observarfoiy and Her Majesty’s<br />

Nauflcal Almanac Offke. ff mvars a 6-monfh<br />

period. N contains tabutatad values of the<br />

Greenwich hwr angfe and declination of<br />

eafecfed cefeetial bodies, plus additional ceteerial<br />

data used in na!dgalion.<br />

Alr Target Charl-(JCS) A display of perflnent<br />

alr target intelligence on a specialized graphic<br />

base. If is deetgned prlrrawlfy to support<br />

operafbn$ against dealgnaled alr targats by<br />

vatious weapon aysferna. me charts provide<br />

grephk ovefprlrs and textual data retatlve to<br />

radar return Information and Installations within<br />

the araa. Air Target Charis are prepared at<br />

MIL-HDBK-850<br />

●ge of pamllax lnequallfy-The time interval<br />

various scales and are produced under the Air<br />

Teroet Materials Pmoram as a eafles of<br />

between the parfgee of the Moon and !he ge+raph=liy integrated chrsria.]<br />

maximum efteci ot the paratlax [clislance ot the<br />

Moon) upon the range of tide or speed<br />

current. Also called parallax ●ge.<br />

ot tiial Alr Terget Msttorlats<br />

(JCS) A O@ program<br />

Pmgmm (ATMP)under<br />

the management<br />

mntrul of the Defense Mq@ng Agency<br />

sge of phase lrsequeltty-The time interval eefebllehed for and limited to the production of<br />

between the new or full Moon and the maxlrnsrr medium- and large-ads msp, ohari, and<br />

eflSCt of these Ptrawrt upon the range cd tide or gaOdBtiC pmducts WhCh auwort WorfCMlde<br />

speed of tidal current. Aleo called Sge of tfde; targeting requlremants ot the untfiad and<br />

phase sw<br />

specified commends, the military depenmema,<br />

and allied partldpants. tf encompasses the<br />

aoe of Wro Moon-The elapsed time, usually determination of produdbn and wverage<br />

expressed In days, slrrm the last new Moon. requirements, alandardiuation of pmducta.<br />

eetabllahments of productbn priorities and<br />

age o? tlda-See age of pfraae Inequality echadules, and the produdmn,<br />

storage, and releaaelexchange<br />

distribulbn,<br />

of fwoducfs<br />

included under it.<br />

ok base-l. (phologramrnetry) The line 10lnlng<br />

two air sta!bne, or the length of that Ilne. 2. The<br />

distance, al the scale 01 the atereosmpk model,<br />

between adjacent perspective centers 55<br />

remnstmcfed in the plotting instrument. See also<br />

alr ●tatlon.<br />

alr coordlnatee—See rectangular apace<br />

coorstlnataa.<br />

alr photograph—Sac aarlat photograph.<br />

ah plot-(JCS) 1. A carrlinuous plot used in air<br />

navigation 01 a grephlc represemation of Irua<br />

headin@ slearad and air diitancas fbwn. 2. A<br />

continuous plot of the position of an airborne<br />

object represented graphksrlly to show tme<br />

fxeadlngs staered and air distances fbwn. 3.<br />

Wtihln ships, a dispfay which shows the positiins<br />

and movements of an aitborne object ratafive to<br />

the pfetting ship.<br />

alr atatton-(JCS) In photogrammatry, the<br />

point in apace occupied by the camera lens at<br />

the moment ot exposure. Atso celled camera<br />

atatlon. See also alr baae.<br />

alr ●urvelllance plottlng board-(JCS) A<br />

~ridded, smell scale, air defense map of an<br />

appmpdate araa. II is maintained at the air<br />

mntrol center. On if are posted wrrem Iocatiorrs,<br />

nurrbar, and aftnudes ot all frtendly or enemy<br />

abaft wtthin range of radar or ground observer<br />

Itaciiitias.<br />

Iair<br />

targat materlala—Sae target<br />

Imatarlala.<br />

7


I<br />

I<br />

I<br />

MIL-HDBK-850<br />

a pWC6ntag6; r6f}eCfWfy, The term genera)fy<br />

Alrbome Control (ABC) Sy6teM-A survey<br />

system for horizontal aml vertkal control surveys<br />

refers :0 energy witmn a specifii frequency<br />

range, ae the visible spectrum. Ila most frequent<br />

irwoMrg ebctrorrwgnatic distance application is to the Iighl reflected by a celealial<br />

measurements and horizontal and vertical angle body.<br />

measurements hmm two or more kmwrr Posifiins<br />

to a ftelkopter hoverfng over tfte urWwwn Albrsrrt conical equal.area map<br />

PoshIon. Tha elavetiirt of the unknown poefriirt ts pro)acllon-An equal-area projection ot fhe<br />

determined by fha use of a apaoiaf phsmb he mrrhaf type, on which lhe maridiirw are slraQhf<br />

cable. lines Ihal meet in a common point beyond tha<br />

limits of the map, end fhe parallels are cersmntrk<br />

Airborne Proflla Racordar (APR%See clrcfas whose cenfer Lsat the point of Intaraaclion<br />

Terrahr Profile Recorder. of the mwidiirrs. Meridians and parellsfa<br />

int6r%6ct al right angles and the arcs of bngifude<br />

.eIrborna ●leotronfc survey control— abng any givan parallel are 01 equal Iangfh. The<br />

Control aurvay% amor?@shed by efecfronlc parallels are spaced to retain tha cot’!dlilon of<br />

maana horn an alrlmme vehicle or pfattorm, such Wual 8raa. m fwO W~cf~ PWaflels, the arce Of<br />

as hiren and shoren.<br />

Iongttuct.e are reprasersfed In their true length.<br />

Befween the selected parallels fhe scale along<br />

afrborne<br />

desi~nad<br />

tencilng model-A specially<br />

assaun rrmdef for use In briefing<br />

fhe meridians<br />

beyond them,<br />

will be a trifle 100 large. and<br />

100 small,<br />

alrfwme troops and supperf paraonnel. These<br />

models emphasize the aspects of objacfs as<br />

seen from the air rather than from the Qround,<br />

alfwmln<br />

making<br />

(albumen) process”—A process of<br />

photolilhogrephic press plates utifizing<br />

bichromaled albumin as fha photosensitive<br />

ahwey+JCS) A comrol area or portion thereof<br />

established in the form of a rnrrtiar marked with<br />

mating, and requiring a true negative<br />

the prinfing plate. See also plate,<br />

10 make<br />

radb navigational aids.<br />

Aldls algnallng lamp-A signaling lamp used<br />

Ah’y ●pherold (elllpsold)-A reference<br />

e[iiisdd used in Great Britain and having fhe<br />

in some cases for night obsewalions<br />

stations in triangulation.<br />

of distam<br />

following dimensions: samimejor exis—<br />

6,37T.563.3S6<br />

6,356,256.910<br />

meters:<br />

meters:<br />

aemiminor azia—<br />

and lhe flatrenlng or<br />

alerte-An<br />

satellites,<br />

ephemeris prepared lor one or more<br />

predicting rise and set times referr~ to<br />

elfiOfiCltV-1/299 . .3249646. universal<br />

elevation<br />

lime coordinated, maximum angle of<br />

above the observer’s frorizon, a-rid<br />

Aky theory ot laoatasy-The lheory that fhe azimuth from fhe observer. Used fo identity<br />

mnfinenfe and Isfands are resflng hydroelallcally $Pecific aatefffie Passes. See also look anUlas.<br />

on hahly pfastic or fiquid maferlal, vflth roots or<br />

pmjecttons penatratlng fhe inner material of the akorifhm-A etatemenl of the steps to be<br />

Earlh. lust as icebems extend downward into the followed in the SOIUtbn of a moblem.<br />

w“ater; The greeter tf% elevation; fhe deeps; the<br />

penetration. II has been celled the roota of rWderYe-The pan of a surveying Instrument<br />

mountaht theory, and has the support of whkh consists of a sighllng dev’ke, with index,<br />

some gaofegl~s. See also Prmtt-Hayford ad reading or MccmJ@r accessories. See also<br />

theory of Iaostesy. paapalght alldasfe; pendulum alldada;<br />

pholoalldade; Ieleacoplc allrtada.<br />

Altotf aqual-araa map pro)ecflon— A<br />

Lamberl equal-area azlmuihal projection or e JIllgnmant (allnemem)-1. (cartography)<br />

hemisphere ctmvertad inso a map projecfiin of Representation of a road, railway, etc., on a map<br />

fhe emire sphere by a manoulafion suggested or than in relation to surrounding tpographlc<br />

by Alfoff. H is a projactbn bounded by an elllpse detail. 2. (general surveying) Tha pfacemem or<br />

in wtrlch lhe fine representing the Equator (major location of pOlnfS abng a stmfght Ilne. 3.<br />

axis) Is doubla the length of the llne representing (highway and mule euweYin9) The Wound Plan<br />

the cenlraf meridian (minor axis), showing the direcffon (cemer line) of the mute to<br />

be followed, as distinguished from proflla,<br />

albedo-The rafio of radiant energy refiected to which shrsws the vamcal elamanf.<br />

fhaf received by a surface, usually expressad as<br />

8


allanmont comecflort+aping) A correcflon<br />

apptisd ~ lhe measured length of a line to allow<br />

for the tape nol bakrg held exacfty in a verlical<br />

ptane containlr@ the line.<br />

●lmanac-A parbsfbsl ~blicalbn of<br />

aetronomts coordinates useful !0 a nsvigator. ft<br />

COt’If6htS tees Informefbn than an ephemeris and<br />

vabes are garraralty Oiven to less preclabn. See<br />

also ●phomorla.<br />

●lmucantar-Sae parallal of allltude.<br />

●long.traco @/T)-The direction of the<br />

tar!gant 10 a bass of points on the eerth, a<br />

COnStam dhtanoa from the aefeliiie ground path,<br />

Posilive In ths direction of satellite motion.<br />

alpharturnerlc grid-See atlaa grlrl.<br />

alphsrrumarlc ●trlng—A string of information<br />

cmraisting 01 both letters and numbers, and<br />

posalbla including other symbots such as<br />

punctuation marks and mathematical symbols.<br />

trequenlly includes olher select character such<br />

as PUtiUafiOn marks and mathematical<br />

symbols.<br />

aftezlmuth lnatrument-An irrstrumenl<br />

equipped with both horizontal and vertical<br />

graduated circles, tor the simultaneous<br />

observation o! horizontal and vertical d+racfbns or<br />

angles. AIw called ●stronomic theodollte;<br />

urrlveraal Inatrumerrt.<br />

OltamSrtO depoatfory-A Iile of originals,<br />

duplicate oopies, computer tapes, reproduced<br />

MStet’fale., e!c., of aelecf~e, current, and<br />

evahated MC&G data Indexed and stored at an<br />

appmpilately sewre location, physically<br />

eaoerefsd from beets Ilbrartes. bul available for<br />

use In the event of destruction of the primary<br />

DoD library file.<br />

●ltimeter—An Instrument that indicates the<br />

haioht above a reference surlaca. See also<br />

barometric altlmeter; preclelon ●ltlmeter;<br />

radar ●ltimeter; ●urvaylng altlmeter.<br />

altlmetry-The art and aciense of measuring<br />

attiiudas by bammetrk means and imerpreting<br />

tha reeutfs.<br />

●ltltude circle-See parallel of altltude,<br />

alfltude contour ratio-See C. factor.<br />

MIL-HDBK-850<br />

●ltltuds daturn+JCS) The arbitrary level from<br />

whbh vartkal diaptacernarrt is measured. Ths<br />

datum for height measurement is the lerrain<br />

diractly bebw tha eirusft or some apacifiid<br />

datum; tor preaaura attiiuda, the ieval at which<br />

Iha afmoapharic praswra is 29.92 inches of<br />

mercury (1013.2 robs): and for true altltude,<br />

mean sea tavel.<br />

●ltftude dlffarenca-The difference between<br />

~mput~ and observed altitudes, or bahveen<br />

prem~uted and sextarsl aitiludas. Atso oallad<br />

●ltltude Intercapt.<br />

●ltltude holrr+.fCS) The blar’W area et tha<br />

ori@n of a radiii d~tay, on a tiar tuba<br />

presentation, the cemer of the periphery of which<br />

represents the point on the ground immediately<br />

beiow the aircraft. In aide-beking eirborne radar,<br />

this is knowm es the altltssde slot.<br />

eltltude lntercapt-Sea allituda<br />

dtfferance.<br />

altltude slot-See aitllssde hole.<br />

altltude tlnla-See hypsomrnrlc tlntlng.<br />

altitude-l. The vertical distance of a point, or<br />

an objecf considered ss a pelnt, meaaured from<br />

a refererwe surface, as mean sea *vet (the<br />

geoic$, ellipsoid, mean terrain. 2. Angular<br />

diatarrca above the horizon; the arc of a verilcd<br />

chcle between the horizon and a point on the<br />

celeWal sphere, measured upward trmm the<br />

horizon. Sea also ●bsolute ●ltttude; angular<br />

altltude; apparent ●ltttude;<br />

clrcummerldian eltltudae; computed<br />

eltltude; denalty altltude; alevatlon;<br />

ellipsoidal height; ●xmarldlan altltuda;<br />

flight ●ltitude: geoldal halght; high<br />

altltude; merldlan altttuda; negatlva<br />

allltuda; obeerved eltltude; orbital<br />

altltude; parallel of ●ltltude; photo<br />

altitude; poaltive ●ltitude; preaeura<br />

altltuda; radar attitude; aextant altltude;<br />

Dlmuftaneous altltudea; ●olar aftltude;<br />

frue altltude.<br />

American Standerd Code for Information<br />

Interchange (ASCII)-A widely used ANSI<br />

$taMard mda which usas seven bfte to<br />

mpreaent nurrtmzrs, Ieffere, and mntml<br />

:haracfers. Shoe eigm-blf codes are more<br />

mmmon on mrmputera then sever%blf mdea,<br />

4SCII is mmmonly embedded In an elohl-blt<br />

mde. II is mainly used to tranemfi data between<br />

3


I<br />

I<br />

diiital devices.<br />

amphlblouo ●ssault Iandlng modet- See<br />

assault Isndlrra model.<br />

amptrldromlc polrrt-A rto-t!ds or nodal point<br />

on a dtan of co!ktal fines from witlcfr the cotidal<br />

lines rediata.<br />

ampttldrorrrlc rsglon-An area aurroundhtg<br />

an amphldromic poinf in whlctr the cotidal lines<br />

radiate from the nss-tide pohrr and progress<br />

thrwgh all hwre of the tidal cycie.<br />

amplltude of vlbratfon--(pendulum) The<br />

length of the arc paeead over by a perrdubm in<br />

movlrrg from tfs mean fxmltbn to the posltiorr of<br />

maximum displacement.<br />

MIL-HDBK-850<br />

amplltude—1. The mesimum value of the<br />

displacement of a wave or other periodii<br />

phenomenon hum a relerenca position. 2.<br />

Angular distana north or south of the prtrna<br />

vertical: the am of the horizon or the angle al the<br />

zenith between the prime verlicsl aml a vertical<br />

circle, nmasured north or south from the prime<br />

vertical to tha venical circle. The term Is<br />

or current as in anabg nahvorks that use<br />

resistance to represent mechanical bsaea,<br />

capadtors end inductors to atore energy and<br />

sinwlete the action ot aprirQs, etc. Stereoscopic<br />

pbffere are examples of photogrammakic stnabg<br />

Ine!rumanls.<br />

analog-A form of data recording thal works on<br />

the principle of continuous measurement, rathar<br />

than discrete cgurtthg. For example a paper<br />

map with ccmflnuous iinas Is analog, a computer<br />

disPIsY9d r7MP b@rIQ meda 0! bitE (pisatS) iS<br />

di@tel.<br />

analyals—A methodological krvesti@bn of a<br />

precass by a crmelstam prooedura, and its<br />

SSPSratiOn iII10 falS\Sd units for further datelled<br />

study.<br />

Analytical Photogrammalrlc Ponltlortlrtg<br />

Systsm (APPS)—A sfarao photogrammelric<br />

WO* statiin used h! conjunction with a Point<br />

Positbmlng Dala Baee (PPDB) for precise point<br />

positioning. See also Point Posttlonlng Data<br />

Base (PPDB),<br />

nnalytlcal aarotrlarroulstiors-A ohoto-<br />

CUslonsarity used only with reference 10 tr@es wis~ulalion procedure _(using aerial<br />

whose centers are on the Celeslial horizon, and is photography) in whlCh the Spalial SduliOII 1S<br />

pretiied ‘f? or ‘W,” es fhe body is rising or obtained by ownputational rwlines.<br />

setting, reapadk’ety, and suffixed ‘N- or ‘S fo<br />

agree with lhe declination. See also compasa analytical nadir.point trlangulatlonampllkrds;<br />

grid amplltude; ma@neIlc Radial hiangulation performed by computational<br />

stmplftuda; truo amplltude. routines in whch nadir points are utilized as radial<br />

centars..<br />

amplltude of vlbratton-(pandulurn) The<br />

Iangfh of tha arc paased over by a pendulum in analytical orientation—Those computational<br />

rtrovlng fmm its mean posltiin 10 the position of s;eps required 10 determine lilt, diractbn of<br />

maximum dbplacement, principal line, fiiihl height, preparation of control<br />

terrplets at rectilicetkrn scale, an@ar elamerrfs,<br />

arraglyph-A sfereogram In wtrkh the fwo views and linear elements In preparing aeriat<br />

are primed or projected suparfmposad in photographs for mdifbation. Devebped data are<br />

rnf@errremay XMra, usually red and Blue. By mnverted to values to be set on cimles and<br />

vmwing through fitter apactaclea of corresponding Scelas of rectifier or transforming printer.<br />

00n@eMSmsrY cobra, a stereoscopic image is<br />

formed. analytical phoiogrammetry— Photogrammetry<br />

in which solutions are obtahrad by<br />

Snslemma-1. A figure eight shaped diagram mathematical Methods.<br />

drawn across the Torrid Zone on a terrestrial<br />

gbbe 10 show the declination of lhe Sun analytical photography—Phof ography,<br />

Ihmughoul fhe year and also the equation of ehher motion pk%rre or still, accomplished fo<br />

firna, 2. A sundial. delarrnine (by qualitative, quamitatlve, or any<br />

other maans) whelher a particular pherwmenon<br />

●nrrlog fnetrumonts-Devices fhat repreeenl does or does nof occur.<br />

numerical quantities by means of physical<br />

variables, giving all vatues wlthln a particular eneffifcaf Pmducta-Products made wlfh ffte<br />

raWe, for exampfe, by Irarralatb% by rotatbn, use of analytic fechnlquas.<br />

as in a machanbal gear system; and by vonage<br />

10


I<br />

analyllcssl mdiat ttlmrgulatlo*Radial<br />

trisngutation performed by com~ational<br />

rorsflnas. Sea also graphical radial<br />

triangulation.<br />

StnalytlCOl tfrrea-point rmectlon radlel<br />

trlarrgulatlon-A method of computing the<br />

mordirtmea of the prtnctpal points of overlapping I<br />

aerial photographs by rasedlng on three<br />

horlzomal<br />

area.<br />

control pokrts appearing in the overfr$ )<br />

anaetlgmatlc lens-A lam which has been<br />

corrected for astigmatism and, therefore, foouse! 5<br />

vertical and horkomal tines with equal brightness<br />

and dSfinftbn. AnasfigmaIic lenses are alsm free<br />

ot moat mmmon aberrations.<br />

anchoraga chart-A nautical charl showing<br />

prescribed or recommended wrchorages.<br />

ancillary data-Auxillary or supplementary<br />

data.<br />

snorold .altlmeter—See barometric<br />

altlmeter.<br />

enetold bat’OMetW-A barometer which<br />

balarwes the atmospheric pressure against a<br />

mechanically alastic rtevice. The ueual term of art<br />

aneroid barometer consists of a thin box of<br />

corrugated malal, almost exhausted of air. Wher I<br />

the atmospheric pressure increases, the bex<br />

cuntracts; when the pressure iessens, the box<br />

expands. By machankal means these<br />

rmvements are amplttiad and mmmunicafed 10<br />

an index hand ~ich registers the changes on a<br />

graduated dial.<br />

●flgh aquatlort-A condition equation which<br />

expraeses the rataiionehfp between Ihe eurn of<br />

the measured angles of a ctosed figure and Ihe<br />

Ihsoreiical vaiue 01 thal sum, Ihe unknowns<br />

bel~ the mrrectbns 10 the obsewed direcfbns<br />

or anglee, depending on which are used In the<br />

adjuetmenl.<br />

●ngle method of ad]uetmenl—<br />

(Iriangulatbmand traverse) A method of<br />

MIL-HDBK-850<br />

adjustment 01 obsewations which determines<br />

srselvikal rOdSr Dr@Illctlo%Prediclion<br />

baaed on proven formulas, power fab4ee, graphs,<br />

mrredbn to obsewed moles. The a~le<br />

of Sdiuslmenf may be used fiere a tiain<br />

method<br />

of<br />

anrUor other ScientK* principles. An analytical singie triangles is 10 be ad@tad.<br />

prsdidbn ccrrtatders sutlaoe helgm, sfnscrural<br />

srrwVorterrain frrfomration and criterta for radar angle of convergence-(JCS) The angle<br />

refladivfty together wfth the espact arrgfa and su~ended by the eyebass of an obaawar at the<br />

range to the targel.<br />

point 0! fmws. Atso called<br />

parallactic ●ngla.<br />

angular parallax;<br />

ang la of coverag~ee angle ot flsld.<br />

engle of currsmf-(hydrography) In stream<br />

gagging, tha argle of current la tha angular<br />

diierencs between 90” and the angle made by<br />

the currant with a measuring section.<br />

angle of depreaatort-(JCS) 1. The angte in<br />

a vertical ptane between the hOrfzWIfai ard a<br />

descending tine [as from an obsarver to an<br />

objecl]. 2. In air photography, the ar@e<br />

between the optical axis of an obiiqualy rrroumad<br />

air camera and the horixordal. Atao callti<br />

depmaelon angie; descending vertlcat<br />

angle; minus angle. See also angle of<br />

elevation; tilt angle; true depreaaion<br />

angla.<br />

angle of dsnrlatlon+opka) The angla<br />

through which a ray is bent by relra~lon,<br />

angle of etavatlo*Tha angie in a vsrticai<br />

plane bafween tha horizontal and an ascending<br />

tine, as from an obsewer to an object. Aiso called<br />

aacmrdlrrg vortlcal angia; plus anole. See<br />

also angle of depreaelon.<br />

angie of tfstd-A property of a lens. The angle<br />

wMendad by fines that pass through the center<br />

01 the tens and tocate tha diameter of tha<br />

maximum Image area within the specifbd<br />

definhbn of the lens. Lenses am ganerslty<br />

classtrisd acmrding to their ar@as ot mveraga,<br />

as follows: nsrmw-angia; wide-angle; nonmafangla:<br />

and wparwide-angle or utmswida-angia.<br />

Aiso caiied angia of covarage; angular<br />

field.<br />

angle ot Incidenca-(optks) As measured<br />

trom the mrrnal, the angle at which a ray ot light<br />

strikes a wrfaca.<br />

●ngle of lnclhtatlon-An angie of alevatiin or<br />

angla of depression.<br />

angle o! reflectlon+opfica) As meaeured<br />

trom the normal, the angle a! which a reflected<br />

ray of light ieaves a surlace.<br />

11


I<br />

●rrgfe of rofractlon-The angle whkh the<br />

refracted ray makes with the normal to lhe<br />

wrtacs separating two tranaparem rnedii.<br />

engle of Ult--see Wt.<br />

●glo 01 vtaw+JCS) 1. The engle between<br />

two raya paastng !hmugh the persfmcfiie canter<br />

(rear ncdal poim) of a camera fens to two<br />

ooooslte aarnem of the format. 2. In<br />

MIL-HDBK-850<br />

●ecsmslon; Screen ●ngle; sidereal hour<br />

sngle; ●lope ●n@e: eolld engle;<br />

●pherlcal ●ng la; apheroldal ●ngla;<br />

trsrvarse angla; vectorial angle; vertical<br />

●ngle; zenith dletance.<br />

●nuular altltude-A maaaura in dagreas 0( a<br />

given objecf above the horfzon, taken from a<br />

given or aswmed polnf 01 observation, end<br />

expressad by the angle between the horizontal<br />

and Ihe observers line of sight.<br />

p%togramrnatry, fw”w the arrgfa whose tarxgem<br />

is one-haff the length of the diagonal of the angulfir calibration conatent-in a<br />

format diviieci by the calibrated focal length. AlSO MUffiple-lenS camera, or IXUJffiplS~MSra<br />

called covarhrg powa~ field of view. assembly, the vatues of angular orientation of<br />

the lens axes of the sevaral lens-camera unita to<br />

angle O! yaw-The arrgla between a line in the a common reference line. For example, in a<br />

direcfbn of ffiiht ard a plane through the trfrnstrogon camera, the angular relalbnshfps of<br />

longitudinal and vertical axes of an aircraft. It is the wing sanrara axis with respect to the axis of<br />

mnsidered odsifive if the nose is disolaced to the Ihe central (verficaf) Camera.<br />

right. Also ~lled yaw ●ngle.<br />

anoular dletence-1. The anoular difference<br />

angle point—A term appfied to a marker al befieen two diradona, numerically equal to the<br />

each poim to Indkate a change In the direction angle between hvo lines axfending In the given<br />

0! a suwey line. directions. 2. The arc of the great circle joining<br />

two ooints, exoressed in annular units. 3.<br />

angle to right-The horizontal angle Dtstance between two poinf=, expressed In<br />

measured clockwise frem the precediW line to angular units of a specifiad frequency. tf is equal<br />

the tolbwirrg one, AlSO called clockwlse angle .“to f.~e..nu~! oj.wa~es bev.een f.~e Points<br />

angle-to-right traverse-in surveying, a<br />

technique applicable to either open or closed<br />

travemes, wherain all anglea are measured in a<br />

CtOCkwiSedirection attar the transit has been<br />

oriemad by a backeigfrr to the precedhtg ssatiin.<br />

angle-The incfinafion fo each other of two<br />

intersecting fines, measured by the arc of a circle<br />

imemxptad between the two finas forming the<br />

angfe, the center of the circle belmJ the point of<br />

hxtersecfion. See also adJW3ttMJ angle;<br />

nltltude: ●zlmuttr; azimuth angle; break<br />

angle; convaralon ●ngle;<br />

countarclockwlee ●nale: concluded<br />

angle; crab angle; crltlcal angle;<br />

crossing ●ngle; detlectlon ●ngle;<br />

dihedral angle; dlp angle; direct engle;<br />

direction ●ngle; dlatance angle; double<br />

zenith dlatance; drlff angle; EulerIan<br />

angles; Greanwlch hour angla; grid<br />

magnetic ●ngle; horizontal angle; hour<br />

angle; Interlocking angle; 10cal hour<br />

●ngle; Iocklng ●nole; look ●nglaa;<br />

meaaured ●ngle; merldlan angle;<br />

obllque ascenelon: observed angle;<br />

parallactlc ●ngla; phaae angle;<br />

reciprocal varflcal angle; refraction<br />

angle; rapetltion of angfas; rloht<br />

Muniplied by 2rI if expressad in radians, or<br />

multiplied by 360° if expressed in degrees.<br />

angular distortion-l. (cartography)<br />

IXstotilon in a map projection because of<br />

rronconfomxafity. 2. (optics) The failure of a lens<br />

to reproduce accurately in the image apace the<br />

angle subtended by two pJinte in the object<br />

space.<br />

angular error of closure-See arror of<br />

closure, definition 2.<br />

angular tlald—See angle of Iiald.<br />

angular magnlflcatlon—The ratio of the<br />

ar@e subtended at the eye by fhe image formed<br />

by an optical device, to the engle subtended af<br />

the eye by the object Itseff wkhoul the optical<br />

device. This is mnvenient where a distance in<br />

the objeci cannot be measured tor expressing a<br />

finear magnification, as In using a telescope.<br />

angular momentum—The quantlly otrtalned<br />

by multiplying the rmment of inertia of a body by<br />

Its angular epaed.<br />

angular perellax—See engle of<br />

convergence.<br />

12


MIL-HDBK-850<br />

change.<br />

●ngular rate-see ●ngular speed.<br />

annual Incquallty-seaeonal variation In<br />

•ngu~r ~hange O! directiin per unit waler fevet or tidal current Speed, trxYrOOr feSS<br />

time. Also celled angular rate. periodic, due chiefly 10 meteorologkal cauaes.<br />

errgufar vdocftY-A representation of Ihe rele ●nnual me9n011C chen9e-See mecinetlc<br />

of rmtetion of a partiile about the axis of ro!a!ion, sinnuel chenge.<br />

wlfh megnituda equal to lhe time rate of angular<br />

dbpfamnent of any gminl of the body. snnual megnetlc verlatfon-See<br />

meanetlc ennual varlatlon.<br />

angulsNor—An Instrumem tor converting angles -<br />

measured on en oblique plane to their annual perellax—The angle subtended at e<br />

a.rre~mling projactfons on a horizontal plane. cefaalial bodv bv Ihe radius of the Efuth’e orbff.<br />

A rectobllque plotter and photoangulator are<br />

fypes of mwsulators. See also aqulanflulator;<br />

topoenguletor.<br />

annex @nt-A pohd used to assist in the<br />

refet(ve orismaticm of verlicaf and oblque<br />

photogrephe, selected in the overtep area<br />

between the verlical and Its corresponding<br />

oblique about midway between the pass ~ints.<br />

Alternate acts of photographs only will contain<br />

annex points. See else pass polrsl.<br />

annOtetSrd photograph—A photograph on<br />

which hypeogrephk, gaobgii, cultural,<br />

hyorographic, vegetation, or place name<br />

Intormadon has bean added to Idemlly, classify,<br />

Outllrre, Clarffy, or descrtbe teatures that would<br />

not otherwise be apparent in examination of an<br />

unmarked photograph. Generally, the Iarm dees<br />

not apply to photofyapbs marked only with<br />

geodetic contrul or pass poirrta.<br />

annotation overprint-The outline delimiting<br />

a target or installation, or a symbol which bcales<br />

fts position together with an identifying refersnce<br />

number as depkxed on e target graphic.<br />

annotation WXS-A descriptive text containing<br />

the idWdifiCStbn. function. krcelbn, ohysical<br />

characteristics, and other “information c%ceming<br />

a target or installation, Descriptive tesls are also<br />

prepared for special areas, radar s&milicant<br />

fmwar lines, and precise radar signitlcam bcation<br />

points.<br />

annotation--(JCS) A marfring placed on<br />

Imagery or drawings for explanatory purposes or<br />

lo kxfiiate Items or areas of special irrpmlance.<br />

ennUal aberration—Aberration caused by Ihe<br />

vebcfry of the Earth’s revolution about the Sun.<br />

ennuat chenge-$ee magnetic annual<br />

Also called hefiocentrlc parallax; efellar<br />

parallax.<br />

annual rate of chang~ee magnetic<br />

annual chanoe.<br />

annual rate-See megnetlc annual<br />

change.<br />

annular ecllpsa-An eclipse in which a thin<br />

ring of Ihe seurce of Iiiht appeara around the<br />

obscuring bedy. Annular solar eclipses occur, but<br />

never annular lunar ecfipses.<br />

anomalistic drfft-The variat!an or dmt of a<br />

trequancy source. For example, the frequency<br />

changes 01 a crystal oscillator due to a variety of<br />

causes, such as temperature varfation and<br />

component aging, none of whmh can be<br />

pradlcted In advance or completely comrollad.<br />

anomellatlc month—The Imewal of time<br />

befwean two successive pssaages of the Moen<br />

in her orbit thruugh perigee. Tha length of the<br />

anomafislic month is 27.55455 mean solar days.<br />

enomafhstlc period-The intewal betwaen two<br />

successive perfgee passes of a satellite In orbit<br />

about its primary. Also called parlgea+fs.<br />

perigee period.<br />

anomallatlc tide cycl%The average period<br />

ot aboul 27 1/2 days, measurad frmm perigae to<br />

perigee, during which the Moon c=xrrptales one<br />

revolution eround the Earth.<br />

anomalistic yaar—The period of one<br />

revolution of the Earth around the Sun, fmm<br />

perihefbn to perihefiirr, 365 daYS. 6 hours, 13<br />

minutes, 53,16 seconds In 1955, and hwreasfng<br />

at the rate of 0.002627 second annually.<br />

enomaloua magnetic varlatlon—See 100s1<br />

13


I<br />

I<br />

magnetic enomaly.<br />

MIL-HDBK-850<br />

Wmrrtely-1. (general) A deviafhn fmm the<br />

norm. 2. (geodesy) A davialion of an obserwed<br />

vahse horn a lheoretkrrf value due to a<br />

correaptmdrrg irregularity in the Earth’s structure<br />

at Ike area of obaervafkm. 3. (astronomy) The<br />

angle bafwaen the radhss vector to an orbithg<br />

Ix@ fmm ifs primary and the line of apairfss of<br />

Iha orbii, rneawmd in Iha duacfion of travel. horn<br />

the point of cbaaaf a~ruach to the primary. This<br />

term ia also called the true ●nornely when if is<br />

desired to diafingulsh If from the eccentric<br />

atWtMaly, which is the correapmdhrg angle at<br />

tha cenfar of the orWf: or from the mean<br />

anomaly, which is what the true artOMSly would<br />

bacems ff the pfanat had a uniformly argufar<br />

motbn. 6s8 also Bossguer ●nomaly;<br />

deflection ●nomaly; free-air ●romely;<br />

gravity smomaly; Hayford gravity<br />

anomalles; height enomaly; Iaoetatlc<br />

anomaly; local magnetic anomaly;<br />

magnetic dlaturbance; mean trae-elr<br />

enomaly; point anomaly; aurlace<br />

anomeliea.<br />

Anlarctlc Circle-The gaogrephlc parallel<br />

heving a south Ia!itude equat to the complement<br />

01 the declination 01 the wimer aoksfiie. The<br />

obl~uhy et the acffpfk Ls$teadlly changing so<br />

that Iha wimar solstice la not a poinl of fiiad<br />

decfinstbn, and the Anfarctk Circla, as defined,<br />

is net a Iirm of Siied position. When the Antarctic<br />

Ctrcle is to be shown on a map, however, If k<br />

desirable that If be traatad as a Ilna of fixed<br />

position, and that a conventional valua be<br />

adopted for its latitude. For thie purpose, tha<br />

vslue 66°33’ south fatifucfe Is used. Alao calied<br />

south polar circle.<br />

antlhalatlorr coatfng-(photography) A fi9hh<br />

abaorblng Coating applied 10 Ihe backside of the<br />

auPPOr’fOf a film or plate (or between the<br />

emulsion and tha suPPort) to suppress halation.<br />

antlporSa-AnythinQ exactly Oppcrtilte to<br />

aomefhing alse. Parfioutarfy, thaf point on the<br />

Earth 180” horn a gfven place.<br />

arrtlaolar point-That point on the calastial<br />

sphere 180” fium the Sun.<br />

antfvfgnafftng filter—(JCS) A flffar traarlrrg a<br />

deposil which Is graduated In density to correct<br />

for the uneven Itlumlnafion given by cerfafn<br />

Ianses, Parllwlerly wide-ar@e fypas.<br />

apareon—The polnf on a Mars-centered orbit<br />

where a satellite is at ffs graatesl distance fmm<br />

Mars.<br />

●paetron—Tfsat Polnf ot Ihe orbti of one<br />

marr_bar of a double star system at whkh the<br />

stars are farthest apart. Opposite of perlaatron.<br />

aperlodlc compaa-fferally “a compass<br />

without a period,- or a compass that, after being<br />

deflected, returns by one dhacf movement to Ifs<br />

pmpar raading, without oscillafiin. Afso called<br />

deadbeat compeae.<br />

●periure ratio—See relatlve ●perture,<br />

aperture afop-(optks) The phyaicaf alernanf<br />

(such as a afop, diaphragm, or fans pa~hery) of<br />

an optkal system whkh limits the size of the<br />

pencil of rays traversing tha system. The<br />

adjustment of the size of fhe aperture stop of a<br />

@ven system regulates the brightness of fhe<br />

Image without nacassarily affecting the size of<br />

the area oovared. Aleo called etop.<br />

aperture-l. The opening In a lens diaphragm<br />

through which light pasaes. 2. The diamefer of<br />

the objecfive lens O! a Ialeaoopa or of her optical<br />

instrument, usually exfxasaad in irwhas, buf<br />

sometimes as the anffla between lines from fhe<br />

principal focus to opfmsffe ends of a diameter of<br />

the objeclive lens. See also relallve aperfura,<br />

apex—See vertex.<br />

aphaflon—The point in fhe alllpffcal orbff of a<br />

planet which is the farthest fmm the Sun, when<br />

lha Sun is the cenler of affracfbn. Opposffe of<br />

perlheflon.<br />

aphylactlc mep projection-A map<br />

projecfiin which ekes not possess any of the<br />

three special pmparlies of equivalence,<br />

conforrnafiiy, or erfuidisfarrca. Afao called<br />

arbitrary pro]ectlon.<br />

eplanatk lens-A lens which transmits fiiht<br />

without spharical ahrrafion,<br />

aplune (apoluna)—The point on the elliptical<br />

Mbif of a aalellffe of the Moon which is farlhes!<br />

Irom the Moon. Alao called epocynthlon.<br />

( Opposite of perflune; perlcynthlon.<br />

1mpoapala-See<br />

apocenter.<br />

!pocenter-in an alfiptical orbii. the poinl in the<br />

xbif whfch is the graalest distance from the<br />

1.4


focus where the affrecrlng mess is bcated. Afso<br />

called apoapslo; apolocus. Opposite 01<br />

pariapsla; perlcanter; perlfocus.<br />

●fsochmmaflc Sana-A lens that has been<br />

corraclsd for chromatic aberration lor fhree<br />

arbrs.<br />

●pocynthion—See ●plune (apolune).<br />

apofocua—See apocarmer.<br />

●pogaan llda~lldea of dacraasad renga<br />

occurring whan the Mrxtn is near apogea.<br />

●~aa+fCS) The point at which a misaifs<br />

trajectory or a satellite orbii is tartheat from the<br />

cemer of the gravitational field of the cormolfirtg<br />

bcdy Or bodis6.<br />

apoaphare-A mathematical surface of<br />

constant wrvetura applicable to the earfh<br />

spharoid over a crmlain fimlfed araa. It may be<br />

either obtate or prolate In shape.<br />

aprsaranl altlltsde-The obsetved vertical<br />

angle ot a cefasfial objecl corrected for<br />

inetrumermrl errors, peraonel errors.. and<br />

inaccuracies in the relsrence level (princlpe[ly<br />

d!p], bul not for raf racfiin, parallax, or<br />

semldiame!er. Also called racflfled altltuda.<br />

aPPerenl horizon-(JCS) The visible thre of<br />

demamfbn benveen Iandkea and sky. Also<br />

called local horizon; lopocentrlc horizon;<br />

vlaifsle horizon.<br />

aPParent motion—Motion relatlve to a<br />

specified or implied raferanca point which may<br />

Rseff be in rrwtion. The expression usually relers<br />

to movement o? celestial bodies as observed<br />

from the Earth. Also called relatlve motion.<br />

apParant noon-Twelve o’clock apparent<br />

time, or tha instant the apparent sun Is over the<br />

u~er branch of the merfdtan.<br />

apperent place-( astronomy) See apparerrl<br />

poaltton.<br />

aPPerant POaltlOIt-Ah astronomic term<br />

applied to the observable posillon of a star,<br />

planet. or the Sun. The posffion on the csleslial<br />

sphere at which a heavenfy body (or a space<br />

vehlcfe) would be seen from the center of the<br />

Earlh al a parfkular time. Also called apparant<br />

placa. See also aatromatrlc poaltlon.<br />

MIL-HDBK-850<br />

apparant precaaalon-(Jcs) The epperenl<br />

deflection of the gym axis, relative to tha Earth,<br />

due to !he rotating effect of the Earth and not<br />

due to arry applied form. Atso called apparent.<br />

wander; wander.<br />

apparent aldsrreal time-The local hour<br />

angle of the true vernal equinox. Also dad trua<br />

●ldareal tlma.<br />

●PPamnt Solar dey-lhe interval of fires from<br />

a trarraJt of the apparent sun across e given<br />

metilsm to its next suwssive transit acmes the<br />

same meridian.<br />

apparent ,?olar time-Time measured by the<br />

apparent dwmal rnotlon of the true sun. Also<br />

called apparent time: true solar time.<br />

apparartt aurt-The actual Sun as n appaare<br />

in fhe sky. Also called ttUO eun.<br />

apparant tlma-See apparent solar ttme,<br />

aPParant wander—See apparant<br />

precaaalon.<br />

apparent—A term used to desfgnate cetiain<br />

measured or measurable asfronom”c quantities<br />

to rater lfIeM to the obsem’ad position of celestial<br />

bodies.<br />

aPpeara nce rat lo—See h yperaterao.<br />

●copy.<br />

aPP~o,aCh chain-An aeronautical chart<br />

provxfmg asserrfial information for making an<br />

approach to an airfield under either visual or<br />

instrument fliim condtfions.<br />

approximate contour—A con!our subsfltufed<br />

for a normal contour whenever there Is a<br />

question as fo fts refisbilfty (refiabifiiy Is dafirrad as<br />

belna aCWmt9 wffhin one-half the comour<br />

Interval).<br />

aPPuJae-The naar approach of one celestial<br />

body to another on tha calestiaf sphare, as in<br />

occultation or cnnjuncf ion.<br />

apae llna-See Ilrte of ●paldea.<br />

apala—Either of the two orbffal points nearast or<br />

Iatlhest from the cemer of affrecfbn, the<br />

pdheibn and aphellon In Ihe c+esa of an Orbii<br />

about tha Sun, and the perigee and apogee in<br />

15


I<br />

I<br />

the C+WSOf an orbii about the Earfh,<br />

mbltrery grid-Any ralarenca ayefem<br />

devebped for use where no grid is available or<br />

practical, or where military security for fhe<br />

ralerenca is desired.<br />

arbltrsry projmtlon-see aphylectlc map<br />

projection.<br />

ARC Dl@tlzsd Rastar Graphics (ADRG)—<br />

Digital raster representalbna of paper graphk<br />

pmCfUCfa. Meps/charfa are mrwerted into digtial<br />

data by reefer scanning and transforming the<br />

map image Info the Equal Arc Second Raster<br />

ChartiMep (ARC) Syalem frame 01 refererce.<br />

Used for electronic map diaplaya. See also<br />

ARC ProjectIon System; Equal Arc<br />

Second Raster Chart/Map.<br />

ARC ProjectIon System-A coordinate<br />

system fhat divides fha worfd into 18 latitudinal<br />

zones. See afse Equal Arc Second Raater<br />

Chart/Map; ARC Dlgltlzed Raater<br />

Graphics.<br />

arc Correctlors-(panduium) The auantitv which<br />

is appfied to the @ricxf of vibral”bn of s ‘<br />

pandulum 10 albw for the perslulum’s departure<br />

hum airr’ple harmonic motion.<br />

arc meaauremant—A survey method used 10<br />

determina fhe stze 01 fhe Earm. A long arc Is<br />

measured on ihe Eanh% surface and the angla<br />

which aublends this measured arc is determined.<br />

By aasumpfions and mathematical Iormufa the<br />

size and shape of the Earth can then be<br />

determined.<br />

arc nevlgatlon-A navigation systsm in which<br />

the posiiion of an airplane Or ship iS mainfalned<br />

abng an arc measured from e comref station by<br />

means of electronic distance maasuring<br />

equipment, such aa ahoren. See else loran.<br />

arc Of parellel-A parl of an astronomic or<br />

geodetic parallel of fetifude.<br />

MIL-HDBK-850<br />

rxxrelafing focal surveys along the arc, furnishing<br />

dafa for [he determination of a geodatic d6tUm,<br />

providing a nafwo~ of corrtml points for a<br />

countrywide survey, etc.<br />

Arctic Circle-The geographtii parallel having<br />

a north IaIltude equal to tha complement of tha<br />

deOlhation of the Summer aolsfica. The obliquffy<br />

of the ec@fic is steadily changing so that the<br />

summer aolsf~ Is not a palm of lied<br />

dedinafion, and the Anxic Circla, aa defined, Ls<br />

not a fine of fixed poslfion. When tha Arctic Circle<br />

Is to be shown on a map, however, If Is dasirabfe<br />

that if fm treated as a fine of ~ued position, and<br />

Ihat a czmventional value be adopted for ha<br />

latitude. For this value SS” 33’ north fefifude is<br />

used. Also called nonh pofer clrcla.<br />

arc—1. (topo!ogy) An Individual line segmem<br />

defined by a series of X, Y coordinefe pake.<br />

Nodes are at the ends of arcs and form the<br />

points of irasrsection beiwean area, 2.<br />

(geodesy) A portion of a geodefic triangulation<br />

network, behveen two high-order stations. 3.<br />

Acronym for Equal Arc Second Baster<br />

Charl/Map,<br />

Araa Requlraments and Product Status<br />

(AR APS)—Dala base which describes DMAS<br />

customer area requirements and forecasts for<br />

various MC&G products. ARAPS is used by<br />

DMA to plan production schadules,<br />

area analyala Intalllganca-lnf alligance<br />

dafa ralatlva 10 a specific geographk area.<br />

araa covarage-1. Complete coverage 0! an<br />

area by aerial photography havin~ parallal<br />

overlapping fright lines and slereoacopic overfap<br />

behvean exposures In the fine of flight. 2. When<br />

appfied to shoran, tha term implias fhat rewrded<br />

shoran dislances ara availabla for aach<br />

exposure. 3. Complete coverage of a<br />

geographical area by maps or other graphic<br />

material.<br />

area pattarn acreerr-A photographic<br />

negative or posffive containing repafifively<br />

arc of vlelbllfty-The horizontal angular range arra~ed smafl feature ayrnbols which hava been<br />

through which a nevlgafion light is visible form designed to prasenf a visual portrayal of a rr@<br />

aaeward, The angular range is defined by or cnarf areaf feature: i.e., swamp, orchard, sand,<br />

limiting bearings of diracfiin. etc. See also contact ecraan: Ilne pattern.<br />

arc triangulation-A. system of triangulation of area tIUWOy-1. A eurvey of areaa large<br />

Iimffed width drssignad to progress In a single anough to raquire a nafwork of camml stationa.<br />

general direction, Arc frfangulafion is axecufecf for 2. An extension and dersefflcafion of survey<br />

fha purpose of connecting Independent and control.<br />

wfdefy separawd surveys. coordinating, and<br />

16


I<br />

MIL-HDBK-B50<br />

in one or rrmre cfimansions.<br />

area targat-(JCS) A target consisting 01 an<br />

area rather than a !$ifrg10point. sSO also erilflclal asteroid-A man-made objecl<br />

plnpolnt target. ptecad in oroil about the Sun.<br />

●rea triangulation-A symam of triangulation artlflclal Earth aelalllIe-A man-made Earth<br />

designed 10 progress In every diractiin. Area Ssfelfite, as distinguished from lhe Moon.<br />

kianoufetion is executed to orovide survev amtrol<br />

pointl over an area, as of the dsy or courify; or<br />

for fifih’rg In the areas bahveen arcs of<br />

triangulation whlcff term a network astendihg<br />

over a county or state. See also ●urvay net:<br />

trlangukstlon net.<br />

araa welohtetf avaraga raaolutlon<br />

(AWAR)—A single average value for Ihe<br />

resolution over the picture formal for any given<br />

focal plane.<br />

araal faetura-A topographic feature, such as<br />

sand, swamp, vegetatbn, ale., which extends<br />

over an area. It is represented on the published<br />

map or chart by a solid or screened color, by a<br />

prepared paftam of symbols, or by a dafimlting<br />

line. 2. (d!gital mapping) Any area ancfosed by<br />

a delimiting fine thal has any unique<br />

charactarfstic, e.g., forest, residential, etc. 3.<br />

(raster) A block of grid cells which repres,am a<br />

homogeneous portbn o! the earrh.<br />

ararx-A level of spatial measurement referring<br />

ro a two-dimensional defined space. A polygon<br />

on the earth as pro)ecfed onto a horizontal plane<br />

ia an example of an araa.<br />

areode8y—(.fCS) That branch of mathematics<br />

whkh dmemrlnes by observations and<br />

measurements, the exact poslfions of polrrts and<br />

the figures and areas of large poriions of fhe<br />

surface of the planet Mare, or the shape and size<br />

of the planet Mars.<br />

arflument<br />

mechanics,<br />

of letltude-in cateslial<br />

the angular dislame measured In<br />

tha orbit okrne horn fha ascendino node to Ihe<br />

orbiiirrg o“bjecf; the sum of the a~-umenf of<br />

perigee and the true anomaly.<br />

arflllclal horlzon+JCS) See atf It uda<br />

Indicator.<br />

artlflclal monumenf-A relatively permanent<br />

object used to idenfffy the location of a survey<br />

station or comer. Objects incbde man-made<br />

structures such as abuhmrmfs, stone markers,<br />

concrate msrkera, ati railroad rails.<br />

artwork predfcllon—See experlanca radar<br />

prediction.<br />

Arundel meihod-A combination of graphkal<br />

afrd analytical mefhods, based on radial<br />

triangulation, for paint-by-poim topographic<br />

mapping from aerial photographs.<br />

ascanstlng node-Thin point af which a<br />

planet, planefoid, or comet crosses the ecliptic<br />

trom soulh to norlh, or a saIellhe crosses lhe<br />

equmor of ifs primary rrom south to north.<br />

Opposite of descending nods. Also called<br />

nonhbound nods.<br />

eacendlng verflcal angle-see angle of<br />

alavetlon.<br />

aacanalonal difference-The difference<br />

between right ascension and oblique ascensbn.<br />

aspect categorlee-Classification of an<br />

aspacl into a grouping based on cardinal<br />

compass direction or a range ot degrees.<br />

aapecf change-(JCS) The different<br />

appearance of e reflecting object viewed by radar<br />

Im”m varying direcficns. Ilis tiuaed by the-<br />

change<br />

target.<br />

in the effective reflecting area of the<br />

argument of perlgae-An ortitat element<br />

defined aa the angle at fhe center of affractbn<br />

from the aacarrdino node 10 the oerioee oolnf<br />

aspact ratfo-Ttre<br />

width to height.<br />

numerical rafio of picture<br />

measured ifl the direction<br />

Orbitill(f body.<br />

of InOtiofl ~f the<br />

aspacta—The apparant positions of celestlal<br />

bOdiOS relatiVe 10 one arrothac perlcufarfy the<br />

aroumant—in astronomy,<br />

apparent positions of the Moon<br />

an angle or arc, as In relative to tha sun,<br />

or a plariet<br />

argumem of periiee.<br />

array-A sysf ematic arrangement of. elements<br />

aapact—Horizontal direction in which a slope<br />

17<br />

,


!<br />

I<br />

I<br />

faces, oomrnonfy expressed as me direction<br />

dodwvtae lmm nofih.<br />

sapherkal lens-A lens in wtich one or more<br />

surfaces dspafl from a true sptserfcal shspa.<br />

assault tandlng model-A 6pr3Cial 10fm of<br />

aasauff ttwfal designed apaclfkally for planning<br />

anmhibbus Iandiwas. Also called amohlbloua<br />

atiault landing ‘model. See also” aasault<br />

models.<br />

MIL-HDBK-850<br />

aasauft modal~arga-scale models giving a<br />

particular representation of vagatafion, Iaaaer<br />

Iandforrna, promlnerzt mart-made features, and a<br />

detailed repreaenfatbn of apacftic or sansltive<br />

ofziacfivaa such Ss alrfbkis, radar installations,<br />

and the Mre. These models empfraslze the<br />

aspects of objects as seen from surlaca<br />

approach<br />

aasoclated Legendre func.tlon-A solution<br />

of me Lagendre equatkmr, whkh is a apeciaf<br />

case of the Laplace equation, in the form of a<br />

power series of a speciaf kind; used In the<br />

spherical harmonic expansion of the gravitational<br />

potential.<br />

aersumed lalltud+The latitude af which an<br />

obaewer is assumed to be located for an<br />

observation or cxwnputaiion, as ihe latitude of an<br />

assumed poaifion or the Iatlude used for<br />

determining the krrrgnude by time sighf.<br />

aeaumed longltuda-The tongitude af which<br />

an observer is assumed to be focatad for en<br />

obaewafkm or computation, as the longitude of<br />

an assumed poshiofl or the brrgirude used for<br />

determinism the fatitude by mar~!an afmude.<br />

aSSWIMrd plaIstS coordlrratee-A iocaf plana<br />

cormlnata eyafem aet up af the convenience of<br />

the surveyor. The referance axes are usually<br />

assumed so that all ceord!nates are in the first<br />

quadrant. The y-axis may be in the direction of<br />

asfronomk north, geodetic north, magnefic<br />

norfh, or an assumed north.<br />

aeaurance level—See confidence<br />

Interval.<br />

aatatlzeri grevlmetar-A gravlmetar,<br />

sornalimae relemad 10 as unstable, where the<br />

forca 01 gravfty is maintained in an unstable<br />

equilibrium wkh lhe rastoring force. The h’ralabifiiy<br />

is provided by the introduction of a third fome<br />

which intensifies the atfecl of any change in<br />

gravity fmm the value in equilibrium.<br />

●atarold—A minor planet; one of the many<br />

small celestial bodies revofving around the Sun,<br />

most of tha orbits being between those of Mara<br />

and Jupiter. Also called minor planet;<br />

planetoid. Sea also artlflclal aalaroid.<br />

aetlgmatlam-An aberration affectfng the<br />

sharpness of imagas for objects off the axis in<br />

which the rays passing through difterem<br />

meridians of the kns come to a focus in dmaram<br />

planes. Thus, an extra-axial polnf object Is<br />

imaged as two mutually perpendicular attort lines<br />

Iocalad at ditteram distances lrom the lens.<br />

astigmatlzer—A iens which introduces<br />

astigmafiam into an optical aysfem. Such a lens<br />

is so arranged Ihat h can be placed in or<br />

removed Imm the optical path at will. In a<br />

sextam, an astipmalizer may be used 10<br />

aSSUMOd ground alevallon—The elevation elongate fhe image of a celesfial body into a<br />

assumed 10 prevail in the local area covared by a horizontal line.<br />

Dartkular DhOtocrraDh or arowz of r3holeoraoh5<br />

Used esticially-lo “denot~ the ele;ation-assumed astre flctlf—Any of several fictitious stars<br />

to prevail in the vickrity of a crilical point, such as assumed to move abng fhe calaatial equator al<br />

a peak or ofher (aature having abrupt bcai rafief. uniform rates corresponding to the speeds of Ihe<br />

several harmonic mnafiruems of the tideproducing<br />

force. Each aslre ficfif crosses the<br />

meridian at the instant the Conslituem II<br />

rapresenls ia at a maximum.<br />

astro compasa-(JCS) An instmmem used<br />

primarily to obtain true heading or true bearing by<br />

reference to celestial bodies.<br />

aatrodynamics—The practical applicatlrm of<br />

celestial mechanics, aslmbaliistba, propuleiin<br />

fheory, and allied fields to the problem of<br />

planning and directing the frajactorfes of space<br />

vehictes.<br />

astrogeodetic datum orientation—The<br />

poaMon 01 a relerance elnpsoid in relation to fhe<br />

geoid in a speciiiad area of a geodetic nefwork. tf<br />

may be expressed by the astmgaodalic<br />

deflection and geoidal height at the datum point<br />

or by an asfmgaodelic geoid charf of fhe area.<br />

aetrogeodetlc deflection—The angfa at a<br />

point between fhe normal to the gaoid and the<br />

18


I<br />

‘/<br />

,1<br />

normal IO the el~pao”kl of an aatrogeodetically<br />

oriented datum. Also called relallve<br />

delloctlon.<br />

●strogeodetlc levellng-A method 10<br />

dafennkse variations in the separation of the<br />

gaold and Ihe ellipsoid using aafrogaodetic<br />

deflecfbns. Afso called aatronomlc Ievellng;<br />

geoldal height protlla.<br />

●strogeodetlc undulatlona-The eeparatlon<br />

between an asvogeodeIic gaoidr defined Ior a<br />

particular datum, and a spacitiad aflipsoid<br />

8urlac6. See also geoldal helgfrt,<br />

●atrogreph rnesn time-A form 01 mean<br />

time,used in setting an astrograph. Aatmgmph<br />

mean time f20Cr occurs when the bcal hour<br />

angla of Aries is O“.<br />

aetrographlc pooltlon—See astrometrlc<br />

poaltlon.<br />

astrograpfs-1. A device for pro)ecflrrg a set of<br />

praco~bsd aftlfude cwwes onto a chart or<br />

pbrrlng sheet, the cvrves moving with lime such<br />

that if they are properly adjusted, Ihay wilt remain<br />

in the czxrect position on the chafl or ploning<br />

shee!. 2. A Ieleacops, usuahy cd moderate local<br />

length, which la desigpad specifically for Ihe<br />

Pu@se Of accurate~ reasrding the positiins of<br />

celastial obpcfs by photographic means,<br />

rsstrogravlmatrlc levellng—A concept<br />

whereby a gravimetric map is ueed for the<br />

h’tfetpolatiorr of the astrogaodalic dallecfions of<br />

tha verlical 10 delarmirre the separation of me<br />

ellipsoid and the geolcf In studying the figure ot<br />

tha Earth.<br />

aatrogravlmetrlc polnta-Astronomic<br />

pOdtiOn6 corrected for Ihe deflection of the<br />

verrkal by gravlmatrk methods.<br />

9!MrOlSSbS-1. (general) Any tnstrurrrent<br />

designed to rrraasura Ihe affiludes of csleafial<br />

bodies. 2. (surveying) An inelrument designed<br />

tor very accarate celestial altitude<br />

meaaurementa. See also ●qulenguletor;<br />

pendulum eetrolabe; planlspharlc<br />

astrolabe; prlematlc aslrolabe.<br />

●etrometrlc posltlon-The position of a<br />

haaveniy body (or apace vehicle) on the celestial<br />

sphera cmracted tor aberration buf nof for<br />

pfanatary sbarration, Astromatdc positions are<br />

usad In pftotcgrapfsic observation where lfte<br />

posfflon of the observed body can be meaaured<br />

MIL-HDBK-850<br />

in reference to the f%%stiionaof @ntparfacrn stars<br />

in fhe fiafd of the photograph. Also called<br />

aatrogrephlc posltlon. See also ●pparent<br />

posltlon.<br />

astromet~-The branch of astronomy daalhrg<br />

with the gaomatrfc ralatbns of the celeafiaf<br />

bodies and thek real and apparanf ntofbns. The<br />

techniques of asfromstry, eapsclally the<br />

determination of accurate poaftion by<br />

pftotographlc means, are used in trac+dng<br />

satellites ad space pmbas.<br />

aatronomlc arc-The apparent arc described<br />

above (diu-1 src) or below (nocturnal arc) fha<br />

horizon by the Sun or another celestial bcdy.<br />

eatronomlc azimuth msrk-A marked point<br />

whose astronomic azimuth fmm a survey station<br />

is determined from direct ob$arvatbna on a<br />

celastial body. me mark may be a tamp or<br />

M,rmineted target placad aspaclally for the<br />

purpose: ff may be a well deflnad Wumfnated<br />

point on a permanerrf afructural point.<br />

astronomic azimuth—The angle between the<br />

astronomic meridian plane of the observer and<br />

the plane containiW the observed point and the<br />

Irua normal lvartical) ot the obsewer. rnaaeursd<br />

in the plane of the horizon, preferably cbckwise<br />

from north.<br />

eStrOnOMIC bearing-See true bearing.<br />

astronomic constants—The elanssnts of the<br />

orbits of tha bodies of the @lar system, their<br />

masses relative to the Sun, their size, shape,<br />

orientation, rotation, and inner constitution, and<br />

iha velocity of light. See also system of<br />

aetronomlc conatanta.<br />

astronomic controf-A network of cmrtrol<br />

stations the poslfions of which have been<br />

determined by astronomic observation. Latitudes<br />

and longitudes thus determined will normally<br />

differ horn the gaodefic latitudes and longitudes<br />

of the same stations by amounts corra~nding<br />

to mntponents ot tha deflection of ths vertical.<br />

astronomic coordlnatea-1. Quantities<br />

defining a poln! on the suflace of the Eatlh, or of<br />

fhe gaoid, in which the local diraciion ot gravity is<br />

used as a raferance. Also called geographic<br />

coordlnstes; gravlmetrlc coordlnatea;<br />

terrestrial coordinates. 2. The coordhra!es<br />

of an astronomic body referred to a given<br />

equinox.<br />

1


stetronomlc deta-DMgnatfon of epoch by<br />

year, month, day, and dacfmal fraction. For<br />

ezsmpfe, the astronomic dale of Dacerrtrer 21,<br />

1978, 18h UTC (univeraaf time morcfhalsd) is<br />

1978 Dacarrtrar 21.75 UTC. The astronomic<br />

date k also used In Omrrecfbn wilh the other<br />

lime systems. me system commences every<br />

cafendar year at Oh on Decatir 31 of the<br />

previous year. This epoch is denoted by .faruary<br />

0.0.<br />

astronomic day—A mean mlar dey beginning<br />

at mean noon, 12 hours feter than the beginning<br />

of the cIvII day of the earns date, Aafmnomers<br />

now genaralty use the civil day.<br />

astronomic equator—The fine on the surface<br />

of the Earth wfmse astmnomk fatituda at everv<br />

point is O“. Due 10 the dafbcfion of the plumb’<br />

iine, the aafronomk equator is not a pla”ne curve.<br />

However, the verficafa a! all points on k are<br />

parallel to one and the same plane, the pfane of<br />

the celestial equator; that is, the zenith at every<br />

point on tha eetmnomk equator lies in the<br />

caleatial er$zalor. When lhe astronomic equalor<br />

is corrected for station error, ii becomes the<br />

geodetic equator. Also called terrestrial<br />

aquator. See aiso geodafic aquator.<br />

astronomic latltud+The angie between the<br />

plumb fine and the plane of celestiai equalor.<br />

Also defined as fha angla be fwean tfra piane of<br />

the horizon and the axis of rotation of the Earth.<br />

Astronomic kitnude appfies only to posltfons on<br />

the Earth and is reckoned from the astronomic<br />

equator (0°) notlh and south through 90°.<br />

Aafmnomic Ietffude is the Iatffude whkh results<br />

directly fmm obaervatbns of celestial fmdles,<br />

urcorrecfed for deliecfion of the vertical.<br />

astronomic lavellng—See aatrogeodetlc<br />

ieveling.<br />

eatronomlc iongltude-The angle between<br />

the ptene of the celastlal meridfin end the plane<br />

of an iniiial merfdiin, arbffrarffy chosen.<br />

Astronomk bngffude la the longitude which<br />

resuffs directly from obsewations on ceiesfial<br />

toches, unmrrected for deflacfbn of the vertical.<br />

aatronomlc merldlan plane-A plane that<br />

cdmains the verrfml of the obsewer and is<br />

~a#rl to the inalanrsnaas rotation 6x19 of the<br />

aatronomlc meridian—A great circle 01 the<br />

MIL-HDBK-850<br />

calestial sphere Imersacfing the ncmh and muth<br />

ceiestial poles. me local astronomk marldian is<br />

[hat meridian whtih intersects the zenffh of fhe<br />

poinl.<br />

astronomic parallef-A fine on the surface ot<br />

the Earth which hes the same eshncmdc<br />

Ialiiude at every point. Because the deffactiin of<br />

the veflid is not fhe SSmS at all pofms on tha<br />

Earth, an astronomic peraflsl IS an irregular fine.<br />

not Iyhrg in a single ptane. See afso<br />

aetronomlc equator.<br />

setronomlc poaltion-1. A pdim on the Earlh<br />

whoaa coordhrates have been determined as a<br />

reeuff of observations of caleslial bodies. The<br />

expression is ueualfy used In connacibn with<br />

positions on iand determined wffh greet erxasracy<br />

for survey purposes. 2. A point on fhe Earth,<br />

defined in terms of astronomic Iatituda and<br />

fongllude.<br />

astronomic refraction error-See<br />

astronomic refraction.<br />

astronomic reflection-Tha apparent<br />

displacement of an object that resuffs hem fight<br />

rays from a source outside Ihe atmosphere being<br />

bent in paasing through the atmesphare. This<br />

rasults in all objects appearfrq 10 be higher<br />

above the horizon than they actuaffy are. The<br />

magnitude of Ihk dbplacemem is greater whan<br />

the object Is near the horizon and decreases to a<br />

minimum assumed to be zero when the object is<br />

al the zeniffr. Afao calied aatronomfc<br />

refraction error; calestial refraction. See<br />

afso atmosptserlc ref racllon; rafractlon.<br />

astronomic station—A point on the Earth<br />

whose position has been determined by<br />

observations on cefestial bodies.<br />

aafronom fc ●urva ylng—The caleafiaf<br />

determination of latitude and bn@sde.<br />

Separations ara cefculaled by mmputirrg<br />

distances corresponding to measured angular<br />

displacements afong the reference spheroid.<br />

astronomic theodolita—See altazlmutft<br />

Inatrumant.<br />

aatronomlc tidal constltuant-See<br />

constituent.<br />

astronomic tfme-sofar time In a day<br />

(astronomic day) that begins at noon. Aafronomic<br />

Ime may be eilher apparem solar Ifme or mean<br />

;olar time. Since 192S, civil tires is generalfy<br />

2‘o


I<br />

,<br />

MIL-HDBK-850<br />

used instead 01 astronomic time. on a map, photo, or other graphic in terms 01<br />

nurr’bars and letters. Afao allad alphanumorlc<br />

siatronomlc<br />

4.<br />

Wsrtmlt-sae tmnsft, definition grid.<br />

●stronomic trfnn@-The navigational<br />

atmosphom-(JCS)<br />

Earth. See also<br />

The ah surwmsfing the<br />

Ionorsphem; ●ratospham;<br />

trfar@e, efthar terrestrial or celestial, used In Ihe lr0pOPau8a; tropowrhore.<br />

eokrtbn of cafaatial obsawatbns. Referrfno 10 tha<br />

Cttk@al sphere If Is the triangle formed by-arcs of atmospheric dreg-A mapr perturbation of<br />

great circiae connacfing the cefestial pole, the cJoaa artificial aalaliite orbits”missed by the<br />

zenffh, and a celestial body. The angles of the rasbtame of the atmosphere. The eecular<br />

.mtronorrrk lrkerrgfes are: al lhe @e, the hour effects ere decreasing SCC8nfrkclfy,major axis,<br />

angle; et the catastial body, the parallactic angle: and period. Afao mllad dreg.<br />

at the zertkfh, the azirruth arrgla. The sidaa arc:<br />

poie to zenith, the cdatltucfe; zenifh to celeatiil atmospheric ralractlon-llre ralracfion 01<br />

body, the zanfth dmtanca: and Cafastjal body to fiiht passing thnrrsgh tha Earth’s atmoephem.<br />

pole, the polar distance. Akur called PZS<br />

Atmospheric retraction includes troth astronomic<br />

trlarrgla.<br />

re?ractfon and terrestrtaf retraction.<br />

aatronomlc unit—A unit of iengfh equal to atomic tlm+l%rra intarval based on the<br />

149,600,000 klfomaters (ecfopf ad 1960) ue8d for frequency of atomb oscjilators.<br />

measuring dlstancas wffhln the adar system. Ttsls<br />

dfatanca approxlmafes the mean distance of the atran—An acronym for “automatic terrain<br />

Earsh from the Sun. recognition and navigatkrn, - a navigation System<br />

which depends upon the cwrelalion of Iarrain<br />

astronomic yeer—See tropicai year. ima~as appearing on a radar cathode-ray tuba<br />

with previously prepsrad maps or simulated radar<br />

astronomic-CX or panaining to astronomy, the images of the terrain.<br />

~ie~ wtrkh treats of heavenly bodtes, and the<br />

arts based on tha! science. attenuation—(JCS) Decrease in intensity of s<br />

signal, Ixram, or wave as a resuff 01 absorption 0!<br />

ASW PredictIon Aree Chert (ASW)—A energy and ot scattering out ot the path of e<br />

etandard DMA hydrographic charr (Antisubmarine delactor, bul not inckrdlng the reduction due to<br />

Warfare) overprfntad wfth homogeneous acoustic oaometrb soreadino, i.e., the inverse sauare of<br />

provinces characterized by a single vebclty ~istance etiecf. -”<br />

profile, a tmffom bss class, and a bafhymefric<br />

relief.<br />

attitude lrsdlcator-(JCS) An instrument whjcft<br />

displays the attitude of the Srlrwatt by refanmca<br />

esymrnetry of object {tsrget)-Lack of to sourma of Information whkh may be<br />

symmetry in Ihe visible aspect of an object aa contained within the in6tnsmanf or be axtamal to<br />

seen from a paniWfar point of observation. A it, When fhe sources of infOMIatlOn are eeff-<br />

square or recfangulsr pole may so faca fhe comained. The instrument may be referred 10 as<br />

I observer thst the line bisecting<br />

not pass through Ifs geometrb<br />

ifs targems<br />

center. Wih<br />

does<br />

a<br />

an artltlelel horizon.<br />

I<br />

equate cupola or tower, the error raauffing frum<br />

obaawfng tangema and taking a mean may be<br />

attitude-l.<br />

determined<br />

(JCS)<br />

by the<br />

The coaition of a body<br />

inclination of the axes<br />

es<br />

to<br />

quffe iarga. The error caused by asymmetry of an some frame of referenca. If not olherwise<br />

observed object fe of the same character and aoacified, lhis trame of reference ie fixed to the<br />

@Wl~ the Same treatment as the error<br />

reSU!hfSg from ObSeWing an SCGantriC object. see<br />

Eanh. 2. Grid bearing relative to tha bng axis<br />

of the target 3. (phOtOgrarrMrStW) The angular<br />

also phaee. orientation of a camera, or of the photograph<br />

●symptole-A sfraighf line or curve which<br />

taken with thai camera, with respect to SOMU<br />

esfemal referanca system. Usually axprecaad se<br />

some csmae of intlnite length eppmach but tilt, swing, and azimuth: or roft, pitch, and Y-.<br />

nevar reach.<br />

attribute fde ntlfler-A Ihree-alphanumeric<br />

atlaa grid-A reference system that permits fhe cheracter designator o! an attribute.<br />

designation of the location of a point or an area<br />

..:


I<br />

1<br />

ettrtbuto tagging-The process of assigning<br />

an attrfbufe to a particular feature.<br />

attrfbuto valua-A specific quelity of quamity<br />

assigned to an attribute.<br />

atfrlbut.-A characteriatii of a site or<br />

phenomenon. May be physical, ~Cktl. economic<br />

or tttutar h nature. For exarrrpfe, road types and<br />

mad names are road attrttwlee.<br />

aUglllanliillOn corr~ctlon-A ~rfe~~n due<br />

to augmamatbn, particularly tfsat sextant aftitude<br />

CWWdOff de to the epparem fncreaee In the<br />

semHiamatar of a cakrstlssl body aa Its SNduda<br />

Increases.<br />

augmentation—The apparent Increase in the<br />

sem”kiiametar of an asimuth celestial body as iis<br />

attitude InCreases, due 10 the reduced dlsta~<br />

hem the obsewer. The term is used principally in<br />

reference 10 the Moon.<br />

auarnontlng fBctor-A tacfor used In<br />

I+NV’Wflen wtth the harmonic enatysis Of tides or<br />

tldSl currents to alfOw for the difference beWeen<br />

the times of frourly tabulation and Ins<br />

corresponding ccmatituem hours,<br />

Australian National apherold-A reterence<br />

spheroid travlna the tolbwino dimensions:<br />

I Stimimajor axi&6,378, 160.ti meters; and a<br />

tiattening or eltiptictty 01 1/298.25.<br />

aUetrel-Of or pertaining to south.<br />

authallc (eoual-araa) latituda-A Ia!llude<br />

based on a ~ara hating the same area as the<br />

apherold, and aucfr that areas between<br />

auccesshre parallels of latitude are exactly equal<br />

to the corresponding areas on the spheroid,<br />

Authaik Iatltudea are used In the computation of<br />

ecfual-araa map projections.<br />

❑uthallc map projection-An equal-area<br />

-P proiecfkm.<br />

auto reflection-The focusing of an<br />

aufocollhrrating thaodolile on the surface of the<br />

mirror or prism rather than focused at infinity. The<br />

Irnqe aaan is on the lace of the refleclor end<br />

the gauss fma~ wIII follow the rndbn of the<br />

ratide. Whereas, In autocollimatlon, the<br />

instrument is focused at Infinity and the gauss<br />

Image movaa In o~sile diracflons to the<br />

reticule.<br />

MIL-HDBK-850<br />

snrtocolllmatlon-( surveying) The procedure<br />

used to dalerrnine or transfer azhruth to an<br />

instrument or devke. This procedure raquims use<br />

of a epacialiy edapted telescope, capable of<br />

bisecting the real image of its own mtkde as<br />

reflected fmm a mirror or Porro prism. When such<br />

bwuiort la accsmspiishad, the line of sight of the<br />

tele~pa ,b parparxjicular to the face of the<br />

mirror or apax adge of the prism.<br />

autocolllmator-A callimetor provided wish a<br />

means of Ilturninatlng tts woes tsalra so that,<br />

when a reflecting plane Lsplaced normal to the<br />

ernargam Iighf beam, the reflected image of the<br />

cross hssheappears to be @incidenf whh the<br />

cross haira themselves. This devise Is used in<br />

calibrating optical at’d mechanical inStrWtSntS<br />

and transferring direction,<br />

srutofocue ractiIier-A precise, venical<br />

photoerdarger whch permits the correction o!<br />

diatoflbn in an aerial negatiie caused by titt. The<br />

instrument’s operationa are motor drtvwn and are<br />

interconnected by mechanical linkages to hssura<br />

automatically maimained sharp tocua.<br />

Automated Alr Facllltlesr Intormatlon File<br />

(AAFIF)+mputer file of structured<br />

information defintng validated attributes relalive<br />

to Iaciiiiies tor each airfield o! concern 10 DoD<br />

flight operations.<br />

Automated Mapping / Facllltles<br />

Management (AM/FM)-A computer aided<br />

mapping system whkh stores annotatbn and<br />

iimiled attribule data. AM/FM systems are<br />

commonly used by the utility irslustries and<br />

municipaiilias.<br />

Automated Tectlcal Target Graphic<br />

(A?TG)-A Iactkal target materiafs item whkh<br />

provides aarfal photographic coverage of a target<br />

and a limited araa surrounding n at a scale<br />

permitting optimum identifbatiin 01 tsroet detail.<br />

Tha ATTG also includas taxtual Inteil!genca on a<br />

shaet separate fmm tha graphic portion. Each<br />

pan can be revised indepanderrl 0! the other.<br />

AITG’s cover single targets and are p+oducad in<br />

two forms: a lithographic sheet and a<br />

miniaturized version in an aperture card.<br />

automated Impoeltlon machlna-(miso,<br />

mlsomax] A step and repeat machhre used to<br />

expose multiple images onto either e printing<br />

plate or sheet of film.<br />

Automatic Digital Annotation System<br />

!2


(ADAS~A system used to reaml camera<br />

positiin and other Informaikm on film at time of<br />

exposure.<br />

●utommk cllpplng/Jolnlng-The system<br />

capability for *ying srnatt portions of a data<br />

besa for nrovarnant and plamrwd elsewhere in<br />

the data base wlthoui operator intervention.<br />

●utomatic gage-Sae self-rafpaterlng<br />

gaga.<br />

●utomatic lavaf-See pendulum Iaval.<br />

●utomatic polygon cerrtrold calculatlon-<br />

The system capabtitty for determinlrsg the center<br />

of a plygon ama without operator Intervention.<br />

Usually aaaocieted with automatic label<br />

plecement.<br />

●ufomatlc rectlflar-Any racfiiier which<br />

ernpbys mechanisms to Insure automatic<br />

tultillmant of the lens law and Ihe Schelmpfkrg<br />

Concffiion. These devices, called Invaraora,<br />

provide a mechanical eolutkm for the linear and<br />

angular elements of rectif”albn. Essentially, this<br />

ctass d rectitiir Is a lilt analyzer using inveraors to<br />

solve lo; the opticat geometric elements needed<br />

for eharp focus.<br />

autometlc rod-see tape rod.<br />

Wiomallc ●Uspplng—The .$yatem capability<br />

for oomplafhrg a line segment whose end<br />

approaches a predefine threshold of ctosenasa<br />

tc an krferaecflon or node, whhwt eny operator<br />

Intewentlon.<br />

automatic trrrvarse ccmpuler—<br />

autoradar plot—See chart comparison<br />

unit.<br />

autoroduclng techymeler-A CISSS of<br />

tadrymeter by which horixcmfal and height<br />

dmances are raad alrruttanaousty. Hortsontal<br />

distance la tha intercept nruttipiied by 100 and<br />

the vet7iil distance is the mkfWre (curve)<br />

rnuttlplied by a taaor which appaare in the optics.<br />

autoecreen film—A photographic film<br />

emifrg a hamone screen wrrich automatically<br />

produces a hatffcne nagatiie fmm mntinuous<br />

tone copy.<br />

autumnal aqsslnox-That point of Intersactlon<br />

of the acliptic and tha celestial equator ocwpied<br />

MIL-HDBK-85D<br />

by the Sun as It changas from notlh to south<br />

declinatbn, about 23 Septen&r. Ako ceiled<br />

flrat point o? Libra; Septamber equlncx.<br />

●uxllla~ contour-Sea supplementary<br />

contour.<br />

rsuxlllaty guide marldlati Whara guide<br />

meridians hava been placed at Intarvala<br />

excatiw tha distance d 24 miles, and new<br />

govaming tines are required, a new gUide<br />

rtsatii is eatebiiahad, and a toed name is<br />

asaigrrad, such ae Twefffh Auxiibry Gulda<br />

Maridien West,” or ‘S3reaa valley Quide<br />

Meridian.. Auxitiary guide meridians are<br />

surveyed, in the same manner as guide<br />

meridians. See alae guide markttan;<br />

prlnclpal marldlan.<br />

auxllla~ meandar cornar-An auxiliary<br />

meander comer ia established at a aultabta point<br />

on the meander iine 01 e ieke lying entirety within<br />

a quarter sacfion or cn the meander Iina of an<br />

lstend falling entirely wtthin a section and which is<br />

found to be too small to subdivide. A line is fun<br />

connecting the monument to a regular corner on<br />

the section boundary.<br />

auxlilary station—Any station connacred to<br />

the main scheme net and dependent upon tt tor<br />

the accuracy 01 ita posilion.<br />

evaraga devlatlon—in ssalislica, the average<br />

or arithmetic means of the deviations, taken<br />

wlthwt ragati to algn, from some fried value,<br />

usuatiy the arithmetic maen et the data. Atso<br />

callad mean davlatlon.<br />

evemge tarreetrlal pots-The average<br />

posttlon of the Inafantenecus pole of mtatlon of<br />

the Earth, aversged ever a apaclfbd time period.<br />

See also conventional international orlgln.<br />

avaraging devlc&A device for averaging e<br />

number of raadirsga, es on a bubble aexfant.<br />

axla of homology—me Intereectbn of fhe<br />

ptana ot Ihe phonograph with the horfxonfai pbme<br />

cf the map or the ptana of nsfamnca of the<br />

utound. Conespomiing lines In the photograph<br />

and map planee interaacl on the axis of<br />

hornciogy. Also callad the S61a of<br />

perapactlva; map pamltal; perspective<br />

axla. See also ground parallal.<br />

axia of Iana-saa optical axla.<br />

axis of laval-S e e aplrtt Iavel ●xia.<br />

23


I<br />

,<br />

(<br />

I<br />

axlo ot perspsrctlve-See axis ot<br />

homology.<br />

axis of the level bubbl=ee aplrlt level<br />

axis.<br />

321s of tiff-A Ilne through the perapadive<br />

cemer perpendkzdar to the principal pfene. The<br />

ask of tiff mufd be any 01 several Ilnas In apem<br />

(e.g., the tsonratrk parallel or the ground fine),<br />

buf the praeem definffbn k the onfy one which<br />

parmifa the smncapf of lifting a photograph<br />

without upaetfing the pxifionsl elements of<br />

exterior orfenrafion.<br />

●x19—See camera axis; colllmetlon axle:<br />

eoordlnato axes; ●quatorlal axla; flduclal<br />

axes; Itorizontal axla; major axis; minor<br />

axis; ~tlcal axis; polar exla; eemlmajor<br />

axla; eamlmlnor axle; ●plrtt level axta;<br />

topple ●x18; tranaverae axle: vertical<br />

axla: x-axla; y-axln; a-axis.<br />

azlmurh engk--l. (JCS) An angle measured<br />

cfmfswfse In the horfzomal pfane between a<br />

reference direcfbn and any other fine. 2.<br />

(astronomy) The angle 1SO” or less between the<br />

pfane of tha cefsstial meridian and the vertical<br />

pfane containing the observed object, reckoned<br />

from the direction of fhe elevafed pole. In<br />

astronomic work, the azirrsrfh angle is the<br />

aphetlcal angfe at fhe zenith h the astronomic<br />

WiarTgle whti k co~aad of lhe pole, fhe<br />

zenith, end the star. in geodetic work, if is fhe<br />

horizontal angle fMrween fhe celestial pofe and<br />

the observed terrestrial object. 3. (suweylng) An<br />

angle in triangulation or in a traverse fhrough<br />

which fhe corrpufatbn of azimufh is carried, In a<br />

airnpfs fraveme, every angle may be an azimuth<br />

angfe. Sornefhnas, in a haversa, fo avoid<br />

UWIW ~~hs over very short lines,<br />

WPPfefnenfarY Obaewafions are made over<br />

rnmPar~ivalY IOW Iiwa, fha angles between<br />

which form ezkrrufh engfes. In triangulation,<br />

certain angles, because o! their size and posilion<br />

in the fiiure, are selacred for use as azimuth<br />

angles, and enter krfo fhe formafisn of the<br />

azimuth ssxsrliiion equatbn (azinwIh equation),<br />

azlmufh bar-Sac ●zimuth Instrument.<br />

ezlmuth by aftftude-An azlmulh determined<br />

by solution of the navlgatkmal triangle with<br />

affitude, declination, and Iattrude given.<br />

azimuth cfrcla-A ring designed fo fif snugly<br />

Ovar a Conrpasfs or compass rapeater, and<br />

MIL-HDBK-850<br />

prcndded with means for observing wrnpass<br />

bearings and azimuths.<br />

azimuth equation-A condition equatton<br />

which axpresses fhe refstbnahip between the<br />

iixed =ifnuths of two fines which are rnnrrecfed<br />

by triarrgufefiin or traverse.<br />

●zimuth ●rror of clowre-See ●rror of<br />

cloaur% definifbn 3.<br />

azimuth Instrument-[magnetic) An<br />

instrumem for measuring azimuths, paniilarfy a<br />

devke which fiis over a cemral pivot in the glass<br />

rover of a magnetic mnpass. Alaa called<br />

azimuth bar; bearing bar.<br />

ezlmufh ffne-(photogremmetry) A radial line<br />

from the principal poird, iaocemer, or nadir point<br />

of a photograph, representing fhe direction to a<br />

similar point 01 en adjacenf photograph In the<br />

same flighf Iina: used extensively in radial<br />

triangulation.<br />

azimuth mark-A me~ aef af a aignftbant<br />

distance from a lriengulsfion or traverse efatbn<br />

to mark the and of a line for whkfr the azimuth<br />

has been determiner!, and 10 sewe as a starfiW<br />

or reference azimuth Ior later use. see also<br />

asfronomlc azlmufh mark; geodetic<br />

aztmuth mark; Laplace azimuth mark.<br />

azlmufh resolution-(JCS) The abNity of radar<br />

equipment to separate two reflectors at simifer<br />

ranges but dtierent bearings from a reference<br />

point. Normally the minimum aeparatiin dfsfanca<br />

between the reflectors is quoted and expressed<br />

as fhe angfe subtended by fha reflectors sf ths<br />

reference poim.<br />

ezlmuth transfer-Connecting, with a straight<br />

line, fhe nadir palms of two vertical photographs<br />

selecfad from overfepping flights.<br />

Sxlh’mfh traverae-A survey travarse in which<br />

the dlrecfbn of fhe measurad murse fs<br />

determined by azirnufh and verified by back<br />

azimuth. To initiate this type of traverse h ks<br />

naceasary fo have a referanca meridian, either<br />

true, magnetic, or assumad.<br />

1ezlmuthel<br />

charf-A charf on an ezirnufhal<br />

Iprojacfion.<br />

Also called zenlthal chatt.<br />

1B21muihal<br />

equldlalanf charf-A chart on fhe<br />

azimufhaf equidlstanf map projection.


●zimuthal equldlstmrt map pro]ectlon—<br />

An szknuthal map projecfiin on which straight<br />

Iiaa radiiting from the center or pole 01<br />

projection represent oreal circles in Ihelr true<br />

azimuths Irom fhal center, and !engths abng<br />

those iinea am 01 exact scale. mia pro@cfion is<br />

neither equal-area nor contormal.<br />

szlmuttral map proJoctlon-A map<br />

projection on whkh the azimuths or direcfiins of<br />

all fines radiating from a central point or pole are<br />

tha same as the azimuths or direcfiona of the<br />

mrraapondirrg fines on the sphere. Afso called<br />

zenlthel map projection.<br />

●zimuthal orthomorphlc map proJactlon-<br />

See ●teraographlc map projection.<br />

azimuth-l. (JCS) Ouamities may be<br />

expressed in positive quamifies increasing in a<br />

cbckwise direction or in x-ly-cmtinales where<br />

south and wesf are negative. They may be<br />

referenced to true north or magnetic north<br />

depend@r on lhe particular waapon aystam<br />

used. 2. (sutveyir@ The horizontal dlrectiin 01 a<br />

line measured cleckwise from a relarence pfane,<br />

usually ths meridian. Also called forwsrd<br />

Eztmuth to diflerenliale Irom back azlmufh.<br />

3. [photogrammetry) Azimuth of lhe principal<br />

plane. See also astronomic azimuth;<br />

●zlmuth by attitude; back azimuth;<br />

computed ●zimuth angle: dlractlon<br />

method Of determining astronomic<br />

azimuth; geodetic azimuth; grid azimuth;<br />

Inarflal azimuth; Laplace azimuth;<br />

magnatlc azimuth; method of repetitions<br />

(derermlnatlon of astronomic azimuth);<br />

MkrOMOter method (data rmlnatlon of<br />

ISStrOnOmlC azimuth); normal section<br />

ezlmuth; true azlmufh.<br />

MIL-HDBK-850<br />

25


MIL-HDBK-850<br />

Bacfro-Wurdom hams-llne ftIsifMrlng<br />

apparatfsa-A compensating bsse fine<br />

rnaasurrng apparatus having a measuring<br />

element corrymsed of a bar 01 hon and a bar of<br />

brass, each a fiila lass than 6 maters in length,<br />

hefd together firmly at one end, with tha free<br />

ends so connected by a mrnpansating lever as<br />

10 lorrn a cxmrpansatlng apparatus.<br />

beck aslmuth-1. (geodetic surveying) If the<br />

azimuth of point B frem point A is given on a<br />

reference sphere or elllpeolcf, the back azimuth<br />

Is the azimuth of point A from point B. Because<br />

of the cmwergaxe of !he rnarfdans, the<br />

forward and backward azimuths 01 a line do not<br />

differ by exactly 180”, except where A and B<br />

have the same geodetic bngitude or where the<br />

gaodefii tetitudes o! bolh pdnts are 0“. 2.<br />

(plane surveying) When referred to a plane<br />

rectangular coordinate system, same as above<br />

except forward and backward azimuths differ by<br />

exactly 180”. See also azimuth, definffion 1.<br />

back bearing-l. A beering differing by 180”,<br />

or measurad in the oppxffe direction from a<br />

gh+en bearing. Also calied reciprocal<br />

bearing. 2. The bearing al the opposite end<br />

of a line from the observer as measured lrom<br />

the true meridian al the opposite end of the line,<br />

The back bearing on all lines (other Ihan norfheoufh<br />

~M3S) are diierenf from the bearing at the<br />

obaerve~s sta!lon. They differ by the amount of<br />

cerwergancy of the meridians between the two<br />

peinte.<br />

back local distance-Se e beck local<br />

Iongth,<br />

back focal length-The distance measured<br />

along the lens axis from the rear vertex 01 the<br />

Iena to the plane of best average definition, Also<br />

calied back focal dlatanca; back tocua.<br />

back tocua-see beck focal length.<br />

backalght—1. A sight on a previously<br />

established survey point or line. 2. (traverse) A<br />

sight on a previously estsbtiehed aunray point,<br />

which is not the closing sight of the traverse. 3.<br />

(leveling) A reading on a rod held on a poim<br />

whose elevation has been previously<br />

detemrinad and which is not fhe cbsing sighf of<br />

a ievel circatit: any such rcd reading used to<br />

B<br />

determine he’~ht of Insfnsrrranf prior to making<br />

a forealgM. Also cetlad plus slgfst.<br />

backatep-The method of determining the<br />

offsata for the bottom krthude of a pro@fbn by<br />

measuring the appropriate distances tiwrr from<br />

the top fatiiude of a chart<br />

backup-An image pdmad on the reversa side<br />

of a map eheaf already printed on one stie.<br />

Also the printing of such Images.<br />

bafanclng a 8urvey-Distributing corrections<br />

through any traverse to eliminate the enor of<br />

closure, and to obtain an adjusfed poslfion for<br />

each traveree station, Also called traverse<br />

adjustment. Sea also Compaaa rula;<br />

dlstence prorate rote; transit rule.<br />

Baldwin solar charl-A chart designed for<br />

orienting a plantable by means 01 fhe Sun%<br />

ehadow.<br />

balllstlc camara—A precision terrestrial<br />

camera, usuatty employing glass plates, used al<br />

nigfw to photograph such objects as rockets,<br />

missiles, or satellites against a star background.<br />

Also caliad tracking camera. See also BC-4<br />

camera.<br />

band Interleaved by llne-A spaciflc<br />

implementation of a nrulfivariate raster detaeat.<br />

For each line in the raster, the values of each of<br />

the variables or bands are stored in sequenca,<br />

bafore the set for the succeadng fine.<br />

band sequen!iaf—A specific implementation<br />

of a rnuffivariate raster data act. The complete<br />

data array for each separate variable or band is<br />

stored indapandenfty of the other variables.<br />

band—A channel. A range of wavelengths of<br />

elactromsgnat!a radiation.<br />

bar check—A mathod of field calibrating the<br />

sounding equipment used in hydrographic<br />

survey by euspanding a bar or disc beneath the<br />

transducer at various depths,<br />

bar scale-See graphic 6cale.<br />

Bsrlow ievellng rod-A speaking rod ma~ed<br />

with triangles each 0.02 foot in heighf.<br />

26


1’<br />

—<br />

. . . .<br />

barorrroter-An Inafrumem for measuring<br />

atmospheric pressure. See 81s0 mmrold<br />

bssrometar; cistern barometer; mercury<br />

barometar; ●lphon barometer.<br />

baromatrlc ●ltlmcter+n instrument that<br />

indicatea efevalkm or hefght abova aea level, or<br />

some other referance height, by maaaurlrrg the<br />

weight ot air above the instrument. Also called<br />

preeeura aftimetar; senaltlve eltlmeter.<br />

See elao ●nerold eftlmeter.<br />

Darometrlc ●levatlon-An elevetion<br />

daremrlned with a barometer or altimeter.<br />

barometric hyp$omatry-The detennlnallon<br />

of elevations by means of ellher merwrial or<br />

aneroid barometers.<br />

baromatrlc levallng—A method of<br />

determining cf~erences of elevation from<br />

dtierancas ot atmospheric pressure observad<br />

wlfh a barometer or barometric altimeter. A type<br />

of indirect leveling.<br />

boryconter-lhe center of mass of a system<br />

of masses; a6 the berycenler of the Earlh-Meon<br />

system.<br />

baeal coplaha-(photogrammetry) The<br />

COndifiOn of expesure of a pair of photographs<br />

in wfrich the two photographs lie in a common<br />

plane parallel to lhe air baae. If the air base is<br />

horizontal, ttre photographs are said to be<br />

exposed in horizomal ooplana.<br />

basal orientation-The establishment 01 the<br />

peaifbn of both ends of an air baae with respect<br />

to a ground ayerem of coordinates. In all, aix<br />

elements are raquirad. Theaa are essantialfy the<br />

three-dimensional coordinates of each end of<br />

the base. In oracfica. hcevever. ti is also<br />

convenient to expre6s these eiemarfi “inone of<br />

two affamatiie ways: (1) The ground rectangular<br />

_tilnSteS Of One end of the base and Ihe<br />

dtiferaxe between fheae and the ground<br />

rec7anguter Cooti)nates 0! the other end of the<br />

baae. (2) The ground rectangular cxrordinates of<br />

ona end of the baae, tha length of the base,<br />

and two alamenrs of direction such as base<br />

direction and baaa tiff.<br />

baaal plana-See eplpolar plane.<br />

baae apparatua-(survay ing) Any apparatus<br />

designed for usa in measuring wilh accuracy<br />

,arrd precision the .Iengttr of a base line in<br />

MIL-HDBK-851Y<br />

trfangukfbn, or tha length of a line In first- or<br />

aewnd-order traveme. See also Bacha-<br />

Wurdemen base-line meeaurlng<br />

aPPemtue; Compensalhra bees.line<br />

maaaurlng ●pparetue; duplex baae-llna<br />

meaeurlng ●pparatua; Haaaler baea-llne<br />

meeaurlng apparatua; Iced-bar<br />

●pparatue; Jaderln wiree (base<br />

●pparatus); OPtiCal baae-llne meaaurlng<br />

apparaiua; RepaOld baee-line<br />

meaeurlrrg ●pparatua; Schott baea-ilne<br />

meaauring ●pparetua.<br />

beae charf-See base map.<br />

baee color-The tiraf cotor primad of a<br />

prrlychroma map to which succeeding cobra are<br />

registered.<br />

baee Conatrsrctlon llna-The bottom line of<br />

a map pfO@fion, al right angles to the central<br />

meridian, along which other martdlana are<br />

established.<br />

baae data—The basic level of map data on<br />

which other Information is placed for fwposas of<br />

CO~arkOn or gaopraphisal correlation.<br />

baae dlrectlon-Thri dr8s7ion of the ieriical<br />

plane containing Ihe air basa. whch mbht be<br />

expressed as a bearing or an azimuth. Sea also<br />

besei orlantation.<br />

base Ilna-1. (JCS) (survaying) A surveyed<br />

line established with more then usual care, to<br />

which surveys are referred for czmrcUntilon and<br />

correlation. 2. (JCS) (phrrfogrammafry) The fine<br />

bafwean tha prfncfpal polnfs of fwu .%wrsecullve<br />

vertical air photographs. If b U&Jally maaaured<br />

on one photograph after the principal point of<br />

the other has been transferred. 3. (JCS)<br />

(tnangulatbn) The side of one of a saries of<br />

connected trfanglas, fhe length of relrkh<br />

measured with prescribed accuracy and<br />

precision, and from which the tengths of the<br />

other triangie ekles are obtained by<br />

mwtiallon. [Base lines in tfianuutafbn are<br />

cfaasffied acCdkIg to the character of the work<br />

fhey are Intended lo amtrol. and tha<br />

Inatrumenta and melhoda used In their<br />

measurement are such that prescribed probabie<br />

errors for each class are not exceedad. Thase<br />

probable ermra, expreasad in terms of the<br />

lengths, are as folbwa: Iiraf-rder baaa fine,<br />

1/1 ,000,000; second-order baae Ilne,<br />

1/500,000; third-order base fine 1/350,000.]<br />

Also called trlangulaflon baee Ilne. 4.<br />

(USPLS) A line which is exiended east and west<br />

27


I<br />

I<br />

1<br />

MIL-HDBK-850<br />

on a parallel of latitude fmm an inWlal point, and<br />

from wfrich are Initfeted other fh’res for the<br />

cadwrral euwey of the Pubfii fend6 within the<br />

araa covered by lhe print’pal me@lan that runs<br />

lhrough the same intttsl point. S. (navigation)<br />

Tfre Iina between two radio trWt6t’fIltfiIVJ 6tati0n6<br />

operating in Cc@mcfbn for the detemdnsfbn of<br />

a line 01 posltiin, as the two sfaibne of a loran<br />

system.<br />

bsee mrsnuacrlpl+ee compilation<br />

manuscript.<br />

bees map-(JCS) A map or charl showing<br />

certain fundamental information, used as a<br />

base umn which eddifiinal data of eoecialized<br />

i~im- i~ con@ed or werprimed. Aiso, a r+ap<br />

containing all the information fmm which maps<br />

Showiw specialized information can be<br />

prepared. Saa also chart base; map.<br />

base net—A small net of trianglas and<br />

quadrilaterals, efati!ng from a meaeured baae<br />

fine. and connec4iW with a line of the main<br />

scheme of a triangulation net.<br />

baas sheet—A sheel 01 dimensionally stable<br />

material upen which the map projection and<br />

ground control are ploftti, ati upon which<br />

stereohiangulation or steremmmpilation is<br />

performed.<br />

base atetlon—1. (surveying) The Pint from<br />

which a survey begins. 2. (gravlfy) A gaogrephic<br />

position whose ebeolute gravhy valua is known.<br />

In expiration. a reference station where<br />

quantities under investigations have known<br />

valuea or may be under rapealad or continuous<br />

measurement in order to establish additional<br />

etalions in relatlon to ft.<br />

beee tape-A tepe or band ot metal or alloy,<br />

so designed and graduated ati of euch<br />

excellent workmanship lhal it is sui!abla tor<br />

msasurlng lengths of lines (base lines) for<br />

mntrollhrg triangulation, and for measuring the<br />

lengths of first- and sscoti-order travarae fines.<br />

baw tltt-Tha Incllnat!on of the ak base with<br />

raspecf to the horizontal. See also baaal<br />

orlsntatlon.<br />

baw.allftude ratio-l%e ratio between the<br />

air basa length and the flight atfflude 0! a<br />

stereoscopic pair of photographs. This ratio is<br />

reterred to as the K-factor. More commonly<br />

called baae.height ratio. Also indicated<br />

functionally as B/H.<br />

28<br />

basa-height ratio—See brsao-altltude<br />

ratio.<br />

baae.llne eatenalon-(navigation) Tha<br />

cati]nuat”mn ot the base tine in both directions<br />

beyorut the tmnsmhfem of a pair 01 rad~<br />

stations o~rating in oonjtmcfion for<br />

datamtinetion of a line of po6ition.<br />

base-llne lavele-A laval Ilne nsn abng a<br />

base line to determine and establish the<br />

elevathn of the base-line stations.<br />

ba$e4ine terminal ●tatlone-The<br />

monumented atatiorre rnatldng the and POims of<br />

a baea line.<br />

basement contoure-Conlours on lhe<br />

surtace of Ihe basemem complex or basic<br />

me!arrwrphic and volcanic rocks underlying an<br />

area.<br />

baelc controf-Horizontal and varflcal control<br />

Of third- or highermrder accuracy, datemnined in<br />

the field and permanently markad or<br />

monumerrted, that is required to control turther<br />

surveys.<br />

basic cover-(JCS) Coverage of any<br />

Installation or area of a permanent nature with<br />

which later twerege can be compared to<br />

discover any changes fhat have Iakan placa.<br />

See also comparative cover.<br />

bathygrephlc—Descnptive of ocean depths.<br />

Bethymatrlc ArChlVe Data (BAD)-in the<br />

DMA Digital Production System, tha Battsymetrii<br />

Archive Data (BAD) layer includes afI soundings<br />

trom all the wrveya taken. Tha eoundiig data<br />

in the BAD layer will evemualiy be extremely<br />

dense. Also Included is accaracy and source<br />

dsta, such as the time the Survey was taken,<br />

whera if was taken, and how It waa tSkWr.<br />

Bathymewlc Modal Data (BMD)-in the<br />

DMA Digital Production Systam, soundings trom<br />

the Bathymalric Archive Data layer are safecfed<br />

to form the Bathymetric Model Data (BMD) layer.<br />

The soundings in the BMD layer are the most<br />

critical of all the eoundings taken. Thesa<br />

soundings form the medel of the esean floor for<br />

the oompifation of Nautical Charts. See also<br />

Balhymetrlc Archive Data.<br />

Bathymetric Nwlgatlon Charte (BNC)-


,<br />

Charta depicting underwater to~graptry in lhe<br />

form o; Mlhynrevic c.wves. BNCa portray<br />

detailed rrultlbaarrvawath bathymatry. BNC<br />

sheets mntorm to tha basic worktwkM index of<br />

Bottom Contour (BC) Charla Ior scale, rxwarage,<br />

and nrsrrker dalenrthsation.<br />

Bathymotrlc Nsrvlgatlon Plannlng Charta<br />

(BNPC)-Charta depkting underwater<br />

topography in tha fomr of bathyrnalric curves,<br />

BNPCS portray detailed muftibaarrt%wath<br />

bathymtrtry collected in the ~anographic<br />

Survey Program and the morphological<br />

irrterpretafion of irrterawalh data. SNPC shaela<br />

mntorm to the basic worfdwiie index of Bottom<br />

Contour (BC) Charte for scale, coverage, and<br />

number daterrninalion. Produced at varkrus<br />

scales.<br />

Bathymfrtrlc Recovery Area Charts<br />

(BRACs)—See PreclEe Bathymetric<br />

Navlgatlon Zone Charts.<br />

bathymetric chert-A topography map of<br />

the iloor of the ocean.<br />

bathymetric conlour—See depth contour.<br />

bathymetric—Relating 10 the measurement of<br />

ocean depths.<br />

bathymetry-Tha science of determining and<br />

interpreting ocean depths end topography,<br />

battle mnp-(JCS) A map showing ground<br />

fealures In sutfiiiem detail for Iactkal use by all<br />

forces, usualfy at a scale of 1:25,000. See also<br />

map.<br />

baud reta-A maasure of the speed of data<br />

transmission between a computer and other<br />

devices [equivalent 10 the number of discrele<br />

cmndiibns or signal events per saco~.<br />

BC-4 canrersr-A trade name for the ballistic<br />

or gaodetlc stellar camera consiatlng of a Wild<br />

Asfrotar or Wtld Cosrnotar lens cena mounted<br />

on the modified bwer parl of the wild T-t<br />

astrormmic theodofite. Originally designed for<br />

Ihe recordhrg of the trajectory of a rocket but<br />

Sines adapted tor fha photographic tracking of<br />

artificial Earth eateliiies for gaodetii purposes.<br />

beacon tracking—The fracklng of a nrovlrg<br />

objwt by rnaane of signals emiired from a<br />

transmitter or transponder within or attached 10<br />

the object.<br />

MIL-HDBK-850<br />

29<br />

bSeM 01 llgtrt-A group of pancifa of Iiih!, as<br />

those ori@rtatlW at me many polrtla of an<br />

illuminated surface. A beam of parallel Iigfsl rays<br />

is a special case in Wish each pancll !s of such<br />

small MOSS sectbn tftat it may be regarded as a<br />

ray.<br />

Beaman arc-A spatially graduated arc fitted<br />

10 the vertical cJrcla of a mmslt or aiiida for Iha<br />

easy raductkxr of stadm observalbns. Also<br />

called atadla circle.<br />

bearing angla+ee bearing, detlnftion 1.<br />

bearing bar--$ee rszlmuth Inafrument.<br />

bearing ClrCIS-A rtng designed to lit .WtUglY<br />

ovar a compass or m~a.ss repeater, and<br />

provided with vanes tor observing mmpass<br />

bearings,<br />

bearl,ng llna-A line extending In the direction<br />

of a bearing.<br />

baarlng of Ih’ra-(plane surveying) The<br />

horizontal angle whkh a line makes wilh Ihe<br />

meridian of relerencs acljscen! to the quadranf<br />

in which fhe fine lies. A beartW is idemitied by<br />

naming the end of the merklan (north or south)<br />

Imrn which it is reckoned and the direction (aasl<br />

or west) of that reckoning. Thus, a Iina in Ihe<br />

norfheasl quadranf making an angle of 504 with<br />

the rnaridan will have a bearing of N 50” E.<br />

In most survey work, it is pralerable to use<br />

azimuths rather than bearings.<br />

bearlnQ traa-A msrfsad tree used as a comer<br />

accessory; its dktance and dkectiin fmm the<br />

wmar being recorded. Bearing traes are<br />

idenlitied by prescribed marks cut into their<br />

trunks: fhe species and sizes of the trees are<br />

atso recorded.<br />

beartng-1. (JCS) (general) The horizontal<br />

argle at a given poim measured clcdrwise fmm<br />

a SPScifii datum to a second point. AISO called<br />

bearing angle. See also grid bearing;<br />

ralatlve bearing. 2. (navigation) The<br />

horizontal direction of one Ierresuial point from<br />

another, expressed as fhe angular dktancs<br />

Imm a reference direction, It is usuatfy<br />

meaaured tmm O“ at fhe referenca dhaction<br />

clockwise through 360”. The terms bearing<br />

mid azimuth are sometimes used<br />

Ikrterchangeably, but In navigation Ihe former<br />

wstomarily applies to terrestrial ob~ects and the<br />

latter fo fhe direction of a point on fhe celeslial


sphere fmm a polm on the Earth. 3. (surveying)<br />

See beerlng of Ilne. See ako aatronomlc<br />

basrlng; back bearing; compass<br />

bearing; computed bearing; curve of<br />

equsl baarlrvg; ●tactronlc bearing; false<br />

bearing; gram. clrcSe baarlng; grid<br />

bearing; Lambwfl baarlng; magnatlc<br />

bearing; polar bearing; rhumb baarlnry:<br />

trssa bearing.<br />

Boll gravity mater-A single-axis, pendulous<br />

torte rebalance accelerometer mounmd on a<br />

stabilized ptetfonn and Interfaced to a cfynamfc<br />

d~ket friar tor measuring gravity aboard a<br />

awvey platform.<br />

trench mark (BM)-A marked vertical cxmtrol<br />

point whkh has been located on a relatively<br />

permanent rnaterfal object, natural or artificial,<br />

and whose etevatbn above or below an<br />

adopted datum has been established. It Is<br />

usually monumenttxf 10 include bench mark<br />

name or number, frequently ffs elevation, and<br />

the name et the respsnslble agency. Since<br />

elevations are computed at a later time, lhey<br />

era aekfom addsd to nawer control bench<br />

marks. A EM (aside horn a vertical anole bench<br />

ma~) seldom ‘kas a surveyed iatltude ~r<br />

lorrgiiude. See also flrat.”order bench mertr;<br />

pctlon bench mark; permanent bench<br />

mark; primary banch mark; second.<br />

order borsch mark; temporary bench<br />

merk; lldef bench mark; verflcal-arrgle<br />

bench mark.<br />

Bessel ●pherold (elllpaold)—A reference<br />

ellipsoid having the following approximate<br />

dimensions: eemimajor axis-6,377,397.2<br />

metem; semiminor exis-6,356,078.9 meters:<br />

and the flattening or elfipticity-1 /239.15.<br />

Bassaf’a mathod—See Wlangle.ol-arror<br />

mathod.<br />

Baaeellan star numbers-Conslants used<br />

in the reductbn of a maan posfrlon of a etar to<br />

an awarenf positbn (used 10 asoount for shortterm<br />

VaI’fatiOiIs In the precessbn, rrutatlon,<br />

aberratbn, and parallax).<br />

Baseelfan year—See flctl:loue year.<br />

bfensia acrean-A photographic negative<br />

COntafnlffg a Conrposfte of two dot screens, with<br />

Ihe screen angles oriented 30° apart. These<br />

screens are used to Mint tones of color for chart<br />

features wffh thin lines.<br />

MIL-HDBK-850<br />

Bllby steel towar-A triangulation lower<br />

mnaisting of two steel tripde, one wifhin the<br />

other. Tha inner tripod holds the Instrument<br />

platform, and the outer tr@od holds Ifw<br />

obsarvets ptefform. me Sowwr can be easlfy<br />

erected and as easily disassembled and moved<br />

to a new location. See also ●urvey tower.<br />

blmarghf forntat-The formal ol a map or<br />

chart on which the cartograptric detail is<br />

extanded to two edges of the sheet, rsxmelfy<br />

north and east, thus Iaavlng onfy two margins.<br />

Ss8 also blaed; bswedlng adge.<br />

blnefy dlgft-kssfly called a Bit, a binary digtt<br />

is the smahest unil of information which can be<br />

s!ored In the computer. See also bit.<br />

blrrocular vleion~imultaneous vision wilh<br />

bolh eyes.<br />

binocular-An optical instrumem tor use wilh<br />

both eyes simultaneously.<br />

bft map-A pattern of bits within a grid, stored<br />

in memory, and used to generate an image on<br />

a raster scan display.<br />

blt plane-A gridded memory in a graphics<br />

device used for storing informatkm for display.<br />

Typically one cobr is ass’@rad to each bfi plane<br />

tor dk.pfay.<br />

bll-A binary digit.<br />

bhrarlate normal dial rlbrstlon funct lon—<br />

Mathematical function describing the behavior<br />

of two dimensional random errors (e ,g., latitude,<br />

longitude; x, x casting, norfhlng). Also called<br />

circular normal dlatrlbUtlOn.<br />

blackbody-An Meal surlace or body that<br />

mmplefely absorbs all radiant energy tafting<br />

upon it. Blacfdndies are used as models in the<br />

design and calibration of renmte eenaing<br />

systems.<br />

tslaza-A mark made upon a tree trunk USUaffy<br />

al about breast height. The bark and a small<br />

amoum of tfre five wood are removed with an<br />

axe or other cutting tool, faevlng a flat,<br />

smoothed surfecs which Iorever brands the tree.<br />

On rough-berked tree monuments or bearing<br />

trees the appropriate marks are ecrfbad into a<br />

smooth, narrow, vertical blaze the bwer end of<br />

whkh is about 6 inches above the root crown.<br />

30


The blaze should be just brrg enough to allow<br />

the marldngs to be made,<br />

bkeedlng arkge-(JCS) That edge of a map or<br />

chart on which cartographic detail is exiendad<br />

beyond the neallina to the adga of the sheet.<br />

See also blmargln format; bleed.<br />

bleed-l. (Iiihogrephy) A mmdifbn wherein Ink<br />

pk#mwrf &adissotved by press fountain solufbn<br />

causing a Ilght film of ink (scum) on the plate<br />

and krqxeesbn. 2. (cartography) Cartographic<br />

deteil extending to lhe edge 0! a map or chart<br />

sheet.<br />

Erllncf Image-see blue Ilrte.<br />

bllp-(JCS) The display of a recalved pulse on<br />

a cathode-ray tube. Also called echo.<br />

bllatsrr-See border break.<br />

block edJuetment-The actjuelrn&t of strip<br />

@Jordhetes or photograph coordinates for two<br />

or more etrips of phoic&iaphs. See also 81rJp<br />

adjustment.<br />

block oul-Sae opaque, definition. 4. .<br />

block—t. (dlgltal slorege) A group of remrds<br />

or wuda treahsd es a krgtif unit of irrformatton.<br />

For example, a VAX megnat!e disk block equals<br />

512 byies, and an urrapacifiad magnetic tape<br />

btock equals 8192 byieS. A fixed or varfable<br />

number ot records. 2. Synonymous with<br />

physlcel racords-.a sequence of words or<br />

characters wrfffen casflguously by e computer<br />

on an exfemal storage medium. Typically, one<br />

block is written each time a WRITE mmmand Is<br />

executed. 3. A set of emities in a CAD system<br />

which can be treated as a single cOmpOUnd<br />

0bjfa3. 4. (aetial DhotOgfSphy) TWO or more<br />

lllght block.<br />

bloomed lene-See coatad Iene.<br />

bloomlng—1. The lerm usad to describe<br />

fCCatizad overexposure caused by incoming<br />

radianf energy levels which exceed film<br />

emulsion latitude Ihereby causing Ihe image to<br />

lack dellnlflon. 2. A process Ior increasing Ihe<br />

Iiiht Iransmissbn of lenses.<br />

blow up-A photographic enlargement. Also<br />

used as a verb.<br />

MIL-HDBK-850<br />

blue lln~A rtonreproduclble blue Irrraoe or<br />

outline usually printed photog~h~lly on -r<br />

or plastic sheeting, and used as a guide Ior<br />

drafting, stripping, or layout. AlSO called bllnd<br />

Image.<br />

blue magnetism—Tha magnetism displayed<br />

by lhe south-seeking end of a freely suspended<br />

meonet. TMs is fhe magnetism of the Earth’s<br />

north msgnatii pole. See also red<br />

magnetlam.<br />

blunder—A mistake generally caused by<br />

rxtrelessnaes. A blunder may be large aml easily<br />

detectable, or smeller and more dangerous, or<br />

very small and indiitinguishsble from a random<br />

error. Bkmdera are detected by repetition and by<br />

external checks, Such es cbsing a traverse or<br />

substituting the solulion of an equation In Ihe<br />

orlglnal. See also random erro~ eytttematlc<br />

error.<br />

boat cheat—The worksheet usad In the field<br />

for pbtfing details o! a hydmgraphic euwey as if<br />

progresses. Sae also field sheat.<br />

Bonne map pro)e:tlon—A modified equalarea<br />

map projetilon of the so-called mnical type<br />

ttaving Iinas represemlng a staMard parallel<br />

and a cemral maridlan intersecting near the<br />

tamer of the map. Tha line representing the<br />

central meridian (geographic) is etraipht and the<br />

scats akmg it is exacs. All gaograpFic psreltets<br />

are represented by arcs of concentric ckcles et<br />

their true dkiances apart, dwided to exad scale.<br />

and all mettiiana, excapt the central ona, are<br />

curved Iinea mnnecfirsg correswndng points on<br />

tha parallels.<br />

Boolaan operetlon-Any operation in which<br />

each of the oWranda and the resuff take one of<br />

We valuea.<br />

border braak-(JCS) A cartographic technique<br />

used whan It Is required to extarsj a portion of<br />

the cartographic detail of a rnep or charl beyond<br />

the shaef lines into tha mar@n. Also called<br />

blletar.<br />

border data—Sea merglnal dafa.<br />

border information—See marginal data.<br />

border matching—The procass by which<br />

individual d~ifal data eels are joined together<br />

through mefgln~smw!hing utilizing computer<br />

applicatbns SOfhVare,<br />

3“1


I<br />

Boston Iavollng rod-A two-piece rod with<br />

fixed ta~l on one end. The target k adjusted<br />

in elevation by moving one @ of the rod on<br />

\ the other. Ra@ by Vemter. FOr negnls greater<br />

than 5 1/2 teal, the target end is up; for lesser<br />

heighls, the target end is cbwn.<br />

MIL-HDBK-850<br />

Bottom Ccmtour Charts (BC)--Charts<br />

depicting detailed underwater topography In the<br />

term of bathymetric cuwes. BCS provide a<br />

general picture of the saafkror and ifs features,<br />

portrayad horn survey data and fore)gn<br />

published charts. Deeigrwd for the use 01<br />

aubmarhe.e or ships by the method of bottom<br />

GOIIfOUr matching.<br />

Bouguer ●omaly-A difference barwean an<br />

observed vatue of gravtfy and a theorel”cal value<br />

at the Foinf of observatbn, which has been<br />

corrected for Ihe elfacf 01 Topography and<br />

efavalion only, Iha topography baing considered<br />

as a pfafe of indefinite axfent.<br />

Bouguer corractlon-A correcfiin made In<br />

gravity work to take amount of the allitude<br />

(elevaliorr) of the station and the density of the<br />

mess between an infiniie plane though the poinl<br />

of observation and the infhsire plane of the<br />

reference elevation.<br />

Bouguer plma-An imagh’rary layer of infinite<br />

Ienglh and of thickness eQual to the height 01<br />

the observation point above \ha reiarance<br />

aurtace (Wualfy the gaoid). In a~lying the<br />

Bouguar corrac3ion, the afrracring layer lessens<br />

me free air effect.<br />

Bouguar raductlon--Geophy sically, fhe<br />

Souguer reduction removes all masses above<br />

fhe reference arsrfaca (usually tha geold) and<br />

then reduces the gravffy from tha tarraln to the<br />

referenca eurfaca.<br />

boundary (d* lacto)-An International or<br />

administrative bwndary whose existence and<br />

legality are not recognized by an csxrcemad, or<br />

are not defined by appropriate documents, but<br />

whlsh is a praabal dk+sion bahveen separate<br />

natiinal or provincial administering authorities.<br />

boundery (de jure)-An ktternalional or<br />

admlniafrative bowdary whose axistenca and<br />

legality are racognlzad.<br />

boundary dlscontlnultles—Ditlerent<br />

alevallon values for common DMA standard<br />

digital terrain elevatbn data (DTED) malrlx<br />

points In adjacenf data files.<br />

boundaw llna-A iine of demarcatbn<br />

belween contiguous poliiical or gaographal<br />

enfltlas. The word %oundary. is SOITB times<br />

omitted, as in “afata Iiie”: some times tha word<br />

.Iine- is omitted, as in “infematicmai boundary,-<br />

“counfy boundary,” efc. The term tsoundary<br />

Ilno la usually appliad to fmundaries befwaen<br />

pofiii territories, and %tate boundary tiia~<br />

bafween two atatas. A boundary line between<br />

prkately owned parcels of land Is taMWd a<br />

propeny Ilna by preference, or if a line of the<br />

Unked Slatas public land surveys, la given lfM<br />

pa~buiar dasignafiin ot that survey systam, as<br />

“sesfion Iina,- %wnahip fine,. elc.<br />

bounde~ map-A map prepared specifically<br />

tor the pu~sa of delineating a boundary Iina<br />

and adjacent territory.<br />

boundary monumant—A material object<br />

placed on or near a boundary tine to presewe<br />

and ktenfify the location of the boundary fine on<br />

tha ground.<br />

bounda~ point e.veraglng-Averaging the<br />

elevations of mmmon poinls fmm two dfilerenl<br />

data sets and reassigning each the average<br />

value; or resolving a discraparq between IWO<br />

elevalbns tor a common poinf by arslgning tha<br />

avarage elavalion vah.m to that polnf.<br />

boundary point waightad ●veraglrtg—<br />

Reaotving a diacrapancy bafwaen a aaries of<br />

overlapping elevations from two dma sats by<br />

biasing one data set utiliuing eithar tha amuracy<br />

01 a data set or the relative dbtance to lhe edge<br />

ot the data.<br />

boundary survey-A survey made 10<br />

aslabfish or to reestablish a boundary fine on<br />

the ground or to obtain data for rxmstrusting a<br />

map or plat showing a brxdary line. The term<br />

boundary survey is usually raslrictad to<br />

surveys of boundary fines berwean poliibel<br />

territories. For the survey of a boundary line<br />

behveen privately owned parcels of land, the<br />

tarm land survey is praterred: except In<br />

United States public land auweys fhe term<br />

cadaatral survey Is used,<br />

boundary vista—A lane cleared afong a<br />

boundary line pasaing through a wooded area.<br />

Bowle affect-The Irtdirecf effeci on Qravlfy<br />

due to the warping of the gaoid, or the elevaflon<br />

of the gaoid with respea to tha spheroid of<br />

3 2


I<br />

1<br />

reference.<br />

Bowl. method of sdjssatrnwrt-A melhod<br />

for the adjusfmerrl o! large networks of<br />

triangulalkrn.<br />

kx compass-see decllnatolre.<br />

brwk ●ngl~The delfecflon arrgfa between<br />

the two vartkxrl phases passing thrcugh the<br />

common nadir polnf and the prfnclpal points of<br />

the left and right obfiie photographs.<br />

break tapa--.see broken t~pa<br />

measurement.<br />

break-clrwuff chronometer-A chronometer<br />

eWbWd with a device wirkh automaticaity<br />

braaks an electric clrcult, the breaks beln~<br />

remrded on a chrorsogreph.<br />

braak-up-(JCS) 1. In detection by radar, the<br />

separation of orm solid return into a number 01<br />

indivkfual returns which correspond 10 Iha<br />

varieua objacfs or arructure groupings. This<br />

separation Is comingarrt upon a number of<br />

facfors including ranga, beam widrh, gain<br />

setting, object size, end dktarrce barween<br />

objects. 2. In Imagery ime~relalion, the resuh of<br />

magnlficatbn or enlargement whkm causes the<br />

imaged Item to Ioaa its idemlry and the resuffant<br />

preeerdatkrn to becwnra a random series 0!<br />

tonal Irrrpresabns.<br />

broakeway method-See breekaway atrlp<br />

method.<br />

breakaway atrlp melhod—A technique used<br />

in photomosaickkrg when two or more sheets<br />

are preparad. The process involvas placing an<br />

exlra wide strip of masking tape along the<br />

oufaide edge of the neatlhse of ona sheet<br />

batore mosaicking photos. Tha moaaicked<br />

overasfge IS then cut along the neafline and<br />

transferred to the adjoining sheet, Also called<br />

breakaway method.<br />

broeklng tapa-Sea brokan tape<br />

measurement.<br />

brldglng—A photogrammetric method ot<br />

establlshlrrg and adjusting control between<br />

bands of existing ground control, both<br />

horizomally and vertically. The (arm is usually<br />

qualified as horizontal or vertical accmdhg 10 its<br />

prfmary purpose. Also called horizontal<br />

bridging; horizontal/vertical brldglng;<br />

vertical brldglng.<br />

MIL-HDBK-850<br />

.<br />

brlghtneaa XCSS10-(phOtOgfSphy) The ratio of<br />

the brightness of highlights to tha deepest<br />

shadow in the actual Iarrain, as measured tmm<br />

the camera stations, for the field of view under<br />

considarafion<br />

brtghtneae valrsa-The amount of reflected<br />

or amlffed energy axffhrg horn the earih%<br />

surlaw as recorded by a remola wnaing<br />

system. Thaae dala are atorad ae dgifal velues<br />

on conywfer@mpafiia tapes (CCT) for digial<br />

image procaaslng purposes. The greater Ihe<br />

brhhtnasa of the acena (CWreturn fmm tha<br />

scene), tha highar Iha digital value. Hence the<br />

vakma stored on Ihe CCT are offen ralerrad to<br />

as briitstnaes values. II is rwt pmpar to call<br />

them reflactarrca valuaa unlass Ihe brightness<br />

vatues have bsen scaled to truly raprasenf<br />

raflectanca values.<br />

Brltlah grid reference ayafern-A system<br />

of rectangular w.ordinales devised or adopted<br />

by the Brilish for use on military maps. ThOre Is<br />

no ralated gbbal plan for fhe many grfds, belts,<br />

and zones which maka up Ihe Brltiah grid<br />

syatam. It is being replamd by the Univamal<br />

Transverse Mercator (UTM] grid systam.<br />

broadcaar ephemerla—A se! of paramalers<br />

broackussl by satellite tmm which Earlh-lixed<br />

satallite positiins can be comfwtad. In<br />

parsicdar, the pararrralers tor the NaW<br />

Navigation Salelliras (NNS) are computed for<br />

each NNS by fifflrg 3G 10 4S-frour orbital arcs to<br />

Dopplar data from four tracking stal”brra and<br />

exiraprlating this arc 12 to 24 hours beyond the<br />

last data used. The Iarigth of the arc lii and the<br />

extrapolation period depend on tha uppar<br />

almespheric air density. The mmpufed<br />

paramelara ara injected into the satellite<br />

memory and are transmtttad abrrg wlfh time on<br />

each even minuta. See also Navy Navlgatlon<br />

Satalllte System.<br />

brokan baa*A base line for triangulation<br />

comisting ot two or more lines that torn a<br />

continuous traverse and have appmxlmataly the<br />

same ganeral diracfbn.<br />

broken g rada-(tapa) Tha change In grade<br />

when tha middle poim ot a tapa Is not on grade<br />

wlfh ffa ends. If the middle aupporf for the tape<br />

is not on Ihe same grade aa the and supports,<br />

tha fact Is notad with a reference ‘bmkan grada<br />

at-,- naming tha particular tape fangfh which<br />

mrrlalrra the broken grade.


MIL-HDBK-850<br />

brokon tspe meeessramont-(rtuweying)<br />

The short ttietaxm measured ati msamsutsfed<br />

to totat a full tape length when a standard 1OOfoot<br />

tape cernof be hekf hortzontatty wtfhout<br />

Pkmbtng from above ehcdder level. Aleo ceSed<br />

break tape; breaking taps.<br />

broken teloecope transit-A precise<br />

aefronomk fransti tn which the light entering the<br />

objedlve isne fa mtlecdad al right anglee by a<br />

prfem pieced wtthln the leleeccpe, the refbctad<br />

Iiht ray peaslrq to Ihe eyeple~, whkh is in the<br />

horizontal ruda of the telescope.<br />

Brown grevlty ●ppemtu~n apparetua for<br />

rnaasurtng the accwlenstion of gravity which<br />

utilizes the Mendenhall pendulum, but has a<br />

clamping devbe for hofd~ the pendulum In the<br />

receiver when beino franaported fmm station to<br />

station, and which ufifizes an efectricel pickup<br />

and amplifying devtce tor raccmting the<br />

oeciltatiins (pendulum) on the chronograph<br />

sheet.<br />

browWng--System capability to find en<br />

undefined feature or set of features in a spatial<br />

data base.<br />

Brunton compas~An instrument combining<br />

the teetures of both the sighting compass and<br />

the clinometer that can be used in lhe hand or<br />

upon a Jacob’s staff or light tripod tor reachg<br />

horizontal and vertical argtes, for leveling, and<br />

tor reading ma magnetic bearing of a line. Afao<br />

called Rrunton pockat tmrmlt.<br />

Brunton pockst transit—Se e Brunt on<br />

compass.<br />

bubble axIa—See splrlt teval axla.<br />

bubble level-See splrlt Ievsl.<br />

bubbkr 8extanl-A aextanf in which the<br />

bubble of a spirit level serves as the horizon.<br />

bucking In—The act of aligning a lheodofite to<br />

a collimator or aumcolfimating theodoiite serving<br />

as mltimator to make their lines of sight perallel<br />

and on fhe same plane.<br />

buO-An error In a rmrnputer program or in a<br />

piaca of electronic equipmanf ttraf causea tf 10<br />

furwtion Improperly.<br />

bull’o-eye level-See circular level.<br />

34<br />

Bullsrd method of Iaostatlc rerluctlon-<br />

See tIayford.Bullsrd (or Bullsrd) mathod<br />

ot Isostatlc mductlon.<br />

burn+tilhogrephy) The process of exposing a<br />

pressplate.<br />

byte—1. A group of adjacent btfs that are<br />

operated on es one unit. Eight bits equal one<br />

byte. 2. A storage unlf ec@velenf to an ASCII<br />

character of Information in a carrputer system.<br />

S= curve method-A method ufillzlng<br />

characferfstka of tha Bz curve for finding the<br />

dk$rtacement o! true photo ptumb pims from<br />

indicated projector plurrb points in rnuftiplex St*<br />

orientation. The method also provides a means<br />

of strip leveling usir’g only the bemmetnc<br />

attimeter readings of the aircraft flying haight.<br />

Sz curve-(photogrammat~) A graphical<br />

representafbn of the vertical errora In a<br />

atereotr’angulatad atnp. In a Bz curve, the xmordinatea<br />

of the verlical comrol points,<br />

referred to the initial nadir pokrt as origlr’t are<br />

pbned as abscissas, and the differences<br />

between the known elevafiins of the mntrol<br />

paims and their e!evelkma as read in the<br />

stereo! riangulated strip are plotted as ordinates;<br />

a srrwoth curve drawn through the ptottad<br />

points k fhe Bz curve. The elavation read on<br />

any pass point in the strip is adpated by the<br />

arnoum of the ordhmte of the Bz curve Ior an<br />

abacisaa mrrespc.nding to the x-coordinate of<br />

the Ooinl.<br />

.


C-constanf—See level constant.<br />

Gfacfor-An entpirkxl value which expreeae6<br />

the vetiical measuring capability 01 a given<br />

stereoscopic system; generally defined as the<br />

ratb of the flbht height to the smallest cmfour<br />

interval accasratety pbffabfa. The C-factor ta nof<br />

a ffsad constant, but varfas over a wnsfderebla<br />

ranoa, =Kfing to the elements and condifbns<br />

of tha photogrammatric systam. In pfannirrg for<br />

aerial photography, the C-factor la used to<br />

dafermlne the Wghf hefght required for a<br />

apacffiad contour krtervaf, camera, and<br />

inafmmerrt system. Aso called attitude<br />

contour ratlo.<br />

cadaatrel map-A map showing :he<br />

boundarfas of suMh4atons of tand, usualfy with<br />

the bearings ati Iertgfhs thereof and the areas<br />

of krdivktual tracfs, for putpoaes of describing<br />

and recording ownarahp. Also called properfy<br />

map. Sae also plat.<br />

crsdaafrel ●mvey—A survey relating 10 land<br />

boundaries and auMivkJons, made to craate<br />

units suitable Ior Irenafer or to define Ihe<br />

Iimftat’kms of title. The term cadasrraf survey<br />

is nmv used to designate the eurvaya of the<br />

pubflc lands of the United States, including<br />

retrac8ment surveys tor the idemiticallon and<br />

resurveys tor the restoration of property iines:<br />

the term can afao be appfied property to<br />

oorresponilng surveys oufsfde the public Ianda,<br />

affhough wch surveys are ueually termad fand<br />

surveys through preference.<br />

cafrn-Arr artificial mound of rocks, stones, or<br />

masonry usually conical or pyramidal, whose<br />

pumose Is to des@ete or to aid in idemitying a<br />

poim of surveying or of cedeatral importance.<br />

colcufated aft ftuda-See computed<br />

sftftude.<br />

cafendar dey—The parbd from rnldnight 10<br />

midnlghl. The calendar day ia 24 hours of mean<br />

solar time h iengfh and coincklea with the civil<br />

day urrleae a time change occurs during the<br />

dey.<br />

cefendar month-A division of the year ae<br />

dafermfnad by a calendar, approximafefy onatwemh<br />

of a year fn ler3gfh. White amtrrary in<br />

character, the calendar momh is based roughfy<br />

on fhe eyrtodical month. The calandar month<br />

ranges In length fmm 281031 mean solar days.<br />

MIL-HDBK-850<br />

c<br />

calendar year-A convetitonal year based<br />

on the tropkal year and adjusted by ‘leap<br />

years- to ffl fhe rrorrhrtegral length of the tro@OSl<br />

year.<br />

caffbratad focaf length-l. (JCS) An<br />

acfjuslad velue of the equfvalant focal length. so<br />

compufed as to equalize the posfffve and<br />

nagativa values of distortion over the emlre fiald<br />

used In a camera. See also tocaf fength. 2.<br />

The distance aforrg the fans axis from the<br />

imerior pempactfve oerrtar fo the image plane.<br />

calibration card-A card having a list of<br />

calibration corrections or calibrated values.<br />

caffbretlon corfatanta-The resutts obtained<br />

by cadfbrafbn, which give Ihe calibrated focaf<br />

Iangfh ot fhe lens-camera unn and the<br />

relationship of the wirctpal point to the fiducial<br />

marks of a camera and give significam<br />

calibration wrrections for lens distortions.<br />

cafltrratlon corroctlon-The vafue to be<br />

added to or subtracted lrom the reading 01 an<br />

instrumen! to obtain the correct reading.<br />

calibration course-See flefd<br />

comparator.<br />

caffbratlon error-Sea Instrument error.<br />

caflbraffon pfale-A glase negative exposed<br />

with its emufsion side mrreepondhg fo the<br />

poslIbn of fhe emulsbn side of the film in the<br />

camera al the time 01 exposure. Thla plata<br />

providas a remrd of the distance between the<br />

fiducial marks of the camera. Also cafled llaah<br />

pfate; master gfase negative.<br />

calibration tabfS-A fist of calibration<br />

mrracfions or calibrated vafues.<br />

callbraffon templet—(phofogrammetry) A<br />

template of glass, plastic, or matal made in<br />

aardance with fhe calibratbn constants to<br />

show the rafalbnshfp of fhe Prhlpaf Polnr of a<br />

camera to fhe tklucial marks; usad Ior tha rapid<br />

arxt accurate marking of principal poims on a<br />

series of phonographs. Afso, for a mufflple-lens<br />

camara, a tempfate prepared from the<br />

calibration data and used In assembling the<br />

Individual photographs into ona wnposffa<br />

photograph,<br />

35


I I<br />

I,/<br />

I<br />

I<br />

calibratlort-The ecf or process of de!erminin<br />

certain spacffk maasuramarrta in a camera or<br />

other it’strumam or device by COMpafbOn with i<br />

atamtard, tor use In correcWW or compansatlng<br />

for errors or {or purposes 01 record. See also<br />

camera callbratlon; Neld callbratlon;<br />

sfsop C.sllbratlon.<br />

Calllppk cyck-A period of four MeIonic<br />

cycfes equal to 76 Julian years, or 27,759 days<br />

cell-( USPLS) A raferanca to, or Statement 01,<br />

an ob]acf course, distance, or other matter of<br />

deacriptbn in a auwey or grant, requiring or<br />

calling for a corresponding object, or othar<br />

matter of rkescdption, on the land.<br />

Camera aXIS dlrectlon—(JCS) Direction on<br />

Ihe horizontal ptane of the optbal axis of the<br />

cemera at the time of exposure. This dhecfion i<br />

defined by ifs azimuth expressad in degrees in<br />

relatbn 10 irualmagnefii norih,<br />

camera axl~JCS) An Imaginary tine<br />

through the optbal center of the fans<br />

perpendmular to the negative photo plane.<br />

MIL-HDBK-850<br />

camera calibration-(JCS] The<br />

determination of Ihe calibrated focal length, the<br />

location of the prirrc@sl poim with respacf to tha<br />

fiducial marks, and lhe lens distonion affactlva i,<br />

the focal plans of the camera amf rekrrred to<br />

the particular calibrated focal length. [In a<br />

muftiple-lens camera, the csfibration also<br />

includes the determination of the mrgles<br />

between the component perepactNe units. The<br />

setting of the fiducial marks and the positioning<br />

of the Iena are ordinarily considered as<br />

adjustments. although they ara sometimes<br />

perlormad during the catihration process. Unies:<br />

a camera is epecificaliy referred to, disIorfion<br />

and other opticaf characferfstica of a lens are<br />

determined in a focal ptene located at the<br />

equivalent focal fanglh and the process is<br />

termed lens calibration.]<br />

cemem Iucida-A monocular irwtrument<br />

using a haff-sifvered mirmr, or the opt!cal<br />

equivalent to permit supertmfxmifion of a<br />

vertical image of an object upon a plane, Also<br />

called Cemem obecura. See also<br />

●ketchmaatar.<br />

camara magazine-(JCS) A removablo parf<br />

01 a camera tn which the unexposed and<br />

expsed portions of film are contained.<br />

36<br />

Camara obscurn—See camera Iuclde.<br />

camara station—See air basa; ●ir<br />

●iatlon.<br />

camara transit-See photo- theodollta.<br />

cemara wlndow+fCS) A window h the<br />

camera compartmem through which<br />

photographs are taken .<br />

camars+A tightproof chamber or box in which<br />

the image of an exterior object k projeUed upon<br />

a aanaitizad plate or film through an opening<br />

usually equipped with a lens or Ienaes, shutter,<br />

and variable aperwe. See also aerial<br />

camera; BC-4 camera; ballletlc Camara;<br />

continuous strip camera; convergent<br />

cemara; copy camara; dlract scannhrg<br />

camara; fan cameras; frame camera;<br />

geodetic stellar camera; horizon<br />

camera; mapplns camera; matrlc<br />

camera; mulllple-camera aaaembly:<br />

multlpla-lans camera; PC.1OOO camara;<br />

panoramic camara; photogrammetrlc<br />

camera: posttloning camera; preclalon<br />

camera; rectifier; rotating prlam camera;<br />

apllt cameras; ●tallar camera;<br />

slereometrlc camera; terrestrial tamers;<br />

trlmetrogon camera; variable<br />

perepacthre camera eyetem; zanith<br />

camara.<br />

Canadian grid—See perspective grkt.<br />

candela—A unff of luminous Inlenaffy.<br />

camliaver extension— Phololriangtrla! ion<br />

from a mntrcdled area to an araa of m ccmtrol.<br />

Also, the connection by relative orientation and<br />

scetirrg of a series of photographs In a Strip to<br />

obtain strip arordinetes. Aiso calied extension.<br />

Cape Canaveral datum-Tfris special<br />

datum ia defined with ita origin at station Cemral<br />

on the John F. Kennedy Spaca Center, Cape<br />

Canaveral, Fbrida, with azimuth to Central SE<br />

Base. The geodetic coordinates of these fwu<br />

StatiOnS were identlCSl to those on Notlh<br />

Amarican datum of 1927. Datum differemea for<br />

other points may be determined by suMracting<br />

North Amerkan datum of 1927 values from the<br />

Capa Canaveral daIum values as estabfbhad by<br />

the USC&GS transcontinental traverse of the<br />

United States. See also North American<br />

datum of 1927.


I<br />

. . -. --,- MIL-HDBK-850<br />

carcfan ltnk—A universal join!. h opf’cal<br />

catdan Ilrrk la a devica for universal scanning<br />

about a ~lnt.<br />

cardinal polht ●ffecf+JC S) The incraased<br />

krfenslfy of a line or group of returns on Iha<br />

rederscops occunfng when tha radar beam la<br />

PWcmsffcufar to the rectangular surla~ of a fine<br />

or gnsup of aimilsrly aliined fealuras in the<br />

ground petlam.<br />

ctsrdlnel polma-1. The dhectiona: north.<br />

south, east, west. 2. [optics) Those points of a<br />

lens used as raference for determining object<br />

ara3 Image distances. They includa prfncipaf<br />

planes and pdrtts, nodal points, and focal<br />

points.<br />

Carpentlar lnvaraor-One of the inversors<br />

which correds for the Scheimpflug COIWifiin in a<br />

racflfier if the negative, lens, or easel planes are<br />

lllfed and not perallal.<br />

carrytng comour-A single contour tins<br />

representing fwm or more contours, used to<br />

show verf”cal or near-vertical topographic<br />

lealures, such as steep slopes and cliffs.<br />

Carfaalan coordlnaraa—A coordinate<br />

system In whktr bcalions of points in space are<br />

expressed by relerence to three mutually<br />

pe~ndilar pIanes, called coordinate planes.<br />

The thrae planes interaecl in three straight IifleS<br />

called coordlnata axea. [Also the valuee<br />

reWeearrfing ihe bcafiin o! a point in a plane in<br />

rafetion to two perpendicular irttarsecting straight<br />

lines, salted axaa. Tha point IS Iocatad by<br />

measuring ffs distanca hmm each axis along a<br />

parellet to the other 8616.]<br />

Carfographlc Automatic Mapping<br />

(CAM)—A mainframe computer mapping<br />

program available fmm fhe Central Intelligence<br />

Agency. If works<br />

.<br />

with Worfd Dala Bank<br />

..<br />

(WDB<br />

upsrromara mes !0 creale map prqecuona arm<br />

generate pbta.<br />

canographlc ●nnotation-lhe dalineafion<br />

of Sddiiional data, rrew features, or daletion of<br />

destroyed or dismantled features on a rrmsaic 10<br />

porlray cument details. Cartographic snmtations<br />

may inciude elevation valuas for ahfiekfa, cillaa,<br />

am! large bodies of wafer; naw construction and<br />

dastroyed or diamenfled made, railroads,<br />

brfdgea, dense, target inafallafiona, and cuffural<br />

faatures of landmark significance,<br />

37<br />

cartographic compllatlors-see compllalion,<br />

definition 1.<br />

carfographlc dala base (CDB)--1. A data<br />

base 01 map graph= captured tmm a map or<br />

used 10 produce a map. A CDB inmxporelea a<br />

hierarchy for feafura dispfacemenf. 2. An<br />

imemel DMA funcfbn which cswrsiafs of actual<br />

dgifal data products, an automated diiecfoty<br />

defining the data availability, data bSSe<br />

management software, corr$suter hardware, and<br />

CDB operations staff and managamenf. The<br />

CDB is rasidem at DMAAC.<br />

cartographic faalure-The natural or WlfWal<br />

objects shown on a map or chart. See also<br />

topography, daflnllion 1.<br />

cartographic film—Film wilh a dimenalonally<br />

stable base, used for map negatives ardor<br />

positives. Usually referred to by trade name.<br />

cartographic Ilcenae-lhe freedom 10<br />

ad)usl, add, or omit map featuras wtihin<br />

allowable Iimifa to aitain Ihe besf csrfographii<br />

expression. License musi nol be construed as<br />

permiifing Ihe cartographer to deviate from<br />

apaclficetions.<br />

cartographic photography—Sac mapping<br />

photography.<br />

cartog raphlc prlmlthre-A type of primitive<br />

thaf does mt participate in topology. Texl k the<br />

only catlographic primitive. Sae also<br />

gaomatrtc prlmltlva.<br />

carfogrephlc acannar—A device for strip-byatrip<br />

acenning of hvodlmensional mPy am for<br />

digital registration 01 the Iighfkfark (bfaclrAvhke)<br />

parts as rectangular coordinates.<br />

cartography-Tfre art and science ot<br />

expressing graphically, by maps and charm, the<br />

known phyaicel and politicalradminfafraflva<br />

featurea of the Earth, or of anothar celestial<br />

body.<br />

carfometrlc acallng—Tha accurate<br />

measurement of ge~raphlc or grid ccardinates<br />

on a map or chart by means of a ecafe. This<br />

method may be usad for plottino the fmsifkrns<br />

o! points, or determining tha location of poims.<br />

carvfng-The development of the model<br />

surface by carving away the steps of the plastar


I<br />

step cast in the pmducf ion of relief models.<br />

cessette-(JcS) In photography, a reloadable<br />

container Ior either unexposad of axposed<br />

sensfflzed materfala whch may be removed<br />

fmm the camera or dsrtrmom equipment under<br />

lightened conditions.<br />

Cseelnl map pro]sctlon-A conventional<br />

map pm)ecf~n conefrucfad by computing the<br />

Iengfhe of arcs atong a ealecrad geographic<br />

meridian and along a greet circle perpendicular<br />

to that meridian, and pbffing these as<br />

rectangular coorrfinatee on a plane.<br />

MIL-HDBK:850<br />

Ceselnl-Soldner maB tsrolsctlon- Similar<br />

to a polycaic map pr6jef%~ excepf that if uses<br />

but one central meridian for a whole series. Best<br />

edapted for north-south belts ad large-scale<br />

maps of small arees.<br />

cestlng—The process 01 reproducing relief<br />

rnedels in plaster or epexy from the terrain base<br />

of the modal, or aftar the surlace of fhe model<br />

has been devaloped. Models are fimf cast<br />

negsflve, fmm filch ❑ny number of poeitive<br />

castings may be made.<br />

casuel error—See random error.<br />

catadloptrlc sysmm-(optics) An optical<br />

svstem containlno both refractive and reflective<br />

eiements. -<br />

catenerv correctlorr-hatrino) Sae eao<br />

. . .<br />

correction.<br />

CathOda ray—1. One of the high-speed<br />

electrons projected in a stream trom the heated<br />

cathsde of a vacuum tube under the propulsion<br />

of a afmng alecrric field. 2. A stream of celhoderey<br />

efecfmns<br />

cathode-ray tube-A vacuum tube in which<br />

cathode rays, uauafly in the form of a elendar<br />

beam, are prolecfed upon a ffuorescerrf screen<br />

fhaf serves aa an errfica!hode where the rays<br />

produce a luminous spot.<br />

csthode-The elecfmde at which electrons<br />

enter a devbe fmm the external circuit.<br />

cetoptrlc system-(optics) An optical system<br />

in which all elements are raflecfive (mirrors).<br />

cautlona~ note-lnformallon cafllng special<br />

attention to some fact, usualfy a danger area,<br />

38<br />

shown on a map or chart.<br />

celestlel coordlnataa—Any set of<br />

coordinates used to deline a point on the<br />

celestial sphere.<br />

celeatlal aquator aystam of<br />

coordlnatas—A sel o? cefestial coordinates<br />

based on the celestial equator as lfre primary<br />

greaf circle; usualfy dacllnatbn and hour angle<br />

or slderaal hour angle. Afao calied aquator<br />

ayatem; equatorlaf system; aquhtoctlal<br />

eyetam ot coordlnataa.<br />

caleeflal equator-Tfre great clrcfe on the<br />

miestial ephera whose pJane Is perpendiilar 10<br />

the axis of rotation of the Earth. Also cafied<br />

equlnoctfal.<br />

celesliaf fix—A position established by means<br />

of observation on one or rnera celestial todies.<br />

cefesllal geodeey—The branch of geodesy<br />

which utifizes obsewalions of near C81aS.til<br />

bodies, including Earth satellites, to datermins<br />

fhe size and shape of the Earth.<br />

celeatlal horizon-That circle of the celestial<br />

sphere formed by the interjection of fhe<br />

celestial sphere and a plane through the center<br />

of fhe Earth and perpendicular 10 the zenith<br />

nadir tine, Also caffed rational trorlzon.<br />

celeetlal latltuda-Anguiar disfanca north or<br />

south of the acllptk; fhe arc of a circle of Iafiiude<br />

between the ecliptic and e point on the celaefial<br />

sphere, measured northward or aoufhwati fmm<br />

the ecliptic lhrough 90°, and labeled “N- or ‘Sto<br />

Indicate the direction of measurement. Also<br />

called acliptic iatitude.<br />

cefestlal fine of poelllon-A fine of PrMflon<br />

determined by means of tha observation of a<br />

celestial body.<br />

cefeaflal longituda-Angular distance east<br />

of fhe vamal aquinox, abng the ecfipfic: the arc<br />

of fhe ectiplic or the angle al the ecliptic pole<br />

between the circle of latitude of the VetTIal<br />

equinox and tfre circla of ialifude of a point on<br />

the celestial sphere, measured eaafward fmm<br />

the circle of Ialilude of the vernal equinox,<br />

Ihrough 360°. Also called acllptlc Iongltude.<br />

celeetlal mechanlca—The study of Iha<br />

fhaory of fhe motions of celestial bodias under<br />

Ihe infiuance of gravitational fiefds.


“ - MIL-HDBK-850<br />

Caleetlal morldlarr-An hour circle of the<br />

calsrsilel sphere, thrwgfr the celestial peles and<br />

the zanlth. The hvo intersections ot Ihe celestial<br />

matiien wlfh the horkon are known as the<br />

north and south points.<br />

caleatltsl obeewatlorr-1. Obsemation of<br />

Wdeefial phenomem. 2. (nevjgation) The<br />

measurement of Ihe altitude or the azimuth, or<br />

both, of a celestial My. Also the data obtained<br />

by such msaeuremant.<br />

calaatlat paraHel-See parallej of<br />

docllnallon,<br />

calaatlaj pole-Eifher of lhe two points of<br />

Imersecflon of the celestial sphere and the<br />

extended axis of the Earih.<br />

celeatlal refraction-See astronomk<br />

retraction.<br />

Celaaflal sphere-(JCS) An imaginary sphere<br />

of hrflnlfe mdkss concemric with the Earth, on<br />

which all celestlal bodies except the Earth are<br />

Imagined to be projected, [For observations on<br />

badieS within the lirr?dsot the solar system. the<br />

assumed center is the center of the Earth. For<br />

bodiis whare I ha parallax is negligible, the<br />

assumed ramer may be Ihe poim of<br />

observation.]<br />

Celaallel triangle-A spherical triangle on the<br />

Caleafial sphere, especially the navigational<br />

triangle.<br />

call-Variable size rectangular geographic<br />

arsa, often rleslgnaled by Iatlludeflongltuda<br />

boundaries. DMA produces standard alevation<br />

(DTED) and faatura (DFAD) data in one degree<br />

by one cfegrwe celks.<br />

center line data (CLD)—Data which<br />

daschea ooinfa, tines and araas as ona or<br />

several cc%rdinete poima selected at the tamer<br />

of the phenomena being described. Attributes<br />

used with camerfine date describe the feature in<br />

real wcrrkl terms and not the display of graphic<br />

O@t. SY*lized oraphis dafa, on the other<br />

hand, contains attribution for the display ot<br />

graphic output.<br />

cantor of gravity—lhe point in any body at<br />

which the tome of gravity may be considered to<br />

be concentrated.<br />

39<br />

center of lnatrument—The point on the<br />

vertical axis of rotation ot an inrsnsmarrt at the<br />

sama alevation as the axis of collimation when<br />

that S6”Bis in a horizontal posifbn. in a transit or<br />

theodoliie, It is cbse 10 or at the intersection of<br />

the horizontal and vert”kel asea o! the<br />

instrument.<br />

center of ma~The point at which ail tha<br />

given mass of a body or bcdiis may be<br />

regarded as being cancentretal as far as<br />

motion is concerned.<br />

center ot oacllletiorr-(pendulum) The<br />

poatiion in a aorrrpound Pandubm ~ me Wkb<br />

which czmesponds 10 the haavy particle of an<br />

equivalent airnple pendulum. The centers of<br />

suspensbn and oscillation are interchangaabla.<br />

It the center Ot oscillation la made the canter of<br />

suspension, the former canter of wspanslon<br />

becomes the naw canter of oscillation. This<br />

principle is the basis of design of cmnpound<br />

reversible pendulums.<br />

center of pro}acIiOn—See parapectlve<br />

center.<br />

center’ 0? radiation—See radial centar.<br />

center of .wapanalon—[pendulum) The<br />

fixed point aboul which a pendulum oscillates.<br />

See aiso cantor of oaclliallon.<br />

centar polrrt-See radial center.<br />

centarlhm-1. (USPLS) The line connecting<br />

oppostie Conesponding quarter cumers or<br />

OPpOSite Subdivislonmf-seCf ion corners or lhelr<br />

theoretical poaifions. 2. A line esfending trom<br />

the tme center point 01 ovarfspping aerial<br />

photos through each of the Transposed canfer<br />

points. 3. (engineering survey) The continuous<br />

cemer of a highway or railroad, with sfat”oning<br />

indicating starling point, culverts, poims 01<br />

curvature, etc.<br />

cantlmeter. gram-eacond (c.g.m)<br />

ayatem—A systam of units based on lhe<br />

cemlmeler as the unit of langlh, the gram as the<br />

unit of masa, and the mean solar second as the<br />

unit of time. A part of the metric system.<br />

central force flald—The spatial dklributlon of<br />

the influance of a cantral force.<br />

central force orbit-The Theoretical orbit<br />

.,-.<br />

I


I<br />

MIL-HDBK-850<br />

achieved by a parl’kle of negligible mass moving<br />

in the vicinity cd a point mass with no other<br />

lorc9s .arsing: an unperturbed orbit.<br />

cantml forw-A force which for purpoeee of<br />

mmputetbn can be mnektered to be<br />

mncammted at orre cemral polm with fts<br />

Imerreiiy at any other point being a funotbn of<br />

lhe distance from the camral point. Gravitation is<br />

considered as a camral force In calestial<br />

mechanks.<br />

CentMl merldte~The Iongffudlnal line of<br />

eymrnetry ot a map projection, and generaliy a<br />

base line for relererd~ the pro)ectbn to the<br />

aaaoclaled grid coordinate system. As such,<br />

grkl north and true r’mrth are coincident along<br />

the central merfdian, but at any other poim of<br />

the projection, gdd north and true north dtverge<br />

as a function of geodetic laWnle and<br />

bngitudinal distance from the central rrrar!dian<br />

due to mrrvergence of the meridians. Meet<br />

map prmjectbns pottray merkfian mnvergence,<br />

twl one notable exception Is the Mercator<br />

Projectbn.<br />

central polm flgur%A triangulation figura<br />

mnsistirrg of a pelygen with an inlerior station,<br />

formed by a series of adpining triangles with a<br />

mmmon vertex al the interior station.<br />

centrlfugnl force-The force with which a<br />

My moving unc@r mnstrainl along a curved<br />

path reacts to the constraint, acting in a<br />

duection opposite from the center of curvature<br />

ot the path, For a body unstrained to Earth,<br />

cwrirflugal force acting on Ihe body due to<br />

Earths rotadon k perpendicular to and away<br />

from Earths rotational axis. The veclor sum of<br />

this cemrifugal force ard the gravttatlonal force<br />

due to lhe total mass of the body and Earth is<br />

defined aa Ihe gravity force acting on the body.<br />

Sae also cantrlpetal force.<br />

Cantrlpetaf fo~The force direcled towards<br />

the center 01 curvature, which mnatrains a bedy<br />

to move in a curved path. See also centrifugal<br />

force.<br />

conlrold+dlgltal mapping) A point interior to a<br />

polygon whose coordinates are the average of<br />

the corresponding coordhates for all nodal<br />

palms which define fhe polygon, This point may<br />

be outskte or inside the polygon and can be<br />

Some point olhar than the geographic center 01<br />

the polygon.<br />

chain gage—See tape gage.<br />

40<br />

chain node-An erc-node topologkal model<br />

that stores the enfiiy deacrptions and apafiaf<br />

axtants in separate records, and finks Ihem with<br />

remrd polntem. The basic emlty is a chain or<br />

arc, a series of coordinates that etan and end at<br />

a node. A node Is a beglnnlrrg, an end, an<br />

Imersactbn, or a Pint representad by a<br />

coordinate pair. see also arc, edge, Unk and<br />

nods.<br />

chain-node date ●tructur*A vector data<br />

structure in whch the entity descnptiin and the<br />

spatial extent of each feature in a vector data<br />

se! are stored in separate records, linked by<br />

record pointars, In addition, all interaacfions<br />

between Ieatures, se well as point features. are<br />

captured and stored as nodes.<br />

chalnlng pin—See pin.<br />

chairrlng-See taping.<br />

chain-A device usad by surveyore for<br />

measuring dblance, or the length of this device<br />

as a unit of distanc8. The usual chain is 66 feet<br />

IonQ, and consists ot 100 links. each 7.92<br />

inches Iorq. See alsq englnaer’a chain;<br />

Gumeds chain.<br />

challan Qar—See Interrogator reaponsor.<br />

chambered Splrlt level—A level tube with a<br />

partition near one end which cuts off a smafl air<br />

reservoir so arranged that the length of the<br />

bubble can be regulated.<br />

changa detection—An image enhancement<br />

technique which mrnpares two images 01 the<br />

same area from differem time perbds. Identical<br />

plciure elemenls are eliminated, leaving<br />

signatures which have undergone changa.<br />

characterlatlc currre+photography) A curve<br />

showing tha relationship between ex~sure and<br />

reaufting density in a photographic image,<br />

usually pbttad se the density (0) against the<br />

logarithm of the exposure (fog E) in candlemeter-sesxmds.<br />

Also called D log E msrva;<br />

density exposure curve; H and D curve;<br />

senaltometrlc curve; tlma gamma curva.<br />

Sea also contmet; denalty, definition 1.<br />

characler-TIIe distinctive Iralt, quafii,<br />

property, or behavior of man-made or natural<br />

faatures as portrayed by a cartographer. The<br />

more character applied to detail, the more<br />

closely it will resemble these features as they


,., ..r.<br />

appear on the SuSfa= of the Earth. See ako<br />

genernllzatlon.<br />

‘MIL-HDBK-850<br />

Chan Updalo Manual (CHUM) — A DMA<br />

publmhad manual which pmvidae aeronautical<br />

chars USEM with carrranf information on a<br />

monthly bask sxrncemlng charts and hazards to<br />

Wgfstsafety for Ifrose charts. Future CHUMS<br />

may be aveilable elactronlcally (ECHUM).<br />

chart baaa-(JCS) A chart used as a prfmary<br />

source for compllarton or as a ftmrrawrk on<br />

wtrlch nw detail fa primed. Afso called<br />

topographic base. See also base map.<br />

charl comparlaon unff-A device parmifflng<br />

aimuffaneous vlawing of mvigational tnatrumem<br />

presenlafion, such as a radarscopa and a<br />

navigatbnal than, so fhaf one appeara<br />

auparimposed upon the other. Also called<br />

autorader plot when used with radar.<br />

chart datum—See hydrographic datum.<br />

charted dept&The vertical dk.tance from<br />

fhe fidal dalum to the bottom surface.<br />

chanlng photography-See mapping<br />

photography.<br />

charflet-A small chart, such as those<br />

annexed fo NotIces to Mariners.<br />

then—l.. A apacial-purpose map, generally<br />

designed for navQatbn or other particular<br />

purposes, in which essential map information is<br />

cornbtnad wffh varfous other data crfflcal to the<br />

inlendad use. 2. To prepare a chart, or engage<br />

in a charting operation. See also aeronautical<br />

than; ●eronautical pllotage chart;<br />

aeronautical plannlrrg chart; Alr Targat<br />

Chart; anchorage chart; approach chart;<br />

azimuthal chart; ●zimuthal equldlatant<br />

chari; Baldwln solar chart; bathymetric<br />

than; chartlat; coaatal chart; combat<br />

chart; conforrnal chart; conic chart;<br />

conic chart with two standard parallele;<br />

Conaol chart; cot idal cfrarf: current<br />

chari; Decca chart; ●nrouta chart;<br />

●quatorial chart; firing chart; general<br />

chart; Global Navlgatlon Cherr;<br />

gnomonlc chart; Oreat-circle chart;<br />

harbor chart; hletorlcal chart;<br />

hydrographlc chart; hypaographlc map<br />

(or chart); ice chart; Indax chart;<br />

Instrument approach chart; Iaobarlc<br />

chart; Iaocllnlc chart; Iaogonlc chart;<br />

Ieogrhr cfsarr; Ieomagnallc than;<br />

41<br />

Isoporlc chart; JaI Navlgatlon Chart;<br />

Lamban conforrnsl chars; local chart;<br />

Iong-rarrge navigation chart; fomn<br />

chart; hrnar Chari; lunar earthalde chart;<br />

lunar tarslde than; mafytatlc chart;<br />

Maraden chert; maan chart; Mercator<br />

chart; metaorolog Ical chart; mileage<br />

then; mlacellaneoua ctrart; modlfled<br />

Lamberf confomsrd chart; new chart;<br />

obllqua chart; otrllqua Marcator chart:<br />

obsolete chart; Operational Navlgatlon<br />

Chart; orthographic chart; orshomorphlc<br />

chart; parspecllva Chart; PIIoI chars;<br />

pllotage chart; planrslrro chart; Plottlna<br />

then: polar chart; polyconlc than; radar<br />

than; ractanguler chart; route chart;<br />

sslllng than; esarch.and-rescue chart;<br />

eacant conic than; eactlonal chart;<br />

aextant than; ●lmple conic chart; star<br />

chart; atereographlc chart; Tactlcsl<br />

Pllotage chart; tidal currant chart; time<br />

zona Ch6ti; track than; tranevarea<br />

chart; tranaverae Mercator chsn; Vlt’fUSl<br />

PPI reflactoscopa chaft; vlslbll}ty chart;<br />

waalhar map; World Aeronautical Chart.<br />

check point—l, (JCS) A pradetennlned point<br />

on lhe Earth’s surface used as a means of<br />

mmrolling movamem, a registration target for<br />

fire adjustment, or a reference for bcation. 2.<br />

(.fCS) Gaographkal Iocalion on iand or water<br />

above which ths posilion of an aircraft in ffight<br />

may be determined by obsewafiin or by<br />

electronic means. 3. A point, selacfad on<br />

obliques only, in the viclnlfy of each tie point and<br />

distant point for the puqmse of checking Ihe<br />

idenlifiia!ion of these pointa.<br />

chSCk proflie-A profile pbffed fmm a field<br />

survey and used to check a profile Wapared<br />

fmm a topography map. The comparison of the<br />

two prollles servas as a check on ~he accuracy<br />

o! the comoura on tha topographic map.<br />

checked apot elevatlort-An elavation<br />

established In fhe field by: closed s@ff leveling,<br />

trigonometric leveling by a clossd circulf of<br />

barometric leveling, or any other method such<br />

tha! proof of accuracy ia obtained.<br />

checking potsftlve-A composite printing on<br />

giaas 01 the contour and drainage drawings<br />

used on the shadow projector Ior checkhg the<br />

horizontal accuracy ot Iandforrns to be<br />

developad on relief models.<br />

chopping—(efar or aatelllte traits) Interrupting<br />

Ihe photographic Image of a afar or satellite trail


;<br />

by a shutter or other device to provkie precise<br />

timing and ofiematlon data for geodetic<br />

ok6enwfions of aaroapaca vehwes against a<br />

eiellar beckgfoumf.<br />

chord-1. (mute auweying) Chord used in<br />

highway and other surveys to Miite a straight<br />

line between two poinfa on a curva. ragatiless<br />

of lhe distance between them. 2. In auweying<br />

and geomeIry, a straight Ilne joining any two<br />

points on an arc, came, clrcwrderenca, or<br />

surface.<br />

MIL-HDBK-850<br />

chorographlc map-Any map repreaanting<br />

large regions, countries, or continents on a small<br />

scale. Atfas and small-emla wall maps belong In<br />

mis class. .<br />

chromatic aberr@tlon—See lateral<br />

chromatic aberration; Iongltudlnal<br />

chromatic aberration.<br />

chmmatlc colors< olors eficiting hue.<br />

chromatlclty coordlnatas—The proportions<br />

of stamlard components required for color<br />

malch, used as an ordinate and abscissa to<br />

represem mlor in a chrornaticity d~Oram.<br />

Chmmatlclty dlagrarm-A plane diagram<br />

formed by pkc.ning one of the chromaticity<br />

Coordinate against another.<br />

chromatlclty—A compxjite of dominant<br />

wavelength and purity.<br />

chronograph-An instrument for producing a<br />

graphical record of time as ahown by a clock or<br />

other dev’kx. In uee, a chronograph produces a<br />

double record: the firer is made by the<br />

associated ckIc& and forma a continuous time<br />

SCSle wlfh si@ficam marka Indkating periodic<br />

beats of the tlmekaepar: the second is made by<br />

some external agency, human or mechanical,<br />

and records the occurrence of an event or of a<br />

seties 01 eveme.<br />

chronometer correction-See clock<br />

corractlon.<br />

chronometer error—The amount by which<br />

the chronometer diem from the correcf time,<br />

chronometer rata-See clock rate.<br />

chronometer-A portable timekeeper wiih<br />

compensated balance, capable of showing time<br />

42<br />

wifh extreme precisbn and accuracy. S8s afeo<br />

break-clrcult chronometer; hack<br />

chronometer.<br />

clne thaodoltMt-A photograph tracking<br />

Inetrumsnf which ramrda on each film frame the<br />

targel and Ihe azimuth and elevation angles of<br />

the OptbSf isxis 01 the inSfmMSM.<br />

circle of contusion-(optics) The circular<br />

image of a distant point object as termed in a<br />

total plane by a tans. A distam point object<br />

(a.g., a star) Is Imaged In a focal plane of a lane<br />

as a circle 01 flfrlle sixa, because 01 such<br />

conditions as: (1) the focal plane% not being<br />

placed al the point of sharpasl focus: (2) the<br />

effed of calain ebemations; (3) ditfractbn at the<br />

lens; (4) grain in a photographic emulsfon:<br />

arallor (5) pmr workmanship in the manufacture<br />

of the lens.<br />

circle of declination-S’ee hour circle.<br />

circle of equal altltuda-See pamllel of<br />

altltude.<br />

circle of aqual declination—See parallel<br />

of declination.<br />

circla of tatlturte-1. A great circle of the<br />

celestial sphere through the ecliptic poles, and<br />

henca Wpendlcular to tha ptane of the actipfic,<br />

2. A meridian along which latitude is measured.<br />

circle of Iongltuda-1. A circle of tha<br />

celestial sphere, parallel to the ecliptic. 2. A<br />

circle on the suriace of Ihe Earth, parallel 10 the<br />

plane of the Equatoc a parallel, afeng which<br />

Iocgitude is measured. Also called parallal of<br />

Iatltude.<br />

clrcla of parpetual apparition-That circle<br />

of the celestial sphare, centered on the polar<br />

axis and having a polar dktarrce from the<br />

elevated pole a~roxirnataly equal to the<br />

latitude Of the obsewer, whhin which celestiaf<br />

bodes do no! act. See also clrcla of<br />

perpetual occultation.<br />

circle of perpetual occuftatfort-That circle<br />

of Ihe celestial sphere, centered on the polar<br />

axis and having a polar distance from the<br />

depreseed pole approxlnrafely equal to the<br />

latitude of the observer, whhln which celestial<br />

bodies do not rise. See also clrcla of<br />

perpetual apparition.<br />

circle of poaltion—A small circle on the globe


,<br />

.,, ..,.. MIL-HDBK-850<br />

(Earth) at every peint o! whti, at iha inslanf of<br />

obaarvefbn, tha observed celestial body (sun,<br />

afer. or F4anet) has lhe same afrnuda and,<br />

Iherelora, me same zardtfi dkdance.<br />

clrcla 01 right aacanalors-see hour<br />

circle.<br />

ClrdO of the ephere-A circle upon the<br />

surface of the sphere, speoifkelly of the Earth of<br />

of the heavens, celled a greet ctrob whan Ira<br />

plana passes through Ihe center of the sphare;<br />

in all other cases, a small circle.<br />

ClrCle posttlorr-see postflon, deflntIbn 4.<br />

clroult closure+levellng) The amount by<br />

which tha atgabrelc aum of the measured<br />

differancss of alevafion arourd a circuit fails to<br />

equal the theoretical cbsura of zero. See also<br />

error of closure, definition 4.<br />

clrcult-(levefing or traverse) A continuous fine<br />

of Ievefs, a sertes of fines of levels, or a<br />

combination of lines or parts of lines of levels,<br />

such that a mntinmus series of measured<br />

differences of elevafion extends areund the<br />

circuit or bop end then back to Ihs starling<br />

point. Also appliid to a continuous line of transil<br />

traveme in a eirnilar manner.<br />

circular cylindrical coorcllnatee-See<br />

cyllnrfrical coordinate.<br />

clrcufer ●rror (CE)-An accuracy figura<br />

representing the slated percentage of<br />

probablliry lhat any point expressed as a<br />

furrcilon of two tinaar components (e.g.,<br />

horizontal poaifbn) will be within Ihe givan fiiure.<br />

Cemmenfy used are CEP (50 percent), CE lo<br />

(6S.3 percent), and CE (90 percent).<br />

circular error probabla (CEP)-The 50<br />

percent error interval based on the bivariate<br />

normal distribulbn function. Also called circular<br />

probable ●rror.<br />

circular leve&A sphft level having the Inside<br />

surface of its upper parl ground to spherical<br />

shape, the outline of the bub41e formed being<br />

circular, ❑nd the graduatbna tsalng concwrfrlc<br />

circfes. This form of spirft level ia used whare a<br />

high degree of pracieion Is not required, es In<br />

pkmblng a level rod or aattlng an krsfrument In<br />

eppmxhmele podrion. Also celled bultl-eye<br />

level; unlvarsal level.<br />

circular map accuracy standard<br />

(CMAS)-Tha U. S. National Map Accuracy<br />

Standerde used tor domestic rrwpplng. CMAS<br />

era spaclfiad separafefy for hortzonfal and<br />

vetikal mapped Ieaturas, Sea also rrorlzontal<br />

accuracy; verflcei ●ccuracy.<br />

circular near-certainty error (3.5u)—Th e<br />

99.78 percent error Inlerval based on the<br />

bwariata normal d~tnbutbn funcfbn.<br />

circular normal dlefrfbuflo- ee<br />

blvarlata normal dlstrlbuflon function.<br />

circular probabla error (CPE)-See<br />

circular error probable.<br />

circular ●lgme-Sae circular efamtatd<br />

error.<br />

circular efendard arror (uC+The SS.3<br />

percent error interval basad on fhe bfvetfate<br />

IIWInal distribution function. Ako called Clfoirlar<br />

algrna.<br />

circulation map-See traffic ckculatton<br />

map.<br />

clrcumterentor—A “type of surveyors<br />

compass having slit sights on projecting arms.<br />

clrcumlunar—Around lhe Moon, ganarally<br />

appliad 10 lrajactories.<br />

CkCUMMStrldlIIn altltudes—Exmaridian<br />

aftiiudes obaamed for detamnlnetlon of Iatffuda<br />

when a heavenly Imdy Is rX06e to ttarrall.<br />

clrcumpolar-Revolving about the alevated<br />

pole without setting. A celestiai body la<br />

circurr@ar when ifs polar dkfance Is<br />

approximately equal to or less than the Iaiiiuda<br />

of the obsenrer.<br />

cislunar—1. This eide 01 lhe Moon. 2. Of or<br />

pertaining to phanomena, projects, or activity in<br />

the space between the Earfh and tha Moon, or<br />

between the Earth and the Moon’s orbit.<br />

cistern barometer—A mercury barometer in<br />

whkh a coiumn of mercury IS enclosed in a<br />

vertk.el glass tube, the upper end of whkh is<br />

eealad and exhausted of air, and the bwer end<br />

placed in a cislarn or resewoir of mercury which<br />

Is exposed to atmospheric pressure. The<br />

atmospheric pressure on lhe free sutface of the<br />

mercury In the cktam determines the height to<br />

which the mercury will rise In the vertical tube.<br />

43<br />

I


,.<br />

This rney be measured, and the pressure<br />

~e~~~, in te~ at that heiflh(, as In inches Of<br />

CRY Omphlc (CG)-Larpe-scale lithographic<br />

map of populated pfaces and environs<br />

porrrsying afreets and through-route information<br />

Features frduda Impcrrtanf buildings, airfields,<br />

mifiiary installations, industrial cwnpfexes,<br />

embassies, etc. Pmduc8d at 1:25,000 and<br />

larger scale. See also cfty pmducfa.<br />

city plan—See city products.<br />

City pmducta-Large-ecale maps of<br />

poputetad plaoaa and envirorra, usually<br />

porfrsylrsg sweat amf through-mule Irrlormalion,<br />

irnpon”am-buildings and othtir urban features,<br />

airfields, port facilities, and relief. drainage, and<br />

vegetation when imporlant. Severel different<br />

types of city pnxfucfs are prcducad by DMA,<br />

among which are cdy graphka, city plans, city<br />

route grsphics, and mifitary city maps.<br />

Specifications (or these maps vary according to<br />

parficufar mlltary requiremems.<br />

City route graphlca (CRG)-See city<br />

products. ,.. .<br />

cfty survey-A speciaffzed type of land survey<br />

restrkxed to work campleted primarily within the<br />

Iimtis of a ciiy.<br />

cIvII day—A solar day beginning at midnight.<br />

The cfvii day may be based on either apparem<br />

solar fires or mean solar fime. See also<br />

metronomic day.<br />

CIVII tlma-Sofar lime In a day (civil day) that<br />

begins af midnight. Civil lime may be either<br />

apparanf solar time or mean solar time; if may<br />

be wumed in two series of 12 hours each,<br />

beginning al midnight, marked ‘am” (ante<br />

meridmn), and at noon, marked “pm” (post<br />

merkllan], or In a sfngfe seties of 24 hours<br />

beginning at midnight.<br />

Clairaut% tfWoram-A theorem that, in its<br />

o~lnal tom, rela!es the value of centrifugal<br />

force at the Equator to the value of gravity at<br />

the Equator. Imfxmancs to physicaf geodesy Is<br />

that the flattening of the Earth can be obtained<br />

from gravlfy maaauranrants.<br />

clamplrsg ●rror—A eyslamatic error in<br />

observatbns made with a repsafing theodolffe<br />

cauaed by atrairrs rjel up by the clamplng<br />

devkes of the Instrumem.<br />

MIL-HDBK-850<br />

44<br />

Clarke ●phamld (clltpaolrf) of 1B66- A<br />

raf erence elfiisoid having the Iotfowing<br />

approximate Wnansions: eemin@or axla-<br />

6,37S,206.4 meters and the tlaffening or<br />

eltipticify-1/294 .9786982.<br />

Clarke epheroid (alllpaold) of 188G- A<br />

reference elfipsokd having Iha follo@ng<br />

approximate dimensions: semimapr axb-<br />

6,37S,249.1 45 maters; and the flattening or<br />

elliplkffy-1/293 .465.<br />

claastlicatlon copy-A speclaiiied item of<br />

sourca maferfal used as a gubte by the wrnpilar<br />

andlor draftsman in preparing a map or chart.<br />

Usually consists of detailed informatbn<br />

pertaining to roads, railroads, cfty data, and the<br />

like that has been devebpad trom tietd aurvaya.<br />

Usually furnished in the form 01 overlays,<br />

annotated maps, drawings, pholographe, or<br />

field sheets.<br />

clasalficatlon survey+ee fbld<br />

Inapectlon.<br />

Claaslfled Hydrogmphlc Information<br />

Processing System (CtflPS)-Ttre DMA<br />

data base which provides rmvigetiin update<br />

information for classified charts and pub ficatbns.<br />

Classllied Notice to Marinera-DM A<br />

publication which provides mrrecfive data<br />

appficsble to classiiiea charts and ~biications.<br />

Tfris informal’km is afao accessible throu~h the<br />

Classified t-fydmgrsphic tntormatfin Process”w<br />

System (CHiPS).<br />

cleerlng y-paraliax-See relattve<br />

orlantatlon.<br />

cllnomater—A simple in. NNfI’tenf used tOr<br />

measuring the degree of slope in percemage or<br />

in angular measure.<br />

clipplng-1. (GIS) The process of<br />

subdividing overlapping potygons to preduce alt<br />

mmbinations of aeparale unique polygons.<br />

Also caliad completing, 2. (computer<br />

grapMcs) The severing of that pzrfbn of a line<br />

segment which falls outside a predafinsd frame.<br />

clock corractlorr-The quantity which is<br />

added, algebraicetly, to the tima shovrn by a<br />

clock to obtain the time of a gben meridian. If<br />

fhe cfock Is slow, the mrracfbn is positive: it fast,<br />

negative, When applied to a chronometer it is<br />

caifed chronometer correct Ion.


I<br />

cfock rafe-The amount gained or bat by a<br />

clodr in a ursh of time. When eppWd to a<br />

chronometer, ft is called chronomcrlar rate.<br />

clockwlae angle—See angla to right.<br />

cloaad travaraa-A’ survey travarae which<br />

starts and ends upon the same station, or upon<br />

efafiirra whose relattve positions have been<br />

defenrrlned by other surveys 01 equal or higher<br />

order of accuracy.<br />

cloeeaf ●ppeoackl. The event that occurs<br />

when two pfanats or ofher celestial Imcfles are<br />

nearest to each olher as they orbit af%wt the<br />

Sun or other @nary focii. 2. The place or time<br />

of such an event. 3. (sateltiie surveying) The<br />

time and bcafion of the setell)te when fi is<br />

closest to the observerhceiver antanna.<br />

cfoelng corrsar-A corner aslabllshad where a<br />

wrvey line intersects a praviousfy fixed<br />

boundary at a point between comers. The<br />

closh?g comer is focaled by law at the actual<br />

point of infarsactlon without regard to its<br />

monumented bcafion.<br />

MIL-HDBK-850<br />

definition 7,<br />

Closura-sae ●rror of cloaura, dalinfflon 1.<br />

chmtarlng aperatlona-Operaf ions allowing<br />

one to aggbmarate (ciuster) individual Items or<br />

faa!ures into groups.<br />

coalfltude-The complement of attitude, or 90<br />

minus the affiide. Tha tarm has signiticafrca<br />

only when used in connecfbn wfth sffffuds<br />

measured from Ihe caleetial hoffzon, when it is<br />

synonymous with zanltl? dfetarsca.<br />

coaat pilot-sae aalllng dlractlons.<br />

Coaat.Survay method-See trlanglo-olerror<br />

mathod.<br />

COaStal chart-A nautlcaf than Intended for<br />

offshore nev”~af’bn of vessels having a need for<br />

positions relative to the coast. Daplcfed<br />

informafkrn supporls coastal navfgafion and<br />

miliiaty operations. Produced from 1:100.000 fo<br />

1:1,000,000 acaie.<br />

coaatal rafractlon-(JCS) The change of fhe<br />

“closing’ error-See arror of closuriT ‘<br />

.- direction of travel of a radio .around<br />

wsvs as ~<br />

““ passes‘“ from land fo saa or fmm sea fo land.<br />

de flnftlon 1,<br />

Also called land effect; ahorellne eftaCt.<br />

closlng the hortzor+Measuring the last of a<br />

serias ot horizomal anglas at a slalion, required<br />

to make fhe cartes compiate around fhe<br />

horizon. At any station, the sum of the<br />

hortzomal angfas bafween adjacent lines should<br />

equaf 360”.<br />

cfo$lng township cornar— 1. (USPLS) The<br />

point of imeraacfion of a guide merkfian or a<br />

ra~e line with a prevkwsly fixed standati<br />

parallal, or a base line. 2. Tha poim of<br />

intaraacfiin of any township or range line with a<br />

orevbusfv fixed Ooundaw at a mint between<br />

pravbus~ establbhsd comers. ‘See alw<br />

townahlp cornar.<br />

closlrxg-The act of finishing a survey process<br />

so fhat the amuracy may be checked.<br />

closure of frorlzon-See arror of closure,<br />

definition 6.<br />

ctoaure of travarae-Sae arror of<br />

closura, deflnifion 8.<br />

closura of triangleSee arror of closure,<br />

45<br />

coestllnlng—The process of obtaining dafa<br />

from wh”ch Ihe coaslline can 0s drawn on a<br />

chart.<br />

coated len%A Ians whose air gfass sufiaces<br />

have been coated with a fhin transparent film of<br />

such index of refraction as to minimize the light<br />

bss by reflection. This reflacfiin loss tor<br />

uncoated tenses amoums to approxlmmely 4<br />

percem per air glass surface. Also called<br />

bloomarf Iana.<br />

codacllnatlon-The mmplemant of lhe<br />

declination: ff carries the sama sign as the<br />

declination: equal to fhe declimflon of the<br />

celesfial fxrle nearest a oalesfiaf position minus<br />

the declination of the celesfial pasffiinel.<br />

COt3fficlant of refractlorr-The raflo of Ihe<br />

refraction angle at the point of observation to<br />

the angle at fhe cenfar 01 fha Earsh whkh Is<br />

formed by fha obsarvar, the tamer of the, Earth.<br />

and point observed.<br />

cogaold—See comperrsatad geold.


, MIL-HDBK-850<br />

col~ldawe method-1. (Iheodotite) The<br />

PfOCedUm by which the circles of the Ihtilife<br />

are reao. See colncldence, detinfrion 1.2.<br />

(pendulum} The defermlnatbn of the perkrd of a<br />

frae-mvfngfng pandufum by obaawing the Ilme<br />

interval between coincidences wllh a c40ck<br />

pendulum or chmnornefer beat.<br />

colncldonce-1. In the measurement of<br />

angfes with theodolifee, the instant at which two<br />

diamafricalky opposed Index marfrs on the circle<br />

are In perfect optkal aliinmem and appear to<br />

form a continuous iina across tne dividkq tine of<br />

the @_cfa. 2. (SWWykl$f) A prtamafk<br />

amangernam common to tavefing instruments<br />

wherein ona-fraff of oppoatte ends of the<br />

leveling bufk4e are broughl imo view in a slngla<br />

image, Coincidence IS achieved when the two<br />

hefvas of the bubble ends match. 3.<br />

(pandu!um) An exw agraemassl in ~curremx<br />

of a prescribed phase of the beat of a freeawinglng<br />

parrduium and a prescribed phase of<br />

lhe beat of a cbck or chronometer.<br />

cola: ituda-The @mplement 01 the latitude,<br />

or 90° minus the latitude. Cotatitude Iorms one<br />

side, zenttp to pole, of the astronomic triangle. It<br />

is the ‘aide opposite the cebasfiil bedy.<br />

coliatfo~l. Tha verification of the order,<br />

number. and dale 01 mapa. 2. The assembling<br />

of pages o! publications in sequexe.<br />

coliecflon (acquisffion)-1. (JCS) The<br />

obtaining of irrformat’ion in any manner, to<br />

idude direct obaervatbn, tiaiacrn with offiiial<br />

agencies, or soiicffation trom official, unoffkiat,<br />

or public aouroea. 2. The process of arranging<br />

for and obtaining exfsting data frem one or more<br />

sources for a library file or a specific mapping,<br />

charting, and geodetic prcducfion program.<br />

collection requlroment—An identified gap in<br />

inforrnatbrr or material hokhgs, irxSuding<br />

general requirement stalemems, intended tof<br />

fiekf mllacfbn acfiirr. Not intended to apply to<br />

requirements of data available from existing<br />

Department 01 Defense data libraries.<br />

colllmafa-1. (physics and astronomy) To<br />

rander parallel to a canain fine or direction; to<br />

render paralfei, as rays of light; to adjust the line<br />

of sight or iens axis of an optical inswumant so<br />

that H Is in ils proper position relative to lhe other<br />

parts Ot the lnWWI’ISm. 2. (photogremmetry) To<br />

adjust the fiducial marfrs of a camera so that<br />

they define the prfncipal point. Also called<br />

46<br />

adjustment for collimation; collimation<br />

adjustment. Sae also collimating marks.<br />

collimating oyepiac*A prismatk eyepiece<br />

used with a collimator.<br />

collimating marke-index marks, rigidly<br />

connected wlfh the camera bmfy, which form<br />

images on the negative. These images are<br />

used to determine the posifkm ot the optical<br />

center or Prk’u@al point of the Imagery, Also<br />

calied fiducial marks.<br />

colllmatiosr ●djustment-sae coillmste,<br />

definition 2.<br />

colllmsrtlon axi*ln an optical instrument,<br />

the fina through the rear nodal Wim of fhe<br />

objective lens that is precisely parallel wtfh the<br />

center line of the Instrument.<br />

collimation error—The angle by which the<br />

line of sight of an optkal instrument dhfera fmm<br />

IIS mllimation axis. Also called error of<br />

collimation.<br />

coliimetlon plane—The plane described by<br />

the collimation axis of a telescope of a transil<br />

when related arour’d ifs horizontal axis.<br />

collimator—An opfiiai device for artificially<br />

creating a target al infinite distance, a beam ot<br />

parallel rays of light; used in testing and<br />

adjusting wrfain optical imrtruments. It uauaily<br />

mnsists of a converging lens and a target, a<br />

system or arrangement of cross hairs, placed at<br />

the principal focus of the lens. See afso<br />

eutocotilmator; collimating ayeplece;<br />

verflcal collimator.<br />

color compoelte-A composite in which the<br />

camponem images are ehown in differem<br />

colors. See also composite.<br />

coior gradiente-See hypsometrlc<br />

tinting.<br />

color mixture CUWC-A graph representing<br />

tristimulus value for unii flux of qsecfral energy,<br />

shown as a function of wavelength.<br />

Color mixture data—Amounls of<br />

mmfmrrents required In a threeabr cobrimater<br />

to malch various wavelengths.<br />

cotor plata-A general term for the press<br />

plate from which any given coior is printed.


Norrnafly, the term is mrsdiied to reflect a special<br />

cobr or type of plate, such as brown plate or<br />

corrfour plsste. See also process platee.<br />

COW proof proc8ee-A photm mechanical<br />

printing process which makes possible the<br />

osrnblnirrg of rtagattve separations by<br />

w-aafve espoaures 10 produce a composffa<br />

cebr proc4 on e vfnyl pfastii shwl. The melhod<br />

la uwally relerred to by the manulacfurefs trade<br />

name of the materials ueed,<br />

mfor proof-A elrrg!e or composffe copy of afl<br />

arbm of a pofychtums (muflimlor) printing wh~h<br />

may be produced by any method.<br />

color reglsfretlon guide-A vlaual dlaplay<br />

on a Iffho copy of a chart which accurately<br />

raflacss the amount and direction of<br />

misregiafration between the graticule and certain<br />

aignffk.rsnf overprh’rf. See also reolster merka.<br />

color separation drawlrtg-one of a set of<br />

drewin#s which mntains similar or related<br />

features, such as drainage or cuffure. There are<br />

as many drawings as mere are mlors to be<br />

shown on the Ilfhographad mpy.<br />

color ●eparatlo”n guld=Se8= guide.<br />

color eepsratlon—1. Tfse procass of<br />

preparing a separale drawing, engraving, or<br />

negative for aach mfor required in the<br />

pmductbn of Iffhographed map or chart 2. A<br />

photograph process or electronic acannlng<br />

prmadure using color fibers IO separate<br />

muffimlorsd mpy into separate Images of each<br />

of the fhree primary colors<br />

colorlmeter-An instrument designed for the<br />

direct msawremenf of wlor.<br />

coluree-The hour clrclas through the<br />

eminoxee and the soltiicas. See afso<br />

●quf noctlal cofura; eotaff thsf cofure.<br />

corns-An aberration affetitng the sharpness<br />

of images off the axis in which rays fmm e point<br />

ob@f oft the axfs passing throuoh a given<br />

Ctrcular zone of fhe lens come to a tows in a<br />

circle rather than a point, and Ihe circles termed<br />

by rays through d~erent zones are of dtierenf<br />

Slzee and are located at dffferanl distances from<br />

tha asla. Therefore, the Image of a polm objscl<br />

is comet-shaped.<br />

combat chart-A apeclal-purpose chart of a<br />

fand-sea area using the characferiaflcs of a map<br />

MJL-HDBK-850<br />

I<br />

47<br />

to represant Ihe land area and the<br />

characfarlsflca of a chart to ra~sarrf the sea<br />

area, with such special chereaarietks es to<br />

make the chart most usetul in mlflfary<br />

operations, particularly a~hiblous qxwatbna.<br />

Produced at t :50,000 scale. Afao caflsd map<br />

chart.<br />

comblrratlon plate-f +afflons and fine work<br />

on ona plate. Ah, two or more Suuecls<br />

cornbkwd on fhe serrM plate. sea also<br />

process pletea.<br />

Command, Confrof, Communfcetfons<br />

and Inlefllgence (C31)-Communlcallon<br />

and automated data proceeding (ADP) systems<br />

and their ssaocfalad iaclfffles, aqupmsnt,<br />

personnel, and procedures, that wpporl the<br />

functions of mmmand, control,<br />

communications, and imelligence.<br />

commercial-off-the-sfself (COTS)—<br />

Production items that are available fmm<br />

commercial stock and need not be either nrWdy<br />

purchaaad or immediately msnufaofurad. Afso<br />

known ae Contractor Oft-the-Sheff.<br />

common control-(JCS) Iior”uonlal and<br />

vertical map or charl Iwatbn of points Ifl the<br />

large! area and posfflon area, tied in wffh fhe<br />

horizomal and vertical control in use by two or<br />

more unffs. Msy be estatrlkhed ~ firing, wwey,<br />

or combination of bofh, or by assumption. Ss8<br />

also conf rot point; ffefd controf; ground<br />

control.<br />

common establishment—See estsb-<br />

Ilshment of the port.<br />

communfcatlone eetelllta-(JCS) An<br />

orbiting vehicle which relays signals between<br />

mmmunicat”nns stafiins. They are of two types:<br />

(1) active communlcatlona satelllte—a<br />

aalellffa which receives, regenerates, and<br />

retransmffs signals between stations; (2)<br />

paeslve communications satelfltea<br />

satellite which reflects cxrmmunkstions algnals<br />

Ibetween<br />

stations.<br />

Eompact dlac-lntoractlve (CD-1)-A<br />

mmpact disc formet ~malninf3 premmtied<br />

iiifal video, audio, and optical text data. Data<br />

xmnol be arased or alfared CD-1 mmplies<br />

Mfh the Green Sook Standard.<br />

:ompact dfsc-read.only memory (CO-<br />

?OM)—A standard 12 cm plastlc optlcaf disc<br />

:raated by Philips and Sony to store large


1.<br />

1<br />

. . . . MIL-HDBK-850<br />

en~w###rf 600 myabytes) of digital<br />

mfmxCpc pits which canba<br />

read try a fsaer beam. Rasmrdad data cannot<br />

be erased or altered. CDROfd mrrpiies with<br />

the Yellow Book standard.<br />

compacted date-f)igital data that have<br />

been reduced In votuma using a bssless<br />

technique. Lossless means no information is<br />

bat arxt afl of the original data will be reaidenf<br />

when urpadmrt. ~hess techniques ara<br />

designed to remove radundanciaa and employ<br />

apadal techniques.]<br />

COSSIpSrStWO covor+JCS) CoveraOe of the<br />

earns area or ob@f taken at diierent times 10<br />

ahow any cha~as In detail. See also beak<br />

cover; cover; coverage.<br />

comparator baae-See field comparator.<br />

comparator—l. An Inefrumam or apparatus<br />

for maasurtrrg a dimension in terms of a<br />

standard. 2. A precision optical instrument used<br />

to determine the rectangular coordinates of a<br />

point with respect to another poinl on any plane<br />

surface, such as a photographic plate, 3.<br />

(surveying) An instrument for cornpsrino<br />

standards of lar@h: for suMtiidhg such<br />

standards: or Ior determining a standard length<br />

ot measuring devices (bar, tape, etc.). See also<br />

tleld comparator; monocomparator;<br />

eteroocompsrator; Valsala comparator;<br />

vertical comparator.<br />

compass amplltude-Ampfitude relative to<br />

compaas aast or west. See also ampllkrde.<br />

compaas bearing—l. (navigation) Bearing<br />

relatffe to compass north. See also mognetlc<br />

bearing, definition 1.2. (surveying) See<br />

magnetic baarlng, definition 2.<br />

compass Index error—The Instrument error<br />

in the magnetic beadrrg given by readings of tha<br />

needle.<br />

compass norsfs-(JCS) Tha uncorrected<br />

direction indicated by the norfh-sseking end of a<br />

compass needle. See also magnetic north.<br />

[Compasa north and magnetic north differ<br />

in that the former may be determined by other<br />

influences than the Earih’e magnetic Iiald.]<br />

compass roaa+JCS) A graduated circle,<br />

usually marked in degrees lndicatin~ directions<br />

and primed or Inscribed on an appropriate<br />

medium.<br />

compass rula-A melhod ot balancing a<br />

traverse survey. Corrections cormmrdii to<br />

the closing errors in latitude and departure are<br />

d@ribulad according to the proptrrfbn (lar@h of<br />

line to lotal length of travarse). The compass<br />

rule is uaad when If & assumed that the cbshrg<br />

errors are as much due to errors in obsarvad<br />

anglaa aa to errors in measured diatancaa.<br />

compsaa surwsy-A traverse survey whbh<br />

reties on the magnatk needle for onenfhg the<br />

sequence as a whole or tor determining the<br />

baarings ot the fines indviclually.<br />

compass—An Ins;rumam for Irrdiialing a<br />

horisomal reieranoe dlrectbn relafiia IO the<br />

Eanh. see alao aperlodlc compass; aatro<br />

compaaa; Brunton compass;<br />

clrcumfsremor; dscllnatolrsr;<br />

declkrometer; Earth Inductor compasa;<br />

gyro compaae; gyromsgnetlc compass;<br />

tensatlc compsss; Ilquid hand compase;<br />

magnetic compass; peap sight<br />

compsaa; prismatic compass.<br />

compensated gsold—A surface derived<br />

from the gaoid by apptiiaiion of computed<br />

values of tha deflection of the vertical which<br />

depend upon the topographic and isos!atic<br />

compensation. Also called cogeold.<br />

compensating backslgfsts ●nd<br />

toraslghls—When backaiglst and foresight<br />

dislancea are aquai al a given poskion of a level<br />

insfnsment, the effects ot curvature, refraction,<br />

arsf lack of adjustment of line of sight (if bubble<br />

is Ieveied when taking a rod reading) are<br />

compensated for. Backsight and foresighl<br />

distances are ammonly comrolled by the use of<br />

pacing or atadia.<br />

compenaatksg base-line measuring<br />

aPPa ratus—A base apparatus having a length<br />

elemant composed of two metala haviW<br />

different coefficients of thermsl expanaion. so<br />

amanged and connected fhat fhe differamial<br />

expansion of tfs camponems will maintain a<br />

COnStant length of the elamem under all<br />

temperature conditions of use.<br />

compansatlng error—An error that tends to<br />

ottsef a companion error and thus obscsxe or<br />

reduce the affecl of each.<br />

compansatkrg lene-(photogrammef~) A<br />

lens introduced info an optical sysfem to wrrecf<br />

for radial dislortbn.<br />

8


I<br />

Componaatlon plate-(photogrammetry) A<br />

gfaae ptate having a surface ground 10 a<br />

pradalarmlrted shape, W irwartion in the optical<br />

system 0! a d~bithre primer or plotting<br />

lt?ammrem, to compensate for radiaj distortion<br />

Imroducsd by the camera lens.<br />

conspllrstlon hlatory-Complete Information<br />

RXJSfdiw the devefopmam of a map or chart, II<br />

explains pmbterne ertcarntered and their<br />

eotibn, and akfa in Simplifying the resaamh<br />

ad ansfyaia of aotmx rna~eriefs considered for<br />

cor@atfon or revision of other maps or chatta.<br />

The corr@atiin history contains information on<br />

the pfannlng iacfora, source materfals uillbwcf,<br />

control, arrnjMation methods, drafting,<br />

rtrpmdudkm, and edit pmcedurea.<br />

compllallon lnstructlona-Wrif ten directions<br />

deacriblno cartographic sources and their use in<br />

determining Inforrnalbn to be compiled.<br />

Compilalbn Inefrucfions are not to be confused<br />

with sfksdlicatione.<br />

MIL-HDBK-850<br />

compilation manuacrlpl-The originaf<br />

drawing, or group of drawings. of a map or chart<br />

as compiled or rmnstructed from various data on<br />

which cartographic and rels!ed detait is<br />

delineated in cobra on a atabie-base medium. A<br />

czw7rpIlaMm manuecripl may consist of a stngle<br />

drawing Calied a base manuscrlpl, or<br />

because of congestion, eeveral overtays may be<br />

prepared showing vegetation, relief, names, arwd<br />

other Irrfofrnalion. Since the latter is usually the<br />

case, the baae and Its approprkle overfays are<br />

collectively termed the compilation<br />

msrnuacrlpt.<br />

compilation scala-The scale at which a<br />

map or charl is delineated on the ork@al<br />

manuscript. Th”b scale may vary from that of the<br />

rapmducfiin scale.<br />

Compllatlon-1. (JCS) Selection, assembly,<br />

and graphk preaentatrnn of atl reievam<br />

Inforrnafbn required ior the preparation of a<br />

map or chart Such information may be derived<br />

from other maps or charts or fmm other sources.<br />

2. (photogrammetry) The production of a new or<br />

recompiled map, chatl, or relaled product from<br />

aartal photographs and geodetic control data by<br />

use of photogrammetric instruments. Also called<br />

photogrammotrlc compllatlon;<br />

●tereocompflallon. See also<br />

recompilation.<br />

compftad map-A map incorporating<br />

Informalbn collected from varbus sources; not<br />

49<br />

@JmPfl~ fmm ?.wey data made for the map In<br />

question.<br />

complex faaturo—sae faature.<br />

component-l. One of the parts fnto whkh S<br />

vecior Wantiiy can be diitiad. For exarr@e, fhe<br />

Earth’s magnetic force at any poinf ran fxr<br />

dMUad LWo horfxontsf aM vertical co~nents.<br />

2. One of the parts of a complete system. See<br />

also conetltuent.<br />

compoalta alr photography-(JCS) Alr<br />

photographs made wfth a oamera hevfn9 one<br />

principal lane and two or more aurroundii and<br />

obfque tenses. me several rasufting<br />

phonographs are corrected or tranafonnad In<br />

printing to permit assembly aa verfkafs wlfh the<br />

same scale.<br />

compoalte faature-A feature composed of<br />

several related Ieaturea. See also<br />

superfaature.<br />

compoelte prfnf—See composite.<br />

composlMr-Reproduction from a successive<br />

series of images. A proof made by exposing<br />

color separation negatives one after the other<br />

on e single sheet of paper. fJsad in checking<br />

and editing. Also csiled Compoafte prfm. See<br />

also color composlta; color proof; Uouble<br />

burn.<br />

compound frarmonlc moflorr-The<br />

projection of two or more uniform circular<br />

rrmfione on a diameter of the ckcfe of such<br />

motion.<br />

compound pendulum-Any actual<br />

pendulum, A compound pandutum may be<br />

considered as composed of an indefinltety large<br />

number of material patitcles, al dflerenf<br />

distances from the center of SUSpS@On, each<br />

constituting a simple perrdutum. The ptrrbd of<br />

vibration [osclflation) of fhe corrpmmcf<br />

pendulum may be taken as a rssuffam of the<br />

periods of the simple pendulums of wlrich f! is<br />

composed.<br />

Compreaaed Aeronautical Chafi (CAC)-<br />

A data base of processed Arc-Second Raster<br />

Chart (ARC) Digitized Reeler Graphics (ADRG)<br />

data produced by the U.S. Navy, and dietrfbuted<br />

by DMA. ADRG digital map Images are<br />

converfed from the Equal ARC system frame of<br />

reference into fhe Tessellated Spheroid ModelfV<br />

(TS) projection uslrw a sfine ftf. The TS dafa<br />

are fhen compressed by a fader of


4<br />

approximately 4S:1.<br />

, MIL-HDBK-B50<br />

(hmprossed Rastsr Graphlca--A data<br />

base of pmcassed Ewaf Arc-Semnd Ras\er<br />

ChmfA@ (ARC) Dighixed Raster graphka<br />

(ADRG) data devatoped lor the Army, and<br />

producad and dkfribufed by DMA. CRG is<br />

Intended to be tfta Army% map fsackground<br />

standard, taqy3tad at bafflefiefd waapon and<br />

command and conlrol systems where typically<br />

data storage and dkspfay device capabffiiies are<br />

Ifmifed. Tha CRG producfbn Iechnfque<br />

cmTmmsaa full reeolutbn 24 bft, 254 dpi ADRG<br />

on CD-ROM to 4 bft, 127 dpl tor a cu~eseion<br />

factor of 24:1. CRG dafa on CD-ROM wifl<br />

contain appmxknafety 100 TLMs, 6 JOGS, and<br />

1 ONC over the same geograph~ araa.<br />

compraeelon retlo-A ratio of digital storage<br />

savings avalfable by compressing data.<br />

comprasslon-1. A method of reducing the<br />

WMume of dffhal data such that the dafa can be<br />

restored (dem~ressed) to ffs offginal !orm.<br />

Loasless Compression (e.g., run fenQIh<br />

erksdng) retains all the information contained<br />

in the data prbr 10 compression. Lossy<br />

comPre=iOn (e.g., vector quamizalion) causes<br />

some radocfiin in the irrfomratlon wnfenl of the<br />

data. 2. See flattening (of the Earth).<br />

computed attitude-Altilude determined by<br />

co~tafbn, table, mechanical computer, or<br />

graphics.<br />

computad azimuth angleAzimulh angle<br />

determined by computation, table, mechanical<br />

device, or graphics for a given pface and time.<br />

computed bearing-8earing anglas<br />

determined by com~tation from known<br />

bearings.<br />

computod data mathod—A mefhod of<br />

I’SCfffiiOn wffh an wtofocua rectifier whereby<br />

Wf exfating in an aerial photograph k computed<br />

and, from these computations, the instrument<br />

SWtlfIgS are established mathematically,<br />

RecfUicaUon k then amompfkhad without<br />

furfhar comparison to Iemplata or other gukle<br />

base.<br />

ComDular Aldad Daalan/Draltlnn/<br />

Compular Aided Man~facturfna-<br />

(CAD/CAM)—The use of computers fo design<br />

ard prockxie a producf.<br />

computar aldad deaian (CAD)-Software<br />

with the capebifily 01 asskting Iha operator 10<br />

perform standard enaineerfng and archifech.rre<br />

design functions. CAD aenerafly Invokes fayers<br />

of dala consisf@ of grephlc pfimfthres and<br />

bfock of data.<br />

computer aldad mstppfna (CAiU)-<br />

Software with the capability of aeekflng the<br />

operator 10 perform standard mapping<br />

functions. Afso known as Compufar M!sted<br />

Mapping.<br />

computar aaslelad cartography (CAC)-<br />

The uae of automated Techniques in mep/charf<br />

production.<br />

Computar aaafefad drafflna (CAD)-<br />

Sdfware which provides capatilifiea tor drawing<br />

graphic primitives,<br />

computer aeslsted drafting/dealgn<br />

(CADD)—See Computer Aldad DesIan;<br />

Computer Assfatad Drefflna.<br />

computer aselated manufacturlna<br />

(CAM)-The use of mm~tara in<br />

manufacturing,<br />

computer code-l. Swrce code, the text o}<br />

Instrucflons of a compufar program (usually In a<br />

high level language). 2. ~jecf mcdufa, e<br />

compiled veraion of the source code, R is<br />

macfrine readable, I.e., in binary.<br />

computar compatible tapa (CCT+<br />

Magnetic fape containing data in mmpufar<br />

raadabla digilal format. Genarally data is<br />

recorded as 6250 or 1600 blls per Inch @pi).<br />

concava lana—See naaatlva lane.<br />

concapt of operatlona (CONOPS)—(JCS)<br />

A verbal or graphic atalement, in bread outline,<br />

of a davaloper’e or mmmandera assumptbna<br />

or intern in regard to an operation or ser% of<br />

operations. The wrwept of operations la<br />

frequently embodbd in campaign pfans and<br />

operation plans; in the fatter case, parflcularfy<br />

when tha plans cover a sarfas of mnnacfed<br />

operations to be carried out simuffanaousfy or In<br />

succession. The concepl is designed to giva an<br />

overall picture of the operation. It k Included<br />

primarily for additbnal cfarfty of purpose.<br />

Frequently, ff is referred to as oommandera<br />

COnCOptor CONOPS.<br />

concludad anola—(trfangufafion) The third<br />

angle of a triangle. not measured, but<br />

50<br />

,.


I<br />

I<br />

cWrSPISI@ from the two other angles.<br />

.,, >.. MIL-HDBK-850<br />

condlllon aqusstlo*A set of adjustment<br />

e~afkms wherein afl variables representing<br />

parameters heve bean eliminated hum the<br />

equations, leaving only variables representing<br />

the acfjusfmatis to the observed quantities in<br />

the equations. A least squares adjustment<br />

e~ying this type of equations is said to be by<br />

fhe mmliiicn melhod, as opposed 10 the<br />

obaefvafion method or variallon ot parameters<br />

method. Nole that it it is desired 10 albw a<br />

previously established parameter to adjust,<br />

ralher than hold if rigidly fixed, ii should be<br />

mnsMerad as an observation with an<br />

appropriate wefght. See also angle<br />

equation; azimuth ●quailon; correlate<br />

●qwstlon; Iatltude equation; Iengtfr<br />

equation; Iongltude equaiicm; normal<br />

equation; obarsnratlon equation;<br />

perpendicular equation; side equation;<br />

aide equetlon taafa.<br />

condltlona-A Iarm used in adjustment<br />

=mWMations 10 define parametric requirements<br />

01 adjusted redundant observal”bns.<br />

cone engle bsndlng—Technique used in<br />

-. analytical phologrammetry tor reducing<br />

mensuration requirements on a ptrotographlc<br />

plate by segregating Images into annular zones<br />

defined by specific bands subtended, usualiy by<br />

5“ of erc. Areas read are then only in certain<br />

outer bands depending on the calibration of the<br />

lens mne.<br />

confidence intewal—A statement of<br />

accuracy beesd on a statistic whose distribution<br />

twwfion is known; e ,g., the normal distribution<br />

function or bivarfate normal distribution function.<br />

Errcva are sfatad ae some percentage of the<br />

total probability of 100 percent; e.g., a 90<br />

percent assurance level. Also called<br />

aasurence level; arror Intanral;<br />

probability Interval.<br />

contlQuratlon management (CM)—A<br />

procedure for applying technical and<br />

admlntafrative dkaclbn and surveillance to (a)<br />

klenttty and documem the tuncfional and<br />

physical charecterist!cs of an Item or system, (b)<br />

mnfrof any changes to such charecferistics and<br />

(c) ramrzf and report the change, process, end<br />

lmpfementatbn status, The CM process must<br />

be carefully telbrad fo the capacity, size scope,<br />

and phase of Ihe Me cycle, nature and<br />

Complextiy of the system Involved.<br />

‘51<br />

configuration of terrain-see topo.<br />

graphic expreealon.<br />

contormal charf-A charl on a wnformal<br />

projection.<br />

conforfrral map projection-A map<br />

pro@tbn on which Ihe ehapa of any emall area<br />

of lha surtaca mapped is preserved unchanged,<br />

arxf all angles around any point are mfredty<br />

represented. Also celled orfhomorphlc SISap<br />

projection.<br />

conic cherf with two standard parallela—<br />

A chart on the mnic pfojacflon with SW standard<br />

parallels. Also called S@Cant Conic chart.<br />

conic ChaII-A chart on a mnic pruject”on.<br />

conic map projection wl!h two standard<br />

paraflela-A conic map projection in which lhe<br />

surface of a sphere or spheroid, such aa the<br />

Earth, is conceived as developed on a cons<br />

which inlarsects tha sphere or spheroid atong<br />

two standard parallels. The Lambd conformal<br />

projection is an example. Also called ●ecent<br />

corslc map pro]ectlons.<br />

conic map projactlon—A map projection<br />

produced by projecting the geographic<br />

mer”tiians and parallels omo a mne whtch ie<br />

tangam to (or intersects) tha wrlasa of a<br />

sphere, and then davebping the mrra thto a<br />

plane. Conic map projections may be<br />

wnsidered as including cylindrical map<br />

projection when the apex of the mne is at an<br />

infinite distance from the sphere, and<br />

projections on a tangem ptane when that<br />

distanca la zero. Conic map pmjactbns may be<br />

Illustrated with a single mne which is tangent to<br />

Ihe sphare or which cuts the sphere abrrg two<br />

parallals; or they may be a series of tangent<br />

cones. all with apexes on an extenabn of the<br />

axis of the sphare, at mnstantty incraasi~ (or<br />

decreasing) distancas from tha sphere. Itis best<br />

ueed to show areas of large bngitudlnal rather<br />

than latitudinal distances. Also called tanOant<br />

conical map projection.<br />

conJugate dlsrtancea-Ttre corresponding<br />

dislances o? otzjacf and image from the nodal<br />

points of the lens.<br />

conjugate Image pofnts—See correapondlng<br />

Image polnls.<br />

conjugete Image raya-See corree-


I<br />

pondlng Image rays.<br />

,,. . MIL-HDBK-B50<br />

cofrjtxgate ~lrrte-The oblecf and Image<br />

poims in an optical system. They are physically<br />

retetad according to the definition for<br />

conjugate dlstencee.<br />

cortjunctiorx-llte alfuefion of two celestial<br />

bodies havhtg the same celestial longitude or<br />

the eerrw sidereal hour angle. See eleo Irrferlor<br />

conjuncilon: opposttton; euperlor<br />

conjunction.<br />

corrnectlng travairea-A traveme which efada<br />

and ends et separate ~ints whose relative<br />

positions have been determined by a survey ot<br />

an atpmi- or higher-order ot accuracy.<br />

@n8Meff@ lees eubjecf 10 undelecfad error<br />

than a bop traverse,<br />

connection-(geodesy) The systematic<br />

elimination of discrepancies behveen adjoining<br />

or overfspplrrg trian@ation networks for the<br />

purpose of establishing a common framework<br />

from whkh bng-renge measurements can<br />

betaken.<br />

connectlvlt y rinslysle-1. Analytical<br />

technique 10 dalermine whether a set of peirrts<br />

(nodes) or lines are rnnnecked to each other.<br />

2. (GIS) Function used to predict or track<br />

ruutings through a nslwrxrk.<br />

conaecutlva mersrt-A arnoothed<br />

represenfatkm of a time series derived by<br />

replacing each obsewed value with a mean<br />

value Cmrqxrfed over e 6electad imerval.<br />

Consecutive means are used in smooming to<br />

atimlnate unwarned psrfocficitles or minlmlze<br />

irregular variations. Aiso called moving<br />

averege; overlapping meen; runntng<br />

mean.<br />

Consol chert-A chart showlrrg Consol lines of<br />

position.<br />

Coneot-(.fCS) A brrg-range redo aid 10<br />

navigation, the emissions of which, by means of<br />

Iheir radio traquency rnodulatiin characferisfba,<br />

enable bearings to be determined.<br />

conatent ●rror-A systematic error which is<br />

the 6ams in both rnagnltude and s!gn<br />

throughout a given eeria6 of observations, such<br />

aa an Indax error of an instrument, See also<br />

accumulative error.<br />

conatent of abarratlon—The maximum<br />

aberration of a star obeawed from the surface of<br />

52<br />

the Earfh, 20.496 seconds of arc.<br />

conetant of gravitation-The ropottbnallfy<br />

taclor (equal to 6.67 X 10-5 rr$kd sac+) in<br />

the universal law of gM*tiOn; i.e., every<br />

panicle of matter attracts every other pertWs<br />

with a force mat k directly pmportbnel to the<br />

product of their masses and Inversely<br />

prmporfbnal to the square of their dietarme<br />

apart. Also called gravitational Conetant;<br />

law of unlvertxal gravitation.<br />

constant pressure chert-see Iaoberlc<br />

chart.<br />

conetellatlon-lm orbital group of Q3tellifas,<br />

e.g., Iha Global Posltbning Syslem(GPS).<br />

conetltuent day-The duration of the Earth’s<br />

daily rotation relafiie 10 a ficffilous efer Mrich<br />

reprasants one of the perbcfk fiie-pmducirtg<br />

forces; it approximates the length of the funar or<br />

solar day and corresponds to the period of a<br />

diurnal constituem of twke the period of a<br />

semidiurnal constituent. The term is rot<br />

applicable to the iong-perbd conetffuams.<br />

constltuant-ne ot the harmonic elements<br />

in a mathematical expre66ion for the tide- . . .<br />

producing force and in the cvrretpnding<br />

iormulas Ior the I’de or tidal current. Each<br />

censtituenf represents a periodic change or<br />

variation in the reieiive positions of the Earth,<br />

Moon, and Sun. Also called aetronomlc tldel<br />

constituent; harmortlc constituent;<br />

partlel tide; tlsfal constituent. See also<br />

component; diurnal conetltuent:<br />

xsemldlurnal conetituarrt.<br />

contect berse-llne rneaeurlng<br />

aPParatua—A base apparatus composed of<br />

bars whose lengths are defined by the disfarce<br />

between their end faces or points. M use, the<br />

bam are laid end to end, one bar balng kept In<br />

pesition while another bar is bairrg rnovad<br />

ahead,<br />

contect glaea—See focal plane plate.<br />

contect pleta-See focal plsne plata.<br />

contact printer—A device which provides a<br />

light eource and a means for hotding the<br />

negetlve and the senaifive meteriai in WntaCf<br />

during exposure. Also, a spaclallzed device for<br />

exposin~ diapxifive plates at the same scale aa<br />

that of the negaflve.


i<br />

..- MIL-HDBK-850<br />

COntOCt pttntlna frama-in photography<br />

and plafemaklng, a device for holding the<br />

negative and rhe sensttive material In contact<br />

during exposure. The fiiht source may or may<br />

not be a separate elamenf. II the frame<br />

mrrtains a vacuum p..wrrp10 exhaust all air<br />

within the frame to insure perfect ca’rfacf<br />

between the negative and lhe sensitive<br />

nzateriai, It is known as a contact vacuum<br />

prlrttlng frame.<br />

COntaCf prlnl—(JCS) A print made frum a<br />

negative or a diaposttive in dkecf mnfacf with<br />

sanaifizad materiai.<br />

contact screen-l. A hafffone scraen made<br />

on a film basa and used in direct mnfacf with<br />

the flim to obtain a haffrone image from a<br />

oominuous tone original. 2. A pattern image on<br />

a fiim base contact wtfh an open window<br />

negative 10 obtain a pattern image on film or<br />

piate. See alao area pattern screen;<br />

magenta contact acreerr.<br />

contact she-in rapmduction, printing to the<br />

same size ss the original. Also called ona-loone<br />

(1:1) copy. See also scale of<br />

roproductlon.<br />

COntacl slide baae-llne measurlrrg<br />

apparatus-A modified contact base-line<br />

measuring apparatus consisting of two aleel<br />

measuring bars (rods), each 4 malers in iength,<br />

so rnoun16d that contact is effacted by<br />

wincidence of Jines on a md and a mntact<br />

sfiie. Each md torrns a metallic therrnomater<br />

with two zinc tubes, one on aach side of the bar<br />

OPPOSffe aIZCfSof the bar arv fastenad to the<br />

ends of the tubes, the other ends of which are<br />

free to move with changes of Iemperalure.<br />

contact vacuum prlntlng frame—See<br />

contact prlntlng frame.<br />

contact vsrnler—The usual type of vernier,<br />

having the vemiar acaie and the graduated<br />

circle in physical cmntact.<br />

contiguity snelysia-An anaiyticat technique<br />

to determine whether a set of areas (polygons)<br />

are situated naxf to aach other. Sometimes<br />

referred to as adjacency analysis.<br />

continental control natwork (CCN)—A n<br />

accurate network of mntrol points established<br />

over a large geographic area.<br />

53<br />

contlnuoua prOC8S410f-(JC5) Equipmant<br />

which processes fifm or paper in rmmirascas<br />

strips.<br />

Continuous Strip camera-(JCS) A camera<br />

in which the fiim moves continuously past a s~t<br />

hr the focaf plane, producing a photograph In<br />

one unbruken length by virtue of the cominuous<br />

torward motion of the aircraft.<br />

conthruous ●trip photogrttphy-iJCS)<br />

Photography of a strip of terrain in which tha<br />

image remains unbroken throughout ffs tengfh<br />

along the line of flight.<br />

Continuous tOn9 gmy SCSIS-A acaie of<br />

tones tmm white to black or fmm transparartf to<br />

opaque, each tone of wh’ch blends<br />

imperceptibly into fhe next without vislbie lexfure<br />

or dot formation. Also calied continuous<br />

wedge. Sea also step wadge.<br />

continuous tone-An Imaga which has not<br />

bean screened and contains unbroken, gradient<br />

tones fmm black lo white, and may be aither in<br />

nagative or pesitive form. Aeriai photographs<br />

are examples of continuous tone prints. See ,, ..,.7<br />

also haittona; line COpY.<br />

continuous wedge—See continuous tone<br />

gray scela.<br />

contour fhrder—A sfereomapplng instrument<br />

of simpie design for use with photographic<br />

prints. This instrument does not pmvkfe a<br />

method of compensating for acaie changes in<br />

dfferenf parts of the model rasufting trom<br />

differences in retief.<br />

contour fntarval-(JCS) Difference in<br />

aievation between two adlacem contour fines.<br />

[Omasionalty, fhe Imervai may vary wtfhin an<br />

individual sheet,] See aiso variable contour<br />

Interval.<br />

contour ilne-(JCS) A line on a map or chart<br />

connecting paints of aquai alavatiorr. Sae also<br />

accurate contour; approximate contour;<br />

carrying contour; dsprssslon contour;<br />

depth contour; form Ilnes; gaoidal<br />

contour; Indsx contour Iins;<br />

Intarmedlats contour ilne; sea Isvsl<br />

contour; supplementary contour.<br />

contour map-A Iopographlc map which<br />

porlrays reiief by the use of mnfour lines.


I<br />

,., . . MIL-HDBK-B50<br />

contour eketctstng-Freehand definealion of<br />

the wrtece refiif on a map as seen in<br />

PSr6P@~e view, WI COmmll@ by bcations on<br />

the rnaIz corresooncthm to salienf rninfs on the<br />

ground’. -<br />

COntOUr walue-A numerical value placed<br />

upon a czmfour tine to denote ifs alevation<br />

refetiva 10 a given datum. usually mean sea<br />

level.<br />

contour-An imaginary fine on the ground, all<br />

points of which are at the same elevation above<br />

or below e apecitied datum surface, usually<br />

mean sea level.<br />

contract-(pholooraphy) The adual ddfarence<br />

In densffy between the higfrti~hts and the<br />

shadows on a nagafffe or positive. Contrast is<br />

not mrtcemed WISII me magnitude ot density,<br />

bul only with the difference in densttiee. Also,<br />

the rating of a pholographt material<br />

corresponding to the relative density difference<br />

which if exhibiis. See also characterlatlc<br />

curve; density, definition 1.<br />

control berse-A surface upon which the map<br />

projection and ground control are p!dted and<br />

upon which templales have been assembled or<br />

aarolriangulation has Imen accomplished and<br />

the control poims thus determined have been<br />

marked.<br />

Control data card—A card containing<br />

poshional data and descriptions of individual<br />

horizontal and/or vetiisal control points, Also<br />

~sl~d geodotlc data street. See also trig<br />

control tllght—See control strip.<br />

COntrOl marking—A note or other term of<br />

caveal shown on an MC&G product indicating a<br />

need for special handllng and tor controlled<br />

dissemination.<br />

control net—See aunrey net,<br />

control pohrt photography— Electronically<br />

mnfrollad aerial photography mnslsling of four<br />

flight lines fbwn in a cloverleaf pattern from the<br />

four cardhal diredions and with the filghls<br />

intersecting over a target or secondary mmrol<br />

point.<br />

COntrOl point— 1. Any station of known<br />

Coordlnales in a horizontal or vertical confrot<br />

network that Is identified in a data sel or<br />

54<br />

photograph and used for cwrelating the other<br />

statkon data The term is uaualfy mortified to<br />

retlect the type or purpose, such es ground<br />

control point, horizontal control polm,<br />

photocontrol point, picture control<br />

point, and vertlcel control point. See also<br />

control station; secondary control point;<br />

aupplamantal control point. 2. (JCS) A<br />

point located by ground suffey with which a<br />

rnrresponding point on a photograph is<br />

matched, as a check, in making moeaics.<br />

control station-An obIed or mark on tha<br />

grouti of known poeifikzn or alevatkon, or both,<br />

in e network 01 ground corrtml, Control stafiins<br />

constitute the tramework by wh!ch map detalfs<br />

are fixad In their correct positbn, azlmufh,<br />

elevation, and scale with respect to the Eerlh’s<br />

surface. Also called ground control point.<br />

See also control point. ‘<br />

control atrlp-(aerial photography) A strip of<br />

aarial photographs taken to aid in planning and<br />

accomplishing later aerial photography, or to<br />

serve as control in assernbting other strips. Also<br />

called control flight; tie flight; lle strip.<br />

See elSO crose-fllght photography.<br />

control eurvey cleeelrlcatlon-A aeties of<br />

designations 10 classily control surveys<br />

according to their tield survey methods and<br />

accuracy, The highesl prescribed order of<br />

control survays is designated first ordar; Ihe naxr<br />

lower prescribed classlficalion, second order;<br />

etc.<br />

control survsy-A survey which provides<br />

positiine (horizontal acd vertical) ot poinls to<br />

which aupplememary surveys are adjusted. The<br />

fundamental axrtrol survey of the United States<br />

provides the gaographc positions and plane<br />

coordinate of triangulation and traverse<br />

stations and the elevation of bench make<br />

which are used as the bases for hydrographies<br />

surveys of the coastal waters, for the control of<br />

the topographic survey ot the Unhed States,<br />

and for the control of many state, city, and<br />

prlvale surveys.<br />

control-atatlon ldentlflcatlon—See<br />

photoldentlflcatlon.<br />

controlled map-(JCS) A map with precise<br />

horizontal and verl!!al ground control ae a basis.<br />

Scale, azimuth, and elevations are accurate,<br />

See also map.<br />

controlled mosaic—(JCS) A mosaic


,,<br />

I<br />

‘1 I<br />

I<br />

-.,,.::-:.<br />

co~ected for scale, recttiled, and fskt to ground<br />

corrtml to provide an acwrata represemalbn of<br />

dletancas and diracfbn. See also mosaic;<br />

somlcontrolled moaalc; uncontrolled<br />

moeetc.<br />

COtTtrOlllng depth—The Iaast dapth in tha<br />

qroach or channel to an area, wch as a port<br />

or anchorage, governing fhe masimum draf! 01<br />

craft fhaf can enter.<br />

control-t. Previously esfabllshed posiiions<br />

ardor ortentalksn data used for determining<br />

addffbnsl ~sifbn data used for diecrsle<br />

to~phk polnfa, or for oonfrolllng<br />

cartegraphc rapreaanfations 10 tha specifiad<br />

datum. 2. A mllacfive term for a ayafem 01<br />

marks or ol$ecfs on the Earth or on a map or a<br />

photograph, whose positions or elevation, or<br />

both, hava been or will ba determined. See also<br />

eetronomlc control; basic control;<br />

common control; olactrorrlc control;<br />

geodetic control; ground control;<br />

trorizontel control; La place control;<br />

Iavel control; photogrammetrlc control;<br />

recover; sterlhtg control; supplemental<br />

control; verflcal control.<br />

conventional International otlgln (CIO)—<br />

The average terrestrial pole of the perbd 1900<br />

fo 1905. Olsen used as tha origin to which the<br />

coordnataa of the instantaneous pole of<br />

rotation of the Earth ara ref errad, In 1967, fhe<br />

IUGG recommended that the C)O be usect to<br />

define the direcfjon 01 the geodetic north pole.<br />

Abbreviated to OIC In French pubticatbns. See<br />

also everage terreatrlal pola.<br />

convergence conetant-Tha angla at a<br />

L?ivanIathuda between merktians 1” apart.<br />

Somatlmas loosely called convergency, a<br />

larm whkh more propsrfy Is the equivalent of<br />

convergence.<br />

convergence of merldlena-The angular<br />

drawing togathar of tha geographic meridians in<br />

passing from Iha Equator 10 the poles. A! the<br />

Equator, all meridians ara mutually parallel;<br />

pasaing from the Equator, they converge until<br />

thay maet at tha polas, Infereecfing a? angles<br />

that are equal 10 their differences of Iongifuda,<br />

The tarm converganca 01 marldlana la<br />

usad to daslgna!e also Ihe relative difference of<br />

direction of merWan6 al Speclfk points on lhe<br />

meridians. Thus, for a geodatic Iina, the azimuth<br />

@f one end differs from fire ezimufh al the other<br />

end by 180° plus or minus Ihe amounl of fhe<br />

oarrvergence of the merldlans at fha and points.<br />

‘MIL-HDBK-850<br />

convergent camara—An assetily of two<br />

aertal cameras which take .sknultaneous<br />

pfzofogmphs and nsaimain a fixed angla<br />

between their opfkal axea. The eflact is to<br />

increasa tha angular covarage in one diracfbn,<br />

abng the longitudinal asis of fhe aircraft.<br />

convergent model deturrr-See model<br />

detum.<br />

convergent photography- Photograph y<br />

taken with a corwergenf camera. In<br />

photogrammewy. the angle of wrwergance of<br />

the two lenses asas Is usually 40” mainfainirrq “a<br />

1:1 base-height ratio. I<br />

convergent poaltlor+A split camara<br />

installation so positioned that fha plane<br />

containing the camera axis is parallel fo lhe line<br />

of ftiiht.<br />

converging lene—See poaillve Iena.<br />

conversion angle-(JCS) Tha angle batwaen<br />

a greatdrcle (orfhodmmk) bearing and a rtwmb<br />

line (Ioxodromic) bearing of a point, measured at<br />

a commen origin. ,. ... . . .<br />

converalon fnctor—A quantify by wfslch the<br />

numerical value in one system of untts must be<br />

mutfiplied 10 antve al fhe numarbal value In<br />

arsolhar system of units.<br />

conversion acala-(JCS) A scale Indksling<br />

the ralatlonshlp between two diffararrt urrffa of<br />

measurement (e g., maters to Iaet). See also<br />

acele.<br />

convaralon—The changing 01 ona aystam of<br />

meawreman! to another; e.g., converting<br />

meters to feet. Conversbn Is usually<br />

accomplished by the use of conversion factors,<br />

scales, and tablas.<br />

convarflbla lens-A lens containing tsm or<br />

more elemants which can be used individuality or<br />

in wmbination.<br />

convex lana—See positive Iene.<br />

cooperaltve mapping agreement— A<br />

formal agreemem between nafional<br />

govammaMs speclfylcg responslblllfles for<br />

MC&G ecfivities such as procuramenf of aerial<br />

photography, execution of gaodelic COIW’01<br />

suweys, and production of maps, charts, and<br />

55


;<br />

[<br />

related products. See also map exchange<br />

agrooment.<br />

MIL-HDBK-850<br />

coordlrreto exsra-in a rectangular coordhrata<br />

system, the eses of reference which intersacl at<br />

right angles srtme polnf.of ortgin.<br />

coordinate Converalo-hanging the<br />

comdhtafe vahses from one type to those of<br />

amlher wfrh the coordinate reference systems<br />

or datuma rul changing; e.g., geographic<br />

coomfinatas to Transverse Mercator grid<br />

rmcdhates.<br />

coordlrtate pair—A sat of Cartesian<br />

coordinates describing the Swodimenabnal<br />

bcatbn of a poim, line, or areas (@ygon)<br />

Ieetura In relatfcn to the common Ccor’dktate<br />

systems of the data base.<br />

coordlnata protrectrsr-A square-shaped<br />

protractor having graduations on two adjacent<br />

edges wtih the cemer al one comer. II is<br />

equipped with a movable arm turning about the<br />

center, and graduated to show linear quamities<br />

on a given SCAE. The protractor is covered wlrh<br />

a grtd of the same scale ami units as the arm.<br />

coordinate ratemrrca notetlo’n~Grid<br />

coordinates are gfvan In terms of linear<br />

measurement in meters. Gecgrephlc<br />

wordfmtes are oiven in tams of annular<br />

measurement, u-wally in dagrees,-mlflutes,<br />

Secands but occasionally in grads.<br />

and<br />

coordinate ralerence notellon—G rid<br />

caordirrates ere given In Ierms of linear<br />

measurement, usually meters but occaaienally<br />

in yards, feet, or olher units. Geographic -<br />

coordinates are g’wen in terms of angular<br />

measurement, usually [n degrees, minutes, and<br />

seconds, but ccoasionslly in grads.<br />

coordinate trarmformatlon—1. A<br />

mathematical or grsphk process of obtaining a<br />

rmdified set ot coordinates by eoms<br />

cornblnalbn of rotation of coordinate axes al<br />

their point of origkt, tranafocetion of the point or<br />

orfgln, rmditicetien or scale along coordinate<br />

axes, or change of the size or geometry of the<br />

reference ~ace. 2. The set of parameters used<br />

to accornpfbh this process. See alsa aftlna<br />

tranaformatlon; Cfrrtealan coordlnataa;<br />

datum tranalormetlon; rectlflcatlon;<br />

UnlVer8al Polar Stereographic grid;<br />

Unlvemal Tranaverae Mercator grid.<br />

Coordlnatad Unhremel Time (CUT)—AISO<br />

56<br />

called unlvemal tlmrr coordlnatrrd (UTC).<br />

See lfnlvemal Tlma.<br />

coordlnatad aertas-A saries ot<br />

gaographkelly integrated target charts and<br />

other graphics of a unftorm scale and format<br />

devebpsd to provide continuous and tort’plete<br />

coverage of a large area. Also called earlea.<br />

coordlnetas+JCS) Linear or angular<br />

quamities which designate fhe position fhat a<br />

point occupies in a given reference frame or<br />

syslem. Also used as a general term to<br />

designate the particular kind of reference frame<br />

or system, such as PISITS racta~utar<br />

coordinates or spherical coordhatea. See efao<br />

aaaumed plene coordlnatea; ●atronomlc<br />

Coordlrratea; Carreslan coordlnrrtos;<br />

celeetlal equator system of coordlnatea;<br />

chromattclty coordinate: Curvlllnaar.<br />

coordlnetee; cyltndrlcel coordlnatest;<br />

Earth-fixed coordinate syetem; ●cllptlc<br />

system of coordlnetea; gatactlc syetem<br />

of coordinates; gaocentrlc coordinate;<br />

geocentric geodatlc coordhrataa;<br />

gaodatlc coordlrrataa; gaogrsphlc<br />

Coordlnatas; geomagnetic coordinates:<br />

grid coordlnatea; grid coordinate<br />

X@thm; Oround-epace coordinate<br />

ayatem; horizon ayetem ot coordinates;<br />

hour engle eystem (of coordlnataa);<br />

lnertlet coordhrete system; local<br />

coordhrate system; model coordinetea;<br />

Of Nlqua Coordlnatas; Orlgln of<br />

coordlnetes; photograph coordlnatea:<br />

plene potar CoOrdlnrXteS; plane<br />

rectangular coordlnatee; plate<br />

coordinates; polar Ooordlnatea;<br />

rectangular coordinates; rectangular<br />

space coordlrrates; ralatlve coordinate<br />

syetem; right eacsnelon ●ystem;<br />

selenocentrlc coordinates; epace<br />

coordlrrsles; space polar coordinates;<br />

spherlcel coordinates; state coordlrrate<br />

syetems; etrlp coordinates; topocentrlc<br />

coordinates; topocentrlc equatorial<br />

coordlnatea; unlveraaf apece<br />

rectangular coordinate syatam;<br />

Unlvereal Transverse Mercator<br />

coordinates: verrlcel coordinate.<br />

coordlnation+wrveying) The placing of all<br />

survey data on the same aocmlnale system or<br />

datum. Coordination does not hrrply the<br />

adjustment of obsemaIlons to rarrmve<br />

discrepancies. Two field surveys over the same<br />

area may be coordinated by computation on tha<br />

aama datum, but there may ramain between


.,. . . ---- MIL.HDBK-850<br />

them dbcrepancias that can be removed only<br />

by mrrelatlon.<br />

coordlnmoo mph-An Instrument used to plol<br />

In Ierma of plane mordiies, tt may be an<br />

Irdegral part of a afereoampfc pbtting<br />

Inatnsmant whereby Use p[anirnetrfc motions (x<br />

and yj of the fbatkrg mark are pbtted dkecfly.<br />

Afao called rectangular coordinate plotter.<br />

coplanar—Lying in the same plane,<br />

copy (Copying) CSSmen3-A preclalon camera<br />

used kr the laboratory for copying purposes.<br />

Also celfed process camera.<br />

x=py-me manuscript or text turnished for<br />

reproduction. See also continuous tone;<br />

line copy; tone copy.<br />

Corange llna-A ffne through points of equal<br />

tidal range.<br />

Confolla cormctlon-A correction applied to<br />

an assumed posftiin, celestial line of position,<br />

Cabstfd Ifs, or to a mmputed or obsewad<br />

attitude to allow for a~arenl acceleration due 10<br />

CWlelfs force.<br />

Corlolls force-See CoriOlls.<br />

Corlofie-A fbtifbus force used 10 explain the<br />

horizontal departure from a straight line of a<br />

movfrrg obpct on or near the Earth’s suflace<br />

caused by viewing the trajectory of the moving<br />

objed while the observer is stationa~ with<br />

respect to the rotating Earth, Ths ?orce- causes<br />

deflecflons 10 the tight In the Northern<br />

Hemisphere and 10 the left In the southern<br />

Hemkptsere Corblis derkct$ objects to fhe west<br />

tt they are moving loward the Equator and to<br />

the aaat tf they are moving away fmm the<br />

Equator. It atfacta air (wind) and water (current),<br />

and introduces an error In the bubbie sexlam<br />

obaervetbna made from a moving craft; the<br />

etfed imreasirrg wfth higher latitude ad greater<br />

apeed of the object. Also alfed Corlolla<br />

Force; deflecting Iorca.<br />

comer ●cceseorles-$learby physical objects<br />

to which cxrrnara are referenced for their tuture<br />

Mantlfiiation or restoratbn. Amessories Include<br />

baarfng tress, mounds, pffs, ledges, rocks, and<br />

orher natural features, to which distances or<br />

drOCfbnS (or both) from the mmer or<br />

monument are known, Such acceesorfes are<br />

actually a parl of the mcnumentatfcm See also<br />

boarlng tree.<br />

57<br />

corner johts-The bcation where three or<br />

more mntiguous map sheets coma tooather.<br />

corner merka-See regleter marka.<br />

corner tfcks-see raglster marks.<br />

corner-1. A point on a fend boundary, at<br />

which hvo or nsora txwwtary ffnes meal. 2. A<br />

poim on the surface of tha Earth, determined by<br />

the surveying procaaa, which defines an<br />

extremtty on a txrundafy of the putrffc fanda.<br />

Sae also ●uxiliary momrder cornor;<br />

GfOXlng oorneq ClOalng townehfp oornor;<br />

double corner.; ●xletent cornen found<br />

corner; Indicated comer; feat comer;<br />

meandar comer; obllleraied corne~<br />

quarter aectlon corner; quarter-quarter<br />

aactlon corner; section corner; slmeenffr<br />

eactlon corner; special meander corner;<br />

etandard corner; theoretical corner;<br />

township co”mer; witneee corner.<br />

corrected eatabllatxment-The mean high<br />

water interval tor all stages of the tkta.<br />

correction code-A code conaistfng ot tetrera,<br />

numbers, and symbols whfch are used to<br />

indica!e edn”mrractkms on’ maps or on overlays<br />

attached thereto.<br />

cormctlon for datum-A conveffifon factor<br />

used In the predkfion ot ties to reaotve the<br />

dillerence between chart datum of the reference<br />

and a secendary station.<br />

corractlon for Incllnatlon of tape-see<br />

grede correction.<br />

correction for Incllnetlon of the<br />

horizontal axis—A mrmctfon applied to en<br />

observed horizontal directfon to efimfnate eny<br />

error that may have been caueed by the<br />

horizontal axis of the instrument not ~fng<br />

exactky horizontal,<br />

cormctlon for mn of micrometer-A<br />

correction applled to an obsemcf raadfng of a<br />

Braduated circle made wffh a mfcromafar<br />

microscope to compensate for run of<br />

micrometer.<br />

Eorrectlon llne-See standard paraflef,<br />

definition 1.<br />

:orractlon nor lcee-A veriety of notfcea (e.g.,<br />

Nolice to Mariners, Notice to Airmen, errata


MIL-HDBK-850<br />

notices, chart updale manuals, target material<br />

bulletins, etc.) utilised 10 Imnemit correction data<br />

tiich the user apfiiis 10 an existing MC&G<br />

product.<br />

corracflon overlay—A transparent material<br />

on which edil cmrecfbns are noted. The method<br />

permits an Immediate bcation ot leaturas to be<br />

revised without the necessity o! marldng the<br />

drawing Or MSP.<br />

corractlon-A quantity, equal in absoluta<br />

magnitude but o~stte in sign to the error,<br />

added to a calculated or observed value to<br />

obta”m the true or adjusted value. See also erc<br />

correction; ●rgmentatlon corractlon;<br />

Bouguar corraotlon; clock correction;<br />

Corlolla correcflon; curvatura correction;<br />

dynamic correction,; dynamic<br />

temperature corractlon; eccentric<br />

reduction; E8tv6a csrrrectlon; fletd<br />

correction; free-elr correction; grade<br />

correction; height-of-eye correction;<br />

Index correction; Ionospheric Correction;<br />

Iatltude correction; Iangth correction:<br />

level correction; orrhometrlc correction;<br />

Polerls correction; rod correction; eag<br />

corractlon; aemldlamaler corracllon;<br />

slope correction; eurfaca corrections;<br />

tape corrections; temperet ure<br />

correction; tension correction; terrain<br />

corractlon; tidal correction; tlmlng<br />

correction; trensll micrometer contact<br />

correction; velocity correction.<br />

correlate aquatlon-An equstion derived<br />

horn an observation or rendition equation, using<br />

undetermined multipliers, and expressing the<br />

rendition that the sum 01 the squares ot the<br />

residuals (or oorrecfiins) reeufting trom the<br />

appliition of these muttipliira to the<br />

observation or conditiqn equstions shall be a<br />

minimum See also condlllon equal Ion;<br />

normel equatton.<br />

Correlarlon Tracking and Trlangulatlon<br />

(COTAT)-A trajectory measuring syslem<br />

Cowssd of several antenna base lines, aach<br />

separated by large distances, used to measure<br />

direction cosines to an object. From thesa<br />

measurements its apace position is computed<br />

by triangulation.<br />

correlation-1. (general) The statistical<br />

interdeperrde~e between two quantities (a.g.,<br />

in gsodasy, gravity enomalies are correlated<br />

with olher gravity anomafies, with elevation, with<br />

58<br />

elevation dtierences, and with geology, etc.). 2.<br />

(aurvaying) The removal of discrepancies thal<br />

axiet among survey dala so that all pane are<br />

interrelated without apparent error. Tha terms<br />

coordination @nd corralatlon are usually<br />

apptied to the harmonizing of auweys of<br />

adjacent areas or of dlffarenf surveys over the<br />

same eraa. Two or more such surveys are<br />

coordinated when they are computed on the<br />

same datum; they are correhted when they are<br />

adjusted Iogether.<br />

correspondence-( steraosmpy) The wndition<br />

that exists when mrrespotilng images on<br />

a pair of photographs lie in the same epipolsr<br />

plane: the absence of y-parallax.<br />

correapondlng Imege polnta-The ImaQes<br />

on two or more overlapping photographs ot a<br />

single ob]ect point. Sometimes incorrectly celled<br />

conjugate Image polnta.<br />

corresponding Image rays—Rays catnecting<br />

each 01 a set of corresfmrding Image<br />

points with its patlicuiar perspective cenlar.<br />

corresponding lmagea—A point or fhre in<br />

one system o! points or tines homologous to a<br />

point or line in another system. Sorrwimas<br />

incorrectly called conJugate potnts.<br />

cotldal charr-A chafl of cotidal Iinas that<br />

show approximate locations of high waler at<br />

hourly imervale measured from a reference<br />

merid! an, usually Greenwich.<br />

cotlsfal hour—The average interval expressed<br />

in solar or lunar hours between the Moon’s<br />

passage over the merictiin of Greerrwich and<br />

Ihe Iollowing high waler at a specified place.<br />

cotldal llnS-A line on a chart passing thruugh<br />

all points where high water occurs et tha same<br />

lime. The lines show the lapse of time, usually in<br />

lunar hour intervals, between the Moon’s transit<br />

over a reference meridian (usually Greenwich)<br />

and the occurrence of high water for any point<br />

lying along the line.<br />

counter-etch—To remove, with certain diluted<br />

acids, Impurities from a Iimographk p!ate,<br />

making if receptive to an image.<br />

countarclockwlss angla-A horizontal angle<br />

measured In a countembckwlse direction: used<br />

primarily for the measurement of deflection<br />

engles.


----<br />

county map-A map of the araa of a county<br />

as a unff.<br />

course-l. (fend surveying) The baarlng of a<br />

Me: 81s0 fhe baarhsg and length 01 a lime. 2.<br />

(traverse) The aslnasfh and lar@h 01 a fine,<br />

considered together. 3. (navigation) The<br />

azimuth or bearing 01 a lie abng whkh a ship<br />

or aircraft is to travel or doas travel, without<br />

Chan(fs of UlrSCfiOn; the the drawn on a chart or<br />

map as tfse Intended Irack. Tha dlrecfton of a<br />

course is atwaye measured In degrees fmm the<br />

hue matilen, and the true coume & always<br />

meant unless h Is othenviee qualified; e.g., aa a<br />

msW~t~ or cO~SS Coume. Sss ateo track.<br />

4. @%fmPhY) A muie on tha Earth abng<br />

which a river ftowa; the rivar ffseff.<br />

covarlance-A mathematical quantity axy<br />

retetad to the coefficient of corretafiin p,ry<br />

between two variables axy. pxy crsuy, whars<br />

c#x and #y ars the variances of x and y,<br />

raspacflvely. Uaad in the variame-covariance<br />

matris of a least squares sotufiin.<br />

cover aorsrch-(JCS) In air photographic<br />

raconnabsance, the prccess of selection of .lhe<br />

most suitable existing cover for s spscHic<br />

requirement,<br />

cover traca-(JCS) (reczmnalssance) One of a<br />

series of overlays showing all air reconnaissance<br />

SOnieS 00Vafing the map shaet 10 which lhe<br />

ovartays raler.<br />

coveraga+JCS) The ground area<br />

represented on imagery, pholomaps, mosaics,<br />

maP5, and other geographical presentation<br />

ays!ems.<br />

covering powar— See angle of view.<br />

covar-(JCS) Photographs or o!her recordad<br />

images whkh show a particular area of ground.<br />

See also batslc covar; comptsratlve cover.<br />

crab an@-(JCS) The angle befwaen Itte<br />

aircraft track or fiiiht fine and the fore and aft<br />

axes of a verflcal camera, whkh are In line wlfh<br />

the Iongttudinsl axis of the akcraft.<br />

crab-1. (aerial photography) The condlllon<br />

caused by faflure to orient a camera wlfh respect<br />

to Ihe track of the akcraft. In vertical<br />

photography, crab is indimted by Iha adgas of<br />

the photographs not being parallel to ths air<br />

MIL-HDBK-850<br />

59<br />

base lines, 2. (air navigation) Sae yaw,<br />

definition 1.<br />

Critical Daslgn RovIew (CDR)-A review in<br />

the deveioprnenvaoqsslslfbrt Pocess to aesura<br />

that the reoommerded daebn of hardware and<br />

software b as cbee to the pmctuclbn<br />

conflguralbn as possible and ready Ior software<br />

mdlng and hardware pmcuramarrl.<br />

crltlcal engla-lhe minimum angle of<br />

irwiderwa at which a ray of radierrl enam<br />

hrrpinging on the surface of a trsmsparenf<br />

medium Ie mmpletety raftectad, no parl of It<br />

entaring lhe medium.<br />

crltlcal deficiency—An item or the condifbn<br />

of information or data which, because of<br />

omission, misidenfttcation, mk.focstbn, or other<br />

such signiliint error, wufd cause serious<br />

adverse impact on navigation eafety or<br />

operational mission acmmplishmenl.<br />

Critical elevallon—The highest elevation in<br />

any group of related and more-or-iess<br />

mntiguous reliet formations on a map or chart.<br />

See also hlghast elevailon.<br />

critical risisga-The spread ot ranges In whbh<br />

Ihere is an element ot uncenainty of<br />

imerpretation of values.<br />

crop-To trim or cut off parts of a photograph in<br />

order to eliminate superfluous portions and thus<br />

Improva balance or compoaifion. Usually<br />

accomplished by masking the Image area<br />

during printing,<br />

cross halre—A set of wires or etched lines<br />

placed on reticle held in the focal pfans of a<br />

Ielescope. They are used as Index marlw for<br />

pdminge of the Ielesmpe such as in a tmnsit or<br />

level when poinlings and read@s must be<br />

made on a rod.<br />

cmas Wt-An error introduced into<br />

atereotrtarrgulation due to the inebilii to recover<br />

the exact camera stations tor eucm.saive pairs,<br />

This condtfion Is generally due to vartslbns tn<br />

equipmem, materials, or to imperfect relative<br />

orientation,<br />

CrOsS-CheCk llnee—A series of data lines<br />

which cress the principal lines of dsvebpmam,<br />

preferably at right angles, which provides<br />

verification of, or reveals dbcrepancles In, the<br />

princlpel lines of the survey development,


MIL-HDBK-850<br />

Croso.Country Mmmrnont MaP (cCM)- A<br />

DMA map de@cfirrg CfOSS-CUI.MfIymobility<br />

eafiiws tor the M-1 ts~ expressad in terms O{<br />

GO, RESTRICTED. SLOW, VERY SLOW, and<br />

NO GO with correaporrdirro everage speed<br />

range pradicfkme. Open water and urban areas<br />

are afao pmtrayed, as are ground movement<br />

obatackas and hydrobgk hkrdrarces. Ptoducsd<br />

at 1:50,000 and 1:250,000 ecale.<br />

croee-coum~ movement study-A graphic<br />

or sertes ot graphics and supporting text or<br />

tables ponraying off-road movement conditions<br />

for e@tic vehicles or a group of vehdea. tf ie<br />

usually overprinted on a medium- or large-scale<br />

topographic rrwp basa.<br />

cross.fllgfrt photography—ShWle photographic<br />

etr@ heving elaraoacopic overlap<br />

behveen exposures and having e flighl direction<br />

at right angles to that of coexistent area<br />

coverage photography. When applied to<br />

shoran, the Iarm hnplies that each of the crosslight<br />

expoeurea la accompanied by remrded<br />

ahoran distances. See also control atrlp.<br />

CrO~.-S0CtiOtiA horizontal grid system laid<br />

out on lhe 5r6i.-nd tor determining contours,<br />

quantifies of earthwork, etc.. by means of<br />

elevations of the grkl points.<br />

crossing sn@s-The angle at which hvo lines<br />

01 pesifiin, cxwae Iinas, etc., intersect.<br />

crossllne glass screrrrs-See halftone<br />

screen.<br />

crystal clock—A device tor keeping accurate<br />

lime. It consists essentially of a generator of<br />

constant frequency controlled by a resonator<br />

made of quartz crystal, with auifable methods for<br />

pm.ducing corsfinuoua rotatiin 10 oparele time<br />

indkxting and related mechanisms.<br />

culmination—The position of a heavenly body<br />

whan af h~heat apparent altitude (zenith).<br />

Kr!own as upper Culmination; also, tor a<br />

heavenlv bodv wftiih la comlnually above the<br />

hortzon,’the bshbn of bwest ep~rent altitude,<br />

known as lower culmination. CUhTtinaliOn<br />

rscwre whan lhe body transits the iocd<br />

meridian. See alao lower tranelt; trsmslt;<br />

upper transit.<br />

cultural dotalla—See culture.<br />

cultural taaturee—See culture.<br />

60<br />

cultura-(JCS) Featurea of lhe terrain thet<br />

have been cmalrucfed by man. Included are<br />

such tiems as roads, buildings, and canals:<br />

boundary Iiies, arsi in a bread sanae, all<br />

names and legends on a map. MO called<br />

cultural detalla; cultural teatures; manmede<br />

Ieaturee.<br />

currancy review—lhe comparison of an<br />

existing MC&G product against eoume materkil<br />

o} later date man that trom which fha producf<br />

was produced, for the pupae of determlrthsg<br />

the products camency.<br />

CUrrOnt chs1l-A map ot a watar area<br />

depicting current speads and directions by<br />

Cuf’renf roses, vectors, or other means.<br />

current CYCIS-A complete sel of Iidal currenl<br />

conditions, as fhose occurring during a tidal day,<br />

lunar month, or Metonic cycle.<br />

current diagram—A graphic presentation<br />

showing the speed of the tiood and abb<br />

currents and the times of slack and strenglh<br />

ovar a conekterable stretch of the channel of a<br />

tidal waterway. The fimes being referred 10 as<br />

tide or wrrem phases at some relarersca<br />

stations.<br />

current meter—A device for determining the<br />

vabcify of fbwing waler by ascertaining the<br />

speed at which a stream of water rotates a vane<br />

or wheel.<br />

current rose-A graphic presentation of<br />

w rrents for speciiied areas, rsliliilng armwa at<br />

the cardinal and inlercardlnal compass pOinlS to<br />

show the dhecfion toward whch the prevailing<br />

currenf flows and the percent frequency of set<br />

for a given period of time The arrows on some<br />

presentatbns may be further subdivided (by<br />

lhkkness or pattern) to designate categories ot<br />

current speeds.<br />

curvature correction—l. (as fronomy) A<br />

correction applied to the mean of a series of<br />

observat”nns on a star or planet to take account<br />

of Ihe d!vargence to the 6pp6reM pelh ot the<br />

star or planet Imm a straighl line. 2. (gaodesy)<br />

The correction appfied In some geodetk work fo<br />

fake account of the divergence 01 the surface ot<br />

the Earth (spheroid) horn a plane. In geodetic<br />

spirll Ieveting, the eflecte of curvalure and of<br />

efmospheric refraction are mnsldered together,<br />

and fables have been prepared trom which<br />

combined corrections can be taken.


. .<br />

‘ MIL-HDBK-850<br />

curvature Of Ee~h-1. (obstruction 10 line of<br />

slghl) The offset horn the tangent to the cuwe,<br />

as a reauti of Ihe curvature of the Earth and<br />

refraction combined. 2, The divergence 01 the<br />

Eanh’s eurisce Irom a plane.<br />

curvature of field-An aberration affecflng<br />

the brrgffudinal position of Images off the axis in<br />

wch a manner fhef objacfa in a p4arw<br />

WWrrlcular to the axis are Imaged in a curved<br />

or dish-shaped surface.<br />

‘. .,,<br />

cut tape-See subtractlrrg tape.<br />

cutoff cyllnder-An accessory apparatus,<br />

used In etandardiiation oparatkrrrs 10 reter the<br />

end of a base tape or bar standard to a gmurrd<br />

mark.<br />

cutoff lhse-A survey line tun between two or<br />

more statbns on a linear Iravarae for @a<br />

purpose of producing a closed traverse of that<br />

pan of the survey.<br />

curve<br />

palms<br />

of allgnmerrf-A line connecting<br />

on the suc?aca of the spheroid and<br />

two cutting poslflw-A priming on glees of the<br />

contour drawing used to make the etched zinc<br />

defined by Ihe currdfiiorr that al avary point the<br />

exlmuths of the IWO end pints of the line differ<br />

by axacrly 180”. A curve of alignment is a fine of<br />

plate. A preliminary<br />

production.<br />

step in rafief model<br />

double<br />

normal<br />

cmwfure slightly less in length than the<br />

section lines connecting its IWO end<br />

cut—1. An obsewation between IWO points,<br />

one of which is known, Aleo a grepfrii<br />

poirrta.<br />

representation of such an obsewation. See ak.o<br />

Interaactlon; reaoctlon. 2. A printed sheet<br />

curve of equal bearing—A curve connecting O! SpSClliC syrnboIs used in cartography, such as<br />

all poims at which the greal


1<br />

.<br />

- MIL-HDBK-850<br />

cylindrical equal-apacad map<br />

pro@llon-A cyfindrioal map projection upon<br />

a cylinder IanB6rrl 10 a sphere, showing Ihe<br />

Oeogrsiphii rnertdlene as a tamily of equalspaced<br />

parallel etralght lines paqxmdicular to a<br />

second family of equal-spaced parallal straight<br />

Ilnes whkh reprasenl the geographic parallels.<br />

Tha ap~ng of the parallels need not be the<br />

aarna 6s that of fhe meridians.<br />

cylindrical lens-A fens in which the surfaces<br />

are segments of cylinders.<br />

Cyllndrlcal map pro]ectiokA map<br />

projection produced by pro}acting the<br />

geographic meridians and parallels onto a<br />

cylinder whiih Is tangent 10 (or intersects) the<br />

sutiace of a sphere, and then developing the<br />

cylinder into a plane.<br />

c yllndrlcal polar coordlnatea—Se e<br />

cylindrical coordinates.<br />

62


.. .. MIL-HDBK-850<br />

D log E curve-See ctrsrac!erlatlc curve.<br />

dally ●berratlorr-See diurnal abermtlon.<br />

deny lnequellty-See diurnal Inaquellty.<br />

denger Ilne-1. A lime drawn on e charl to<br />

indk.ate the Iirrrffs of safe navi@on for e vesset<br />

of epactiic draft. 2. A tine of smaU dots used to<br />

drew the navigetots aftenfiin to a danger which<br />

WOufd not stand wt dearty enough if it wara<br />

represented on the chart solely by epaciflc<br />

symbols.<br />

Dete ExtractIon Segmen! (DE/S)—<br />

Segmenl of DMAs Digital Production Sy61am<br />

which will provfde the capabllify to extract terrain<br />

elevatbn and feature data horn stereo aoff copy<br />

(dgltal) imagery. Terrain data will be estracfed<br />

aufornat!cally using digilal correlation techniques<br />

as well as Interactively by an operator. Featura<br />

data will be extracted interactively utilizing<br />

aUIOMatiC feature recognition techniques,<br />

Digital image processing techniques will eid the<br />

erralysl in tha ime,rpretation and extract”km of<br />

feetures. See also Dlgltal Production<br />

System; MARK .95; MARK 90.<br />

Date Integretlon Sagmen! [Dl/S)—<br />

Segment of DMAs DPS which will provide<br />

Suppon tor DMA planning and production<br />

management activities as well aa an automated<br />

management system for source library holdings<br />

and other data bases. Aaslgnmenl generation,<br />

achedufing took, and production reporting<br />

capabilities will be available to all Ievek of DMA<br />

management. See elso Dlgltal ProductIon<br />

Syatam; MARK 90.<br />

Date Services Segment (DS/S)—Segmenl<br />

of DMAs Dtgital ProdurMon System which will<br />

provide data management arid communication<br />

services for the MARK 90 phase. 11will also<br />

provide for data basa menagemerrf and<br />

archiving of digital data as well as much of the<br />

management data required for operation of the<br />

DPS. This aagment will have the cepabiiiiy to<br />

store one milfiin gigabits 01 data. It is one of<br />

the fargeat data bases In existence. In ac!diiion<br />

to Ifs other furcsions, Data Servkas will provida<br />

an ehscfronio txrmrrwnlcation network for [he<br />

OPS. Sae also Dlgltal ProductIon<br />

System; MARK 90.<br />

D<br />

Ltata ECqUISdtlWI stetlon-A ground station<br />

uead tor parformlng the various functions<br />

necessary to control satalUle oparatkrns and to<br />

obtain data trom the aatelliie.<br />

deta bfsnkhlemrchy-A formalized structure<br />

which provides for I he o~anization of data at<br />

various quantitative levels; e.g., data bank, data<br />

base, file, record, field (elamenf); character, bit.<br />

data base system-A collection of peopte,<br />

machines, and methods organized to<br />

accorr$dish all of the fundiorrs of a dSta bSSe.<br />

data baea-1. A set of data, part or the<br />

whole of anothar sef of data, and wnsisting of<br />

at least one file that is suffkierrf tor a givan<br />

purpose or for a given data processing SySteITt.<br />

2. A coflecflon of data fundarnenfal to 8 system.<br />

3. (digital mapping) An organized set of<br />

evalualad MC&G data stored In either graphic,<br />

textual, or digital form. A data base may contain<br />

one file of data, e.g. terrain elevatiin data, or<br />

several da!a files, e.g., cartographic, gaodetic,<br />

There are three kincs of data bases: 1) those<br />

that contain irdormation eboti Information; 2)<br />

those thal contain information shut data: and<br />

3) those that contain the actual data.<br />

data category (layar)-Rafars 10 data<br />

having similar characteristics baing contained in<br />

tha same data set, eg., roads, rivers. Usually<br />

information contained in one data category is<br />

related and is designad 10 be used with other<br />

categories.<br />

deta chamber—The porf”mn of a cartographic<br />

aerial camera where ancillary date k recwded<br />

abng the film margins. Data usually includas<br />

flme, attitude, frame number, and othar<br />

information required for idenfifkafion arxf<br />

carefetbn purposes. It may tnclude a character<br />

data generator block and ezfansive binary<br />

coded inforrnafion to include aircraft positbn<br />

and camera orianfation data.<br />

data dlctlonaW-Repository of Information<br />

abouf the dafinltion, structure, and usage of<br />

data. It does not comain the actual data.<br />

data elament-(JCS) A basic unff of<br />

information heving a uniqua meaning and<br />

subcalagorias (data items) 01 dktirwt unffs of<br />

values.<br />

63


MIL-HDBK-850<br />

data ●ncodlng-To apply a code, frequently<br />

one consisting of binary numbers, to represent<br />

Irtdiiktr.sai or groups of data. sometimes used as<br />

data capture.<br />

dam ●nfry-The process of bading data Irrto<br />

a Computerampalibla formal dkectly Into a<br />

data base.<br />

data Sssafon+digifal mapping) The<br />

cartographic mgbtralbn, or fit, of two or more<br />

MC&G data acts. Fusbn may scar between<br />

dMeranf MC&G data forma such as raster and<br />

vector, and between data sefs of the same data<br />

form, The degree of fit required b related to<br />

intended use and data set resolution.<br />

data link+JCS) The means of mnnecfing<br />

one location to another for the purpose of<br />

transmitting and receiving data.<br />

data manipulation-The performance of<br />

those data processing chores common 10 most<br />

users, sucfr as aorflng, Inpurroutput operations,<br />

and reporl generations.<br />

date quallty—Reters to the degree of<br />

exc@ance axhlbited by the data in relation to ils<br />

actual pw’trayal of the actual phenomena.<br />

data raducflon-Process of transforming<br />

masses of raw data info useful orderad, or<br />

simplified, basic information..<br />

data sat-A collection of slmllar and related<br />

data records that are recorded for use by a<br />

wmput er.<br />

data smoolhlng-A process which reduces<br />

the frequercy content or digital data. The<br />

infonmtkm eliminated may be real or artiiialty<br />

introduced fmm collection processes. The intent<br />

is to eliminate and replace inconsistent digital<br />

deta to provide a more understandable portrayal<br />

of the earth’s surface.<br />

data epaclng-The distance between centers<br />

of digital data elements in any digital data matrix<br />

or evenfy spaced array along a givan dkecfion,<br />

Since the spacing between elements in one<br />

direction can be differem fmm that between<br />

etemarrts In the other, a complete matrix<br />

deflnilbn usually raqulraa an expressbn of tmlh<br />

data spacings.<br />

date SWUCNN6-A syntactic structure of<br />

64<br />

symbotic expressbns and their storage<br />

allocation characteristics, Sae also chain<br />

node; Ilrtk and noda; apaghattl vactor;<br />

topological entltlaa.<br />

data Iopology-llefera to the order or<br />

relalionahip of apecifii items of data or othar<br />

hems of data.<br />

data tranafar modulae (DTM)-Sloraga<br />

devicas, commonly magnatic tape cerfrfdgss,<br />

used for dma exclmnge or transler bafwean<br />

planning system compute= and weapon system<br />

computers.<br />

date llna-See International data Ilne.<br />

datum centered elllpsofO—The eltipeoid<br />

that gives the best fil to the astrogeodetic<br />

network of a particular datum, and hence does<br />

nol necessarily have its centar at the canter or<br />

the Earth.<br />

datum level+JCS) A surface to whbh<br />

elevations, heights, or deplhs on a map or chart<br />

are related, Aleo called datum plane;<br />

refarence level; reference plane. See<br />

also altltuda.<br />

datum llna-See reference Ilne.<br />

datum plene—See datum level.<br />

datum point—(JCS) Any reference point o!<br />

known or assumed coordinates from which<br />

calculations or measurements may be taken.<br />

Also called reference point.<br />

datum shifts-Three constants which C&relate<br />

the relationship between the origins of two<br />

coordinate reference systems.<br />

datum transformation—l. The systematic<br />

determination of differences in origin, orientation<br />

and scale between adjoining or overta~lng<br />

dah.rms or Irfangulation nshvorfre. 2. The acl<br />

of transforming the coordinates of one datum to<br />

another.<br />

datum—1. (JCSj Any numarical or geometrical<br />

quemity or set 01 such quamifies which may<br />

serve as a reference or bsse for other<br />

quarrfilies. Where the ooncepl is gsomstric, the<br />

plural form Is “datums- In cmtraat to the nermal<br />

plural Wata.- 2. (geodesy) In geodesy, datum<br />

rafers to the geodetic or horizontal datum. The<br />

classical datum Is defined by fiva alemems<br />

,,


I<br />

. . ...4..,. . M!L.HDBK.S50<br />

glvlng the posltbn of the origin (two elements),<br />

the otiw’rtalbn of the network (one element),<br />

and the parameters of a reference elllpsokf (two<br />

efamants). More racenf definitions express lfre<br />

position and orientation as Iunclbtts of the<br />

deviations In the matian and in the prima<br />

vertical, the gaoid-ellipedd separafiin, ane the<br />

parameters of a refererwe ellipsoid. The Wortd<br />

Gaodatk System (WGS) is a gsocarrtrfc system<br />

that provides a bask reference trarne and<br />

(faomatrk figure for the earth, models the earlh<br />

grevlmatrically, and provides the means for<br />

ratallrtg positions on varioue datums to en earth.<br />

cantered, earth fkad coordinate system. Atso<br />

called horizontal detum; horizontal<br />

gaodetlc datum. See also horizontal<br />

control datum. 3. (leveling) A fevaf surface to<br />

wtrich efavatfons are referred, usually, mean sea<br />

level Imt may also include mean low water,<br />

mean bwer bcw waler, or an arbttra~ etarffrrg<br />

elevation(s). Also called vertlcel datum. See<br />

also allltude datum; Cape Canaverel<br />

datum; Department O! Da fenee World<br />

Geodetic Syetem; Europeen datum;<br />

hydrographlc datum; Indfan datum;<br />

Internatfonaf low water; local datum; low<br />

water datum; low water epringa datum;<br />

lower low watar dstum; Mercury datum;<br />

model drmrm; National Geodetic<br />

Vertical datum of 1929; North American<br />

datum o! 1927; North American detum<br />

of 1983; pfrotographlc datum; prefarred<br />

datum; Pulkovo 1932 datum; reference<br />

datum; eoundlng detum; tidal datum;<br />

Tokyo datum; vertical control datum:<br />

World Geodetic Syetem.<br />

day—The duratioir of one rotation of the Esrth,<br />

or occasionally another celestial body, on its<br />

axis. It is measured by successive transits of a<br />

reference point on the celestial sphere over the<br />

meridan, and esch type takes its name trom<br />

the reference used. See also apparent eoler<br />

dey; eetronomlc dey; calendar day; clvlf<br />

day; constituent day; Julian day; lunar<br />

day: mean eolar day; modiflad Julian<br />

day; Sidereal day; aotar day.<br />

de-integration—Definition of feafure or<br />

tfremafic singles or sets from an Infegraled data<br />

base.<br />

deadbeat compaas—See eperlodlc<br />

cortlpaee.<br />

OECCa chaI1-A cffan showing Oecca IInes of<br />

position.<br />

Decca-A trade name for a radio phase<br />

comparison ayatem which uses master and<br />

slave stations to establish a hyperbolic fettice<br />

arxt provide auxmte position fixing facifiilee.<br />

December ●aletlce-see wlnlar aolstlce.<br />

declination dlfferencs-The difference<br />

between two dactinatione, patikufariy between<br />

the declination of a cdestial body and the value<br />

used ae an argument for entering a table.<br />

decfinaflon of grid notih-see. grid<br />

declination.<br />

declfnaf Ion of the Moon-See lunar<br />

declination.<br />

declination of the Sun-See eolar<br />

declination.<br />

declination—1. In a syetem of polar or<br />

spherical coordinates, the angle at the origin<br />

between a iine to a point and the equafortal<br />

plane, meesured in a plane perpendicular to the<br />

equatorial plane. 2. me arc between the<br />

Equator and the point measured on a great<br />

citie parpendicuiar 10 the Equator. 3. (JCS)<br />

(astronomy) The snguiar distance to e body on<br />

the celestial sphere measured north or south<br />

through 90” from the ceiestial equstor along Ihe<br />

hour circle of the body. Comparable to latitude<br />

on the terrestrial sphere. 4. Dtten used as a<br />

shortened term for magnetic dacllnatlon<br />

although this uee is not prefemd. sea also grid<br />

decllnatlon; Orid magnetfc angle; lunar<br />

decfinatlon; parailei of decflnetion: solar<br />

cfeclinaflon.<br />

decllnatoire—A combined magnetic compass<br />

arvd afraighl-edge, suiiabla for use on a<br />

plantable 10 martr the magnetic merfdian. Also<br />

called box compase; trough compaas.<br />

decllnometer-A magnetic instrument similar<br />

to a surveyors compass, but arranged so that<br />

the line of sight can be rotated to conform with<br />

fhe needle or to any dasfred setting on the<br />

horizontal circle. Used in determining the<br />

magnetic declination.<br />

decompraaa-The process by which<br />

compressed dats is expanded to Its former file<br />

size.<br />

65<br />

defltrltlon-in imaoery Irrterpretetion, the<br />

. —


. ..- MIL-HDBK-850<br />

degree 01 clartty and sharpness of an image.<br />

deflecflng force-see Corlolls force.<br />

deflection angle traverae-A survey,<br />

usually an open traverse, in which the<br />

maaauremanf is made on the deflection angle<br />

of each course or fag from Ifre direction of the<br />

precedhfg leg. See also deflactlon angla,<br />

dafinifion 1.<br />

deflection angle-1. (survaying) A horizontal<br />

angle measured from !he prolongation 01 the<br />

preceding Ikra to the folfowing line. Defbcfion<br />

anglaa to the right ara posttive: those 10 the left<br />

are neQaWa. 2. (photogrammetry) A varflcal<br />

artgla, measured in the vertical plana containing<br />

the flight line by which the datum of any model<br />

in a slereotriangulatad strip departs from the<br />

datum 01 the preceding nwdel.<br />

I deflactlon rmomaly—The difference<br />

between an uncarected value of lhe deflection<br />

of the varlkal as detemrinad by observation and<br />

tha value after being cerrecfed in accordance<br />

with Cefiain aaaumotions made with reference to<br />

the physical condition 01 the geoid.<br />

I<br />

I<br />

deflectbn of the plumb lina-Deflection of<br />

the plumb line has tha same value as the<br />

deflection of the vertical except the sign of the<br />

value is reversed. See also deflactlon of fha<br />

verslcal.<br />

daflecflon of fha venlcal—The angular<br />

dfierence, at any place, between the upward<br />

dkecticn of a plumb line [ltxe verfkal) and the<br />

pe~endkular (the normal) to the reference<br />

spheroid. This difference seldom exceeds 30<br />

seconds except In mountainous terrain or great<br />

depths of the sea. Often expressed in two<br />

OJmPnent% MSfidian and prime vertical. Also<br />

called dafkrctlon of the plumb Ilna;<br />

ataflon wror. See also aatrogeocletlc<br />

daflectlon; gravlmefrlc deflactlon;<br />

topograpnlc daflectlon.<br />

degauaslng ranga-A station for determining<br />

magnetic signatures of ships and other marine<br />

craft. Such aignalures are used to determine<br />

requlrad dtrgaussing coil currant settings and<br />

other requlrad correcflve action.<br />

degenerate amphldromlc eyalam— A<br />

system of Cotidal fines whose center or nodal<br />

(no-tkfe) point appaam to be Iocaled on land<br />

rather than in the open ocean.<br />

66<br />

degrea of curva-Tha number of dagrees of<br />

angular measure et the tamer of a circle<br />

subtended by a chord 100 feet in length. in<br />

highway surveying, a 100-foot arc is wrnatimes<br />

used Instead of a 100-foot chord in defining<br />

degree of curve.<br />

degreaa of fraedom-The number of<br />

independent equations that may be wrftten from<br />

a redundant set of observations In excess of the<br />

number of equations required for a unique<br />

aoknion ot the unknown parameter. That is, if<br />

from a eel of radundant observations, n<br />

observation equations can be writfan to<br />

associate m numbar of unknown parameters<br />

(nzm), then the independent set ot equations<br />

(n-m) Is known as degrees of freedom tn any<br />

least squares adjustment of these redundant<br />

obsewaflons The speclaf, but very mmmon,<br />

case of establishing one parameter as the<br />

mean ot observations establishes u-1 and m-n,<br />

I.e., there b only one parameter and It may be<br />

uniquely determined by any one of the<br />

observatbns. (In this case, each observatbn is<br />

an equation, e.g., xl-10.2). Therefora, in fhis<br />

special case the degrees of treadom equal (n-<br />

1),<br />

..<br />

delay-(JCS) 1. (radar) The ground distance<br />

trom a poinl directly benealh the aircraft to the<br />

beglnnlng of Ihe area of radar scan. 2. The<br />

electronic delay of the start of the time base<br />

used to select a particular segment 01 the total.<br />

danelflcatlon network—Triangulation<br />

stations based on a brig-line trtangufation<br />

scheme but with shorler station-to-alation<br />

distances established to provide more easily<br />

available control of higher aocuracy to local<br />

users.<br />

danaltorrretar-An Inafrumant which Is used<br />

for measuring fiihl (elfhar trsnsmlftad or<br />

reflected) in terms of density tolerances.<br />

Transmlsslon densitometers measure the full<br />

density range 01 negatives and the reflection<br />

densitornaler measures the reflectbn range<br />

(density) of opaque coPy. A numbered scale or<br />

digital display allows armxrate readinge of<br />

specilk areas for comparisons or coniml<br />

purposes.<br />

cfenalty altltuda—(JCS) An atmospheric<br />

density expressed in terms of the effitude which<br />

corresponds wifh that density in fha Standard<br />

Atmosphere.


,<br />

,, .,,,<br />

donolt y ●xposuro cuw*See<br />

charsctorlstlc curve.<br />

“’- - MIL-HDBK-850<br />

dendty-1. (photography) A measure of me<br />

degree of blackening of an exposed film, plate,<br />

or papar after developmam, or of the dlracr<br />

Image (In fhe case of a prlnfouf matertal). It IS<br />

defined slrfctfy as the Iogartthm of the optical<br />

crpacky, where the opacity is the mtii of Ihe<br />

incident to fhe transmitted (or reftacfed) Iiihl. If<br />

variaa wtfh fhe use of scattered or specular fight.<br />

See also chamcferlatlc curve; contraat. 2.<br />

(catiogmphy) The amount of detail shmvn on a<br />

map Or Chaff. Density varies with scale and fhe<br />

nature of tha araa being cmrtpiled. 3,<br />

(surveying) The number of control points In a<br />

given survey or area.<br />

Department of Defenee lltrrarlea-Those<br />

Depafiment of Defansa Iiiraries designated es<br />

responsible for maintaining files and prov!ding<br />

library servkes ratalad 10 specific MC&G data of<br />

mmmon DoD interest, and designated as the<br />

primary IIbrary of that dala wilh the responsibility<br />

for providing service Ior all authorized agencies.<br />

Department of Defense World Geodetic<br />

System (DoD WGS)--A unified wortd datum<br />

based on a cornbhation of all available<br />

astrogeodetic, gravimetric, and safelfiie tracking<br />

obeervalione. Previous World Gaodelic Systems<br />

wera WGS 59, WGS 60, WGS 66, and WGS<br />

72. The currem sysfem is WGS S4. Ttra syslem<br />

is reviati as new geodetic, gravimetric, and<br />

salellfte data materials change the currently<br />

aczepted values.<br />

dapamrre-1. (plane surveying) The<br />

orthogmphic projection of a Iina on an easf-wesf<br />

axis of reference. The depariure of a fine is the<br />

difference of the meridian distances or<br />

kmgitudas of the ends of the line. It k east or<br />

positive, and aometirnes termed lhe eaatlng,<br />

for a line whose azimuth or bearing Is in the<br />

norfheaet or southeast quadrant; it is wesf or<br />

negetlve, and eomef)mes temxad lhe waef Ing,<br />

for a tine whose azimuth or baaring is in the<br />

notlhwest or southwest quadrant. Also caffad<br />

Iongftude dlffererrca. 2. (navlgaflon) The<br />

dkfanca between two meridians at any given<br />

parallal of Iattiuda, expressad in linear units,<br />

usually nautical miles; fhe distance to Ihe easl<br />

or wesl made good by a crafl In proceeding<br />

horn one point to another.<br />

ttependanf reeurvey-A resurvey for<br />

accomplishing a restoration based on fhe<br />

67<br />

orfginal condilbne according to the records. The<br />

dependarrl resurvey is made, Wt. by Identifying<br />

existing corners and other recognised and<br />

acceptable peims of control of the original<br />

survey and, second, by restoring the MISSIIW<br />

comers by proportionate maaauremanfa In<br />

harmony with the original aurvay. This ~ of<br />

raaurvey is used where Ihere Ls a fair agreement<br />

berwean the conditions on the ground and the<br />

racorda of tha original survey. Titles, areas, and<br />

descriptions should remain um5tan@. See<br />

ako Independent roaurvey.<br />

depraaaad pola-The celestial pole below<br />

the horizon. Opposite of alevated pole.<br />

depresalon angla-See angle of<br />

depreeelon.<br />

deprxraslon contour—A closed contour<br />

delimiting an area of Iowar elevallon than the<br />

surrounding terrain. Directional ticks extend from<br />

the contour in a downhill direction.<br />

depth contour+JCS) A line mnnecting<br />

peints of equal depth below tfxe hydrographic<br />

datum. Aiso called bathymetric contour;<br />

depfh curve; isobath. . .<br />

depth curva-See depth contour.<br />

depth number—A numerical value placed<br />

upon a depth contour 10 denote Its depth<br />

relative to a given datum, Also a depth<br />

sounding as h appaami on a chart.<br />

depth of field—The disfance between the<br />

points nearast and farthest hum the camera<br />

which are imaged with acceptable sharpness.<br />

depth of focus-The distance that the focal<br />

piane can be moved fonvard or backward fmm<br />

fhe poinl of exact focus, and 61111Uk’e an lMS9e<br />

of acceptable sharpness. Also called total<br />

range.<br />

depth of Isoetatlc compeneatlon-The<br />

depth babw eea level al which fhe conditbn of<br />

equllbrlum known as Iaoataay IS complefe.<br />

depth+JCS) The vartical dletenca fmm the<br />

plane of fhe hydrogrsphlc delum to the bad of<br />

the sea, lake, or river.<br />

dascerxrllng node-The palm at whkh a<br />

planat, planefold, or comet crusaes the acllptlc<br />

from norlh to south, or a aalellite crosses the


equator of ns fnimary from north to south.<br />

~sne of ●scondlng node. IWO called<br />

southbound nod..<br />

MIL-HDBK-850<br />

dencondlng vertlcsl sngle-Srre angle of<br />

depression.<br />

dMC?lptlOI+l. A Ierrn for the formal<br />

pubflehad dafa of eaCft trlar@atbn SfatlOn,<br />

bench merk, etc. The data Include Informalbn<br />

of the focaflon and type of mark and enable<br />

anyone to go to the Immediate iocafitiy and<br />

klantify the mafi with certainty. 2. (cedastraf<br />

surveyin@ A dorarmsnt listing the metes and<br />

btmds of a property.<br />

descriptive name-(JCS) Written indication<br />

on maps or charfs used to specify the nature of<br />

a Ieature (natural or artitiiial) shown by a<br />

general symbol. See also OeoQraphlc name,<br />

place nama, and Ioponym.<br />

Design Concept Review (DCR)—A<br />

milestone in tha development of a syslem<br />

where the review team determines if the<br />

raquirsmants hrrpossd are Iully underwood by<br />

the daveloper and are completely accounted for<br />

and delemrines if the System Design<br />

Architecture is reasonable and Ieasible. The<br />

requirements must be allocated to hardware,<br />

software, and operations.<br />

delall pohttbSelected identified points,<br />

especlalty on ob~que photographs, used to<br />

assist in cwmctiy positioning leatures displaced<br />

as a result of elevation.<br />

detalllng—(surveying) The process of tying<br />

topographic details to the control net. Objects 10<br />

be Waled in a survey may range from single<br />

points to mearutanng streams and complex<br />

geological torrnations.<br />

detection—in Imagery infetpretation, the<br />

discovering of the existence of an object but<br />

withwt reoognltion 01 the object.<br />

develop (dovelopmenl)-in photography, to<br />

subject to the eotbn of chemical agants for lhe<br />

PUPOSe Of bringing to VISW the Invisible or latent<br />

Image produced by the acfion of light on a<br />

SenSfliZSd surface; a160, 10 produce or render<br />

visible in this way.<br />

developsblo—A surtace that can be flattened<br />

to form a plane wilhout comprasslng or<br />

stretching any pafl of ft, such as a cone or<br />

cylinder.<br />

devlstlors-(JCS) The angular ditterense<br />

between magnstii and compass haadinga. Also<br />

called magnetic devlatlom See also erroc<br />

residual dsvlatlon.<br />

diagnostic polrtl-A point wlthkr a data sat<br />

with accwrste and known gsographk location<br />

that Is used to verify the edequeoy or<br />

inadequacy of transformatbn raeuff to the dSta<br />

set. (The diagnostic point ia not part of ttte<br />

transformstiin sotutiin.)<br />

diagonal check-fdeasuremente made<br />

across the opposite comers of the bask trams<br />

of a map projactlon to Insure the aocuraoy ot Ita<br />

COnStWCfiOn, or to establish ancVor check the<br />

scale of reproduti!on.<br />

diagram on the plane of the celeatlal<br />

equelor—See time diagram.<br />

diegrsm on the plane of the colesllal<br />

marldlart-A diagram in which the local<br />

celestial meridian appears as a circle with the<br />

zenith at the lop, and tfre horizon as a<br />

horizontal diameter. See also time diagram.<br />

diagram’s% “the--plane of the<br />

equlnocllel—See time dle.gram.<br />

diameter enlargement—A term used to<br />

indicate tha degree of enlsrgarnent of rXi@naf<br />

COPy. A One-diaITIeIer enlargement of a 4- by 5inch<br />

original would tm S by 10 inches. See alSO<br />

tlmea (X) enlargement.<br />

dlemeter—(magnification) See magnifying<br />

powar.<br />

diaphragm Stop—See relative apsrature.<br />

dlapoeltlve printer—A phofographlc device<br />

for producing dlaposltiies trom aerial nsgativea.<br />

Also called reduction printer. See alaO<br />

fixed-ratio projection printer.<br />

dlaposftlvs—(JCS) (photogrammetry) A<br />

pesitive photograph on a transparent medium.<br />

The term is generally used to refer to a<br />

transparent positive on a glass plafe used In a<br />

plotting instrument, a projector, or a mmparator.<br />

dlfferenca of elevatlon—Ttie vertical<br />

distance between two points, or the vertical<br />

distance between the Ieval surfaces that pass<br />

through fhe two points.<br />

68


.,<br />

MIL-HDBK-850<br />

dlffefunce of Iafftude-1. The shorler arc 01I<br />

any meridian between tha psrallals of hvo<br />

places, expressed in angular measura. 2.<br />

(plane surveying) The diierence of latitude o!<br />

the two ends of a tine is fraquenlly called<br />

tetltuda 01 tha Ilna, and deflnad as the<br />

orlftogrephic projection 01 Iha kina on a<br />

raferenca merldlan. The Iatltude (as ebovs<br />

defined) of tha middle of a Iina is also rererred to<br />

as Iatltude of the Ilna.<br />

dlfterence of longlWde-The smaller smgla<br />

at the POlS or lha shorter am of a parallal<br />

betwean the maridians of hvo places, expressed<br />

in angular maaaure.<br />

dlfterentlel abarratlon-The difference<br />

between the aberration of stare and that of a<br />

moving objacf (e.g., a satalfile). Also called<br />

parallactlc aberration.<br />

dlfferantlal dlstorfion-The resultant<br />

dimensbnal changes in length and width in any<br />

medium. See also differential aftrlnkage.<br />

dlfterantlal levallng—The process 01<br />

measuring the difference of alevation between<br />

any two ~ints by spirit leveling. See also dlracf<br />

Iavaling.<br />

dlftetentlel atwlnkage—The difference in<br />

unit contracfbn abng the grain structure of the<br />

matadal as mmpared to the unit conlractkm<br />

acmes the grain sdructure; fraquenlly refers to<br />

photographic film and papers and 10 map<br />

maferiafe in general.<br />

differential temperature-A natural error in<br />

surveying whereby temperahsre variations in the<br />

instnsmant cause reading errors that cannot be<br />

detecled. It is usually caused by direct sunlight<br />

on the inslrumsnf which can be minimized by<br />

ehading the Instrument during survey<br />

operations.<br />

cllflractlon--(oplice) The bsnding of light rays<br />

around the edgea of opaque objects. Dua to<br />

diiraclbn, a point of Iiiht scan or pmjactetf<br />

through a circular apetlure will always be imaged<br />

as a bright center surrounded by light rings of<br />

gradually diminishing Intanslty. Such a pattern is<br />

called a diffraction dlek, elry dlek, or<br />

centric.<br />

diffuse reflection-Any reflection process in<br />

which ma reflected radialion is sent out In many<br />

directions usually baarlng no simple relationship<br />

fo the angle of Incldance. See also cliff ufslon;<br />

●pecular reflection.<br />

dlffuelon-The scattering of fight rays either<br />

when reflected tram a rough surface or during<br />

tfl#~~#mlssion of light through a Translucent<br />

Dlgltal Aeronautlcel Fllght Information<br />

Flla (DAFIF)-A DMA flight fnforrnetiin data<br />

basa confalnksf airport, runway, navigafiinal<br />

aid, and enroute data. Both the high affttuda<br />

(18,000 feet and abova) and bw attitude (bebw<br />

18,000 fae!) enroule structures ara included.<br />

Dlgltal Bathymatrlc Deta Sass! (DSDB)—<br />

A grtided bathymetric data besa portraying<br />

depths in uncorrected meters for each 5<br />

minutes of latitude and Iongftude. Available on<br />

magnatic tape.<br />

Digital Chert of tha World (DCW)<br />

Project—A DMA R&D project designed to<br />

develop, ratina, and establish a suite of<br />

standards to support future Defense Mapping<br />

Agency digtfal data products and enhanca the<br />

utility of digital inlormatlon in vector Iormat. See<br />

also Vactor Product Format.<br />

Dlgltal Chan of the World (DCW)-D C W<br />

Is the firsl DMA product employing the Vector<br />

Product Standard (VPS). It provides global<br />

soveraga of the earth’s land surtecs at a<br />

1:1,000,000 scale information content wtrbh<br />

includes all the information found on tha baee<br />

map tor tha Operational Navigational Chart<br />

Series. Appticafion SOftwara is provided to albw<br />

data baae queries by feature/aftribute or epefial<br />

selection. Data output is 10 hard disk, tazf tile,<br />

or ploI tile. Sea afeo Vector Product<br />

Format.<br />

yDlgltal Cltlaa Data Baae (DCDB)—A DMA<br />

standard product consialing of the outfinea of<br />

cities digitized from Operational Navigation<br />

Charts [ONC).<br />

Dlgltal Comparator Segment (DC/S)-A<br />

segment of DMAs MARK 85 modemizatiirr<br />

process. The Digital Comparator is a dignal<br />

phologrammetric system used to measure mint<br />

Iocalions on digtial imagary. Points may be<br />

measured infaractively by the operator or<br />

automatically using d~ital correlation<br />

techniques. This segment also has the<br />

capabilny to estract elavation dafa in soft copy.<br />

Sea also MARK 85.<br />

69<br />

. .


’<br />

I<br />

Dlgltal Elovatlon Model (DEM)-A<br />

numer’kcal model of the elevations of points on<br />

the earth’s surface. Dlgitaf records 0[ Ieffain<br />

ekavaficrrs tor ground positions et regularly<br />

spacfid horizontal intervals. Data are available<br />

for some USGS 7.5 minute topographic<br />

quadrangle and 1:250,000 scale maps. See<br />

also Dlgltal Terralrs Elovntlon Data;<br />

Dlgltal Tarraln Uoslal.<br />

MIL-HDBK-850<br />

Dlgltal Faature Arsalysla Data (DFAD)— A<br />

data base consisting of aalected natural and<br />

cuttural ptarrimatric features, type classified as<br />

polrrt, Ilne. or area !esmsres as a hmctlon 01 Ihelr<br />

CuMPosttbn and aixe. Each faature is assigned<br />

a ~e and further described with Iimlted -<br />

attribution. The data am stored In @ygon<br />

format and eegregafed into 1 degree tilas.<br />

Primary apptiitbns are radar relurn, almulaiion,<br />

navigation, targeting and terrain obstruction<br />

studies. When combined with DTED, an ofl-line<br />

data baae is created tor use by almulators<br />

needing Ilne-of-sight, obsfructlon, and<br />

perspective VISWS. DFAD may also be used for<br />

sensor corretatiin, targel recqfnffion, lines ot<br />

communication anafysis, or for map production<br />

acfiviiies.<br />

. . ..r.<br />

Dlcsltal Geotrraohlc Informaflon (DGl)—<br />

Th~ riigiral re~e~entatbn of elevation and “<br />

sounding information, geographic k.ature<br />

geometry and feature attribute information,<br />

information corwarning Ihe appearance and<br />

status of the aarth’s aurtaca and ifs features in<br />

the alectronsagnefic spectrum (e.g., radar,<br />

infrared, etc.), Mifiiary Geographic Information<br />

together with othar ancillary information, and<br />

othar digftal information.<br />

Dlgltal Gaographlc Information<br />

Exchanga Standard (DIGEST)—A se! of<br />

atendarde devekrpad by NATOS DQital<br />

Geographic Informatbn Working Group<br />

designed to support the exchange of digital<br />

geographk data between m-pmducers. These<br />

standards apply to geodetic, geographic,<br />

geobgical, and geophysical data of mlfiiafy<br />

interest, as well aa pesiiioning, navigation,<br />

simubtbn, target recognition, map and charl<br />

automated production, and data display and<br />

manipulation applications.<br />

Dlgltal Landmaaa Blanklng Syatam<br />

(DLMBj-A larrd/water matrix of elevation<br />

values, where a value of 200 meters k arbitrarily<br />

assigned to fand and a value of O meters ie<br />

assfgned over water. These matrix data are<br />

70<br />

used by the E-3A Airborne Wamlng arxt Control<br />

Systems (AWACS). operating in a<br />

msritimelcoastal environment to filler out<br />

unwanled radar returns trom land and albw tor<br />

better delection of ship arxt aircraft movement<br />

near the ehoreline.<br />

Digital Landmasa Syetam (DLMS+A n<br />

otf-fins cartographfo data base cunakfing of fwo<br />

basic types o! diital data files, one czmtainirsg<br />

Tarraln Elavatlon Data and the olhar @ntainirrg<br />

cultural and natural feature data, malnfained by<br />

DMA to support various user systems e.g.,<br />

simulators and weapon systems. Formerly<br />

known as DIgllel Radar Landmass Simulator<br />

(DRLMS). See also DFAD; DTED.<br />

Dlgltal Line Graph (DLG)-Line map<br />

information produced by the U.S. Geobgical<br />

Survey in digital form Data are available at<br />

several scales, for several themes, and in<br />

saveral formata.<br />

!JIgltal Lina Graph-Entranced (DLG-E)—<br />

An extension of the DLG topological model<br />

which builds a cartographic feature layer upon<br />

the topology. Nonvocational characferistlcs 01<br />

feature objects are linked with the spatial or<br />

locational objects. See also DlglIal Line<br />

Graph.<br />

Dlgltal ProductIon Syatam (DPS)--DMA’S<br />

production system tor accurate and timely<br />

digital or aottcopy products and services. DPS<br />

includes hardware and software developments<br />

as wall as an MC&G digital data base which<br />

aupporrs the generation of multiple Producis<br />

over any geographic area. The first phaae,<br />

MARK 85, waa to achieve maximum eftactive<br />

enhancement of existing DMA production<br />

capabilities. The MARK 90 phase Imegrates<br />

porliona of MARK S5 wfth additional hardware<br />

and aottware for dqital or soft copy operations.<br />

See also Data Intagratlon Segment;<br />

Source Acqulaltlon Sagment; Hardcopy<br />

Exploltatlon Segment; Urslversal<br />

Ractlfler Segment; ProductIon<br />

Management Segment; Data Servlcee<br />

Sagment; Source Preparation Segment;<br />

Data ExtractIon Segment; Product<br />

Generaflon Sagment; MARK e5; MARK<br />

90.<br />

Dlgltal Terrafn Analyals Date (DTAD)-<br />

Data in diicrete diiital (numerical) term<br />

representing natural and manmade featuras.<br />

Fealure data are attributed and typically<br />

grouped In tiles for transportation, vagetatbn,


I<br />

wrfaca configuration, surface materials, wtiac4<br />

drainage, and abslacla analysis. The varbus<br />

data base pmducta cmwrisad of DTAD are<br />

used In Ienain analysis, largeli~, battlefield<br />

modeling and simulation.<br />

Dlgltal Terreln Elevation Data (DTED)—A<br />

uniform matrix of terrain elevatbn vafuee<br />

pmducad by DMA. DTED provides basic<br />

quantitative data for au military trainii,<br />

planning, and opamflng systems requiring<br />

Ierrain elevation, abpe, andor auriace<br />

roughness inlormstion. Level 2 post spacing is<br />

1 arc eeoond Iaftiudinalfy, Level 1 PSI spacing<br />

Is 3 arc second Iatifudlnallfi for both, Iongiktdlnal<br />

spacing varies wills Ialilude.<br />

Dlgltal Terrain Matrix (DTM)-A regular<br />

grid of geographic or model coordinates fhaf is<br />

fhe orimaw outcut of Ihe collection process. Tha<br />

data contained “fherain consists of elevation<br />

data raferred to a grid (row and mlumn<br />

occurrences) systam. Grid spacing may vary<br />

according lo surlace model accuracy<br />

requirements.<br />

dlgltal data basa (oli.llne)-A digital dsla<br />

base maintained in a common format fhst<br />

supperts diftarant user syslems, e.g., simulator<br />

or weapon systems Normally the data must be<br />

transferred belore it can be used by a specific<br />

user system. This term is commonly expressed<br />

as the off-line dafa base.<br />

digital data baae (on-llne)-A digital data<br />

base In the format needed by a user syslam,<br />

e.g., simulator or weapon system, and which<br />

can be badetf into the user system. This term is<br />

commonty relerred 10 as Ihe on-fine data base.<br />

dlgltal data-These are data represented In<br />

alphanumeric Iormst readable by a computer.<br />

dlgftal feature data—1. (cullural data) Manmada,<br />

natural and landscape features in digital<br />

Iorm, data in discrete digiial (numerical) Iofi,<br />

Incbdlng all man-made features on the Easfh’s<br />

surface, e.g., lines of communication, built-up<br />

araas (cifiea), transmission fines and Iardmsrk<br />

structures. 2. (hydrogrephic data) Data derived<br />

from Ihe meawremanl and description of<br />

physical features of the oceans, takes, rfvera<br />

and other WSfam, and their adpinlng coaflal<br />

araas (with particular refarence to navigational<br />

usage) In dlgffal form. 3. (landscape feature<br />

data) Data of all natural Ieaturas and man’s<br />

afferalbn to fhose features, e.g., lake wlfh dam,<br />

agricultural features, etc., in digital form. 4.<br />

MIL-HDBK-850<br />

71<br />

(natural feature data) Naluml features on the<br />

Earth’s wdace which are not rwrn-msde, e,g.<br />

vegetation, water bodies, desert, etc. in dlglfaf<br />

form.<br />

digital Image-An image digital format<br />

oMainad by parlitbning the area 01 the Image<br />

into a finite fwo-dimensional array of uniformly<br />

shaped, rrwtuafly exclusive regions called<br />

plxela (pbfura etanwnts), arxi assigning a<br />

descriptive tone or shade lo each such epafial<br />

region.<br />

dlglfaf map-1. A map expressed and stored<br />

in dgltal form. 2. A repreaentafion In diglfal<br />

form, diicrete points on Ihe Earth’s surlaca. Also<br />

called numarlcal map.<br />

dlgltal eynthaalzed data—Data derived<br />

from fhe analysis o! IWO or more different IypeS<br />

of dafa wch ae Digital Terrsin Elevation Data,<br />

D@ilal Natural Feature Data, and Dighaf Cultural<br />

Feature Data, An axample Is the derivaffon of<br />

data which can assess the effects of soil types,<br />

vegetation slope, drainage and microrafief on<br />

cross-coum~ movemem 01 vahbfas.<br />

dlgftal synlhagc- dats-Dafa in numerical<br />

format Ihat describes either totally or parfiatiy<br />

fictitious information generated trom lower<br />

resolufion?frequency input.<br />

digital terrain model (DTM)-A statistical<br />

rapresenlalion 01 tha cominuous wsiace of the<br />

ground by a large number 01 seleclsrd points<br />

with known rectangular coordinates In an<br />

arbitrary coordinate Iiald. See also Dlgltal<br />

Elevatlon Model.<br />

Digltlzed/Dlgftal Pofnt Posltfonlng Data<br />

Base (DPPDB)-Tha digitized PPDB Is a<br />

rastar-scanned digital randffion of the currant<br />

anabg PPDB product. DMA Is investigating the<br />

petential for a completely digital PPDB product.<br />

dihedral ang Ie—lhe angle between two<br />

inlersecfing planes.<br />

dimensional atablllfy—1. Ability lo maintain<br />

size. 2. Resistance to dimensbnal changes<br />

caused by changes in moiafure content and<br />

{emperafura.<br />

DIN—The German Industrial .Starrdad<br />

(Deutsche lndustrie-Norm), a Europaan systam<br />

of standardization for mechanical, engineering,<br />

and scientific manufactured producfs. In MC&G,<br />

the most nofable application is the


measurement 01 film speed.<br />

tYlopter-A unit of rnaaauremenf of the power<br />

01 a lens, especially a spectacle type lens. The<br />

power In diopters equals the reciprocal of the<br />

focal length In meters: thus, a lens whose local<br />

length Is 20 cm has a power 015 dbpters.<br />

dloptrfc ey$tern+optica) An optical system<br />

comairting only refradlve elernams (lenses).<br />

MIL-HDBK-850<br />

dlp angle-l. (surveying) The vertical angle O!<br />

the obeervefion point between the plane of the<br />

true horfzon and a sfght line to the Spparem<br />

horizon. 2. (phologrammelry) The vertical<br />

angf% at the air station, between the true and<br />

the apparent horizon, which is due to ffiihl<br />

he)ght, Earth curvature, and refraction.<br />

dip clrcla-An instrument for measuring<br />

me9nel~ dfP. ii consists essentially of a dip<br />

needfe, or magnetic needle, suspended In such<br />

a manner ae to be free to rotate about a<br />

horizomal ezis<br />

dlp correction-See trelght-ot-eye<br />

correction.<br />

dlp eqrsator-Se6” megnetlc equator.<br />

dlp needle—See magrrellc dlp needle,<br />

definition 1.<br />

dip of the horizon—See dip, definition 1.<br />

dlp pola-See ma~netlc pole.<br />

dip-l. The vertical angle, at the eye of an<br />

observer, between the horizontal and the line 01<br />

sight to the visible horizon. Also called dlp of<br />

the horfzon. 2. Tha angle between the<br />

horizontal and the fines of force of the Earth’s<br />

magnetic field at any poim. Afso celled<br />

Incllnatlon; magnatic dip; magnetic<br />

Incllna:lon; magnetic Iatltude. 3. The first<br />

detecfabla decrease In the attitude of a celestial<br />

body after reaching its maximum altitude on or<br />

near meridian transit.<br />

direct angla-An angle measured directly<br />

between two lines, aa distinguished in tranait<br />

traverse frmm a deflection angle.<br />

dkect levellng—The determination of<br />

differences of elevatbn by means of a<br />

72<br />

continuous series of short horizontal lines<br />

Venical distances from thesa tines to adjacem<br />

ground marks are determined by direct<br />

observations on gresiualad rods with a leveling<br />

irrstrumam equippad wilh a qzirif level. Sea aLso<br />

difterentlal Ievellng.<br />

direct meaeurement—Any measurement<br />

obtained by applyhg a tape to a fine or a<br />

protrador to an angle, or by turning en angle<br />

with a transit; espcially af@icebie to surveying.<br />

See also Indirect measurement.<br />

direct motion-The appsrent motion of a<br />

planet or other objeci eastward among the<br />

stars.<br />

direct obaarvatfon-A measure of the<br />

quantify whose value is deeired, such as a<br />

single measure of a horizontal angle.<br />

direct photography-Phonography In which<br />

the image of a subject is recorded directly by Iha<br />

camera in the conventional manner.<br />

direct posltlva-A positive image obtained<br />

directly without the use ot a negative.<br />

rtlrect problem—The datermlnatlon of the<br />

geodelic position of the end point and the back<br />

azimuth at position two when the given<br />

information IS the Iatkude and longitude of<br />

position one, along with the torward azimuth<br />

and the distance between the Iwo points.<br />

direct redlal plot-See dlrecf radial<br />

triangulation.<br />

direct radial trlangulatton—A graphic radial<br />

triangulation made by tracing the direcliarrs from<br />

successive radial cenlers directly onto a<br />

Iransparenl plotting sheet rather than laying \he<br />

triangulation by the templet method. Also celled<br />

direct radial plol.<br />

direct acannlng camerss-A type of<br />

panoramic camera wherein the tenses awing or<br />

relate about the rear nodal point at a given rate.<br />

direct telescopa-A telescope Is aald to be<br />

direct when it Is in ifs normal position.<br />

direcf vernfer—A vernier scale which has<br />

spaces or divisions slightly shorter than those o!<br />

the primary scale. The numbers on the vernier<br />

scale coincide with the numbers on the p!tmary<br />

scale,


I<br />

dlroction ●rgla-in lra~ing, the angle<br />

between the mtenna base line and an<br />

hrre@rary line cixmecfing the cenler 01 the base<br />

line with the target .<br />

dlractlon Instrument theodollte-A<br />

tha@oiiie In which the graduated horizontal<br />

C4rcle remains fixed during a 6erfaa of<br />

obaervatbna, the telesco~ being poinlad on a<br />

nurrtiar of signals or objjcfs In succession, and<br />

the cfirectbn of each read on the circle, usual~<br />

by mearra of mlciumeler mlcroecopas. Direction<br />

krstrumenf lhaodoliles are used abrrost<br />

excbaively In first- and eacorxkrrder<br />

Irirmgulafion. Atao called dlrectlon<br />

theodollte; triangulation theodollte.<br />

dlrsctlon method of adjustment—<br />

(trlarrgufstfon and traverse) A melfrod 01<br />

adjustment of observations which determines<br />

Corrections to obsenred directions. The direction<br />

method Is used in the adjustment of first- and<br />

eecxmkrder suwey obsewalions.<br />

dlrecflon method of dotermlnlng<br />

astronomic aslmuth-The determination of<br />

the astronomic azimuth of a line by measuring,<br />

with a dkection theodolite, the horizontal angle”.<br />

between a selecled star and e suitable mark<br />

and applying that ar@e to the azimuth of the<br />

star computed for the epoch 01 the observation.<br />

direction method of meeaurlng<br />

horizontal anQlee—See dlrectlon metfSOd<br />

of obatsrvatlon.<br />

dlrectlon method of obaarvatlon-A<br />

melhod of obsewing angular relationships<br />

wherein fhe graduated circle is hetd in a fixed<br />

position, and the directions of the various<br />

signals are observed around the hortzon. Thus,<br />

directions are poimings whereby angles are<br />

found by the differences in directions. Also<br />

called sflractlon method of maaaurhrg<br />

horizontal anglea.<br />

dlrectlon ot grevlty-See dlrectlon of the<br />

Iorco of gravity.<br />

dlrectlon of relallve movement—The<br />

direction of motion relative to a reference pcint,<br />

Ifeeff uaualfy In motion.<br />

dlrectlon of the force of gravity—Th e<br />

direction indiiated by a plumb line. It is<br />

perpendicular to the surface 01 the geoid. Also<br />

called dlrectlon of gravity.<br />

MIL-HDBK-8S0<br />

73<br />

dlractlon Ot tilt—The direction (azimuth) of<br />

the prtncfpal plane of a phoksgraph. Also, the<br />

direction of Ihe principal line on a photograph.<br />

dlrectlon theodollte-See dlrectlon<br />

Instrument theodollta.<br />

directional radar prediction-(JCS) A<br />

prectktion made for a particular heading.<br />

dlrectlonel reflectance-Reflectance<br />

measured for a specific mode of Irradmtbn and<br />

collecfbn.<br />

dlrectlorr-1. (JCS) A term used by a spotter<br />

Or ObSaWEr In a call tor fire to Indiie the<br />

bearing of the spotting line. 2. The poaftiorr of<br />

one point relative to another without reference<br />

to the dk.lance between them. Direction may be<br />

either twodimensional or three-dimenskwral, the<br />

horizontal being the usual plane 01 the latter.<br />

Direction is usually incketed In terms of Ifs<br />

angular distance tmm a reference diiectlon. See<br />

also gteat-circle direction; grid dlrectlon;<br />

horizontal direction; magnetic direction;<br />

Mercator dlrectlon; reference dlrfrctlon;<br />

reletlve direction; true direction; x.<br />

dlreclion.<br />

discrepancy—A difference betwean results ot<br />

dupliia!e or comparable measures of a quantity.<br />

The difference in computed values of a quantity<br />

obtained by different processes using data from<br />

the same suwey.<br />

diek oparatlng system (DOS)-One of<br />

many operating ayaleme tor computers which<br />

act as an interface between e user end the<br />

computer hardware. DOS was ap.acMcally<br />

designed lor personal comrnstem (PCs).<br />

dlapereton—(oplice) The separetiin 0! tight<br />

Inlo its component cobm by its passage through<br />

a diffraction grating or by refraakm such es that<br />

provided by a prism.<br />

displacement—l. (cartography) The<br />

hortzomal shift of the plotted position of a<br />

topographic feature from Ifs true position,<br />

caused by required adherence to prescribed line<br />

weights and symbol sizes. 2. Any shii in the<br />

position of an image on a photograph which<br />

does not alter the perspective characteristics of<br />

the photograph (I.e., shill due to lilt of the<br />

photograph, scale change in the photograph,<br />

and relief 0! the objects photogrephedj. See<br />

also refraction displacement; relle?


dleplacsrment; Illt displacement; xdlsplacement;<br />

y-displacement.<br />

display—The graphic presentation of the<br />

output data 01 any device on system.<br />

dlmolve-(digifal) The process of removing<br />

shared common attributes by eliminating the<br />

shard boumtarias when merging two or mora<br />

polygons.<br />

dletanca sangle-An angle In a ttiangle<br />

ofWOstie a side used as a basa in the solution<br />

01 the Mangle, or a side whose length is to be<br />

computed.<br />

dltstenco measuring ●quipment (DME)-<br />

See electronic distance measuring<br />

equipment.<br />

dkstance prorate rule-A method of<br />

bel.ancing a survey. A rule for holding angles to<br />

their racorded values and pforatlng the lengths<br />

of the lines In the traverse; oparaled by locating<br />

the beartngs to a wnvanlenl meridian,<br />

preferably the cbsing fine of the traverse, and<br />

prorating the dimensions through a<br />

trigonometric precess.<br />

distance-lhe spalial separation of two<br />

poims, measured by the length of a line joining<br />

them. Sea also ●ngular dlatanm; double<br />

merldlan d18tance; double zenith<br />

dlstanca; ecllptlc polar dlatence;<br />

electrical distance; external dletstnce;<br />

felllng; front focal distance; great-circle<br />

distance; grid length; ground distance;<br />

hyperfocal distance; Interocular<br />

dlatance; lunar dietance; merldlan<br />

distance: marldlonal distance; plus<br />

dletance; potar dlatance; prhtclpal<br />

dletance; projection dlatance; relatlve<br />

distance; rhumb Ilne distance; slant<br />

range; Sun-zenith distance: tangent<br />

dletence; time dletance; zenith<br />

dlatance.<br />

dlatant polnte-Similar to tie poinls but which<br />

appaar only on the obllques lacing outward on<br />

the perimeter of a mmpilation. Distant points<br />

unfte the sets of a sfrlp Into a flight unit; bul,<br />

unlike tie poima, do not serve to join several<br />

flight strips together.<br />

dletortlon compenaatlon—<br />

(photogrammstry) In a double projection direct<br />

viewing pbffer sysfem, that corracflon applied to<br />

offset the effect of radial distortion introduced in<br />

MIL-HDBK-850<br />

74<br />

an original negative by the objective tens of an<br />

aerial camera.<br />

diatortlon curve-A curve represeming the<br />

finaar distoflion charactarbtka of a tens; ii is<br />

plotted with image radial dislance from the lens<br />

axie es abscissae and Image radial<br />

dbplacements as ordinatas.<br />

dlatortlon-Lens aberrations affecting the<br />

posltbne of Images from their true relative<br />

poaitiirrs. See also aberration, detinftiorr 2;<br />

angular dlstortlon, definl!ion 2; dllferentlal<br />

distortion; flim dlaforllon; Image<br />

dlstortlon; Image motion Compenaetlon<br />

dlatortlon; lane dletortlon; linear<br />

dlstorflon; panorsmlc dlsitortlon; radial<br />

dlatortlon; seen poeltlonel dlstonlon:<br />

tangantlal dlatotllon; tfpped panoramic<br />

dtatortlon.<br />

distributed data baaa-A data basa with<br />

unique mmponents in geographically dispersed<br />

locations finked through a telemmmunications<br />

netwok<br />

dlstrlbutlon map-A map which shows the<br />

geographic arrangement of a specific product,<br />

commodity, or formation.<br />

dleturblng tunctlon—Sse dlaturblng<br />

poientlal, definition 2.<br />

Uiaturblng potential—l. (geodesy) The<br />

difference betwean the gravity potarrtial of the<br />

actual Earth and the potential function of tha<br />

normal gravity. Also called potantlaf<br />

dleturbance; potential of disturbing<br />

maaaes; potantlal 01 random maaeaa. 2.<br />

(astronomy) The diffarerrca bafwaen the total<br />

gravitational potential and the pofemial<br />

petlaining to a spherbel mass dbfr~}on. Abo<br />

called disturbing function,<br />

diurnal aberration-Aberration reaufring horn<br />

the rotation of me Earth on Rs asis. The value of<br />

diurnal SberfafiOn varies with the latitude Of the<br />

observer and ranges trom zem at the poles to<br />

0.32 second of arc al the Equator. A correction<br />

tor dlumal aberration Is applied to astronomic<br />

ObSeNatlOflS for longitude and azimuth. Also<br />

called daily aberration.<br />

diurnal age—Sae aga ot diurnal<br />

Irrequaflly.<br />

dfurnaf arc—See aetronomlc arc.


I<br />

1,<br />

dlUI’IISSl clrcla-The apparent datfy path of a<br />

cefaaflaf body, appmxlmamrg a parallel of<br />

declination.<br />

Ukmrai conatltuent-Any tide conerituent<br />

Wtroae parbd apprmximales that of a lunar day<br />

(24.84 solar houffi). See also conatlruant.<br />

MIL-HDBK-850<br />

Sflurnal lnequsdfty-The difference In heighte<br />

and dumtfons of the two successive high wafers<br />

Or of lhe two aumessiva bw waters of aach day;<br />

atm, the dfierarrca In spaed and dkactiin of tha<br />

two fbod CUmWrfa or the two ebb currents of<br />

each day. Also callad dally lnSqUallty;. low<br />

water Inequality.<br />

diurnal motion-The a~arent daily motion of<br />

a celesflal body.<br />

diurnal parallax—Ses geocentric<br />

parallax.<br />

cflurnal varlatlon-Thai component of a<br />

determinable magniiude which passes through<br />

a wmplete cycle in one day.<br />

dlumel—Having a, period. of, occurring in, .or<br />

related to a day.<br />

dlvorgenca-(ieveiing) The difference<br />

bafween ffia numerical values of fwo nmnings<br />

over the same seclion of a line of levels,<br />

dlvarglng lane—See negative Iana.<br />

DMA Automated Publlcat/on ProductIon<br />

Systam (DAPPS)-An electronic imaging<br />

davica used to crea!e text and manipulate<br />

graphic images. Output is either 10 a laser<br />

printer or a phototypesetter.<br />

dodging-(photograj?hy) Tfre process of<br />

hotdlng back Ilght trom carlain areas of<br />

senaftiied material to avoid overexpoaura of<br />

thase areas.<br />

domeatlc map-A map of an area within Ihe<br />

timits 01 the United Stales.<br />

dominant waveiangth-The wavelength of a<br />

spectrally pure energy that if mixed with white<br />

Sgfrl woufd match a color.<br />

Doppler cone angla-The engle batween<br />

the ratarence velocity vector and the refarence<br />

range vactor.<br />

Doppler eNect—(JCS) The phenomenon<br />

evidenced by tha change In the obearvad<br />

lraquency ot a sound or radii wave caused by a<br />

time rata of charge in the affactive length of Ihe<br />

path of travel bahvean the =urce and Ihe point<br />

of obaervalbn. Also called Doppfar shltt.<br />

Dopplar navigation—1. A system which<br />

measures ground speed and drift of an airrxaff,<br />

baaed on the Doppler affed Ot 6WfmnbSw<br />

generated signals emhtast from the crafi frrxf<br />

reflected from the Iarrain. 2. A system whbh<br />

dalermirras posifiins basad on the Doppler<br />

effacf o! aafellifa aignala. sea atao broadcaat<br />

ephemeris; Doppfer sonar navlgatlon;<br />

Navy Navlgatlon Satefllto System; point<br />

posltlonfng; pracfaa ephemerla;<br />

translocatlon.<br />

Dopplar satolllfa survey ●yofam-A<br />

receiver/antanna combrnatierr capabfe of<br />

receiving signala broadcast by aateiliies Of the<br />

Navy Navigation Salelllfe System (NNSS). The<br />

position of the antenna is mmputad by Point<br />

poallionlng, translocation, or shon arc geOd8fiC<br />

adjustment (SAGA), ush?g the mllacfed signals<br />

from the satellite passes.<br />

Doppler ehltl—See Doppler effect.<br />

Doppler sonar navigation-A syatam by<br />

whch speed and drtfl of a marine craft are<br />

determined horn the Doppler effect o! aoner<br />

genaratad signals amitfad from fhe craft and<br />

reflected from the ocean bottom or suspended<br />

particulate in the aaawafer. Sea alao Doppler<br />

navlgat(on; ●onar.<br />

dot ecreen-A photographic negative<br />

confalning equal-sized dots which are equally<br />

spaced in parallel and perpendicular rows. The<br />

prfmed area o! mverage determines the screen<br />

percen!. The percentage of tha printed area of<br />

mvarage IS measured by trrmemiaeion danaffy<br />

andlor by dot diametar. Dot screens are uaad to<br />

print tones of a mbr. Also called ffaf tlnf<br />

acraan.<br />

doubls optlcsl proJactlon r3tareoplotler—See<br />

doubla-projection dlrectvlewlng<br />

stareoplotter.<br />

double burn-The Imentional expoaura of two<br />

or more Ikra and/or hafffone negatfves In<br />

auccasaion and ragistar on the same sanaitizad<br />

aurtace. Not to be confused with doubla<br />

exposure, which Is usually unintentional. Also<br />

75


called double shooting. See also<br />

composltts.<br />

doublo CW’Iter theodollta-see repeetlrrg<br />

theodollto.<br />

.MIL-HDBK-850<br />

doublo conterlng-A method of prolonging a<br />

line fmm a tfxed point whereby the backsight is<br />

taken wlfh the telescope direct. The Instrument<br />

is FJungad, arxt the formighl is made with the<br />

teleempe inverted. The pint et whch the<br />

vertical cross hair intersects Iha hub b Ihen<br />

marked. The lrarraJt la then rotated 10 take a<br />

becka.ight on tha fixad point with the telescope<br />

Invarlad, the foreeighl la made wilh the<br />

iele~pe dlreci, and a second projected poktf is<br />

meilmd on the hub. A point midway between<br />

the two marked points Is the lrue point on the<br />

profongad tine, Atso called double reveralng;<br />

double reversion; double slgh!lng;<br />

reversing In aslmuth and eltltude;<br />

wlggllng-lrr on a Ilne; working-in on a<br />

Ilne.<br />

double cornere— Normally the two sets of<br />

rnmara along e standard parallel; the standard<br />

townsnip, sectiin, and quarter section comers<br />

placed at regular intervals of measurement;<br />

additionally, the closing corners established on<br />

the Ilne at the poims 01 Intersetilon 01 the guide<br />

meridians, range, and section lines of !he<br />

surveys brought in from the south. In olher<br />

cases, not hIlfy in conformity with the rectangular<br />

ptan, two comers, each common to IWO<br />

townships only, Inataad of one comer of the four<br />

tOwnShi@. SimilSrly, two comers, each common<br />

10 two sections, and two quaner section corners,<br />

aach referring to one aeclion only. The term is<br />

eomalimes used incorrectly to denote two fines<br />

established on Ihe ground although the field<br />

note record Irslicates only one fine, thus creating<br />

a hiatus or overlap.<br />

double ●xpossssra-Two photographic<br />

exposures on the same sensitized surface.<br />

double interpolation-Derivlrrg a value from<br />

tatwlared computations where two or three<br />

P~bn6 may be required, as in an hour<br />

angle observation of Polaris for azimuth, where<br />

an interpolation is made suitable to the time<br />

factor, another to arrive al a result conforming<br />

with the latitude of the observing station,<br />

double merldlan dlstancGThe algebraic<br />

sum of the peqzendicular distances from fhe two<br />

ends of any line of a fraverae to the initial, or<br />

reference. marldlan.<br />

76<br />

double model stereofemplat—A templet<br />

representative of the horizontal pbt of MU or<br />

three adjacent stereoscopic models that have<br />

been adjusted to a common, though random,<br />

scale.<br />

double proponlonete meesuroment- A<br />

mathod for restoring a feat wrner of four<br />

townships or a bat imerbr corner of tour<br />

sactbne. If is baaed on tha principte that<br />

monuments nmlh and south should oomrol the<br />

Ialiludinal posilion of a bat mmer, and<br />

monuments aast and wast ahoutd control the<br />

longitudinal position. In this method the<br />

influence of one identified original comer is<br />

baianced by the cmntrol of a corresponding<br />

original corner upon the opposite side of a<br />

particular missing corner whkh is to be restored,<br />

each identified original cnmer being given a<br />

controlling weight inveraefy prmpetilonal to fts<br />

dklame from the bst comer.<br />

doubfa reveralng—See double centering.<br />

double reveralon—See doubla centerlrsg.<br />

double ehootlng—See double burn.<br />

doubla sighting—See double centering.<br />

double target leveling rod-Any target rod<br />

having graduations on two opposite faces.<br />

double zenith dlstenceA value of twice<br />

the zenith distance of an object, obtained by<br />

observation and Mt by mathematical process.<br />

doufzle-projection direct-vlewtng<br />

stereoplotter—A class of stereo-plotters<br />

employing fhe principle of projecting the images<br />

of IWO correctly oriented overlapping aerial<br />

photographs onto a reference datum so the<br />

reaultam images may be viewed directly wllhout<br />

addtiional optical system support. Also called<br />

double optical projection rstereoplotter.<br />

dOUble-rOdded llna-A fine of differential<br />

levels wheraln IWO sets of tumlng peints, one<br />

high and one low, are used to give independem<br />

measures between bench marks.<br />

doubly azlmuthel map projoctlon-An<br />

azimuthal map projection having two poles.<br />

dove prlBftt-A prtsm which reverts the Image<br />

but does not deviate or displace Ihe beam. A


I<br />

Ii<br />

I<br />

given angular rofafion of Vre prism SIbouf its<br />

longitudinal asis causes the image to rotate<br />

Ihmugh twice the angle. Also called rotating<br />

prism.<br />

draconic month—See nodlcal montrs.<br />

drattlng gulda-See gulda.<br />

drattlng-The arf of drawing from given<br />

apacfflcetions.<br />

drag-(lheodotile) A slight movemenl of the<br />

graduafed ckcle of a fhaodolffe produced by lhe<br />

tOtatlOn of the aikfade. See also atmosphetlc<br />

drag.<br />

drahtage pattern—The pattern or overall<br />

aPPaafance made by the network of drainage<br />

lealureS on a map or chart.<br />

dralnag~ln mappirr~, all features associated<br />

with waler, such as shorelines, rivers, lakes,<br />

maretsea, etc.<br />

drltt angle-(JCS) The angle measured in<br />

degrees between the heading of an aircrall or<br />

ship and the track made good. [Drift angle is<br />

designated right or Iefl to indicate Ihe direction<br />

of drfft.]<br />

drltf station—A term sometimes usad in<br />

ehoran operations to designate the ground<br />

Stafion abouf which fhe aircraft flies during arc<br />

navigation. The second ground station is fhen<br />

referred fo as the rate atatlon.<br />

drltt-1. (JCS) In ballistics, a shift in pmjecfile<br />

direction due 10 gyroscopic actiin which resufts<br />

from gravitational and atmospherically induced<br />

Iorques on the spinning projectile. 2. The Iaferal<br />

shift or dieplacemem of a ship or aircraft from tfs<br />

course, Oue to the ac!”bn of wind or other<br />

causea. 3. Aariaf photography obfained under<br />

this wrrdffbn produces successive photographs<br />

whose edges are parallel tit sidestepped. 4.<br />

(precession) see total drift.<br />

dummy pendulum—A pendulum of simifar<br />

construti!on fo fhe workin~ pendulums excepf<br />

thaf If }s equipped with a thermometer and is<br />

fastened rigidfy in the receiver so that ii cannof<br />

swing during observations. The dummy<br />

perrdufum la eub]ect fo fhe same Iemparalure<br />

cxsnditbrta aa fhe working pendufums, and k<br />

used In deferminlng their temperature when In<br />

use.<br />

MIL-HDBK-850<br />

dummy—1. A preliminary drawing or Ia.youf<br />

showing the posltbn of ilkrafratiom and text as<br />

fhey will appear in the final reproduct”bn. 2. A<br />

set ot bfank pages mada up 10 chow the sire,<br />

shape, and ~eneral style of a book, bc4det, or<br />

pamphlet.<br />

dumpy laval-A Ievefing instrument which has<br />

its telascopa permanently attached to the<br />

Ieve)ing base, effher rigidly or by a hinge thaf<br />

can be manipulated by a micrometer screw,<br />

duplex baaa-llne maaeurlrtg stpparatua—<br />

A contacf base-line measuring apparafua,<br />

composed of two disconnected bare, one oi<br />

brass and the other of etaal, eac$r 5 maters &t<br />

length and so arranged as to indicate the<br />

accumulated difference of length of the<br />

measures from the brass and steel<br />

componams,<br />

dupllcata Ieval llna-A Ikre of epiril leveling<br />

composed of two airrgle lines run over fhe same<br />

route, but in opposite directions, and using<br />

different turning points.<br />

dupllcate r?egat)w-(JCS) A negafive<br />

reproduced from an orginal negative or<br />

diaposilive. ~he duplicate negative may be a<br />

fnre reproduction of the original or a<br />

reproduction possessing greater or less contrast.<br />

With dracf poaftiva materials, chemical reversal<br />

process, and cfupfiiating film if is not atways<br />

necessary fo maAe a posl!ke IO obtain a<br />

duplicale negat}ve.]<br />

DX-9D—An lMO/lHO proposed standard for the<br />

exchange of digital data.<br />

dyfux—A Iiiht-sensftiie papar or film usad for<br />

proofing, usualfy has a bfue postfive reading<br />

image wtth a blue background.<br />

dynamic correction—The quantity that must<br />

be added to fhe orfhomelric elevation of a poinf<br />

to obtain ifs dynamic number.<br />

dynamic elevaIlon—EIevation expressed in<br />

Iengfh uniis, buf determined by dynamic<br />

number.<br />

dynamic gravity meter—A type of gravity<br />

Instrument In wh’ch Ihe period of oscillation is a<br />

function of gravity and is tha quamity directly<br />

obae wed.<br />

77


. . . MIL-HDBK-850<br />

dynamk height-A height derived by dividng<br />

the geopotenfiel nunber by a constant, usually<br />

the value of normal grevity at 4S” Ialih.rde.<br />

dynamic number-The work required 10 raise<br />

a untf mass from sea level to a given point,<br />

expressed in abaotule units.<br />

dynamic tom~rsituro correctlon—<br />

(penduhxm) The correction to tfse observed<br />

period of a pendulum for the rate of change of<br />

its temperature.<br />

dynamical mean wn-A fictitious sun<br />

conceived to nmve easrward along the ecfiiic<br />

at the average rafe of the apparent sun.<br />

dyne—The dyne is the unit of lorce of the C.O,S.<br />

systems of units. When acting on a mass of 1<br />

gram, a dyne imparts to that mass an<br />

acceleration of 1 centimeter par secomi per<br />

second. Unfil abouf 1930, me dyne was used by<br />

the U.S. Coaar and Geodetic Survey (now the<br />

National Gaodatk Survey) in atatino values of<br />

gravity. Since Ihal time, gravity has been<br />

reported in terms of the gal, the e.g. s unit of<br />

accaleratiin.<br />

78


11/10 peg adjustment—See peg<br />

esfjrxetmsmt.<br />

Eerth fixed coordinate eyeterrt-An y<br />

inordinate system in which the axes are<br />

afatiinary wtih respect to the Earth.<br />

Eatlh Inductor compasa-A compasa<br />

depending for ite Irrdlcatione upon the caurenf<br />

generated In a coil revolving In tha Earfha<br />

rnagnetlc fiefd.<br />

Earth Inductor-An Inslrumenl designed tor<br />

use in magnetic surveys to delermhre magnetic<br />

dip. In principal, lhe instrument is a small<br />

dynamo by which the electrical flow can be<br />

introduced to the cdl of the Instrument. The<br />

presence or abaense of current is indicated by a<br />

ga!vanometer which provides for direct reading<br />

of rnagrratic dip.<br />

Earth Rersourcee Obeervetlon System<br />

Dsta Center (EROS or EDC)-A user<br />

,. .,.. cervices and eaies office established by the US<br />

Department of fnlerior. EDC also processes<br />

LANDSAT data using the EROS Dighal Imaging<br />

Proceaaiw System (EDIPS) and the EROS<br />

Diiital Image Enhancement System (EDIES).<br />

Earth aatelllW-A body thaf orbits about the<br />

Earth; epectficafly, an erlificlal seteltite placed m<br />

Otmf.<br />

Eatih tide-A periodic movement of the<br />

Earth’s crust caused by tide-prcducing forces of<br />

the Moon and Sun.<br />

Earih-centered elltpeold—A referenCe<br />

ellipsold whoee geometric cemer cofncldes wlfh<br />

the Earth’s center of gravity and whose<br />

semimlrwr axis coincides wnh the Earth’s<br />

rotational axis.<br />

easement curve—See eplral curve.<br />

eaet point—See prime verflcal plane.<br />

●eming-1. (grid) Eaefward (that Is left to right)<br />

readlrrg of grid vafues on a map. See elso talee<br />

eaatlng. 2. (plane eurveylng) See<br />

deperture, definition 1.<br />

ebb tld-The porlion of the tide cycla<br />

MIL-HDBK-850<br />

79<br />

E befween high water and the followi~ bw water.<br />

Also celled talllng fldsr.<br />

eccentric anomtrly-See ●nomaly,<br />

definition 3.<br />

stccentrlc error-Cemerirrg error.<br />

eccentric reduction—(trlanguleflon) The<br />

correction which rraJef IM applied to e dlracfion<br />

observed by an instrument with effher the<br />

Instrument or sfgnal (swlrrg), or both, amentric,<br />

to reduce the observed value to what if vmufd<br />

have been ii there had been no eccarrfrldfy.<br />

Also called eccentricity corractlon.<br />

eccentric slgnaf-A signal (target) which is<br />

not in the same veriical line with the station<br />

which if represents.<br />

eccentric etatlon-A survey point over whii<br />

an instrument is cantered and obsenrafkms<br />

made, and which la net in the same vertical tine<br />

with the stal”mn which it represents and to which<br />

fhe observations will be reduced before being<br />

cumbinad with observations al other stations. In<br />

ganeral, an eccentric station is established and<br />

occupied when ff Is impracticable to occupy the<br />

station center, or when If becomes necessary in<br />

order to see points which are not visbie from the<br />

station center.<br />

eccentricity correcflon-ilriangulation) See<br />

sccentric reduction.<br />

eccentricity of alldedeThe distance<br />

between fhe center of figure of the index POlnts<br />

on an alidade and the center of figure of Ihe<br />

graduafed circle. See also eccentricity of<br />

Instrument.<br />

eccentricity of clrcla-The distance between<br />

the center of figure of a graduated circie and ifs<br />

center of rotation. See also eccentricity of<br />

instrument.<br />

eccentricity of elllpsa-The ratio of the<br />

distance between the center and a focus of an<br />

ellipse to the Iengfh of ifs semimajor asis.<br />

eccentric It y of instrument—T h e<br />

combination of emerhriciiy of circle and<br />

eccentricity of al!dade.


I $<br />

II<br />

I<br />

I<br />

II<br />

II<br />

eccentricity of spheroid (elllpeold) of<br />

revolution-The eccmtrklty of an ellpse<br />

forrnirrg a meridian aactbn of the spheroid.<br />

.,, .,.. ..<br />

MIL-HDBK-850<br />

eccentrlclt y—1. Amount of deviation from a<br />

center. See also eccentric stetlon. 2.<br />

(surveyors cumpass) An ettect caused by ona<br />

or a combination of the folbwirtg conditions: (1)<br />

a straight line through Itra ends of the magnetic<br />

needle fails to pass through the canter of<br />

rotation of the needle; (2) the center of rotation<br />

of the needle is not coinckient with the center of<br />

figure ot the graduated circle; (3) the tine of sight<br />

tailS 10 peas through the vertbal axis of the<br />

instrument. 3. The ratio of the dtslances from<br />

any pc.im of a @nit sect”k.n to a locus and lhe<br />

ccrrraspardlng dkecfrlx.<br />

ecllptlc<br />

latlttsrJe-Se e celeetlel Ismtude.<br />

ecllptlc longltude—See celeetlal<br />

Iongltude.<br />

eCllptlC merldlen—A circle on the celestial<br />

sphere containing points 01 Ihe same celes!lal<br />

Iongftude.<br />

ecllptlc nods-See node.<br />

ecllptlc parallel-A circle on the celeslial<br />

sphere mntaining points of the same celestiel<br />

Iatltude.<br />

ecllptlc pCrlar dlatance-The complement of<br />

the celestial Ialiiude.<br />

eccentric-Nol having the same cenler.<br />

ecllptlc pole-On the celestial sphere, eiiher<br />

echo ●ounder—An echo sounding instrument<br />

of the two points 90” from the ecliitic.<br />

used for depth measurements in water. ecllptlc system 01 coordinates—A Sy6tem<br />

echo eoundlng—A method tor measuring<br />

depths by rssordlrrg the tlma intewal required for<br />

sound waves to go from a source of sound near<br />

the surfsce to the bertom and back again.<br />

echo tlmlng—The measurement of time<br />

required for a short train ot energy waves to<br />

travel the round trip path from en originating<br />

station to a raflecfor or transponder.<br />

echogrem-A graphk record of depth<br />

meaauremems obtained by echo soundhg<br />

equipmem. Called !athog ram when obt sined<br />

from a Fathometer echo sounder.<br />

echo—See blip.<br />

ecllpaa year—The Imewal between two<br />

successive conjunctions ot the Sun with the<br />

same node of the Moon’s orbit.<br />

eclipet+l. The reduction in visibitit y or<br />

dissppearamxr of a nonluminous body by<br />

passing into the shadow cast by another<br />

nonluminous body. 2. The apparent cutting off,<br />

wholiy or partially, of the fight horn a luminous<br />

body by a dadr body coming between If and the<br />

obserwer. See also annular ecllpae; iunar<br />

eclfpee; soinr eclipee.<br />

ecllptlc coordinate eystem—See ecllptlc<br />

eyalem of coordlnatea.<br />

80<br />

Of Curvilinear CeleStial coordinates which uses<br />

the ectiptlc as the primary retererrce plane and<br />

the ecliptic meridian through the vernal equimx<br />

ss the secondary plane. The points 90” fmm the<br />

ecliptic are the norlh and .aouth .ecliplic poles.<br />

Angular distance north or south of the ecliptic<br />

analogous 10 latitude, is celestial Iatifude.<br />

Celestial bngitude is measured eastward alOng<br />

the ecliptic trom the vernal equinox through<br />

360’.<br />

ectlptlc—The great cimle formed Lrythe<br />

intersection of the plane of the Eanh”s orbit<br />

around the Sun (or apparent orbii O! the Sun<br />

around the Earth) and Ihe celestiai sphere.<br />

edge matcftlng-lhe comparison and<br />

graphic adjustment ot features to obtain<br />

agreement along the edges of adjoining map<br />

sheets.<br />

edge mating—Sac metchlng.<br />

edge-l. (imagery) The boundary of an object<br />

in a photograph or image, usually charactartzed<br />

by a drastic change in the brightness value from<br />

the immediate interior of the boundary to the<br />

immediate exterior of the boundary. 2.<br />

(Iopobay) A line used to represent the Iocatun<br />

of a linear faature and the bordara of faOeS.<br />

Edges may be topologicslly fintrad to males,<br />

edges, and taces.<br />

editing—The process of checftihg a map or


1’<br />

I<br />

I<br />

I<br />

chart in ffs varbus stages of preparation to<br />

Insure eccssracy, corrgrlelenasa, and correct<br />

preparation fmm and interpretation of the<br />

sources used, and to assure legible and precise<br />

reproduction. Edns are usually relermcf to by a<br />

parfidar produdion phase, such as cnmpifatbn<br />

Scfii, acdbhlg edit, etc.<br />

effsctlve arsa-For any aerial photograph<br />

Ihal la one of a series in a ffiiht strip, that mntral<br />

part of fhe photograph delimited by the<br />

bmactors of overfs~ with adjacent photograph.<br />

On a vertical photograph, all imagea wifhin the<br />

effective area hava lass dlspfacemenl than their<br />

mrjugale Images on adjacent phonographs.<br />

●ffsotlvo Earth rsdlue--$ee ●ftectlve<br />

radius 01 the Eanfr.<br />

atfec!lve focal length (EFL)-See<br />

prhrclpsl dlatance, definition 1.<br />

effective radlua of the Eanh—A fictilious<br />

value for the radius of the Earfh, used in place<br />

o! lhe geometrical radius 10 correcf for<br />

atmospheric rehacfbn when lhe index of<br />

refraction In the atmosphere changea linearly<br />

with height.<br />

Egault laval-A French tnslrurnent having the<br />

spirit level attached to a level bar which also<br />

carries wyes in which the telescope rests.<br />

electrical dlstencs-LengttI measured in<br />

terms of the distanca traveled by radio waves in<br />

unit fima.<br />

elactrlcal survey net edjueter (ESNA)— A<br />

device used for obtaining least squarea<br />

adjustments of level, traverse, and veriical angla<br />

nets through fhe medium of an analogous<br />

electrical net.<br />

electromagnetic spectrum—Tha entire<br />

mnge of wavelengths or frequencies of<br />

elacfromagnatic ratilatlon extendhtg from<br />

gamma rays to the bngeaf radio waves and<br />

including visible fighl. Moat remofe aenshrg<br />

aystema are desfgrred to oparate within the<br />

elecfmmagnetlc spesfrum,<br />

Elactronlc Chart Dlapley end<br />

Inforrnatlon Sysfam (ECDIS)—A system<br />

whkh In Ifs mosf mmptete design integrates all<br />

essential alda to nav~afion into one system<br />

krclucflng charl Informstbn, posirlonal<br />

Information amf ships’ parameters such as<br />

came and speed. Echosounder, readings,<br />

MIL-JiDBK-850<br />

81<br />

radar, compieta or selective and other inputs<br />

may also be included.<br />

Electronic Chart Lfpdata Manual<br />

(ECfiUM)-The elesfrurric version of the Chari<br />

Update Manual (CHUM). See Chsrf Update<br />

Manual.<br />

elecfronlc bsrarlng-A bearing obtained by<br />

means of eledronic equipment.<br />

elscfronlc confrol-fhr!tol obtained by<br />

elecfmnic devices.<br />

electronic dlatence-meaaurlng (EDM)<br />

equipment—Devkes that measure the phase<br />

difference behvean irsnsmfftad and retumad<br />

(i.e., reflected or retransmfffad) elacfromagnaflc<br />

waves, ot known frequency and speed, or the<br />

round trip transil time of a pulsed signal, fmm<br />

which distance is computed. A wlda range of<br />

such equipment Is available for surveying and<br />

navigational use. Also sailed dlalance<br />

measurhtg equipment (DME). See also<br />

eiaclronlc poaltlon Indicator;<br />

Elactrotape; Geodlmeter; Iaaer; sonar;<br />

Telluromeler.<br />

electronic Ilna of po$ltlon-A line of<br />

position established by means of electronk<br />

equipment,<br />

alectronlc map data (EMD)—Se e<br />

etectrontc map.<br />

electronic map-Consisfs of fhe information<br />

of a map or chart, fhat is captured, stored, and<br />

displayed by electronic means. See akO<br />

raster: rasfer data structure; Raster<br />

Product Standard(s) (RPS); vector;<br />

vector Osta; vector Product Format<br />

(VPF); Vector Product Standsrd (VPS).<br />

electronic poeltlon fndlcator (EPI)- A<br />

type of elecfmnlc distance measuring<br />

e@PmeM used primarily in hydmgraphic<br />

surveying. Tha offshore range has been<br />

esfendsd from the fimita of shoran diafancas to<br />

more than 500 miles by use of EPi.<br />

electronic refraction—The refraction due to<br />

the elfects of the atmosphere and fhe<br />

ionosphere, which infrdma appreciable<br />

changes in the quantities measured by means<br />

of alactronk devices, such aa in the phase<br />

dtiferences measured with interfemmefara, in<br />

Ihe rale of change of phase measured with fhe<br />

Doppler systems, and in the change in phase


1’<br />

I<br />

between the times 01 lransm’Rfing and receiving<br />

a signai by Ihe ranging instruments,<br />

electronic sketchmaster—See universal<br />

●nalog photographic rectlflcatlon<br />

system.<br />

.Iacfronlc survey-Any survey utilizing<br />

eledronic equipment.<br />

electronic telemeler—An electronic device<br />

that measures the phase difference or tranail<br />

fhna between a transmitted electromagnetic<br />

~~~,e of known frequancy am speed and tts<br />

tilL-HtiBK-850<br />

Elecfrotapa-A trade mme for a precise<br />

electronic surveying device which fransmffs a<br />

radio frequency signal to a responder unil which<br />

in turn retransmits the signal baCk to the<br />

imerrogalor unit. The time Iapsa between<br />

original transmission and receipt of return signal<br />

is maasurad and displayed in a direct digital<br />

readout for eventual reduction into a precise<br />

finear distance. f! operatea on the same<br />

principal as the Tellurometer.<br />

elaments of a fix—The sDecific values Of the<br />

coordinates used to define ‘a positim.<br />

alevatad pola-The celestial pole above the<br />

horizon, Oppaile of depreaaed pole.<br />

alevatlon angle-See anale of elavatlon.<br />

efevetlon denelty category-A term used<br />

thmugfmut sizing of digital elevation data<br />

transactions within the MARK 90 system.<br />

Elevation density category 1 represents<br />

elevation post spacing at 3 arc second imervals.<br />

A pmducf having a scale smaller !han 1:50,000<br />

woufd typically be represented by this density.<br />

Elevation density category 2 represents<br />

alevation post spacing at 1 arc second intervals,<br />

A prockmf having a scale of 1:50,000 or larger<br />

would typically be represented by this density,<br />

elevatlon matrfx-A series 01 height values<br />

for points spaced at regular intervals and usually<br />

expressad In the form of a two-dimensional<br />

array of numbers.<br />

efevallon meter-A mechanical or<br />

eiecfromechanical davice on wheels that<br />

measures slopa and distance, and automatically<br />

and cominuousty klfegrales their product into<br />

dMferenca of elevation.<br />

82<br />

efevatlon Poata-A point with a known<br />

horizontal and vetliml poaifbn with respad to<br />

some defined referense system. Poaf pints<br />

are cmnrrmn elevation pints between two<br />

different digital terrain files. Dgifsti Ter@n<br />

Elavalion Data are eievatkon posts in dffifal<br />

form. A dqffal alevation matrfx consfata of<br />

elavallon posts evenfy distributed in a<br />

rectangular pattern.<br />

elevation tints—See hypsomatrlc tlntlng.<br />

elevation-VerfW dkifance horn a datum,<br />

usually mean sea level, to a ~inf or object on<br />

the Earlh’s aurlace; nol to be contused wtfh<br />

altlludo whfch refers to pofnts or ok+scts above<br />

the Earfha surface. In geodetic formulas,<br />

elevatkms ara heighls: h is height above<br />

ellipsoid, His height above lhe geoid or local<br />

datum. Occasionally the h and H may be<br />

reversed. See alsa adjusted elevetlon;<br />

assumed ground elevrstlon: barometric<br />

elSWe!lOn: CfIaCkfJd apd eleve;lon;<br />

crftlcal elavatlon; dfffarence of<br />

elevatlon; dynamic elevatlon; flald<br />

alevation; fkad elevation; frlghaaf<br />

elevallon; mean ground elevation;<br />

optimum ground eievation; orfhometrlc<br />

elevation; preilmlnary elevation; spot<br />

elevallon; standard elavellon;<br />

Supplemental elevatlon; unchecked<br />

spot aievation.<br />

ellipsold of revolution—See elflpsold of<br />

rotation.<br />

ellipsoid of roletion-The surface generated<br />

by an ellipse rotating about one of ifs axes. Also<br />

called allipsoid of revoluflon. See also<br />

obiafe epharold; prolate epharold.<br />

alllpsoldal height—The height above fhe<br />

reference ellipsoid, measured along the<br />

ellipsoidal outer normal through the point in<br />

question. Also called geodetic height.<br />

ellipsoidal reflacfor-A mirmr rjurlaca which<br />

Cunforms fo a portion of an ellfpsold of<br />

revolution, Principally employed in several types<br />

of slereoploner pmjecfora such as tha ER-55<br />

ellipsold-An t3111paoldIs a mathamalical figure<br />

genarated by the revolution of an ellipse about<br />

one ffs axes. The ellipsoid that approximates the<br />

geoid is an ellipse rotaled about its minor axis,<br />

or an oblate spheroid. See also datumcentered<br />

elflpaoid; Earth-cantered


MIL-HDBK-850<br />

elllpoold; Fischer elllpsold 01 1960;<br />

trlaxlal ●lllpaold. and lap-See overlap, dafinffion 1,<br />

●lllpllclty of ●n alllpse-The ratio befwaen end node-l. The 6econd node of an edge<br />

the dffferenco in length of the semi-axes of an (an edge is traversed from the ste!l mds to the<br />

alfiise end ifs eamimapr axb. end node) .2. The last mde of a teatura wilh<br />

●ltlptlclty of the apherold—See Ilattonlng<br />

several<br />

feature<br />

adgas. 3. The fast nods of an areal<br />

which Ie coincident with the first node.<br />

(of the Earth).<br />

Englnaer Topographic LabOMtOrlea<br />

elongation—1. (surveying) The posffion of a (ETL)—See Topograpfslc Englneerlrsg<br />

celasfiil body rrdalive to the observets meridian, Center (TEC).<br />

Is such that the apparent azimuthal movement<br />

Is at a minimum. 2. The angular distance of a ang Ineer’a chain-similar to a Guntere chain<br />

My of the solar eystem from the Sun: tha except that ii is 100 feet in length and contains<br />

angle at tha Earffr between fines to the Sun and 100 finks, each 1 toot long.<br />

another Weetlal body of the .eolar eyafem. See<br />

also greateat alongatlon. englnaa~a leval—Any of a group of precision<br />

emargancy run—See tlda ovar run.<br />

Iavefing instrumanls tor aslabtiihing a horfzonfal<br />

fine of sighl, used 10 determine differences of<br />

elevation.<br />

emargam nodal point—See nodal point,<br />

daflnffion 1. anginearlng map—A map 6h0wlng<br />

infomsation that is essential for plrmntrrg an<br />

amlaalvlty—The amount of enargy given oft engineering project or development and for<br />

by an objacf ralalive to the amount given off by estimating its rest.<br />

a %Iackbody - al the same temperature.<br />

Normally expressed es a posilive number<br />

between zero end one.<br />

enghreerlng survey-A survey executed for . . .<br />

lhe purpose of obtaining inlormatkrn that k<br />

assential for planning an engineering pnsjeci or<br />

●mplrlcal orlantation (rectiflcatlon)— The devalopmenl and estimating ifs msl. The<br />

compsited rectified adjustments ot information obtained may, in pan, be recorded<br />

magniflcafion, swing, easel titt, y-displacement, in the term cd an engineering map.<br />

and Ak-placemenl used to corractfy racreate<br />

the exact condfiions in the projected image that angraver aubdJvlder—A specially dasignad<br />

existed in the negative at the instant of<br />

exposure.<br />

scribing instrument whkh permits the selection<br />

of unitorm tick spacing in aubdvicfing or tfcklng<br />

map projatilons.<br />

emulalon-to-baae—A mntacf exposure in<br />

which the besa of the mpyirrg film is in mmacf angravar—Sae acrlber.<br />

with the amuls”on side ot the shaet being<br />

copied. See also amulalon-to-amu lslon. anlargemant factor—Sac acata of<br />

raprorfuctlon.<br />

emulalon-to-amulelo n—A mntact exposura<br />

in which Ihe ernuls”km of the copying film is in enlergemant/reduction diagram-Chart<br />

mntacf with the emuleion of the sheel being<br />

mpied. See also emulsion-to-baae.<br />

amulalon—A auapension of either lightaenaffive<br />

silver satfs, Dlazos, or photopolymers,<br />

In e mlbidal medium which is used for coaling<br />

tilms, platea, and pepars.<br />

showing tha necessary fens extension and mpy<br />

board axtansion raquired for various<br />

enlargamanfs and recfucfkma.<br />

an fargemaftl-A nagative, diaposffiva, or<br />

paper print made at a larger scale than the<br />

original. Aiso csllad blow up.<br />

encode—To mnvarf data by the use of a coda anroute chari-A chart of air mufaS in epacifc<br />

or a coded set in such a manner that areas that shows the exact bcelion of elacfronfc<br />

reconversion to the original form is passible. aids to navigatbn, such as radio dlrecfbn finder<br />

stations, radio and radar marker beacons, and<br />

83


I<br />

radm range atatiina. Also called redlo facility<br />

chart.<br />

en:lty node-A primitive used to represent<br />

featurea thal are truly zam dimenabnal. Entity<br />

nodes are Iopobgically linked 10 their containing<br />

face when tecee are praeam.<br />

OnIffy point-Pointe used to represent<br />

teeturee that are zem-ctimeneional (such ae<br />

survey points). Enliy poims may be<br />

topobgicaliy finked 10 a containing face.<br />

.trtlty Set-An attribute table or group of<br />

attributes.<br />

entrance pupil—The image of the aperture<br />

atop formed by all the lens elements on the<br />

object aIda of the aperture stop,<br />

entrance ellt-slit through which energy<br />

emera a spactroec4plc Inswument.<br />

entrance window—The image of me tield<br />

stop formed by all the Iena elements on the<br />

object side of the fietd atop.<br />

Ebtv6s correcrlon-Component of .uncorrected<br />

observed gravity obtained on a<br />

rrwving ptatform thal is attributed to Ihe easlwest<br />

comporram of the velocity that either<br />

increases or decreasee ihe effect of the<br />

centrifugal force caused by the Earth’s rotation,<br />

The formula for the correction usually includes<br />

the term for the secondary vebcity correction,<br />

E6tv6s effect—A vertical torte experienced<br />

by a t=zdy movin~ in an east-west direction on<br />

the rotating Eafth. In gravity measurements, a<br />

posfriie correcfiin is apptied if moving eastward,<br />

and a negatfve correction if moving westward.<br />

E6tv6a unft—The unit of gravitational gradient<br />

10-9 meters par second per second per meter.<br />

ephemerle time-The uniform meaaure of<br />

time defined by the laws of dynamics and<br />

determined in principal fmm the orbital motions<br />

Of the planete, specifically in the orbital motion<br />

of the Earth aa represented by Newcomb’s<br />

Tables of tha Sun.- Ephemaris fima for close-<br />

Earth Salelliles, or more cmrectty the llme<br />

associated wfih satellite ephemerides, Is<br />

observation dependem. For example, It the<br />

observaflona were made In universal lime (UTJ,<br />

the ephemetis time is UT; ff the obsewations<br />

were made in imemafional atomic time (IAT),<br />

MIL-HDBK-850<br />

84<br />

the ephemeris time is in IAT.<br />

ephamerla—(JCS) A publication giving the<br />

computed places of lha celestial bodies lor each<br />

day of the year, or tor olher regutar intervata. [A<br />

publication giving similar krformettin in a iomr<br />

suitable for use by a nevlgator la catted an<br />

almanac. An ephemeris la also a statement,<br />

not necessarily In a pubtiiation, presenting a<br />

correlation of time ard position of caleslial<br />

bodies or man-made satellites. A short<br />

ephemeris of future focation/time of salelfite is<br />

known as a set of alerts.] See also<br />

broadcast ephemarle; precise<br />

ephemerle.<br />

eplpolar plane-( photogrammetry) Any plane<br />

which mntakrs fhe eplpoles, therefore, any<br />

plane comaining the air base. Also called basal<br />

plene.<br />

eplpolar ray —’The tine on the plane 01 a<br />

photograph joining the epipole and the image of<br />

an object. Also expressed as the trace of an<br />

epipolar plane on a photograph.<br />

epfpolee—in tha perspective setup of Iwo<br />

prolographs (IWO perspective projections), I he<br />

points cm the planes o: the photographs whara<br />

they ara cut by the air base (astended line<br />

joining the IWO perspective centers). In the case<br />

of a pair of truly verlical photographs, the<br />

epipoles ara intiniiety distant from the principal<br />

points,<br />

epoch—1. A particular instant for which cerlain<br />

data are given. 2. A given period of time during<br />

which a series of related acts or events takes<br />

place. 3. An arbitrary moment in time to whjch<br />

measurements of position for a body or<br />

orientation for an orbit are referred.<br />

Equel &c Second Baeter Qhart/Map<br />

[ARC)-A rectangular coordinate and<br />

projection system at any scale for the<br />

entire elfipsoid based on the World Geodetic<br />

System 1984 (WGSG4). The ARC syslem<br />

divides the eltipaoid surface into 18 overtapping<br />

latitudinal band acafed zones.<br />

equal energy—Spectral distribution<br />

characterized by equal ftux per untt wavelength<br />

imervai.<br />

equal-altltude obaervatlona of the<br />

Sun—Azimuth Observalbns that consial of<br />

measuring horizontal angles from a southerly<br />

reference ooinf to the Sun’s timbs at an identiial


MIL-HDBK-850<br />

vertical angle, if meaeurest to the right timb in<br />

lhe a.m., then the angle should be measured to<br />

Ihe feti limb in the p.m. The same limb shoutd<br />

be observed In vertical angle. The mean of the<br />

two horizontal angles, with smell correction for<br />

the change in the Sun’s declination during the<br />

Interval from the a.m. 10 Ihe p.m. readings,<br />

@res a reeutling horizontal angle 10 the<br />

meridian.<br />

equal-eltltude obaervatlona—<br />

Observatbns of celestial objects al a fixed<br />

altitude (such as by an aatrolabe) taken at more<br />

or teas uniformly spaced azimuths around the<br />

horizon<br />

equal-araa map projactlon—A map<br />

prmjectbn havin~ a mnstant area scale. Such a<br />

projection is not mntorrnal and is not used for<br />

navlgarlon. Also called aUthallC map<br />

projection; equivalent map projection.<br />

eqIJ8t10n of tha equinox—The difference<br />

behveen the mean and true right ascensions of<br />

a body on the Equator, thus the difference<br />

between mean and apparent sidereal time. Also<br />

called ntnatlon In tight aacenslon.<br />

equallon of tlma-The algebraic dillerence<br />

in hour angle between apparent solar time and<br />

mean solar time, usually labeled “+. or .-. as h is<br />

to be applied to mean solar time to obtain<br />

apparent solar time.<br />

equation—Seis angle equation; azimuth<br />

equetlon; condition ●quation; correlate<br />

equallon; error equation; Euler”a<br />

equation; hydr08tatlC equation; Laplace<br />

equation; latllude equation; length<br />

equation; Iongltude equation: lunar<br />

equation; normal equation; obaewatlon<br />

●qustlon; parametric equationa;<br />

perpendicular equation; personal<br />

equation; elde equation; elde equation<br />

teata.<br />

equator ayatem—See celestial equator<br />

eyatem ot coordinates.<br />

equatorial axl-1. The diameter of the<br />

Earth described between two points on the<br />

Equator. 2. (astronomy) A telaacopa mounting<br />

axis oriented parallel to the Earth’s rotational<br />

axki.<br />

equatorial bulge-The excess of the Earth’e<br />

equatorial dtameter over the polar chameter.<br />

85<br />

equatorial chart-1. A chart of aquatotial<br />

areas. 2. A chatl on an equatorial pmjeCS~n.<br />

equatorial cylindrical orthomorphlc<br />

chart—Sac Mercator chart.<br />

equatorial cylindrical orlhomorphlc map<br />

projection—Sae Marcator map<br />

projection.<br />

equatorial diameter—Tha diameter of the<br />

Earth at the great circle comprising the laweatrial<br />

equator.<br />

equatorial grevlly value-The mean<br />

acceleration of gravity al the Equator,<br />

approximately equal to 9.7803 rrVae~.<br />

equetorlel horizontal parallax—The angle<br />

at a celestial object subtended by the equatorial<br />

semldiameter of the Earih used to indicate tha<br />

distance of the object from the Earth.<br />

equatorial lntewala—The englea, expreseed<br />

in units of time, between the varbua lines which<br />

mmpose the raticle of an astronomic transit and<br />

the maan pesition 01 .Ihose Iinaa.<br />

equatorial map projection—A map<br />

projection canterad on the Equator.<br />

equatorial node—Elrher of the two poims<br />

whera Iha orbit o? the satellite Imer’eects Ihe<br />

equatorial plana of its primary.<br />

equatorial redlua-The radius aesignad to<br />

the great circle mmprlsing lhe terrestrial<br />

equator.<br />

equatorial aatelllta-A satellite whose otbit<br />

plana coincides, or almost coincides, wfth the<br />

Earth’s equatorial plane.<br />

equatorial etara-Stars having declinations<br />

closa 10 zero and whose diurnal path k a<br />

parallel of declination cbsa to the Equator.<br />

Equalorlat stare, because o~ thalr apparently<br />

graatar speed of lravel, are preferred for tima<br />

and bngitude determinations.<br />

equatorial ayatem-See celeatlal equator<br />

ayetem of coordlnataa.<br />

Equator—The great circle on !he Earth midway<br />

belwean the poles and in a plane perpendicular<br />

to the Earth’s azia of rotation. II is the line of O“


!<br />

latitude. See also atrtronomlc equator;<br />

celeetlal ●quator; flctltlous squator;<br />

galsctlc equator; geodetic aqusstor;<br />

geomagnetic aquator; grid aquator;<br />

lunar caleatlal ●quator; rnagnatic<br />

●quator; obllque ●quStOr; Iranaversa<br />

equator.<br />

eqularr@ar ●plral-see rhumb Ilne.<br />

equlangulator-An opticsl instrument,<br />

em@Yi~ a 60° prism, used to determine<br />

astrmnomc fetifude and bngifude by equal<br />

affiiudes 01 heavenly b@es when the tima of<br />

the prime meridian (Greenwich) is known at the<br />

p~ce oi observation.<br />

equlgeopota;tlal eurtece-See<br />

equlpotentlel eurtace.<br />

MIL-HDBK:850<br />

equlllbrlum ●ptrarold-The shape !hat the<br />

Earth woufd attain ii il were entirely covered by a<br />

Ikteless ocean of constant deplh. See also<br />

geold.<br />

aqulllbrlum theory-A hypothesis which<br />

assumes an ideal Earth which has no<br />

mntinental barriers and is unilormly wvered with<br />

waler of mnsiderabie depth. 11‘also ‘assumes<br />

that the waler responds instantly to the lideproducing<br />

tortes of the Moon and Sun to form a<br />

surface in equilibrium and moves around the<br />

Earth whhout viscosity or friction. See also<br />

geold.<br />

equlllbrlum—A state of balance between<br />

forces. A body is said 10 fM in equilibrium when<br />

the vector eum of all tortes acting upon 11is<br />

zero.<br />

aqUlnOCtlal colure-The hour circle through<br />

the equinoxes.<br />

equlnoctial day—See sidereal day.<br />

equlnoctlal polrrt-See equinox.<br />

equlnocflal ayatam of coordlnalae- See<br />

celestial equator eyatem of coordlrsatea.<br />

aqulnoctlal yeer—See tropical year.<br />

equlnoctlal—See calestlal equstor.<br />

equhrox-One of the two points of intersection<br />

ot the ecfipt”c and the celestial equator,<br />

occupied by the Sun when its declination is OO.<br />

86<br />

Also called equlnoctlal point. Sae also<br />

autumnal equlrsox; mean aquhtox;<br />

vernal aqulnox.<br />

equlpotenllal ●urtace-A surtaoe having lhe<br />

same ptenlisl of gravity et every point, Also<br />

called level surface. See also gaold; OSOP;<br />

geopoterrllal aurlace.<br />

aqulecalar—A surface along whbh a scalar<br />

quantify has a constant vafue.<br />

equivalent focal lenglh—(JCS) The<br />

distance measured along the optical axis of the<br />

lens trom the rear nodal point 10 the plane of<br />

best average definition over the entire tiefd used<br />

in a camera. See also focal length.<br />

equivalent map projection—See equalarea<br />

map projection.<br />

aquhralent scale-The relationship which a<br />

small distance on a grephic bears to the<br />

mrresporrding distance on the Earth, expressed<br />

as an equivalence, such as 1 inch (on the<br />

graphic) equals 1 mile (on the ground). Also<br />

called verbal scale.<br />

equlvelenl vertical photograph—A<br />

theoretically, truly vertical photograph taken al<br />

the same camera station with a camara whose<br />

local length is equal to lhal 01 a camara taking a<br />

mrresponding tilted photograph.<br />

erasable opllcal disc (EOD)—A class of<br />

mmpact discs which allow users to rerecomf data<br />

onlo the disk.<br />

erect Image-An Image that appears upri9hi,<br />

or in lhe same ralatlve position as the object.<br />

arecllng telescope-An observer sees<br />

objacts right side up when Iooklng through an<br />

erecting telescope and upside down whan<br />

twking through an inverting telescope. The<br />

eyepiece In lhe optical syslem of an erecting<br />

teleswpe usually has four lenses, and the<br />

eyepiece in the opticel system of an inverling<br />

telescope has two lenses. See also Inverflng<br />

tefeacope.<br />

erratic error—An error caused by an<br />

incomplete element in an inatrumenf, such as<br />

backlash in a gear train. Sea also Instrument<br />

arror.<br />

error budgel—A correlated set of the


MIL-HDBK-850<br />

individual major error sourezw with the quantified 01 closure. See also Ilnear error of<br />

error or uncertainty which each mnlribules to a closure; relellve error of cloeure.<br />

total system eccwrscy or probable error.<br />

error of Colllmatlo*See cofllmstion<br />

●rror equstlort-The probability equation error.<br />

which expresses the laws of tha occurrence of<br />

random errors. This equation expresses the error of obsenuNlon-Thsr difference<br />

relafbnshlp between obsewed vafues, pfus first- between an obsewad vafue of a quantity and a<br />

order mrrecfion terms, and theoretical values. value sdopfsd as representing Ihe idesl or true<br />

The error squalksn Is the basis of the method of value of thaf quantity.<br />

least squares, used In me stljustment 01<br />

oteervalions for determining the most probable error of mn_(micmmeier) The difference, in<br />

vabe of a resuff from those observations. semnds of src, between fhe infemfed value of<br />

one turn Ot the micrometer screw and tfs actual<br />

error lntervef-See corsfldence Interval. value as determined by measuring the space<br />

between two adjacent Qradustbn marks of the<br />

●rror of closure-l. (general) The amount circle with the micmmeter. Atao called mn; mn<br />

by which a quantify obtsined by a serfes of of micrometer.<br />

related measurements differs from the true or<br />

fixed value of the same quantity. Also called error Oi survey-See error of closure,<br />

closlng erroc closure. 2. (angles) The definition 8.<br />

amount by which the actual sum 01 a series of<br />

angles fails to equal the theoretically eXaCf value error of the maan-See etandard error of<br />

of thaI sum. Afso celled engular error of the mean.<br />

closure. 3. (azimuth) The amount by which<br />

two values of the azimuth of a line, derived by<br />

dfierent Wrveys or alOmJ difterenl rOUtI?S, fail to<br />

error—1.<br />

Or ~m~ted<br />

The difference between an observed<br />

value Of a ~antify and the ideal or<br />

be exacfly equal to each other. Also called<br />

rsxlmuth “error of closurs. 4. (leveling)- The<br />

amoum by which two values of Ihe elevation of<br />

wua vaiue of that quanfffy. 2. An error is<br />

- generally classified es one of three types: (1) a<br />

blunder (mistake) which can be identified and<br />

the same bench mark, derived by dfflerent<br />

surveys or through different survey routes or by<br />

independent observations, fait to be exactly<br />

equal to each other. Abo called leVelln9 error<br />

mrrecled; (2) a systematic error, either mnstant<br />

or variable, which must be compensated foc<br />

ad (3) a random error, one of the class of small<br />

inaccuracies due to imparfecfions in equipment,<br />

of closura. See also clrcult cfosure. 5. surrountilng renditions, or human timitatione.<br />

(@) The error In the closure of a survey on<br />

itseff. Loops do not pmtecf egainst systematic<br />

errors in dietence msaaursment or blunders in<br />

See also ebeofute error; ectuel error;<br />

accumulative error: blunder;<br />

chronometer error; clrcult cloeure;<br />

starting poshbn or azimuth. Atso celled loop circular error; circular error probebfe;<br />

error of closure. 6. (horizon) ,The amount by circular near. cefiatnty error; circular<br />

which the sum of a series of adjacent measured atandsrd error; ctemplng erro~<br />

horizontal angles around a point fails to equal<br />

exacfk 360”. Measurement of fhe Iaat angle of<br />

the StSr’lW is called Cioslng the horizon; abo<br />

collimation<br />

compeneatlng<br />

curved-path<br />

error; compees Index error;<br />

error; constent ●rror;<br />

error; sccentrlc erroC<br />

calied closure of horizon; horizon<br />

closure. 7. (triangfe) The arnmmf by which the<br />

errstlc<br />

emo~<br />

error;<br />

gross<br />

external •rro~ graduation<br />

error; Index error; Inherited<br />

aum of Ihe three observed angles of a triangle<br />

faile to equsl exactly 180” pfus the spherical<br />

excess of tha triangle. Atso celled cloeure of<br />

triengle; triangle cloeure; triangle error<br />

of closure. 8. (fraverse) The amount by which<br />

error; trmtrument error; law of<br />

propagation of error; Ihteer erroc meen<br />

equare error: modulation error; netural<br />

error; near-certainty error; onhometrlc<br />

error: paraf Iacf Ic error; perf odlc errora;<br />

a value of the posltbn of a fraverse statbn, as<br />

obtained by computation Ihrough a !raverae,<br />

falls to agree wffh another vaiue of tha same<br />

statbn as determined by a dltferent sat of<br />

observations or mules of survey. Also called<br />

personal arror; pointing error; posltlonel<br />

efror; principal-distance ●rror; principal.<br />

point error; prlsmsstic error; probable<br />

error; random error; residual error;<br />

resuttant error; scale error; ●hade error;<br />

cloeure of treverse; error of eurvey;<br />

standard error; syetemetlc error;<br />

horizontal closure error; traveree error thaoretlcal error.<br />

87


I<br />

escape and evasion graphic—A map,<br />

chart or other graphc, usually produced on a<br />

l@rtweighl durabla material, apaciikally<br />

designed to @fe personnel to safety from<br />

enemy trefd tsirrilory.<br />

●atabllahmsmt of tha port-Tfre average<br />

Iraervel between uppar and bwer kmar franail<br />

naar tiie of new and full Moon and the next<br />

hfgh water. Also called common<br />

esrtabllshment; high watar tull and<br />

change: vulgar eatabllshmant. See also<br />

Iunltidal Interval.<br />

eatabllshment—See Iunltidal Interval.<br />

etch ellp-A pencil-shaped abrasive used in<br />

removiq unwanted marks on a metal<br />

preaaplate. Also called anakeallp.<br />

etchad zinc plata-An etched copy 01 Ihe<br />

mntour drawing of the base map, used aa Ihe<br />

guide in cutting the stepped Ierrain base of a<br />

model for making relief models.<br />

Mli-HDBK~650<br />

tstckl. To remove selected areas of the<br />

emulsion eiihpr che,micalty or manually. 2.<br />

Chemical treatment of a lithographic plate to<br />

make ncrnprfntlng areas grease-repellent and<br />

water-receptive or 10 produce the image on<br />

deep etch plates. 3. An acid solution mixed with<br />

the dampening fountain water on an offset<br />

press to help control ink on tha pressplale.<br />

Euler”a equation-A relation in a parebolic<br />

orbit Involvlng IWO radius vectors, their chord,<br />

and the time Interval between tham.<br />

Euler% thaoram-A mathematical expression<br />

to obtain the radius of curvature of a normal<br />

section in any azimuth on the reference<br />

ellipsoid. The czlrnulh angle, and the radius of<br />

curvature in the meridian and in the prime<br />

vertlml must be known,<br />

EulerIan anglea-A system of three angles<br />

which uniqualy dafkses wllh reference to one<br />

coordinate system (e.g. Earth axis) the<br />

orientation of a secand coordinate system (e.g.<br />

the axis of an orbff).<br />

Europaan datum-The Initial point of this<br />

system Is located at Potadam, Germany.<br />

Numerous national systams have been joined<br />

Info a large dalum based upon the International<br />

elllpsold which was ortented by fhe<br />

astrogaodelic method. The European and<br />

88<br />

African triangulation chains have bean<br />

connected and the gap of the Afrfcan am<br />

rnaasuremem from Csiro to Cape Town has<br />

been filled. Thus, all of Eurupa, south Afrka,<br />

and North Africa are rmaldad into one system.<br />

Through comrrmn survey stations, If wae also<br />

possible to convert data from the Russian<br />

Pulkovo 1932 system 10 the Europaan datum<br />

and, ae a result, tha Eumpaan dafum irvSudea<br />

triangulation as far aast as the 84ih mer’tiin.<br />

Adddbflal lies Suross the Middle Eaat heva<br />

permitted connedlon of the Itilan and<br />

Europaan datums. Sea also prefarred<br />

datum.<br />

evectlon—A perturbation of the Moon in its<br />

orbu due to the attraction of the Sun. This<br />

reaufte in an increase in the eccentricity of the<br />

Moon’s orbii when the Sun passes the Moon’s<br />

Ilne of apsldas and a decrease when<br />

perpendicular to it. See alee lunar Inaquellt y,<br />

definition 1.<br />

Evereai spheroid (elllpaold)—A referance<br />

ellipsoid having the following approximate<br />

dimensions: semimajor axis-6,377,276.3<br />

meters: flattening or etlipticity—1/300 .80. Used<br />

in India, Burma, Pakistan, Laos, Cambodia,<br />

Thailand, and Vietnam,<br />

exaggerated aterao—See hyperatareoscopy.<br />

exlatent corner—A corner whose position<br />

can be identified by verifyi~ the evic!emce of Ihe<br />

monument or its accessories, by refereffie to<br />

the description that k conlalned in the field<br />

notes; or whare the point can be bcated by an<br />

acceptable supplemental survey remrd, some<br />

physical evidence, or Ieslimony.<br />

extstlng data-Source material antior<br />

krforrnatwn assumed or krrewn to be in the<br />

possession of a gtien source ard subject to<br />

“elf-shel~ collection, as In mntraal to data<br />

obtained by operational field surveys.<br />

exit puplf-The image of the aperture @op<br />

Iorrnad by all the lens elaments on the image<br />

side of the aptmure stop.<br />

exit window—The image of fhe field stop<br />

formed by ali the lens elements on the image<br />

side of fhe field slop.<br />

exmarldlan altitude-An altltude of a<br />

celestial body near the celestial meridian of the<br />

observer to which a cerrect!!n is to be applied to


I<br />

I<br />

I<br />

!<br />

determhre the meridian attitude.<br />

●xmorldlan observation-Measurement of<br />

the attitude ot a celestial body near the celestial<br />

merfdian of the obsenfer, tor conversion lo a<br />

meridan altitude; or the altiiude ao measured,<br />

●xperfence radar predlcllon—Tfr e<br />

determination of size, shape, and relative<br />

intensity of radar returns and a determination of<br />

radar shadow and nc-retum araas based<br />

prtmartty on the radar knowledge and<br />

experience of the individual making the<br />

prediction rather Ihan on proven formulas,<br />

power tables, or graphs. Also called artwork<br />

prediction.<br />

MIL-HDBK-850<br />

experimental map—A sample of a new map<br />

product prepared either 10 obfain user approval<br />

of the adequacy of rmntenl and symbolization or<br />

to dkclose any problems which may occur in the<br />

various production stages. Also called<br />

prototype. See also pilot ahael.<br />

eXXpt~~O~ll-The difference belween an angle<br />

exfMoltatlon—The process ,of. obtaining usable<br />

data lrom imagery.<br />

exploratory survey-A survey executed for<br />

the purpose of obtaining general Information<br />

Corcernhrg areas about which such inlormalion<br />

Is not a maner of record,<br />

exposure Interval-The time required<br />

behveen successive ex~sures of a series of<br />

photographs for the purpose ot obtaining<br />

dasirad forward lap.<br />

exposure etatlon—See alr etatlon.<br />


l-number—See relative aperture.<br />

fats-l. (Imagefy) The ernulsbn side of a<br />

negative or layout plate, or the printing surface<br />

of a plate. 2. (topology) A fwo-dimensional<br />

topological entity defined as an undivided are<br />

surrounded by topofoglcaf e~es representing<br />

all or pan of the exlenf of a feature or of an<br />

attributed area.<br />

Iacslmllo chart-see modlfled lacslmlle<br />

char!.<br />

Iectored transparency—A system of radar<br />

aimulafion which utilizes a pair of phonographic<br />

imaoes on a glass plate or plates to store<br />

topogmphkc and radar reflection data. The dala<br />

ara scanned by a ffyingspot scanner cathoderay<br />

lube, and the density of the imagas is read<br />

by two photornuff@ier tubas. The two planar<br />

dimensions of the two images are lhe x- and ydimensiorre<br />

of the Iopgraph’k and reflectance<br />

data respacffvely. The danetfies of the<br />

reflectance imeges are used to store the intrinsic<br />

strength of radar lar~el. reflectance. The images<br />

are idamical in ttreir x- srrd y-values but<br />

separated In one dimension by the optical<br />

spacing of fhe dual raadoul system. Also catted<br />

land mass simulator plate.<br />

factory acceptance test (FAT)-A formal<br />

teat of the eystem under procurement in the<br />

rrumufaclura


I<br />

I -..<br />

I<br />

measurements ob!ainad by echo aoundksg<br />

equipment. Alao called echogram.<br />

fat horn curve-se a daplh contour.<br />

fathom llna-See depth contour.<br />

Fathometer—A trade name for an echo<br />

aoundar.<br />

Fssye ●nomaly—Sac free.alr anomaly.<br />

Faye correctiort-See free-air correction.<br />

‘ibiL-tibBK-850<br />

featheradglng-1. (cartography) The<br />

technique of progressively dropping contours, to<br />

avoid congestion on ataep slopss, and taparfng<br />

ihe fine weight near the end of the contour to be<br />

dropped, Aleo called leelherlng, 2.<br />

(photormaabklng) The thinning of overlapping<br />

edges of photographs bafore assembling into a<br />

mosaic in order to rnaka match fiiaa lass<br />

nolicaable. Whan ovarlepplng edges are<br />

Iealhared, shadows and sharp changes In<br />

mmraaf are reduced or eliminated. Also called<br />

feathering.<br />

feathering—See teatheredglng.<br />

Feelure ●nd Attribute Coding Catalog<br />

(FACC)—DMA Glossary which contains the<br />

Feature and Attribute Coding Standard (a<br />

nmdiiisatbn Of DMA’s FACS), See<br />

Faature/Attribute Coding Standard.<br />

Feature Extrectlon Segment (FE/S)—A<br />

segment of DMAa MARK S5 which implememe<br />

a mrn~ter suppmtad, analytical steraoplotter<br />

system capable of extracting Iaature data. This<br />

segment intagratea, on a sfngle system, all ot<br />

Iha varbus Stapa involved in the mostly manual<br />

feature extraction process prior to DPS. See<br />

alao MARK 8s; Dlgltal ProductIon<br />

System.<br />

feature analyals codo (FAC) number-A<br />

unique number (usually sequential) assigned to<br />

each area or Ieature ce.rfraved on the feature<br />

manuscr@ arm used iO rel~te Iealtire aislysis<br />

data @da (FADTJ information to the digital<br />

information which portrays the shape 01 the<br />

feature. See also faature analyala data<br />

table.<br />

feature erralyala deta table (FADT)—A<br />

tabfe mntaining the teature anafyais rmde<br />

numbers and the numeric codes whkh<br />

,<br />

represent the physical characferfstka of features<br />

aelecfed for portrayal. Sea also feature<br />

analyala coda (FAC) number.<br />

taature analyala-The process of locating,<br />

examining, and classifying the physiml<br />

characferiatka of cuftural Ieatures on the earth%<br />

surface.<br />

faeture attrlbuta-A property of a feature.<br />

faature claaa-A aet of teaturee ahartng a<br />

mnsistem set ot attribute types. A leature ctass<br />

Is irr’@ememed by using a set of tablee that<br />

Includes at least one primitive table and al least<br />

one attribute table. A feature class has fhe<br />

same columns (aftrfbule types) ot attribute<br />

irrforrnatbn tor each teature. Cfasses o! Ieatures<br />

are creatad in order to allow the rafational model<br />

10 oparala on them as sals. Every feature cfaas<br />

has one and only one feature tSble.<br />

feature coda-A unique identifier assigned to<br />

a feature.<br />

teature extraction—The arf of extracting and<br />

classifying features mntained in an image.<br />

teature Identl?lcation data (FID)-<br />

Intormation pertaining to the classification of a<br />

teature as to kind, tunction, and deacriptiin,<br />

e.g., heavy fabricaflon Industry wfth aaw-toelh<br />

roof; fruss bridge; powerfine pylon, etc. Each<br />

classification has a unique feature ktentfiication<br />

coda. See also featura anelyala data<br />

table, Iaatura enalysia code; featura<br />

analyals.<br />

faatura table—A table made up of the<br />

primary-keyed rows ot the features in a laature<br />

class. These rows mliecfively form the feature<br />

fable for that feafure class.<br />

Ieature typa-A classification of featuras into<br />

three categories: (1) poim of faatura-an objea<br />

whose location can be dascribed by a alngle set<br />

of coorcWmtee; (2) Iinaar (or Iinas) taaturaporfrayed<br />

by a line that does nol repraserrf an<br />

area; (3) areal fealura-a topographic feature,<br />

such as sand, swamp, vegetation, etc., which<br />

axtends over an area or in digital mapping any<br />

area encbsad by a delirrdfing Iina thaf has any<br />

unique characteristic, a,g., induafriaf araa, forest,<br />

residential area, etc. Feature type is thus an<br />

attribute defining ffse fopologic proparry of a<br />

feature (poinf, fine, or area).<br />

feature. oriented-A term used to describa<br />

92


.. . . .<br />

MIL-HDBK-850<br />

the approach Ior ertccxfing geographic entities in<br />

which a series of Inferrelstad geographic objects<br />

are organized Info e network-like struclure of<br />

data and pradefinad relalionahips.<br />

Ferstsrre/Attribute Coding Standard<br />

(FACS)-DMA standard for assigning fea!WeS,<br />

affribufas, values, and relationships lo all digital<br />

enflfies under the Oiiffaf Pmducfion System.<br />

See also Feature and Affrlbuta Coding<br />

Catalog.<br />

taature-A aat of phanomena with mmmon<br />

attributes and relatbnships. Tha concept of<br />

feature encompsssee both entity and object.<br />

See also Primary row.<br />

Fadaral Inforntatlon Proceaahrg<br />

Standarda (FIPS)-Wtcial source within the<br />

Federal Government for information processing<br />

standards. FIPS are developed by the fnsfitufe<br />

for Computer Sciences and Technology at the<br />

National Institute of Standards and Technology<br />

(NIST, formerfy called the National Bureau of<br />

Standards).<br />

fait aids-The top or smooth aide of paper<br />

-. thal is.confacfed by the feff bafl tor. ex!racfion of<br />

moisture during manufacture. This is the correct<br />

aide ot the papar for printing.<br />

fence-1. A line of readouf or tracking stations<br />

for pickup of signals from an orbtting satellite. 2.<br />

A fine or network of radar or radio stations for<br />

detectbn of a satellite in orbit.<br />

farmantlng dough thaory—See Pratt-<br />

Hayford theory of Iaostasy.<br />

ferrotyp%To burnish photographic prints by<br />

aqueegeeirrg wet upon a japanned sheel of iron<br />

or stainless plate and allowing to dry. This<br />

produces a harder, glossier surface on the<br />

photogr~hic print.<br />

fiber optlca-A device for relaying an image<br />

by means of a fa~e number of transparent<br />

fibers (tifements) by multiple total internal<br />

reflection. The fibara are moat sommonfy glass<br />

and less often a highly transparent plastic. Each<br />

fiber carries only one clement of the Image, so<br />

thaf lhe image is a mosaic in which fhe cell size<br />

la the tiir cross aectbn rather Ihan a<br />

continuous picture.<br />

flcflttous equsstor-A reterence Iina serving<br />

as the origin for measurement of fictitious<br />

Iatilude.<br />

flctltloua gratlcule-The nehvo~ of fines<br />

rapresanting fictitious parallels and fictftbua<br />

meridlana on a map or chart. Ssa also obllque<br />

gratlcula; tranavaraa grstlculo.<br />

flctltioua lafffude-Angular distance fmm a<br />

fictitious equator. ft may be called transverse,<br />

oblique, or grid Iattfude dapetii~ upon ihe<br />

type of fictitious equator.<br />

flctltloua longltudeThe arc of Ifcfftious<br />

equator between the prime fkfifiiua nsarfdian<br />

and any gfven Ilclffbus mertdian. It may be<br />

called tranaveraa, obllque, or grid<br />

Iongltude depending upon the type of Iiiltkxs<br />

meridian.<br />

!Ictltloua loxodroma—See flclltlous<br />

rhumb llne.<br />

flctltloua Ioxodromlc curve-See flctltloua<br />

rhumb Ilne.<br />

flctltloua marldlan-One of a series of great<br />

circles or fines used In place of a merfdlan for<br />

certain purposes. It may be called tranaverae,<br />

oblique, or grid meridian dapand!ng upon<br />

fhe type of fictitious meridian. See also prime<br />

flctitloua marldlan.<br />

flctltloua parallef-A circle or fine parallel to a<br />

fictitious equator, connecting all points of equal<br />

fiti!tious latitude. It may be cal lad tranavaraa,<br />

obllqua, or grid pamllal dePendin9 uPon the<br />

fype of ficfitlous equator.<br />

flctltloua pole-One of the two points 90”<br />

from a fbtffiOus equator. tt may be called<br />

transverse or obllqua pole depending upon<br />

the ty~ of fictitious eqUaIOr.<br />

flctltloua rhumb llrre-A line making the<br />

same obfique angle with all ficfifiius maridiina.<br />

It may be callad tranaveree, obllque, or grid<br />

rhumb Ilne depending upon the type of<br />

fictit’kws meridan. Also called flcfltloua<br />

Ioxodroma; flctltioue loxodromlc curve.<br />

flctltlous sun—A ticflfbus point termed the<br />

mean sun, which is imagined 10 move at a<br />

uniform rate along the Equator. Ifs mte of<br />

motion being such fhaf If makes one apparent<br />

ravolulbn around the Earth In the same !ima ae<br />

the actual Sun-ftIaf is, in 1 yaar.<br />

93<br />

flctltloua yaer—The period barween


auccasswe returns of the Sun to a sidereal hour<br />

angle of 80” (about Jatwary 1). The length of<br />

tha Wfltkxrs year Is the aama as thal 01 the<br />

tropical yaar, since both are based upon Iha<br />

position of the Sun with respacl to the vernal<br />

equinox. Aleo called Beaaellan year.<br />

flctitloue-in cartography, pertaining to or<br />

measured from an arbitrary reference line.<br />

fldellty—Tha degree with which a eystem<br />

arxarralely reproduces the dala input into il.<br />

fiducial asrea-The lines joining opposite<br />

fiducial msrlca on a photograph, The x-asis is<br />

generally considered 10 be the one nearfy<br />

parallel with the line of ffiiht.<br />

fldr.rclel mark(e+l. (surveying) An index line<br />

or point. A line or point used SS a basis of<br />

reference. 2. (JCS) (pholegrammetry) See<br />

Colilmatlng marke. 3. Also, markers in any<br />

instrument which detine the axes wfrose<br />

infarsecfion fixes the principal point of a<br />

photograph and tulfills the requirements of<br />

interior orfemation.<br />

field callbratlorr-A term generally applied<br />

where only a corrrbhalion of fietd and office<br />

wmputar techniques are available 10 check<br />

instrument accuracy. Adjustments, other than<br />

normal operator adjustments, cannot be made<br />

during field calibration.<br />

field check-The operation of checking a map<br />

compilation manuscript on the ground. See also<br />

field clesalficstlon.<br />

field claeelflcatlon-Field inspection and<br />

idenfifiition of faaturas which a map compiler b<br />

unable to delineate: identification and<br />

deiinaatlon of pofitical boundary lines, place<br />

namaa, road ciassitications, buildings hidden by<br />

trees, and so forth. Fietd classification may be<br />

Included aa pan of Iha comrol survey efiort snd<br />

Mrmslly la wmplemd prior to tha actual<br />

stereocompilation phasa. See SISO field<br />

Inapectlon.<br />

flald comparator-A shori Iina whose length<br />

is measured with accuracy and precision, and is<br />

used to check tha lengths of apparatus (tapes)<br />

used in tha actual Siald operations. Also callad<br />

calibration couraa; comparator base.<br />

fiald completion-A combination of field<br />

Inspections or surveys, either bafore or arter<br />

armpilation, to classify and mmplete the map<br />

MIL-HDBK-850<br />

content, correct erroneous data, and add<br />

intormetion such es names, civil boundaries,<br />

and similar classifiialion data. its Wrpxe is to<br />

till in or confirm that portion of a map manuscript<br />

prepared by atareocompilstion.<br />

tleld contouring-Contourirrg a topography<br />

map by field methods accomptishad by<br />

planeteble surveys on a prepared base or by<br />

stadla survey. Ganerally, this operation applies<br />

to tarrain unsuitable for contouring by<br />

phologrammetric methods. Also used in limited<br />

areae when engineering dasign (drainage)<br />

raquiras 1-foot contours. Sea also contour<br />

aketchlng.<br />

field control-(JCS) A series of points whose<br />

relalive positions and elevalbns are kmwn.<br />

These ~sifions are used in basic data in<br />

mapping and charting. Normal~, these positions<br />

ara established by sufvay mathods and are<br />

sometimes referred to as trig control or<br />

trlgonomatrlcal net (work). See also<br />

common control (srsllleW); control<br />

point; ground control.<br />

flald corractlon copy—A map or lracing<br />

prepared in the field, delineating CU@C@rS for<br />

subsequent reproduction of a’ tip.<br />

Ilald correction—Adjustments made to field<br />

measuramenls, such as angies or distances, 10<br />

correct for geometric or iength dkcrapancias.<br />

field elevatlon—An elevation taken trom the<br />

fiaid computation of a Iina of Ievals.<br />

flald lnspecllon—The process of comparing<br />

aerial photographs with conditions ae lhay exist<br />

on the ground, and of obtaining informatbn to<br />

supplement or Clartiy that which is not raadily<br />

discernible on the photographs themselves.<br />

Also catted classlflcatlon aunrey.<br />

field lntenalty—See field strength.<br />

flald of view—(JCS) In photography, lhe<br />

angla between two rays passing lhrough Ihe<br />

perspective center (rear nodal point) Or a<br />

camera ians to the two opposite sides of the<br />

Iormal. Not to be cxmlusad with angla of<br />

viaw. See also engia of view.<br />

Ileld poaitlon—A position computed while<br />

field work is in progress to determine the<br />

acceplabliily of the observations or 10 prov”kkea<br />

preliminary poshion for other purpsee,<br />

94


. .. . . . . . .<br />

field shaat-The hydrographer’s or<br />

topogmphers work sheet: if presents s graphis<br />

display of all surface and subsurface teatures in<br />

the area being surveyed. See also boat<br />

sheet.<br />

Nold stfsndardlxatlon of tspe-Th e<br />

mwrrparbon 01 the ferrgth of a laps to be used<br />

for survey meaauremenfs with the length of a<br />

standard tape, 10 determine the hue Ienglh of<br />

Ihe former.<br />

field afop-The physical element (such as a<br />

afop, diaphragm, or fens periphery) of an optical<br />

syslem whish limits the field of view severed by<br />

the system. See also eperture stop.<br />

field strength-For any physical field, lhe flux<br />

density, intensity, or gradient of the field al the<br />

point in question. Also called flsld Intensity.<br />

flsld—An individual dats element. In an<br />

attribute table, a field is a single attribute value<br />

of e single emny.<br />

figure adjustment—(survey ing) The<br />

,- . . . adjustment of a single chain of Iriangles made .<br />

!O satisfy the requirement lhal the sum of the<br />

anales in each trianole eauals 180°. and in the<br />

sa~e of a quadrileta;al that the sum of lhe<br />

ar@es equal 360”. An office computation,<br />

figure of the Eaflh-See gaold.<br />

fllar micrometer—A device at!ached to a<br />

telescmpe or micraasope, consisting of a wire<br />

thread (filament) connacfad with a screw in such<br />

manner that as Ihe screw Is tumad, the wire<br />

moves through a continuous succession of<br />

parallel positions, all in the Iasal plane of the<br />

instnsmanl<br />

fne structuring-The logical form of a file that<br />

results from applying a particular file organization<br />

end layout to a group of records.<br />

film beae-A Ihin, flexible, transparent sheet<br />

of stable pfaefic material to which a lightaensitive<br />

emulsion may be appliad.<br />

film distortion-The dimensional changes<br />

which occur In photographic film with changes in<br />

humidity or temperature, or from aging,<br />

handling, or other causes,<br />

film mosaic—See panel bese,<br />

MIL-HDBK-850<br />

film negalltra-See negative, definition 1.<br />

fIIIII positive-see posltlvs, datinition 1.<br />

film tltllng—See tltllng.<br />

film—A film base whkh Is mated wtih a Iiiht<br />

aenslfive emulsbn for usa in a camera or<br />

printing frame. See alao aerlsl film;<br />

autoacrean film; cartographic fllnf:<br />

Infrared film; Stable-base film; Strip film;<br />

tOpOgr8phlC bese film.<br />

fllterhrg—The removal of serfaln speofrel or<br />

spalial frequencies ia enhance featurea In the<br />

remaining Image.<br />

filter-Any transparent meterkd whmh, by<br />

absorption, selectively modifies fhe light<br />

transmitted through an optkaf system.<br />

final composlt~A mmposile of the prlnclpal<br />

color separations made after all sorrectbns have<br />

been compleled.<br />

FIR EFINDER Operational Data B8r3e<br />

(FODB)-Digftized triaxial coordinates collected<br />

on the preferred datum (usually WGS B4) at 12S<br />

meter pest spacing within 100 by 12.5 km araas.<br />

Values are collected kern DTED and<br />

transformed to UTM coordinates, w~h varticel<br />

values assigned wilhin 256 elevation bands<br />

defined between minimum and maximum<br />

values occurring in the area, Source tapes are a<br />

soecial-ouroose DMA DmdUCl that reouire<br />

dibbing’ onto field cas6effes priar to use by the<br />

FIREFiNDER ava!em. The FIREFINDER omvides<br />

hgh spaed w“rnpufalion 01 mortar and fjefd<br />

artillery firing positions from radar Intercepts of<br />

projectile trajectories.<br />

flrlng charl-(JCS) Map, photomap, or grid<br />

sheet showing the relative horizontal and verfkal<br />

positions of batleries, base poims, baae point<br />

lines, check points, targets, and other details<br />

needed in preparing firing data.<br />

ftrat approximation chart-See hlstorlcsl<br />

chart.<br />

first of Aries—See first point of Aries;<br />

vernai equinox.<br />

first pofnt of Arlee- Alea called first of<br />

Ariee. See varnal equinox.<br />

“95


flret point of Canca-Se e summer<br />

aolstlcs, definition 1.<br />

. . . .<br />

firer polnf of Caprlcornus-S e e winter<br />

eolatlce, definition 1.<br />

first point of Libra-See aut urn nal<br />

equhtox.<br />

flrat.order bench mark-A bench mark<br />

cmwsacled to the datum (usually mean sea<br />

level) by continuous Sirat-omfer leveling.<br />

flrsf-order levellng—Spklt leveling<br />

cordormlng to the specifications of the current<br />

‘Cfassiticalion, Standards of Accuracy and<br />

General Spectlications of Geodetic Control<br />

Survays.- Formerly known as preclaa leveling<br />

and IeVellng of high preclslon.<br />

Recommended for prfmary National Networks,<br />

es a basis for all subordinate elevation<br />

delemrinations, scientific studies such as cruslal<br />

rrxrvemerrt over la~e regions, extensive<br />

engineering projects such as hydroelectric<br />

dams. Such leveling generally includes the<br />

determination of geopotential values through<br />

simukanaoua gravity measurements.<br />

flrat-order lavel—A leveling instrument which<br />

mSats the 10lbwhtg Crftaria: (1) the sensit ivily 01<br />

the level bubble vial must be 10 of arc or less<br />

par dlvbion 012. mm: (2) the instrument must be<br />

mnslrucfed 01 bw expansbn metal to minimize<br />

lhe effeci of unequal heating; (3) the objective<br />

Ians must have an effective opening ot at Ieasl<br />

40 mm and a magnification of 40X.<br />

first.order traveres-A survey traverse which<br />

extends between adjusted positions of other<br />

first-order control surveys and conforms to the<br />

torrent specifications of firai-order traverse, per<br />

‘ClaaeifiiVwn, Standards ot Accuracy and<br />

General Specifications of Geodetic Control<br />

Sunfeys..<br />

flret-order trlssngulatlon-First-order<br />

Viangidatbn was at one time known as primary<br />

trfangutetion; changed in 1921 to precise<br />

triangulation; arkj in 1925 to first-order<br />

trfangutatbn. These surveys contorm to the<br />

rxmenf “Ciaeaifiition, Standards of Accuracy<br />

and Genaral Specifications of Geodetic Conlrol<br />

Surveys. - Recommended for primary National<br />

Networke, as a basis for all subordinate surveys;<br />

metropolitan area surveys, where high value is<br />

attached 10 iend and Its fine of communication<br />

frontage: and in scientific studies, such as<br />

MIL-HDBK-850<br />

crustal movement and space expbralion.<br />

Iirat-ordar wortt-The designation given<br />

survey work of the hlghesl prescribed order of<br />

precision and accuracy. Such surveys were<br />

torrnerly tailed prlma~.<br />

Fischer etilpaold of 1960-A refarence<br />

ellipsoid with two primary uses. In the Merctny<br />

datum it has the approximate dimensions of<br />

semimajor axis-6,378,166.0 melere, and fhe<br />

llattenlng or etlfpticny-11288 .3. In the south<br />

Asia datum the semimajor axfa is 6,378,155.0<br />

meters, and the flattening or eitip’wtty la 1L?98.3.<br />

Fischer ievet-A dumpy iavet capable of firalordar<br />

ievefing.<br />

flxad elava!lon—An elevation which has<br />

been acbpled, either as a result of Me<br />

observatbns or previous adjustment of spirit<br />

leveling, and which is held at its accepted veiue<br />

in any subsequent adjustment.<br />

fixed posltlon—See adjuated poaitlon.<br />

rlxed saleillle—See synchronous<br />

satellite. ..-<br />

Uxed-length recorde-A compuler data<br />

element formal in which all retards have the<br />

same length. These records allow dhecf access<br />

without searching or indices. See also<br />

varlebie-length records.<br />

fixed-ratio pantograph—See pantograph.<br />

fixed-retlo projection printer-A dlaposftive<br />

printer having an optical syalem In which a fens<br />

is placed between the negative and the<br />

diapositive piate, the object and image<br />

distances being set al nominal values according<br />

to the iaws ot optics, but with freedom of<br />

adjustment wilhin narrow iimhs, to produce<br />

dlaposltives whosa acaie Is at a predatennlned<br />

ratie to the negative scale.<br />

tlxer network-(JCS) A comblnallon of radio<br />

or radsr direction finding Inetalietione whfch,<br />

operating in conjunction, are capabie of piotting<br />

the position relative to the ground of an aircratf<br />

In fright.<br />

fixing-The process of rendering a developed<br />

photographic image permanent by removing the<br />

unaffected iight-sensitive materiai.<br />

96


., .,. !,-<br />

fix—A relatively accurate posilion determined<br />

without reference to any former posilion, from<br />

terrestrial, electronic, or astronomic data Also,<br />

the poirxf Ihus established.<br />

flare triangulation-A method of<br />

friartgufafion In which ahrrtrltaneous observations<br />

are made on parachute flares. This method ia<br />

used for extendi~ triangulation over lines too<br />

bng Io be observed by ordinary methods.<br />

flash rspparatua-An auxUlaW apparatus<br />

used in timhxg a pendulum during obsen’aliona<br />

for intensity of gravity.<br />

ffaxrh plata-See callbraflon plate.<br />

flat model—Any spatial model which is<br />

capable of being leveled. See also warped<br />

model.<br />

flat stock-1. Charls or maps which are not<br />

folded and kept Ior filllng ollicial and sales<br />

orders. 2. Flat sheets of map paper as opposed<br />

to roll paper.<br />

flat tlnf screen-See dot screen.<br />

. . . .<br />

MIL-HDBK-850<br />

Instrument. 2. (steraoscopy) me alfemafe<br />

bllnking of the eyes and mentally com@ring Ihe<br />

appearance of images in a stereoscopic pair to<br />

determine diflererces between the two photos.<br />

flight altltuda-The verfkaf disfance above a<br />

givan datum, usuaUy mean sea level, of an<br />

aircraft in flight.<br />

IIlght block—An adjustable unit of<br />

photographic coverage cmrairdi~ of overfepping<br />

strips of phonography. A minimum size block<br />

consists of at least three overiappiig ffiiht atrips.<br />

flight cherf-See route chart, definition 2.<br />

fllght Information and alr facllltles<br />

data-Data concerning airfields and aeapfane<br />

atalions and retated information required for the<br />

operation of aircraft.<br />

fllght Ilne apaclrrg-The distance betwaen<br />

adjacent tracks in a series of parallel aerial<br />

photographic flight strips.<br />

fllght lhxa-(JCS) In air photographic<br />

reconnaissance, the prescribed ground pafh<br />

over which an air vehicle moves during, the , .,<br />

execution ot its crlroto miss”km.<br />

flattening (of the Earth)-The ratio of fhe<br />

difference between the equatorial and polar radii fllght map-A map on which ara indicated tha<br />

of the Earth (semimajor and semiminor axea of DroIJoaed Iines 01 Worst ancUor oosifions of<br />

the apharoid) to tts equatorial radius (semimajor<br />

axis). Alao called compreaeion; elllptlclty of<br />

the apharofd. See also eccenttlclty of<br />

alltpae: eccentricity or apharold of<br />

revolution; elllptlclty of elliprsa.<br />

flat—1. (Iiihography) An assembly of<br />

photographic negatives or positives on<br />

goldenrod papar or vinyl acetate tor contact<br />

exposure with a sensitized metal press plate<br />

May contain Ulustralbns as well as text. See<br />

also key flat; layout. 2. (photography)<br />

Lacking in contrast. 3. (optba) See opttcal<br />

flat.<br />

flexura-1. (pendulum) The banding of a<br />

ewinging pendulum, due to its lads of pertecf<br />

rfgidity. 2. (pendulum eupporf) The forced<br />

movament of a parrdulum aupporf caused by<br />

the mofion of ffre swinging pendulum.<br />

fllckar method—1. The alternate projection<br />

of corresponding photographic Imagas onto a<br />

tracing table platen or projection screen, or into<br />

fhe optical frain of a photogrammetric<br />

&x@sure stations. @fht data are piotred on the<br />

best available map 01 the area. Generally used<br />

[or planning purposes.<br />

fllght etrip-A succession of overlapping aerial<br />

photographs Iaken along a single murse. Atao<br />

called atrlp.<br />

fllpplng—The act of superimposing and<br />

mmparing identical areas of two overfapphxg<br />

vertical photographs as an aid in faylflg an<br />

unwntmlled mosaic.<br />

float gage—Any of tha tide or stream gages<br />

which prrrif direct reading of changes of water<br />

height by the action of a float, contained within<br />

a restricted pipe or channel, anached fo a<br />

gradua!ed tape or chain.<br />

floatlng llnes-(JCS) In phologrammetry,<br />

lines connecting the same two points 01 detail<br />

on each print of a alereo pair, used to determine<br />

whether or not the points are intervislble. The<br />

Iinas may be drawn directly onto the prints or<br />

superimposed by means of strips o? Iransparenf<br />

97


I<br />

material.<br />

floetlng mark+ photograrnmelry) A mark<br />

Sean as occupying a pxition in the lhreedlmensbnal<br />

apace formed by the stereoscopic<br />

fueion ot a pair of phonographs and used as a<br />

relerenca mark in examining or measuring the<br />

stereoscopic model.<br />

fbrsflng-(cartography) The technique of<br />

making mlntrr adjwstmenfs of delail In order to<br />

maintain fheir proper relative position.<br />

flood control mep-A special map, or set ot<br />

maps, designed for study and planning the<br />

control of areas subject to inundation.<br />

ftood lld~The porlion of the tide cycle<br />

between low water and the following high water<br />

Also called rlelng tide.<br />

flowllna-The slope axfandino from the<br />

heights abng the neatline to the model datum,<br />

at an angle no greater than 45°, to preclude<br />

forming the ptastic Sheet al a 90- angle al the<br />

nealline of a plastlc reliaf map.<br />

fluorescent maD-A Mao raoroducact wllh<br />

IIuorescem Ink or’ on fluorescern paper, “which”<br />

enables the user to read the map in darkness<br />

under uftraviole! light.<br />

flux-gato magnatomaler-An instrument<br />

desfgned 10 measure the Earth’s magnelic field,<br />

Also called saturabte raactor.<br />

ttuxmeter—An instrument for measuring the<br />

Intensify of a magnetic fiakf.<br />

fly levettng-Sae ftylng levels.<br />

fly-by mathod+aurveytng) A fechrdque 01<br />

dalerminlng approximate elevations where<br />

exlremefy rugged terrain is anmuntered. The<br />

principle Is tdenfical to the two-base method<br />

axcepf the roving barometers are air transpcmed<br />

and raad In tha aircraft as II passes on a level<br />

wtth the topographic feature whose elevIJtiOn is<br />

raquired.<br />

flylng Ievai.s-l. A Ieval line run at the close<br />

of a working day to check the resuffs of an<br />

extended line run In ona direction onfy. Longer<br />

etghts and fewer setups are used as Iha<br />

WfPoee ia Io delect We mislakes. Also Mlted<br />

fly levellng. 2. Level Ihras run with the<br />

engineer’s ordinary ieveling equlpmant but with<br />

MIL-HDBK-850<br />

a dislinctty bw order of accuracy. Enor of cbsure<br />

may be perhaps one fcmt (or mora) times the<br />

square rool of the diilarwe in miles.<br />

total langfh-A general term for the distance<br />

between the canter, vertex, or rear node of a<br />

lens (or tha vetiax of a mirror) ard fhe poinf al<br />

which the hnaga of an Inflnttefy distanf ob)act<br />

comas into critical focus. The term must be<br />

praceded by an adjective such ae “equlvatentor<br />

“calibrate~ 10 have a precise meanfng. Saa<br />

also back focal length; callbretad focal<br />

length; effacttve focat length;<br />

equivalent total length; nominal focal<br />

length.<br />

focal plane-(phonography) Tha plane,<br />

perpendicular to the axis of the lens in tijch<br />

images of points in the object fiekf of the tens<br />

are focused.<br />

focat point—See focus.<br />

focal range—See depth of focus.<br />

focal-plane ptala-A glass plate sat in Iha<br />

camera so that the surface away from tha lens<br />

.@incides with Jhe focal plane. Its purpose is 10<br />

posilwn the emulsion of the film in the focal<br />

plane when the film is physkelly pressed tnto<br />

contact with the glaas plala. Atso catled<br />

contact gtaaa; contact plate.<br />

focus-The point toward which rays of light<br />

converge 10 form an image after passinp<br />

through a fens. Ateo defined as the condition of<br />

sharpest imagery. Also called focal point;<br />

prlnclpal tocus. Sae also hyparfocat<br />

distance; eldereal focus.<br />

foldad opllcs—(phologrammetry) Any optical<br />

or Ians system containing rattecling cemponenfa<br />

which reducas Ihe physical length of a<br />

phonographic or sensing system, or changes the<br />

path of an optical sxis.<br />

foldlng vernier—A single vernier so<br />

conshucred and numbered that it may be read<br />

In aither dhection.<br />

fool-meter rod—A sladia rod, marked in fact<br />

and tanths on one side, and metara and<br />

hundredths on the other side, used to<br />

determina distances and elevations in one unit<br />

of measuramem and to check tham by readings<br />

in a difterent unit.<br />

force tunctlon-See potential.<br />

98


individual major error sources with the quarrfifled<br />

error or uncalainty which each contributes to a<br />

total system accrsracy or probable error.<br />

●rror ●queflo-The probability equation<br />

wtrbzh expresses the laws 01 the occurrence of<br />

random errors. This equation expresses the<br />

relatbnship between obsemed values, PIUS fketorder<br />

cxwredrnn terms, and theoretical vafues.<br />

The error equatimt ie the basis of the method of<br />

feast squares, used fn rhe adjustment o!<br />

obeewalions for detarminirrQ lha most probable<br />

vah.re of a resuft from those observations,<br />

error lntervaf-Sea confldance interval.<br />

error of cloeure-1. (general) The amount<br />

by which a quanftty oMainetY by a serfes of<br />

related measurements diffem from me true or<br />

fixed value of tha same quanffly. Also called<br />

clonlng error; closure. 2. (angles) The<br />

arneum by which lhe actual aum 01 a series of<br />

angles fails 10 equal the theoretically exact value<br />

of that sum. Also called angular error of<br />

cioeute. 3. (azimuth) The amount by which<br />

two va!ues of the azimuth of a line, derived by<br />

dtierent surveys or along ditferanl mutes, fail to<br />

be exactly equal 10 each other. Also called<br />

azimuth error of closure. 4. (leveling) The<br />

amoum by which rwo vatues of the elevation of<br />

the same bench mark, derived by difterem<br />

surveys or through diflarent survay routes or by<br />

independent observations, fail 10 be exacily<br />

equal 10 each olher. Also called levellng error<br />

01 cloaura. See alaa clrcult closure. 5.<br />

~loop) The error In lhe closure of a swvay on<br />

ttseff. Loops do nof pmtecf against systematic<br />

errors in dietenw measurement or blunders in<br />

starting posifbn or azimuth. Atao called foop<br />

error of cloeure. 6. (horizon) The amoum by<br />

which Ihe sum of a series of adjacent measured<br />

horfzomal anglas around a point falls to equal<br />

axactiy 360”. Meaauremarrf of the last angle of<br />

the series Is called cioalng tha horizon; also<br />

callad ctcxauro of horizon; horizon<br />

closure. 7. (triangie) The amount by which the<br />

sum of Ihe three observed angies of a lriangfe<br />

falls to ecpal exactly 1SO” ptus the spherical<br />

axcem of tha triangle. Atao callad closure of<br />

triangie; triangfe cioeure; triangle error<br />

of cfoaure. 8. (traverse) The amount by which<br />

a value of the positkm of a traverse station, as<br />

obtained by computation through a travarse,<br />

fails to agree with another vatue of tha same<br />

atatbn as determined by a different set of<br />

observations or mu!ea of survey. Also calied<br />

closure of traverse; error of survey;<br />

horizontal cloeure error; travarse error<br />

MIL-HDBK-850<br />

87<br />

of cloeure. See also Ilnaar error of<br />

ctoaure; reiative error ot ciosure.<br />

error of Collimation-See collimation<br />

error.<br />

error of Obaewatlon-The difference<br />

between an obsewed value of a quamity and a<br />

value adopted as representing the fdeai or true<br />

vaiue of that quantity.<br />

error of rurt-(micmmeter) The dfflerence, in<br />

eeconds of arc, between the infemMd vaiue of<br />

one tum of lhe micmmeter screw and ifs actual<br />

value as determined by maasuring tha spaca<br />

batwean two adjasant graduation ma~a of Ihe<br />

circle with the micrometer. Aieo calied mn; mn<br />

of micrometer.<br />

error of survey-See error of ciosure,<br />

cfetinition 8.<br />

arror of the maan-See standard error of<br />

the mean.<br />

error—1. The difference between an obearved<br />

or compuled vaiue of a quantify and Iha Idaai or<br />

true value of that quarrtffy. 2. An errer is<br />

genersliy ciasstfied as one of three types: (i) a<br />

blunder (mistake) which can be identified and<br />

corrected; (2) a systematic error, either constant<br />

or variable, which must be compensated foc<br />

and (3) a random error, one of the ctaas of small<br />

inaccuracies due 10 imperfections in equipment,<br />

surrounding condiiiona, or human fimifations.<br />

See aieo rsbsoiute error; actual erro~<br />

accumulative error; biunder;<br />

chronometer error; Clrcult CIOSUrO;<br />

circular error; circular error probable:<br />

cfrcular near-cerfrxlnty error; circular<br />

standard error; clamplng error;<br />

collimation error; compass fndex error;<br />

compensating error; constant ●rror;<br />

curved-path srror; eccentric errori<br />

erratic error; extarnal srrofi gnsdueflon<br />

arror; gross error; Indax error; inherited<br />

error; Instrument srror; iaw of<br />

propagation of error; ilnear error; mean<br />

square error: moduiaflon error: natural<br />

arror; naar-cenafnty error; orthomefric<br />

error; parallactfc error; periodic errors:<br />

peraonaf error; pointing error; poslffonal<br />

error; principabdlafance error; prlnclpalpolnt<br />

error; prlsmafic error; probabie<br />

error; random error; reslduel error;<br />

resultant error; scafe error; shade error;<br />

standard arror; ●yetemsflc error;<br />

fheoretlcal error.


,<br />

’<br />

escape and ovaaion g raphlc—A map,<br />

chart or olher graphic, usually produced on a<br />

f@rhveighi ckmb)e malarial, Spr3@Wally<br />

designed 10 guide personnel to safety from<br />

enemy held territory.<br />

●atrsbllsfrmerrt of tha porl-The average<br />

interval between upper and lower lunar fransif<br />

near fiia of new and full Moon and the naxt<br />

high waler. Ako called common<br />

esrtabllshment; high water full end<br />

CftSn!J@: vulgar eatabllahment. See alsm<br />

Iunllldal Interval.<br />

eetabllahment—Sae Iurtltldal Interval.<br />

etch ellp-A pencil-shaped abrasive used In<br />

rarrwving unwanlad marks on a metal<br />

presaplate. Also called enakeallp.<br />

etched zinc plat~An etched mpy of fhs<br />

Comour drawing of the basa map, used as the<br />

guide in cuffing the slepped ferrain base of a<br />

model for making relief models.<br />

MIL-HDBK-850<br />

etch-l. To rsmove selected areas of the<br />

emulsion either chemically or msnually. 2.<br />

ChemEal Ireatment of a Iithoorahic otate to<br />

make nonprin!lng areas grea~e-fepefienl and<br />

waler-receptive or to produce lhe image on<br />

deep atch @ales. 3. An acid solution mixed with<br />

fhe dampening fountain water on an offsef<br />

press to help mntrol ink on the pressplate,<br />

Euler’s equallofr-A relafion in a parabolic<br />

orbit Irrvofvlng two radius vectors, their chord,<br />

and the time interval between fhem.<br />

Euler”a theorem-A mathematical expression<br />

to obtain the radius of cuwalure of a normal<br />

aecfion in any azimuth on the reference<br />

elllpsold. The azimuth angle, and the radius of<br />

curvature In the rnarid!an and in the prime<br />

verilcal must be known.<br />

EulerIan anglesr-A system of three angles<br />

which uniquely defines with reference to one<br />

coordinate syetem (e.g. Earth as is) fhe<br />

orienlafion of a second coordinate system (e.g.<br />

the axis of an otblf).<br />

Europoan tfatum-The Inifial polrrf of fhk<br />

system Is located at PrMadam, Germany.<br />

Numarous national eystems have been joined<br />

Info a large datum based upon the International<br />

ellipsoid which was orlenfed by fhe<br />

astrogaodefic method. The European and<br />

88<br />

African triangulation chains have been<br />

COnneCfed and the gap of the Alrfcan am<br />

rnaaaurament from Cairo to Cape Town has<br />

been filled. Thus, all of Europa, south Africa,<br />

and Norfh Africa we molded into one system.<br />

Through comnmn survey stations, If was alSO<br />

possible to convert dafa from the Russian<br />

Pulkovo 1932 system to the European Afut’n<br />

and, as a resutf, tha European datum includes<br />

triangulation as far east as the 84th meridian.<br />

Addii”knal tiaa across tha Middla Eaat have<br />

permitted connection of fhe Indian and<br />

European dstums. See also preferred<br />

datum.<br />

evection—A perfurbafion of the Moon in ifs<br />

orbit due fo the attraction of fhe Sun. This<br />

resutts in an Increaae in the ecwrnlrtcity of the<br />

Moon% orbii when the Sun passas the Mmn’s<br />

line of apsldes and a decreasa when<br />

perpendicular 10 il. See also lunar Inequality,<br />

definition 1.<br />

Evaresf apherold (elllpaold)—A reference<br />

ellipsoid having the following approximate<br />

dimensions: semirnajor axis-6,377,276.3<br />

meters: flattening or ellipticity—1 /300.60. Used<br />

in India, Burma, Pakistan, Laos, Cambodia,<br />

Thailand, and Vietnam.. ~.. ---.= -- -.<br />

exaggerated stereo—See hyperatereoecopy.<br />

existent corner—A corner whose position<br />

can be identified by verifying the evidenoa of Ihe<br />

monumenf or its accessories, by raference to<br />

the description that Is contained In the field<br />

notas; or whera the pelnt can be bcated by an<br />

acceptable supplemental survey record, some<br />

phye’cal evidance, or testimony.<br />

exletlng data—Source material and/or<br />

information assumed or knewn to be in the<br />

possession of a gken source and subject to<br />

.ott-shel~ mllacfion, ea in comraaf to dafa<br />

obtained by operational field suweys.<br />

exlf pupil-The image of the aperture stop<br />

formed by aU the lens elements on the image<br />

side of the aperture stop.<br />

exit window-The Image of the field slop<br />

formed by ell the lens elemsnfs on the imege<br />

side of the field slop.<br />

exmerldlan aftltuda-An altitude of a<br />

celestial body near the celeetiaf meridian of fhe<br />

observer 10 which a correction is fo be apptied to


,<br />

1<br />

1<br />

determine the meridian altitude.<br />

●xmorldlan obaarvatlon-Measurement of<br />

the attitude of a celestial body near me celestial<br />

mertdiafl 01 the observer, for conversion to a<br />

mer’idan altitude; or the altitude so measured.<br />

●xperlanca radar pradlctlon—The<br />

determination of size, shape, and relative<br />

intensity of radar returns and a determination of<br />

radar shadow and no-ratum araas based<br />

primarily on the radar knowledge and<br />

experience of the Individual making the<br />

prediction ralher than on proven formulas,<br />

fmvver tables, or graphs. Also called artwork<br />

prediction.<br />

MIL-HDBK-850<br />

experimental map—A sample ot a new map<br />

product prepared either to obtain user approval<br />

of the adequacy of content and symbolization or<br />

to dkclose any problems which may occur in the<br />

various production stages. Also called<br />

prototypa. See also pilot sheet.<br />

explamanl—The difference between an angle<br />

and 360”.<br />

axploltatlon—The process of oblaining usaole<br />

data lrom imageV.<br />

exploratory suway—A survey execuled for<br />

the purpose of obtaining generat Information<br />

concerning areas about which such inlormalion<br />

is rrol a matter of rewrd.<br />

exposure Interval-The time required<br />

between successive exposures 01 a series of<br />

photographs for the purpose of obtaining<br />

dasired forward lap.<br />

exposure atatlon—See alr station.<br />

exposure tlm%The time during which a<br />

Iighf-sensitive material is subjected to the action<br />

Of light.<br />

●xpoaura-1. The total quanlity of fight<br />

received per unit area on a sansilized plate or<br />

tilm; may be expressed as the product of the<br />

Iighl intensity and the exposure time. 2. The act<br />

ot axposiW a Iigh!-sensitive material to a light<br />

source. 3. One individual picfure 01 a strip 01<br />

photographa, ueually called frame.<br />

extended color—See bleed.<br />

exlenalon of conlrol—Execution of<br />

89<br />

addfiional control from exiatlng control by any<br />

method.<br />

axtanalon—1. (surveying) See<br />

prolongation, 2, (photogrammetry)<br />

Extending existing cmlrol Irom a controlled area<br />

info an area wilhoq comrol. The term is usually<br />

ftsrlher qualified as horizontal or vetlical<br />

according to the primary purposa. Also called<br />

horizontal axtenalon; horizontal/vertical<br />

extension; vartlcal exfeneion. See also<br />

centilaver extenalon.<br />

exterior orientation—The determining<br />

(analytically or In a photogrammetric Inatrunrenf)<br />

of the position of the camera Stalin and the<br />

attitude of the taking camera al the Inefam of<br />

axpxiure. In stereoscopic Instrument practice,<br />

exterior orientation is divided into two patiS,<br />

relative and absolute orientat”bn. Also called<br />

outer orlantatlon. See also reeectlon,<br />

definition 3.<br />

exterior perepectlve center—See<br />

perapectlve center.<br />

exterior to e cuwa-Any area adjacent to a<br />

curve Iying toward ils Convax side, the area MI<br />

included wlfhin the circle of which the curve is<br />

pad of fhe circumference.<br />

external distance-The distence from the<br />

vertax O! a circular curve to the middle point of<br />

the curve.<br />

axternal arror—The repealability of a<br />

measurement with any condition extraneous to<br />

!ha measuring method itself changed;<br />

contrasted to internal error. See alao standard<br />

error.<br />

extra forealght-(leveling) The rod raading<br />

made at an inSttUmeM station In a fine of Ievek<br />

and on a leveling rod standing on a bench mark<br />

or another point not In the @XIflfWOUa WIe of<br />

levels. In spirit leveling fhere may be one or<br />

more extra foresight from a single instrument<br />

station or setup, but Ihere can be only one<br />

backsight and one foresight from any one<br />

instrument station.<br />

exfrapolatlon—The process of estimating the<br />

value of a quantity beyond the limits of krmwn<br />

values by assuming that the rate or system of<br />

change between the last few known vafues<br />

continues.<br />

eye baaa—See Interocular dlatance.


f.number—See ralatlve aperture.<br />

la-l. (imagery) The emulsbn side of a<br />

negative or faycul plate, or the prfrrting surface<br />

of a pfafe. 2. (topology) A two-dimensional<br />

to@ogical enfffy defined as an undivided are<br />

surrounded by topological edges represeming<br />

all or part of the extent of a feature or of an<br />

attributed area.<br />

tacslmllo chart-see modlflsrd facttlmlle<br />

chart.<br />

lrsctorad tranaparancy—A system of radar<br />

simulation which ufifizea a pair of phonographic<br />

ima9e6 on a glass pfate or plates to store<br />

topographic and radar reflection data. The data<br />

are scanned by e ffylng-spot scanner cathoderay<br />

lube, and the density of the images is read<br />

by two photomulfiifier tubes. The hvo planar<br />

dimensions of the two imagea are the x- and y-<br />

&lmenaiorra of the topography and reflectance<br />

data respectively. The dansifies of the<br />

reflectance images ara used to store fhe intrinsic<br />

strength of radar target rallectance. The images<br />

are identical in their x- end y-values but<br />

separated in one dimension by me optical<br />

spacing of the dual readout syslem. Also called<br />

land mass elmuialor plete.<br />

factory acceptance test (FAT)-A formal<br />

test of the system under pmwrament in the<br />

manufacturers envfmnmerrf In order to verify<br />

succeesfut pmducfion of hardware or Software.<br />

Recipient personnel witness lhe test to verify<br />

requirements and successful product generation<br />

before the system is shipped lo the recipiant.<br />

FAF block—A block of 1024 by 1024 pixels of<br />

image data. See also fast access fOrMal.<br />

fafflng tfda-See ebb tide.<br />

fallln#—The distance by which e rarulom line<br />

falls to fhe right or left of a comer on whch the<br />

tnse line IS too cbse. Usually the dhectbn of<br />

falling fa expressed m cardinal.<br />

falee bearing—The difference befween the<br />

true bearlno and the back bearinc! caused by<br />

the mnve~ence of maridiana, -<br />

fafae See Infrared.<br />

MIL-HDBK-850<br />

F<br />

false eesting-A value assigned to the orl@<br />

of castings, in a grid cmrdinate system, to avoid<br />

the inmnvenience of using negative<br />

coordinates. See also grkt coordlnataa.<br />

falaa fix p~fSablllty-A stallsticat value or<br />

ratio which reflects the likelihood of a fafSe<br />

match ocasm”ng between Weeforsd digilal<br />

cartographic data and data or Imagery acquired<br />

by electronic aerial sensor eystama. See also<br />

Imege corralatlon; terrain contour<br />

matchkrg (TERCOM); terrain corralatlon.<br />

false horlzor+A line resembling the visible<br />

horfzon, but above or bafow ft.<br />

falsa norfhlng-A value assigned fo the origin<br />

of norfhh’rgs, in a grid coordinate system, to<br />

avoid the inconvenience of uairsg negalive<br />

coordinate. Sae also grid coordfnatea.<br />

falsa orlgln-(JCS) A fixed polm to the south<br />

and west of a grid zone from which grid<br />

distances are measured eastward and<br />

northward, See aleo grid orlg in.<br />

felee paraltax--(JCS) The apParent vetil=l<br />

displacamerrt of an object from its true posifiirr<br />

when viewed stereoscopically, due to movement<br />

ot the object ifseff as well as to change in the<br />

poinl of Observation.<br />

false atere*An Imaginary Impression of<br />

aleraoscopic relief. See also paeudoacopfc<br />

sferao.<br />

fan camera photography—(JCS]<br />

Phonography taken simultaneously by an<br />

assembly of three or more cameras,<br />

systematically installed at fised angles refatfve to<br />

each other so as to provide wide lateral<br />

coverage with overkpplng images. See also<br />

trlcemera photography.<br />

fan camara%(JCS) An assembly of three or<br />

more cameras systematically disposed at fixed<br />

angies relafive to each othar so as to provide<br />

wide lateral coverage with overlapping Imagas.<br />

fasf acceea formaf (FAF)-A filing scheme<br />

for breaking digital imagerf into smaller chunks<br />

of data. See also FAF block.<br />

fathogram—A graphic rsmrd of depth<br />

9“1


measurements obtained by echo sounding<br />

equipment. Also called echogram.<br />

fsthom curva-.See ctaplh contour.<br />

fathom llne-See depth contour.<br />

Fathometer—A trade name for an echo<br />

sounder.<br />

Faye ●nomaly-See fre-alr anomaly.<br />

Faye correcflon-See free-air eorractlon,<br />

MIL-HDBK-850<br />

featheredging—1. (cartography) The<br />

techniqua of prograsslvely dropping contours, to<br />

avoid congestion on steep slopes, and tapering<br />

the line we”ght near the end of the contour to be<br />

droppad. Alao called faatherlng. 2.<br />

(pholorrmaaiddng) The thinning of overlapping<br />

edoes of Dhotooralstrs befora aesemblino into a<br />

mc-saic In “order-to “make match lines les~<br />

noticaabte. Wfsan ovarkpplrrg edges are<br />

feathered, shadows and sharp changes in<br />

contrast are reduced or eliminated. Also called<br />

feathering.<br />

isratherlrrg-See taatheredg}ng.<br />

Feeture ●nd Attribute Coding Catelog<br />

(FACC)—DMA Glossary which contains the<br />

Feature and Attribute Coding Standard (a<br />

modiiilbn o! DMA’s FACS). See<br />

Feaiure/Attribute Coding Standard.<br />

Feature ExtractIon Segmenf (FE/S)—A<br />

segment of DMA’s MARK S5 which Implement<br />

a mrrtpster supported, analfilcal slereoploffer<br />

system capable of extracting feature data. This<br />

segment integrates. on a alngle aystam, all of<br />

the various atepa “revolved in the mostly manual<br />

feature attraction pmcasa prior to DPS. Sae<br />

also MARK 85; Dlgltal ProductIon<br />

Sy*tem.<br />

feature ●nalyala code (f AC) number—A<br />

unque number (usually sequanfial) assigned to<br />

each area or feature portrayad on the feature<br />

manuacr@ ar-sl used to relata feature analyais<br />

data tabfa (FADT) information to the digital<br />

irsforn?dticn whkh partrays the shape of fhe<br />

feature. See also Iaature analyels data<br />

table.<br />

faature analyala data fable (FADT)-A<br />

tabfe containing the feature anatyais code<br />

numbers and the numeric codes which<br />

represent the physkal characferfstba of features<br />

selectad for portrayal. Sae afSO feature<br />

analyata code (FAC) number.<br />

feature analysla-The process of bcafing,<br />

examining, and classifying Ihe physkal<br />

characferfafica of cuffural features on the earlh’s<br />

surface.<br />

feature attrlbuW-A properly of a feature.<br />

faafure claee-A Sel of feafures eharfrrg a<br />

consistem set of affrlbute types. A feature class<br />

is irr@emerrted by using a aet 01 fablea that<br />

Includes at least one primitive tabte and al Iaast<br />

ona attribute fable. A feature class haa the<br />

same mhsmns (attribute types) of atfrfbufe<br />

Information Ior each Iaature. Cfasses of features<br />

are created in order to allow the relatkmal mdel<br />

to operata on fhem as sets. Every feature cfass<br />

has one and only ona feature table.<br />

faatura coda-A unique identifier assigned to<br />

a teature.<br />

feature extraction—The arf of exfracficg and<br />

classifying features contained in an image.<br />

feature Identlflcatlon data (FID)-<br />

Information pertaining to the dass~cation of a<br />

faature aa to kind, function, and dascrfptkrn,<br />

e.g., heavy tabricafion industry wfth saw-footh<br />

rool: lruss bridge; powerfhne pylon, etc. Each<br />

classification has a unique feature identification<br />

code. See also feat ura anal yala daf a<br />

table, faature analyala code; feature<br />

analyala.<br />

featura fable—A table mada up of the<br />

primary-keyed rows of the features in a feature<br />

class. These rows collectively form the feature<br />

table for that feature class.<br />

faature typ*A classification of features into<br />

three categories: (1) point of feature-an objea<br />

whose Iocariin can ba described by a single aet<br />

of coordinates; (2) linear (or lines) featue<br />

pomayed by a iine that doea nol represent an<br />

area: (3) areal feature-a topographic feature,<br />

such as sand, swamp, vegetation, etc., which<br />

extends over an area or in d~ifal mapping any<br />

area encbsad by a delimiting line that haa any<br />

unique characteristic, e.g., industrial area, forest,<br />

residential araa, etc. Faature fypa is thus an<br />

attribute dafining fhe topologic propady ,of a<br />

Ieature (point, fine, or area).<br />

92<br />

leature.oriented—A term used to describe


MIL-HDBK-850<br />

the approach for encoding geographic entities in<br />

which a series of Interrelated geographic objects<br />

are o~nlzed into a network-like structure of<br />

data and predefine relationships.<br />

Feature/Attribute Coding Standard<br />

(FACS)-DMA standard for assigning features,<br />

effribufes, values, and relationships 10 all digital<br />

errfifiea under the Dgiral Pmducfiin System.<br />

See also Feature end Attribute Coding<br />

Catalog.<br />

leeture-A set of phenomens with common<br />

attributes and relatb”nefsipe. The concept of<br />

feature encompasses both entity and object.<br />

See also Primary row.<br />

Fedaral Information Processing<br />

Standards (FIPS)-Official source within the<br />

Federal Government for information processing<br />

standards. FIPS are developed by the Institute<br />

for Computer ScierCes and Technology at the<br />

National Institute of Standards and Technobgy<br />

(NIST, formerfy called the National Bureau of<br />

Standards).<br />

feff nids-The top or smooth side o! paper<br />

thal is contacted by tha Ieff bell tor exlracfion 01<br />

moisture during manufacture, This is the correcf<br />

side of the paper tor printing.<br />

fence—1. A tine of readout or tracking slat ions<br />

for pickup of signals from an orbiting satellite. 2.<br />

A fine or network of radar or radio stations for<br />

detecfbn of a sateltile In orbit.<br />

fermenting dough theory—See Pratt.<br />

Hayford theory of Isostesy.<br />

lerrotype-To burnish photographic prints by<br />

equeegeaing WEI upon a japannad sheet of imn<br />

or stainless plale and allowing ro dry. This<br />

produces a harder, glossler surface on the<br />

photographic prinl.<br />

flbar optics-A device for relayirg an image<br />

by MSah5 of a large number of transparent<br />

fiiers (filaments) by rnuffiile total infernal<br />

raflecfion. The fibers are most comrnonfy glasa<br />

and less often a hlohlv transparent plastic. Each<br />

fiber carlas only orie clement of the image, so<br />

that the image is a mosaic in which the cell size<br />

is the fiir cross secfbn rather than a<br />

ccmtinuoua pklure.<br />

flcflfloue equator-A raferenca Iina sarvlng<br />

as the origin for measurement of fictitious<br />

Iatlfude.<br />

flctlfloua gratlculs-The nefwor% of fines<br />

representing ficflfious parellefs and flcfifbus<br />

meridians on a meP or chart. see also obllque<br />

graflcule; transferee gratlcule.<br />

flcfltloua latffude-Angular dlsfance from a<br />

tictilious equator. It may be celled trsnsvame,<br />

oblique, or grfd Iatituda depending uF9n the<br />

type 01 fictitious equator.<br />

flctltlous longltud~The arc of Iicrifioue<br />

aquator between tha prime fictitious rnerfdian<br />

and any given flcfifbus merfdian. II may be<br />

called transverse, oblique, or grid<br />

Iongltude depending upon tha type of fiiifiius<br />

meridian.<br />

Ilctitlous loxodrome—See fictitious<br />

rhumb line.<br />

flctltlous Ioxodromlc curve-See flctltloue<br />

rhumb llne.<br />

flctltloue merldlan-One of a series of great<br />

circles or fines used in place of a meridian for<br />

certain purposes. It may be called tranaverea,<br />

oblique, or grid meridian depending upon<br />

the type of fictitious meridian. See SSISoprime<br />

tlctltlous merldlan.<br />

flcftflous parallel—A circle or fine parallel to a<br />

fictitious equator, conrsecfing all points of squsl<br />

fictitious Iaiitude. II may be called Wansverae,<br />

OfSllqUe, or grid parallel depending upon the<br />

type of ficfitlous equator.<br />

flcfltioua pole-One of the two points 90”<br />

fmm a ficfltlous equator. tt may be celled<br />

tranaverae or obllqua pole depending upon<br />

the type of fictitious equator.<br />

tlctltlous rhumb llne-A line making the<br />

same oblique angle with all ficfifiius meridiirsa.<br />

It may be called traneveree, obllque, or grid<br />

rhumb line depending upon the type of<br />

fictitious meridian. Also cal~ed flcfltloua<br />

Ioxodrome; fictltloue Ioxodromlc curve.<br />

flctllloue eun—A ficfifbus point termed fhe<br />

maan sun, which is Imagined 10 move at a<br />

uniform rate along fhe Equator, ffs rate of<br />

motion being such thst If mSkeS one apparent<br />

revolution around the Earth In the same time as<br />

the actual Sun-that is, in 1 year.<br />

flctlfloua year—The period between<br />

93


successive returns of the Sun 10 a sidereal hour<br />

angle 0180” (about January 1). The length of<br />

the Iicflfkssa year Is the same as that of the<br />

tropisxsl year, since tmlh are based upm the<br />

posffiin ot \ha Sun whh respect to lha vernal<br />

equinox. Also called Beaeellan year.<br />

flcfltlouts-in cartography, pertaining to or<br />

measured from an arbdrary referetwe fine.<br />

fldellty-Tha degrea with which a system<br />

acxxrralely reproduces the data inpul into it.<br />

flduclssl exea-The lines pkrlng opposite<br />

fiducial martss on a photograph. The x-axis Is<br />

generally rmnaidered 10 lx the one nearfy<br />

parallel wifh the line of fflght.<br />

flduclal merk(s>l. (surveying) An index line<br />

or point. A line or point used as a basis of<br />

reference. 2. (JCS) (photogrammetry) See<br />

Collimetlng marks. 3. Also, markers in any<br />

instrument which deline the axes whose<br />

intersection fixes Ihe principal point of a<br />

phofogreph arsl fuffills the requirements of<br />

interfor orientation.<br />

field csrllbratlon-A term aenerallv aozdied<br />

where only e corrridrration of-field in-d Ott’ice<br />

computer techniques are available to check<br />

insfnsment accuracy. Adjustments, other than<br />

normal operator edius!ments, cannot be made<br />

during field calibration.<br />

field chack-lhe operation of checking a map<br />

compilation manuscript on the ground. See also<br />

flehl cleeslflcatlon.<br />

MIL-HDBK-850<br />

field claeelflcntlon-Field Inspection and<br />

idenfffiiation of features which a map compiler is<br />

unable to de fineate; identification and<br />

delineation of pofitcal lxsundary lines, place<br />

names, road classfficatkrns, buildings hidden by<br />

lrees, and so forth. Field classification may be<br />

Included aa parf of the OJnfrol survey efiorf and<br />

normally Ls completed prior to the actual<br />

slereocompilation phase, See also field<br />

Inapectlon.<br />

field comparator-A short line whose Iengfh<br />

b measured wiih accuracy and precision, and Is<br />

used to check the iengths of apparatus (tapes)<br />

used in the actual fieid operations. Also called<br />

calibration course; comparator beaa.<br />

field complation—A combination of fiefd<br />

inspections or surveys, either before or after<br />

compilation, to classify and fnmplefe the map<br />

content, correct erroneous date, end add<br />

Information such es names, civil boundaries,<br />

and similar classifiifion data. Its purpose is to<br />

fill in or confirm that portion of a map manuscript<br />

prepared by alareocompilation.<br />

Ileid contouring-Corrtouring a topographic<br />

map by field methods accomplished by<br />

planateble surveys on a prepared base or by<br />

stadia survey. Generaliy, this operation applies<br />

to Ierrain unsuitable for contouring by<br />

photogrammelric methods. Also used in limited<br />

areas when engineering design (drainage)<br />

requires 1-toot contours. See also contour<br />

aketchlng.<br />

field control-(JC S) A series of points whose<br />

relafive positions and efevatbns are known.<br />

These positions are usad in basic data in<br />

mapping and chariing. Normally, these positions<br />

ara established by survey malhods and are<br />

sometimes referred to as trig control or<br />

trigonometrical net (work). See also<br />

common control (arflllary); control<br />

pohrt; ground control.<br />

fiafd correction copy—A map or tracing<br />

prepared in the field, delineating corrections fOr<br />

subsequent reproduction of a map.<br />

field correcIlon—Adjustments made to field<br />

measurements, such as angles or distances, to<br />

correcl lor geometric or length discrepancies.<br />

field alevaUon-An elevation taken from the<br />

field computation of a line of levels,<br />

field lnapectlon—The process of comparing<br />

asrial photographs with condMcms as lhey exist<br />

on the grourxl, and of obtaining informatbn to<br />

supplement or clarity that which Is not readily<br />

discernible on the photographs themselves.<br />

Also called classlftcatlon survey.<br />

field lntenslty—See field strength.<br />

field of view—(JCS) in photography, the<br />

angle between two rays peasing through the<br />

perspective center (rear nodal palm) of a<br />

camera lens to the IWO oppmite sides of the<br />

format. Not to be can fused with angle of<br />

view. See also angla of view.<br />

field posltlon—A position computed while<br />

lie!d work is in progress to determine lhe<br />

acceplabifity of the observations or to provide a<br />

preliminary position for othar purposes.<br />

94


I<br />

Ileld shaat-The hydrographe~s or<br />

tof%rgmphers wwk sheet: if presents e graphic<br />

disptay of all surlace and subsurface tealures in<br />

the area being surveyed, See also tsoal<br />

sheet.<br />

field Stttndarcflxation of tapeThe<br />

Comparison of the kmgth of a tape to be used<br />

tor survey measurements with the length of a<br />

standard tape, to delerrrrlrre the true length of<br />

the former.<br />

ikald Mop-The @ysical element (such as a<br />

afop, diaphragm, or lens periphery) of an optical<br />

syalem which limits the field of view aoverad by<br />

the system. See also aperture atop.<br />

MIL-HDBK-850<br />

Itlm negfrtlve-See negative, definition 1.<br />

film poeltlvs-see poaltlve, delinilkm 1.<br />

fflm tItllng-See tlttlng.<br />

film—A film base which Is mated wffh a fiiht<br />

sensiliva emulsion for use in a camera or<br />

printing frame. See also aerial film;<br />

autoacreen film; cartographic film:<br />

Infrared film; Sfable-baae fnm; elrlp film;<br />

topographic basa film.<br />

fllterlng—The removal of certain spectral or<br />

spatial frequencies to enhance features In the<br />

remalnlng Image.<br />

fiald atrangth—For any physical field, Ihe ffux. fi)iar~ny transparent material which, by<br />

densffy, intensity, or gradient of the field al the absorption, selacfively modlflas the light<br />

point in question, Also called fletd Intensity. transmlfted through an optfcal system.<br />

field—An individual data element. In an<br />

attribute table, a field is a single attribute value<br />

of a single entfiy.<br />

figure adjustment—(survey ing) The<br />

adjustment o! a single chain of triangles made<br />

to satisfy the requirement that me sum of me<br />

angles in each triangle equals 180”, and in !he<br />

case of a quadrilateral that lhe sum of the<br />

ar@es equal 360°. An office computation.<br />

figure of the Earth-See geold.<br />

flfar m lcrometer—A device attached to a<br />

telescope or microsmpe, consisting of a wire<br />

lhraed (fitamerrl) connected with a screw in such<br />

manner that as the Xrew is turned, the wire<br />

moves through a continuous succession of<br />

parallel positions, all in the focal plane of Ihe<br />

Instrument<br />

ftle structurh’rg-The logical form of a file that<br />

results from applying a particular file organization<br />

and fayout 10 a group of records.<br />

film bnee-A thin, flexible, transparent sheet<br />

of stabie plastic materiel to which a lighlsensifib’e<br />

emulsion may be applied.<br />

fllnt dlatorZlon-The dimensional changes<br />

which occur In photographic film wifh changes in<br />

humkfiiy or famperature, or from aging,<br />

handling, or other causes.<br />

film moselc—See panel base.<br />

flnaf compoalte-A conzposhe of the pdncfpal<br />

color separations made after all mrrectbns have<br />

been completed.<br />

FIR EFINDER Operational Date Base<br />

(FODB)-Digitized trisxiel coordinates collected<br />

on the preferred datum (usually WGS S4) at 125<br />

meter post spacing within 100 by 125 km araas.<br />

Values are mllecfed from DTED and<br />

transformed to UTM coordinates, with vartk.sl<br />

values assigned wtihin 256 elevation bands<br />

dafined between minimum and maximum<br />

values occurring in the area. Soume mpee are a<br />

special-purpose DMA producf Ihaf require<br />

dubbing onto field cassetfas prfor to use by fhe<br />

FIREFINDER system. The FIREFINDER provides<br />

high speed compufalion of mortar and field<br />

ariillery firing positicns from radar lnte~apfs of<br />

projacWe trajectories.<br />

firing charf-(JCS) Map, photomap, or grid<br />

sheet showing the relative horizontal and vertical<br />

positions of batteries, base points, baae point<br />

lines, check points, targets, and other details<br />

needed in praparing firing data.<br />

flrat approximation charf-See hletorlcel<br />

chart.<br />

flrat of Aries—See first point of Aries;<br />

vernal equinox.<br />

first point of Arlea- Also called flraf of<br />

Arlea. See vernal equinox.<br />

95


flrot polnf of Cancer-See summer<br />

eoleflce, definition 1.<br />

flref point of Ceprtcornus-See winter<br />

eolstlce, definition 1.<br />

first point of Llbre-See autumnal<br />

equinox.<br />

flraf.ordar bench mark-A bench mark<br />

mnneded to [ha datum (Usually mean saa<br />

Ievef) by continuous first-order levell~.<br />

flret-order lovellng—Spirit Ievatlng<br />

Conforming to the speciilcstlona of the current<br />

‘Cleeaifkafiin, Standards of Accuracy and<br />

General Specifications of Geodetic Control<br />

Surveys; Formerly known as preclae Ievallng<br />

and Iavellng of high preCISlOn.<br />

Recommended lor primaty Nationsl Nerworlm,<br />

as a basis for all subordinate elevation<br />

determlnafions, scientific studies such as cruslal<br />

movemanf over large regions, extensive<br />

engineering projects such as hydroelectric<br />

dams. Such leveling generally includes the<br />

determination of geopotenlial values through<br />

simu!4ane0us gravity measurements.<br />

flrsd-order level—A leveling inatrumenl which<br />

meate the folbwing Crfterta: (1) tha Sensilivit y 01<br />

the level bubble vial must be 10“ of arc or less<br />

per division of 2 mm: (2) the instrument must be<br />

wnstrucfed of bw expsnsbn metal 10 minjmlze<br />

lhe effect of unequal heating; (3) the objective<br />

lens must have an effective opening of at least<br />

40 mm and a magnification of 40X,<br />

first.ordar travarse-A survey traverse which<br />

extends between ad@sted positions of olher<br />

first-order control surveys and conforms to the<br />

crmenf spesiflzafions of first-order traverse, per<br />

“Cfessifiition, Standamb of Amuracy and<br />

General Specffbstions of Geodetic Control<br />

Surveys. -<br />

flraf-order triangulation—First-order<br />

trianguladcn was at one time known as primery<br />

trlangutatlon: changed in 1921 to preciee<br />

triangulation; and In 1925 to first-order<br />

Irfangulalion. Theee surveys contorm to the<br />

current ‘Claeetfiition, Standards of Accuracy<br />

and Ganeral Specifications of GecdeW Cormol<br />

Surveys.” Racummended for primary National<br />

Networks, aa a basis for all subotilnate surveys;<br />

metropolitan area survey:, where high value is<br />

attached 10 land and Ifs hne of communication<br />

frontage; and in scientific etudies, such as<br />

MIL-HDBK-850<br />

crustal movement and space expiration.<br />

flraf-ofdar wotk-The designation given<br />

survey work 01 the Nlgheet prescribed order 01<br />

precision and accuracy. Such eurveya were<br />

formerly called primary.<br />

Fischer allipeold of 1960-A reference<br />

ellipsoid wtih fwu primary uses. In tha Mercury<br />

datum if has the approximate dhmsnsions of<br />

semima]or axis-6 .378,166.0 meters, and the<br />

flattening or ellipticlly-1/296,3. in the South<br />

ASa datum the sarnlmajor axis is 6,378,155.0<br />

meters, and the flattening or eliipficffy Is 1/238.3.<br />

Fischer laval-A dumpy level capable of fimtorder<br />

leveling.<br />

flxad alavatlon—An elevatlon which has<br />

been adopted, either as a resutf of tide<br />

observations or pravious adjustment of spirit<br />

leveling, and which is held at its accepted value<br />

in any subsequent adjustment.<br />

fixed posltlon—See adjueted posltlon.<br />

fixed salelllte—See aynchronosse<br />

aatelllle.<br />

flxad-length recora*A computer data<br />

element format, in which all recorde have the<br />

same length, These remrds allow direct access<br />

without searching or indices. See also<br />

variable-length records.<br />

fixed-ratio pantograph—See pantograph.<br />

fixed-rstlo projection prfntar-A dlaposnlve<br />

prinler hsvinQ an optical ayslem in whiih a lens<br />

is placed between the negative and the<br />

dispositive plate, Ihe object and image<br />

distances being set al nominal values according<br />

to the laws of optics, but with freedom of<br />

adjustment within narrow Ilmlts, to produce<br />

diapc.silives whose Scala is al a predetermined<br />

rafio to the negative scale.<br />

tixer nerwoti+JCS) A combination of redb<br />

or radar dkectlon firdng installations whkh,<br />

operating in mnjuncfiorr, are capable of plotting<br />

the positon relative to fhe ground of an aircraft<br />

in flight.<br />

flxlng—The process of rendering a devatoped<br />

photographic image permanent by removing the<br />

unaffected light-sensitive material.<br />

96


-– .<br />

fix—A relatively accurate position determined<br />

withoul relerence lo any former position, from<br />

terrestrial, electronic, or aswcmomk data Also,<br />

the poinl thus established.<br />

flare trkfrngulksllon-A method of<br />

triangutetkrn In whicff slrrrultaneous obaervalions<br />

are made on parachute flares. This method is<br />

used for exlending triaWulatlon over lines too<br />

long to be obsewed by ordinary methods.<br />

flash sppafatue-An auxllia~ apparatus<br />

used In lining a pendulum during obsewalione<br />

for intensity of gravity.<br />

flash plate-See calibration plare.<br />

flat model—Any spatial model which is<br />

capable of being leveled. See also warpad<br />

model.<br />

flat stock-1. Charta or maps which are not<br />

folded and kept for filling official and sales<br />

orders, 2. Flat sheets of map paper as opposed<br />

10 roll paper.<br />

flat tlnl screen—See dot screen.<br />

flatienlng (of the Earth)-Ttre ratio of the<br />

difference between the equatorial and polar radii<br />

of the Eaflh (semimajor and semiminor axes of<br />

the spherokf) to its equatorial radius (semimajor<br />

axis). Also called Compresalon; elllptlclty ot<br />

the epherold. See also eccentricity rrf<br />

sllipee; accentrlclty 01 epherold of<br />

revolution; ●lllptlclty or elllpee.<br />

flat—1. (Iiihmraphy) An assembly of<br />

photographic negatives or positives on<br />

goldenrod paper or vinyl acetate for contact<br />

exposure wilh a sanitized metal press plate.<br />

May cxrntain illuatratbns as wall as Iexl, See<br />

also key flat; Ieyout. 2. (photography)<br />

Lacklno<br />

flat. -<br />

in comrast. 3. foolica) . See oLstlcal<br />

Ilaxurel. (pendulum) The bending of a<br />

swinging pendulum, due to ifs lack of perfect<br />

rfgidity. 2. (pendulum suppert) The forced<br />

movement of a pendulum suppert caused by<br />

the rnotbn of tha swinging pendulum.<br />

fllckar method-1. The allemale projection<br />

01 mrresponding photographic imagea onto a<br />

fracing table platen or projection screen, or into<br />

fhe opllcal train of a photogrammefric<br />

MIL-HDBK-850<br />

Instrument. 2. (sleraoscopy) Tfte alternate<br />

blinking of the eyes and mentafty comparing the<br />

appearance of images in a sleraoacapk pair to<br />

delermine differe~es befwaen the IWO photos.<br />

Illg ht altllude-The vertical distance above a<br />

given datum, usually maan sea level, 01 en<br />

aircratl in flight.<br />

fllght block—An ad]ustabfa unit of<br />

photographic sxrverage consisting of overlapping<br />

strips o! photography. A minimum size block<br />

consists of al least three overfeppiig fliiht strips.<br />

flight charf-Sae route chsrs, definition 2.<br />

fllght information and air taCllltlaSS<br />

date-Data concerning airfields and seapfana<br />

stations and ralated information required for fha<br />

operation of aircraft.<br />

fllg ht Ilne apsclrrg-Tha distance batween<br />

adjacent tracka in a series of parallal aerial<br />

photographic flight strips.<br />

fllght llna-(JCS) In air photographic<br />

reconnaissance, the prescribed ground pafh<br />

over which en air vehicle moves during Ihe<br />

executior, of its photo mission.<br />

flight map-A map on which are Indicated tha<br />

proposed linee of fligttf arrdlor positions of<br />

exposure stations. FliQhl data are plotted on the<br />

best available map 01 Ihe area. Genaraliy used<br />

for planning purposes.<br />

flight atrlp-A succession of overlapping aerial<br />

phonographs Iaken along a single murse. Afeo<br />

called atrlp.<br />

fllpplng—The act of superimposing and<br />

comparing identical areas of two ovarfappfng<br />

vertical photographs as an aid in ISying an<br />

uncontrolled mcsaic.<br />

float gage—Any of the tide or stream gagas<br />

which permit direct reading of changea of water<br />

height by the action of a fbat, conlakred wffhin<br />

a restricted pipe or channel, attached to a<br />

graduated tape or chain.<br />

floating llnee-(JCS) In phologrammetry,<br />

Iinas connecting the same hvo poima of detail<br />

on each print of a slereo pair, used to determiwe<br />

whether or not the points are Intervisible. The<br />

lines may be drawn diracffy onto the pdrtfe or<br />

superimposed by means of strips of transparent<br />

17


1’<br />

,’<br />

,-<br />

material.<br />

Iloetlng mark-( photogrammelry) A mark<br />

seen as occupying a poaifion in the threedimensbnal<br />

apaca formed by the stereoscopic<br />

fusion of a pair of photographs and used as a<br />

rafarenca mark in examining or measuri~ the<br />

stereoscopic mcdel.<br />

lloetlng-(cartography) The technique of<br />

making minor adjuatnwnrs of detail in order 10<br />

maintain their pruper relativa position.<br />

flood control map-A special map, or set of<br />

msP, *ai!3@ for study and planning the<br />

control of areas subject to inu ndafiin.<br />

flood tide-The portion of the tide cycle<br />

between low water and the following high water.<br />

Also called rlslng tlda.<br />

IIOWllnS-The slope extending from the<br />

heighte abng the neatline to the model datum,<br />

al en angle no greater than 45°, to preclude<br />

Iorming the plaslfc shee! at a 90” angle at the<br />

neatiine of a plasfic relief map.<br />

fluorescent map-A map reproduced wllh<br />

fluorescent ink or on fluorescerrl paper, which<br />

enables the user to read the map in darkness<br />

undar ulfravlofaf light.<br />

flux-gate magnatometar—An instrument<br />

designed to measure the Earth’s magnetic field.<br />

Also called aaturabla reactor.<br />

ffuxmefer-An krsfmmenf for measuring the<br />

infeneity of a magnatlc field.<br />

fly lavaling—See flylng Iavala.<br />

fly-by mathod-(surveying) A technique of<br />

datermhrlng approximate elevations where<br />

extremely rugged terrain is enmuntered. The<br />

principle Is Idarrtkal to the two-base method<br />

except the roving barometers are air transported<br />

and read in the aircraft as it passes on a level<br />

with the topographic teature whoee elevation is<br />

required.<br />

Itying Ievale-1. A level tine run at the close<br />

of a working day fo chack the results of an<br />

extended fine run In one direction only. Longer<br />

slghfs and fewer setups are used as fhe<br />

pur’pese is 10 deteci large miefakes. Also callad<br />

fly Iavalhrg. 2. Level Ilnes run with the<br />

engineer’s ordinary leveling equipment buf wllh<br />

—<br />

MIL-HDBK-850<br />

a distinctly bw order of acsuracy. Enor of cbsure<br />

may be perhaps one foot [or more) fintas the<br />

square root of the dstanm in mifee.<br />

focal len@r-A general farm for tha distance<br />

between the center, vertex, or rear rmda of a<br />

lens (or the vartex of a mirror) amf the point al<br />

which tha Image of an Infkrffefy distant object<br />

mmas into critical fores. The term must be<br />

preceded by an adjective such as %qulvalen!or<br />

%slibrated- 10 have a precise rrwankrg. See<br />

also back total Iangth; callbratad local<br />

length; ef Iectlve local Iangth;<br />

equivalent focal Iangth; nominal focaf<br />

Iangth.<br />

focal plane--(pholography) The plane,<br />

perpendicular to the axis of fhe lens in which<br />

images 01 points in the object tieki 01 the lens<br />

are focused.<br />

focal point—See focus.<br />

focal renge—See depth of Iocua.<br />

focal.plane plateA glass plate set in the<br />

camera so that the surface away from the lens<br />

mincides wifh the focal plane. Its puqmse is to<br />

position the emulsion of the film in fhe focal<br />

plane when fhe film is pnye.icelly pressed Into<br />

confad with Ihe glass plate. Afso called<br />

contact glaaa; contact pteta.<br />

tocua-The point toward which raye of light<br />

mnverge to form an image aftar passing<br />

through a WM. Also defhmd as tha condMon of<br />

sharpest imagery, Also called fOCaf point;<br />

prlnclpal focus. See a160 hyperfocal<br />

dlstanca; sideraal focus.<br />

folded optlca—(photogrammetry) Any optical<br />

or lens system containing reflecting ccmnponams<br />

which reduces the phyalcal iengfh of a<br />

photographic or sensing system, or changas the<br />

path ot an optkal axis.<br />

foldlng varnler—A single vernier so<br />

mnstmcted and numbered that it may be raad<br />

in eilher direction.<br />

toot.meter rod—A stadia rod, marked in feet<br />

and tenths on one side, and meters and<br />

hundredths on the other aide, used to<br />

determine distances and elevatbns in one unit<br />

of maasuremenf and to check them by readings<br />

in a different unit,<br />

torca tunction—See potential.<br />

98


MIL-HDBK-850<br />

foresight—l, An Observation of the distance irectel-A family of mafhematicel fumtione<br />

arsl direclion to the nest instrument station, 2. which are somatimss uaad to describe natural<br />

(trarralt traverse) A peint set ahead 10 be used phenomena and shapes such as coastlines.<br />

tor reference wfren resetting the transil on line or irrountains, river pafk%s, etc.<br />

when verifying the alignment. 3. (leveling) The<br />

reading on e rod that is Ireti at a point whose<br />

etevation Is to be determined. Also called<br />

mlnue ●ight. See also backsight.<br />

forestry map-A map prepared principally to<br />

shcw the s)ze, ctarrsj)y, kiml, ard value of Iraes<br />

on a given area.<br />

form llnaa+JCS) Lines resembling contours,<br />

but representing no actual elevations, which<br />

have been sketched from visual observation or<br />

from inadequate or unreliable map sources, to<br />

show collectively the configuration of the terrain<br />

lormat-Predetermined arrangement of<br />

characters, fields, tines, punctuation, page<br />

numbar, etc.<br />

forming machlrra-The equipment Ior<br />

forming, by heat and vacuum, preprinted plastic<br />

maps over a mold representing the Ierrain of Ih(<br />

area.<br />

formule for theoratlcal grevlty—A Iormula<br />

expressing gravily on the spheroid of reference<br />

in terms of geographic posilion, it being<br />

assumed the! the spheroid of relerence is a<br />

level surface.<br />

forward azimuth—See azimuth, definition<br />

1.<br />

forward lap-See ovarlep, definition 1.<br />

found cornar—A term adopted by the U.S.<br />

Geological Survey to designate an exislent<br />

I cametiof the pubiic-land sinweys which has<br />

been recovered by field investigation.<br />

four.pole chain—See Gunter% chein.<br />

four-rod chalrr-See Gunter’s chain.<br />

fourth-order trssversbA survey traverse of<br />

an accuracy less than third-order travarse or<br />

which fails to meet third-order official atandarda<br />

In tourth-order traverse, angles are observact<br />

with a tranah or sezfant ‘or are determined<br />

grephicalty, and distances are measured wilh<br />

taoe or stadia<br />

fractional seals-See representative<br />

frectlon.<br />

fractional aectlon— A sectbn containing an<br />

arsa appreciably different from 640 sores,<br />

usually as a reautt ot an invasion by a<br />

segregated body of water, or by other land<br />

which cannot properjy be surveyed or disposed .<br />

of as part of that section. See also sractlorr.<br />

frecflonal township- A township Conlairrlng<br />

less than 36 normal sections, uaualfy lv3Gause<br />

ot invasion by a segragaled body of water, or by<br />

other Iansf which cannot property be surveyed as<br />

parl 01 lhat township, or by closing the public<br />

tand surveys on State boundadss, or other<br />

limiting lines. Half ranges and half<br />

Iownshlps are fraclbnal townships by<br />

definition. See ab.o township.<br />

trame camera—A camera in which an entire<br />

frame or format is exposed through a lens that<br />

is fixed relative to the tocel plane, See atSo<br />

panoramic camera.<br />

framework of conlrol—See survey nat.<br />

frema-(JCS) In photography, any single<br />

exposure centained whhin e continuous<br />

sequence of phonographs.<br />

free-air enomaly—(JCS) The ditlerance<br />

between obsewed gravity and theoretical gravity<br />

which has been computed for Iatltude and<br />

corrected for ejevalion of the atatlon above or<br />

below the gaoid, by appfbatbn of the normal<br />

rate of chenge of gravity for change of<br />

elevatlon, as in free air. Also called Faye<br />

anomaly.<br />

free-ok correctlorr-Correction factor, usually<br />

expressed as milligals per reeler, which Is<br />

appflad 10 obsawed gravity to reduce the value<br />

to sea level. Also called Faye correction.<br />

free-swlnglng pendulum—A pendulum<br />

moving wholly under the influence of gravjty and<br />

an initial momsrrfum imparled to it by<br />

mechanical or olher means. In gravity work, the<br />

initial momentum may be imparled by drawing<br />

the pendulum slightly out of plumb and Ihen<br />

releasing il.


Frosnsd larr-A lens which corsslsls of a Ifrin<br />

stepped disc with each slep having the<br />

curvature 01 a rruch thiier lens. A similar<br />

design wwld be the roof o! a factory that boka<br />

like the teeth of a saw. This pattern, embossed<br />

in ptaet’c, la used to dtstribufe image (or light)<br />

brightness over a given area.<br />

frllllng-The separation, along the edges, of<br />

the photographic ernufaion from its base.<br />

front ●lement—Sea lens elemant.<br />

MIL-HDBK-850<br />

front focal dlafance-The distance<br />

measured trom the vertex of the fronl surface of<br />

tha lane to the fmnf focal point.<br />

front nodaf point—See nodel point,<br />

definition 1,<br />

front eurface mirror—An optical mimer on<br />

whkh the reflecting surface is applied to the<br />

frxrnt surface of the mirror instaad of to the back;<br />

i.e., to the first aurlace of Incidence.<br />

Fulcrum—A videodisc-based electronic map<br />

display system tor the presentation arw analysis<br />

of muniam.rrce data including maps, da!a bases,<br />

imagefy, gazetteers, and graphic symbols.<br />

Developed by Interactive Television Company.<br />

fundamental circle-See prlmery great<br />

cfrcle.<br />

fundamental etar pfaces—The apparent<br />

rfght ascensions and declinations of standard<br />

Cm’Parkon stare obtained by faadkrg<br />

observatories and published annualiy.<br />

fundamental tablea, deformation of the<br />

geoid end Ite effect on grevity—Tables<br />

gtimg the deformation of the gaoti and its<br />

effect on gravity, computed for masees of unit<br />

densfry extending to various dstances almve<br />

and below the surface of the geoid.<br />

Fundamental tablaa sarve aa the basia for the<br />

preparation of special tablas cxmrasporrding to<br />

particular assumptions respecting dansfry,<br />

Iaostasy, etc.<br />

100


’<br />

,<br />

I<br />

gdnctlc clrcta-sae gnlsctlc squator.<br />

galactic Squator-fl great circle of the<br />

caleefial sphere, incfinad 62° to the cafeef”=l<br />

equator and odncidhw approximately wilh the<br />

cmfer line of the Milky Way, constituting the<br />

primary great circle for the gafectic eyelem of<br />

coordinates. If is everywhere 90° from the<br />

galactic poles. Also called galedk clrcfa.<br />

galactic latltude-Angufar distance north or<br />

eoulh of &re gsbcfic equatoc the erc IX a great<br />

circle through the galactk poles, between the<br />

galectk equster and a peinf on Ihe celestial<br />

s@rere, m.aesurad nerfhwerd or aeufhward from<br />

R %%%7%%’E%3%n%’ ‘b’d<br />

meesuremant.<br />

galactic longltud*Anguler distance eesl of<br />

sidsreal hour angle (SHA) 94.4” abng the<br />

galactic aquatoc the erc of the gskfii equetor<br />

or the angle at the galactic pols between ths<br />

greet circle through ths interaecfkm of the<br />

gelastic aqustor and the celestial aquslor in<br />

Segiffarius (SHA 94.4°) and a great circle<br />

threugh the gstsdic poles messured eastward<br />

from ths grasl side through SHA 94.4” through<br />

360”.<br />

gelactlc pole-On the celestiel sphare, aifher<br />

of the two points 90° fmm the gelactic aqustor.<br />

galactic system of coordlnataa-A n<br />

astronomic morchma syatam using Iatfiude<br />

measured north and aoufh fmm the galactic<br />

equator and longitude measured in tha sense of<br />

incmesing right escensien from 00 to 36oo. The<br />

system was ori inelty dafined such thet the pde<br />

wss et FM = 12‘140m, Dec - + 28”; howevar, in<br />

1958 the Intametionel Astronomical Union (lAU)<br />

infmducad the IAU gafedic eyatern which<br />

defined the pda at FM . 12h49m, Dac = 2724’.<br />

gallay proof—A prod from type on a gellay<br />

bafere h is made up in psgaq also, such proofs.<br />

gal—A unit d mxaleretion equal to 1<br />

oemimeter par aacorrd per second, or 1000<br />

milligsla, used in measuring the actelarstion of<br />

gravity.<br />

gamma—1. (photography) Tha Iengenl of the<br />

MI L-HDBK-B50<br />

G<br />

101<br />

angle wtrkh the stre”ght-iina pat’bn d the<br />

charedaristii curve mkae with the b~axpc6um<br />

asia. If indkefas fhe alcpa of the sfraigM-fine<br />

pertien of Ihe curve and is a measure of tha<br />

exfem of davabprnant and fha czmtresf of the<br />

photograph metarial. 2. (gaomegnetism) A<br />

smell unit M rrmgn~ic tiald itienaify Sometimes<br />

usedindaadbm g the Eertfr’e rrmgrratic fiefd. II<br />

is defkd aa bsing aqusl to lfY5’oerstad. *e<br />

also nanotesla.<br />

gap-(JCS) (imegary) Any specs whara<br />

imagery feifs to meet minimum coverage<br />

raquiremerrta. Thii might be a space not<br />

cxwerad by imsgary or a spece whera the<br />

minimum apecifii overfap was not cbfa’brad.<br />

Sea sko holiday.<br />

Gauas-Kruger grid-See transveras<br />

Mercator grid.<br />

gauaa—A centimeter-gram-second alacfm-<br />

M.S9netiC unit of msgnstic indudion squal to<br />

104 teds. See also tesla.<br />

gazatte=r-An alphebetisal list ol place<br />

nemas giving feature idenlifiition and<br />

geographic ancVor grid motilnates.<br />

Ganaral Navigation Charts-Smell scale<br />

(1:1 ,000,000 or emsller) chsrts designed for<br />

epan sea aurfsce navigat”m. Depktad<br />

information supports voyage plenning, ecaan<br />

navigation, and mifiiery opamliona.<br />

general chart-A nsufid chart intended for<br />

offshore coasfwisa nsvigeticm. A general cherf is<br />

d srrsillar scala then a caest cfwt, but of larger<br />

scele thsn a =iling chert.<br />

ganerel map-(JCS) A mep d small scale<br />

used for ganeml pisnning purposes. See alse<br />

romp.<br />

ganeral proceadon-llra motion of the<br />

equinoxes westward along the acfiplic at the<br />

rate of about 50.13’ par yaer. see afso<br />

Iunleolar pracosslon; planatary<br />

pracasslon; precasslon In decllnetlon;<br />

prsces.elon In right sscenelon;<br />

pracaaalon of the equinoxee.<br />

ganeral-purpose mep–A map wtich<br />

provides “a bmsd range of information and which


’<br />

tattiles the twsds of a lwosd range cd users.<br />

genomllzatlon-1. The pmoaasas of<br />

reducing rew data tor trsnslwrration into a dats<br />

base or rrmp. Gensrdzaticm involves<br />

aggqathno Isggiomtrmticn (conbhtslion),<br />

aalactbn, maolution faafure elinsinafbn<br />

(omission), claaaifkstion, smoothing,<br />

raeampling, sirrpfiiketion, semggemtion,<br />

dispfacemant, ~ting variables,<br />

measurement Isvai reduction, dimmeiona iiiy<br />

chsnge, and ayrnbofiiat”km. 2. (line<br />

ganerelization) Cornmonty refers to cmordiite<br />

thmring or line thinning atior .wncothing.<br />

Sss also Iina thlnnlng.<br />

MIL-HDBK-850<br />

gsmeratlon-(photogmphy) The preperatian of<br />

successive patiwahegetive reproductions fmm<br />

an origii nsgsfive (first generedon). The first<br />

positive pcxhrced is m secciut-generetkm<br />

pmducf; lha nagetive mede fmm this paitivi is<br />

a third-genamtion product, end the narrt pasitiva<br />

or pint fmm thst nagelive is a fourth-genamtion<br />

product. Wmh asch swoassive genemtion,<br />

quelii deteriorates.<br />

generic tornt-lhal peri of .s neme which<br />

dars%bas he kind of fasture to which the nsrne<br />

k SpPfid, and whiih hes the -ME rnaening in<br />

current Iocsl usage. For axampfe, the generic<br />

term “wan” in .Tokywvan- means ‘hey.’<br />

goo-mforoncod data—Spatiai deta thet<br />

pettain to a ~tion on the aarrfr’s surface.<br />

Geocelver-Trade name for an antennaracaiver<br />

capable of racalvkrg slgnais from the<br />

Navy navigation sateiliies, fmm whiih !hrsadimensionsl<br />

positiins can be mrnpulad for the<br />

entenne focstion. See also Doppler<br />

navlgatlon, defin~lon 2.<br />

gsiocentrlc coordinate syetem-See<br />

geocsmtrlc coordinates.<br />

goocentrlc coordlnatee-(terrestrial)<br />

Coordinates thst define the position of a point<br />

wfth respect to the center of the Esrth.<br />

Gsc@enfrk coordkwtes csn be either Cmteabxn<br />

(x,y,z) or spherical (gaocantrfc latitude end<br />

tongitude, end mdkrl distence). Also called<br />

geocentric coordinate system;<br />

geocentric poaltlon.<br />

geocentric dlamoter-llre dwmeter of a<br />

celestial beefy measured in aacmsfs of am es<br />

viewed from the Eerth% center.<br />

102<br />

goocontrlc geodetic coordlnsttee-<br />

Gaada+ic coordinates referred to e gaocantrk<br />

rslarance ellipsoid.<br />

geocentric gmvftational constant— The<br />

product of the Eritth’a mess amd the<br />

grsvitatianel wnatsrrt. Thii product is known to<br />

a far greater prsclaion than either fader.<br />

goocentrlc horfzon-Tfta piene through the<br />

center of the ES*O pemllel to the topocantrk<br />

horizon.<br />

geocentric latltud*Tha angle at the canter<br />

of the Earth between the pbne of the cafaafiii<br />

aqustor and a fine to a fmint on the aurfsoe of<br />

the Earth. Geocentric Istitude Lsused as an<br />

ausilicry fstilude in some computations in<br />

astronomy, (pactesy, errd csrtogmphy, in which<br />

wnnection it is defined se the engte fwrnad with<br />

he mpr sxis of the elliiea (meridiinel *ion<br />

of lhe Wheroid) by the mdius vector from the<br />

center of the eltipae to the given point. In<br />

satmnornic work, geocentric iatittzle is eteo<br />

celled reduced latitude, e t.wrn that is<br />

LXXWEtimeSspplied to pammatrk Ietitude in<br />

gedasy ad artogrsphy. The gentric and<br />

isometric latitudes ere approximately equal.<br />

geocentric longltude—See gwdetlc<br />

longitude.<br />

goocentrlc paraliax—The dfierence in the<br />

apparent dtractbn or position of a celastiel body<br />

es observed from the canter of the Earth and a<br />

point on fls surface. This varies with the ~s<br />

altiiude and distance from the Eaith. Aleo ceiled<br />

diurnal parallax.<br />

geocentric position—See geocentric<br />

coordinates.<br />

geocentric mdlus vector—The vector from<br />

the center c4 the Eerih to the point in question.<br />

See also geocentric coordlnstea.<br />

geocentric stetlon posltlon—The iocation<br />

of a etatii defined in terms of gaocentr”k<br />

coordinates.<br />

gaocentrlc zenitfr-The point where a line<br />

imm ihe center of the Earth through e paint on<br />

its surface meets the celestial sphere.<br />

gsOcsntrlc— Reiative to the Earth as a oantec<br />

msasurad from the center of the Earlh.


1<br />

MI L-HDBK-850<br />

g80d0dc fine-A tine of SfWfSd d-nctt<br />

bafween my fvm pdnta en any !nafhenmticelFy<br />

dafinad surface. Agaodadclkmfcfan aU@ecid,<br />

in ganerat, h a Ens & rbtble curvature, and<br />

usuauy Iii bafwaan the two ncirmsl sectibn fines<br />

wttikh the two pohte determine. tf the M<br />

t-1 pdnts are in naarfy the wna fslfiude,<br />

the gacdaeb fbta may cross owe of the normal<br />

eactbn lines. n should be nofed that, except<br />

abng lhe Equator and abng the marfdtane, the<br />

gaodesic llnalenot eptanacrsve end cennc4<br />

Lw dghfed over directly. Hewcwer, for<br />

conventkmal trfangulatkm the lengths and<br />

dtiicna of gacdasic lines dtiar kmppreciabty<br />

fmrn cm-responding pek’s d norrnel ~ion lines.<br />

Also called gaodealc; geodetic Ilrm.<br />

geodealc-sae geodesic line.<br />

geodesy—lle science whkh deals with the<br />

fb~inalion d the size and figure of the<br />

Geodotlc Reterenco Systsim 1960 (GRS<br />

BO)-Thta gaodatic reference systam was<br />

ado@d by the XVII General Assembly of the<br />

international Union ef &odesy and Geophysics<br />

at Canberra, Australia in 1979. The GRS SO is<br />

defined by the four fundamental mnetents:<br />

aerni-mejor axis 6,378,137m, gravitatiomd<br />

constent d the Earih (including Ihe atmosphere)<br />

3,9S6.005 x 108 n# S-2, -nd degrae zonal<br />

coaffiiienl 108,263 x l@, and anguler<br />

relational velocii 7,292,115 x 10-11 radkms.<br />

geodotlc ●td geophysical data (G6G)-<br />

Infcrmat”mn or earth data, pertaining to the<br />

sciences of geodesy and geophysics. Typicalfy<br />

includes gravity infomralkm, geodetic peinf<br />

posifiining data, datum definition, etc.<br />

gciodotlc ●nd goophyslcal data<br />

roductlo*The process of enhancing the<br />

value of geodetii and geophysical data by<br />

anefyais, evefuatien, computation, and<br />

adjuatmant. The pmcaea includes (1)<br />

transforming unadjusted survey data and<br />

ebservafiona into an adjuafed form with reliability<br />

afatemanfs; (2) establishing basic frameworks of<br />

horizontal and va.ttiil cantml in advance of<br />

-P. Chad, ad fargat rrwleriels pmducfion, snd<br />

publiihmg d trig Iiita; and (3) arbsfyais,<br />

evaluation, and campufalicn of geodetic and<br />

!W@Yabl data obtained by awface, ahboma,<br />

or tmteffife hschniquee to establish, exiend,<br />

connect, and transform daturns and to relets<br />

datum to the Dapamrranf of Defenea Workt<br />

Geodetic System.<br />

geodetic ●nomaly-Sea ●nomaly,<br />

definiiicn 2.<br />

geodetic ●dronomy-The branch of<br />

gecdesy which Ufifiiee astronomic Obearvsfbns<br />

to asfracf gecdatb Irkmnafiin.<br />

goodetlc aztmuth mark-A rwked potnt<br />

astsbfished in connection with a friengufatbn (or<br />

tmverae) station to provide n starting azimuth for<br />

dependent euwaya.<br />

gaodetic ●zimuth-l%a angle between the<br />

gacdefii meridian turd the tangent to the<br />

geodesic fins at the chsarvar, measured in the<br />

pklne peqmndiculet 10 Ihe allipaoid rrc.rmal of<br />

the observer preferably cJockwiae from north.<br />

Although older suweys, particularly by the Coasl<br />

and Gaodatic Suwey (now National Geodetic<br />

Survey), used sculh, the Daparfment of<br />

Defense now uaas north.<br />

geodatlc control data-information<br />

concerning the pracise horizontal and vertical<br />

geodetic bcetion of pints on the surface d the<br />

Earth end ceiestkl bodies, includ@ points<br />

obtained by phc.!ogmmmetric techniques.<br />

geodatlc control—A system of horizontal<br />

rmdlor vefiicsl mntrol statione that have been<br />

esfeblishad and edjuslad by geodetic meihode<br />

❑nd in which the shape and size of the Earth<br />

(geeid) have baen considered in position<br />

computat”mns.<br />

geodatic coordinator—Tha quantities of<br />

latitude, bngifude, and height (ellipse”@, which<br />

define lhe posifiin of a point en the surface of<br />

tha Earth with respect to tha raferance spheruid.<br />

Also imprecisely called googrttphlc<br />

coordinate.<br />

gaodatlc<br />

card.<br />

geodetic<br />

data sheet—See control data<br />

datum—See datum, definition 2.<br />

gaodatic equatOr-Tha line of zero geodetic<br />

ktifude the uraaf circle described ly tb<br />

semimejor asis d the reference alliisdd ea if ie<br />

roteted about<br />

aatronomlc<br />

the minor asis.<br />

●quator.<br />

See also<br />

103<br />

geodetic he4ght-See ●lllpsoldel holght.


I<br />

l<br />

podstk kt\tude-The angle whiih the<br />

norrnai et n point on the referenoe spheroid<br />

rrmkae wffh the pfsne of the geodetic aqueier.<br />

Geodatii latitudes are reckoned from ttw<br />

Equator, but in the horisc+wsl confrd survey d<br />

the United States they are ~ed from ths<br />

fatifude of afafiin Mearka Ranch as pmecrbad<br />

in the North Amarican detum d 1927. The new<br />

North American dsfum of 19S3 wifl be Emt&<br />

resee centered. A gecxfel”c fstiftie differs hum<br />

the c==Pondiw ~~ fstitude b the<br />

amount d the rnerfdbn coqmnanf of tL<br />

daffecikm of the varfbsl, Aim cafied<br />

topographlml Iatltudo.<br />

MIL-HDBK-850<br />

geodetic kavaflng-spirif Ievefing of a h~h<br />

order of smu~cy, uerzslfy azfandad over fsrga<br />

arms, to fumrsh amurate vertkef control as e<br />

ksis for the mnfrd in the vertical dimension for<br />

all surveying and mapping epsretkms. Spirit<br />

Ievefing follows the gacrid and ifs associated<br />

level surfacae tiich are irragufsr, rather fhsrr<br />

any mathemst”wliy determined @heroid or<br />

ellipsid and samcieted regular level surfaces.<br />

geodetic lhm-See geodmlc Ilna.<br />

gaodotic iongltuda-lhe angie between the<br />

plane of the geodetic rneridiin and the plane of<br />

sn inifisl nzerfdmn, arbh%uffy chosen. A geodetic<br />

fongffude can be measured by the angle al the<br />

pd. of mtsfion of the reference spheroid<br />

between the focsf and initiil maridiins, or by the<br />

arc C4 the geodetic equator intercepted by these<br />

rnerWans. In the Unftsd Statae, gaodet”k<br />

bngifudea are numbered fmm fhe maridiin of<br />

Greenwich, but are mmpufsd fmm the maridiin<br />

of sfatbn Meedas Ranch es prescribed in the<br />

North Amsricsn datum of 1927. The new North<br />

American datum of 19S3 will be Eerth-msss<br />

centered. A geodetic bngifuda differs from the<br />

corresponding aetmnomk fongifude by the<br />

ernount of the prims verfid caponent c4 fhe<br />

Iocsl daflactkm of lhe vertiil dwided by the<br />

cosine of the fatifude. Also csrliwf geocentric<br />

Iongl:uda.<br />

goodotlc meridian plane-A piane that<br />

cwrfsins the normal to the reference eliiisoid at<br />

s dven odnt rmd the rotetion arris c4 fhe<br />

reierencb etfipacid.<br />

geodetic merldlen-A line on a reference<br />

ellipseid which has the esma geodetic fongifude<br />

et rwery pint. Also called gaographlc<br />

meridiwr.<br />

104<br />

geodetk pmalld-A line on the ref.smnce<br />

SPhamid whiih tMS ihe asma @odatic hthtdn<br />

M every point. A gsodefic panel, other ttwrr<br />

the Equator, ie nd a geodesb (gmdatic) Ime. h<br />

form, II m a emsfl ckcle wtmaa plsrra is psraiiaf<br />

with the plane d the gecdafii aquetor.<br />

gaodotb pOSftiO# pfxifkrtl d a POil’d On<br />

the surface of the Eerth e~aaeed in terms of<br />

gamielic Iatikde, geodetic Iengiiuda, and<br />

geodetic hdit A ~tc Pwifii rrr@aa an<br />

adopted geedetic datum.<br />

gaorktlc setelllt*Any eateifide wfzma orbit<br />

and payload render it useful for gaodalic<br />

purposes.<br />

gerodetlc stellar camere—A precision<br />

Ierrastrisl csmsra, usually employing giass<br />

plales, used to photograph ekwatsd illuminslad<br />

objscfs against a star bsckgmund.<br />

geodetic survey-A survey in whch the<br />

f~ure and size d ths Esrfh is considarsd. if is<br />

appbbfa for Large areas and tong iina.e end is<br />

U* for the pracisa Imation of beeii points<br />

suitabka for controlling ofhw surveys.<br />

geod.stlc zenith-The point whare the nermsl<br />

(to the refarenca spheroid) exfanded upward,<br />

masts the ceieet”-1 sphere.<br />

Geodimeter-A trsde nsme for an instrument<br />

the! measures distance by pradce elecfrork<br />

phesa mmparison of mcdufated light waves<br />

vhii trsvei to a refbctor and return.<br />

geoakctrlc sunrey-A survey to dalermine<br />

M elactricii or resiefivii pofential of the Earth<br />

recks.<br />

Geographic Baae File/Dual<br />

independent-Uap-Encoding<br />

(GBF/DIME)-Topologicalfy structured files<br />

developed by the Bureau of the Census whiih<br />

serve as a relatively inespensh’e geogrephk<br />

inforrnslion dste source. GBF/DtME fries<br />

irduds street networfre, street addreseas,<br />

Pofiiical boundsrfee, and msjor hydmgrsphc<br />

faaturas. Esch street eagmant is rewasanlad<br />

as a strsighf fine ragtudleca d its red wwfd<br />

shape.<br />

Geogrephk Information System (GIS)-<br />

The generic ferm used for a system d cumpufer<br />

software moorems and aaukzmant that is used<br />

to acquiri, s~ore, manipulate, enafyze, and


,/<br />

I<br />

d-y C’$Ndialdata.<br />

Gsogmphk Nsrw*s Procosslng Syskm<br />

(GNPS)-Ths DMA system which includes the<br />

hardware, cmffwsre srsj eras to nminfain<br />

the geographic nsmee data requirsd for digital<br />

maps ad gsztmeam.<br />

MIL-HDBK-850<br />

gsogm hlc (~oogrephbel)-Signify ing<br />

bade MRfbnehpto the Eartfrcxmddamd asa<br />

gbbe-ahapad body. The term geographic is<br />

applied dike to dsta bad on ths geeid and on<br />

othw spheroids.<br />

geographic coordlnat@a-(JCS) The<br />

qusnfitbe c4 fatituda and Iengituda wlriih ds&ne<br />

the~indapnfonffnswf~ efm.s<br />

Edh with respect to thtr rsferenca spheroid.<br />

Also called astronomic coordlnetes:<br />

gravimetrlc coordlnatea; tormotrial<br />

coordinates. See also coordlnatas;<br />

geodetic coordinates.<br />

geographic lstltude-A general term,<br />

aPPbinjl afike to asfrancsnic 181iidBs ~~<br />

geodetc latitudes.<br />

geographic llmlta-The lines heving Istirude<br />

and Iongkde values bounding the area of a<br />

mm or chart: that eras exclusive of overlao<br />

areas. See siseneatlh-rsis.<br />

geographic location-see geographic<br />

pooltlon.<br />

geographic longltude-A general term,<br />

a@Yin9 afike to astronomk and to geodetic<br />

longitudes<br />

geographic merldlan—A general temf<br />

;~~~~,atike to an as!ronomio or gsodetrc<br />

geogmphlc nama-Aleo called place<br />

name and toponym. sea also Board of<br />

Geographic Names.<br />

geographic nonllnoarlty—The error<br />

introduced by digitization and subsequent<br />

processing 10 Ihe total error of both abdute<br />

ard reletfie positioning of any Ieature on the<br />

gmphk.<br />

geographic perallef-A general term,<br />

applying atike to an eafronomic parallel or e<br />

geodetic parallel .<br />

gaographlc posltlo~Tha position of a point<br />

Ontheaurfea c4the Earfhuupmeed krmrrtw<br />

of latiiuda end bngitude, either geodetic or<br />

astronomic.<br />

gaographlc ●urv*y-A general term. mt<br />

~pfibk & defined Iirritsfion, covering a wide<br />

mWe & Wweye fying between and merging<br />

into axpbmfory wrvaye on the one hand and<br />

bsdc topogmphii eurvays on the cdher.<br />

Gaographk etevays WJ.4y cover kwga areas,<br />

are based on coordinated control, end am uaad<br />

to record ptryskal and statistical ctssmcferfsrks<br />

of the area surveyed.<br />

geographic vertical-See vertical.<br />

googrephlcaf ●ma claaWtcatlon<br />

eyatern-A fogicsl snd orderfy gaographksl<br />

division of the world using nufirs, Iattem! and<br />

ccmbinaticms of the same for the deeignakxr of<br />

areas and subsraas.<br />

goographlcef ●xploretlon trmrome-A<br />

route followed scross some parts of the Earth,<br />

approximate positions ebng whmh are<br />

determined by surveying or nevigslional<br />

methods.<br />

gaographlcel mile-The length of 1 minute<br />

of erc at the Equator, or 6,067.08 feel (on the<br />

Clarke cpheroid of 1666).<br />

gaographbrd pofe-Eiiher of the two points<br />

cd intersection of the sudece of the Earth tih its<br />

axis, where all meridtans meet.<br />

geoidaf contour-A line on the suriace of the<br />

geoid of mnstant elwation with reference to the<br />

surface of the spheroid of reference. Geoidd<br />

contours depend on the surta of reference as<br />

wellaeon lheahapedthegeoid. Theeama<br />

gecid referred to different surfeoes of refemnos<br />

will give different sets of gaoirhl contours.<br />

geoldel holght profile-See<br />

●strogoodetlc Ieveflng.<br />

gooidal height—The distence of the gaoid<br />

above fpodive) er bebw (nagative) the<br />

methemalicsl reference spheroid. Also celled<br />

geold separstlon; undulation of the<br />

geold. See alw sstrogeodetic<br />

undulations.<br />

geoldd horlzors-llat circle of the celestial<br />

)5


MIL-HDBK-B50<br />

splwre formed by the inleraaction cd the<br />

calsdsl sphere end a pfwre fangsnf to the s6e<br />

fawel mxfsca of fhs Earth at the zenith nadir fine<br />

geoldel separation-See gaoldal halght.<br />

gaold-The equipomntial surface in the gravity<br />

field of the Earth MA appmximaIrrs tha<br />

undktwbad mean see fcwel extanded<br />

ccmlinueusfy Ihmugh the confinerrls. The gaoid<br />

is the surfa~ d raferanrx for asfroncarric<br />

ObCONti .8rd fOr @OdOfb k?dl~. .%tr dk3<br />

companaated goold; ●qulllbrlum theory;<br />

●qulpotantlal ●urfaea; gaoldal horizon;<br />

gravlmotrlc gaoid; Ieoatatlc gaold;<br />

rafarenca apharold.<br />

gooklnatlcs-imcsl and globel rnetion of the<br />

Earth ar sea, its -umrnem: iadetion from,<br />

arxl etl=t upcm pracisii equ~mant and<br />

maaauring instrumnt.x. Usually applied to the<br />

design and teat of inertial instruments and<br />

sydems and sfabis pisffonna.<br />

gecrloglc survey-A surwey or investigation of<br />

the Earth, of the phye”~l changas whwh ths<br />

Earth’s crust has undergone w is undargaing.<br />

end of the muses producing those changes,<br />

Geological Long Ranga Incllnad Asdlc<br />

(GLORIA)-A low ramlution side scan sonar<br />

used for racennaicsanm surveys ef the ocean<br />

floor.<br />

gaologkal msp-A map showing the<br />

structure and rnmposit”mn of the Earths cruet.<br />

gaomagnatlc coordinates—A system of<br />

spherical cc.ardinsles baaed on the best fm of a<br />

centered d@fa to the actual magnetic field of<br />

the Earth.<br />

gaomagnatlc ●quator-The terrestrial great<br />

cimia aerywhara 9@ fmrn the gaerra~Ic<br />

poles. Geomagnetic aquator should not be<br />

confused with magnetic aquator, Iha iina<br />

connecting all pdnls of zem magnetic dip.<br />

gaomagnetlc latltude-Angular distance<br />

from the geomagnetic equator, msasurad<br />

rrorlhward or southward through 90° and labeled<br />

“N” w ‘S to indicate the duaction ~<br />

measurement. Goomagnetlc latitude<br />

should not be confused with magnetic<br />

Iatltudo. Sae also dip.<br />

goomagnotlc morldlan—Tha meridional<br />

lines of n gmrnegnetb coordinafa system. Not<br />

106<br />

to be csmfuwd with magnatlc meridian.<br />

fraomapetlc Pole-Either of fwe ant@edal<br />

poima rrwking the inraraaction d tha Earth’s<br />

surface with the exlsrdsd axis of ●powadul bar<br />

msmet SSSti to be bested at the canter of<br />

the Earth arxt Sppmximeting the eourca d the<br />

actual msgnetic fiefd of the Earth. The<br />

expresskm geomagrtetk polo sheutd rmf be<br />

mrdusad with magnetic pole, whtch ralates<br />

to the dual magnetic fisfd of the Eatth.<br />

goomagnetiam—1. The magnetic<br />

phanomanen, collectively cortsidared, exh~sd<br />

by the Earth and ite atmosphere, and by<br />

extension fha magnatic phenomena in<br />

interpisnsfnry apace. 2. The etudy of the<br />

~9netic fii~ d the Earth, Abe @IIsd<br />

Wrroatrlai msgnatlsm.<br />

geometric latltude-See parametric<br />

Iatituda.<br />

goomatric map pro)actiOn-Saa<br />

parepectiva map projection.<br />

geometric nonlinearity-Any dktoriion<br />

irrkducad by digitization snd subsaqusnt<br />

pmcesaing d a mathamaticdy-cerract reference<br />

system or grid, other than aimpk mtatian,<br />

tranatstion, or scale change,<br />

geomatric primitive-one of the three basic<br />

geometric units of re+mraenlatien: nede, edga,<br />

❑nd face. Equivalent with gaagraphc prim~we.<br />

geometrical dl~The verfiil engla, at the<br />

eye et an absatver, between the Froriiontai and<br />

a straighf fine tangent to tha surface of the<br />

Earth. It is larger than dip by the amount of<br />

terraeliiel refrsdion.<br />

gaomatrlcal horizon-riginally, the ceiestiel<br />

horizon; now more mrmnonly the irrtersedion of<br />

the caiestial sphere and an infinite number of<br />

straight finaa tangent to the Earth% surface, and<br />

radiating from the aye of the obaervar. If there<br />

ware no terrestrial refrscfiorr: geematricai and<br />

visible horizons would rmincide.<br />

geomorphic dats-A sat of model<br />

coordinates defining the tram of a geomorphk<br />

feature. Thsce consist of ridgeiinas, valleys,<br />

drairwge and lnkea whwh are uaad to refine the<br />

elevation data grcqr during tha production<br />

process.<br />

goomorphlc-Patleining to iand forma.


1<br />

gaophydca-l?re SCISI’IIX of the Earth with<br />

_ tO Ifs structure, mmpeeifkrrr, and<br />

devakpmant. Qaophysice is s bmnch d<br />

OXPSfiMSnffd phySiCS daslinE with the Earth,<br />

including ha atmosphere and hydrosphere. tt<br />

includes the adancea d dynamicd gadegy and<br />

physical gOO@#ry, and makes uaa d gadDw,<br />

aatsrrrolegy, meteorebgy, oceanography,<br />

mW@~m, ar’ld c4her Earth s.ciencas in<br />

oollectmg and interpreting Earth date.<br />

g.oposltlonlng-lha purpose of<br />

photegremmetric gecpoaMinbg is hvo-fdd: (1)<br />

upgrade metric data aesodelad with aoume<br />

irmgery. This -ata r5 measuring tii and<br />

mrrtrd pe”mts, and ergu.stkrg pc.aitii and<br />

attitudes of bfccke of imagery. The resufta form<br />

tha bade for eteraeacopk orientalien ef inmgary<br />

and supply medal informafia for morroacopic<br />

operatkms and (2) dsdarrnine accurately the<br />

boatierr of target points. Targeting operations<br />

resutf in ground coordinates and associated<br />

errer data for aelecfd bcations.<br />

gaopotentlal number—The difference<br />

between the geopotential on the geoid and lhe<br />

geepetentiel at a point.<br />

goopotorrtlal ●mfaca-See geop.<br />

geopotentlal—The gravity potential et the<br />

actual Earth. The sum of the gravitational<br />

(attraction) potential and the potential of the<br />

centrifugal force. A function daacribhtg the<br />

variation of Ihe gaopotentiel in apace. The<br />

function whose parliel derivative in any dir-tin<br />

gives the gravity conponenl in tlml dkdiwr.<br />

geop-An equipefentisl curface in the gravity<br />

field of the Earth. Alse IAled geopotontlal<br />

surface.<br />

GEOREF-(JCS) A world- pedtii<br />

rafarerroa system that I-MY be epp4ii to any<br />

map or chart graduated in latitude and Iorrgfiude<br />

[with G mernvish as prime meridian] regardless of<br />

projection. It m ❑ method d espmaaing latitude<br />

and brrgitude in a form aukable for rapid<br />

reperting and plotting. This term is derived frem<br />

the wc+de “The Worid Geogrsphw Reference<br />

System.”<br />

geoepher.-The solid and ~quid portiene of<br />

the Earth; the Iithesphare plus the hydrosphere.<br />

giant planeta—See major planets.<br />

MIL-HDBK-850<br />

107<br />

gigabyte (GB A unii of memory<br />

rwe~in9<br />

Commonty,<br />

t<br />

2 3 (1,073,741 ,s24) WES.<br />

a g“-e may mpraaent ona trillii<br />

bytas or 1,000 megabytee,<br />

glaomont—see grid dacllnatlon.<br />

Global Navlgatlon Chart (GNC)-A<br />

1:5,000,000 tie aeriea d mufficdorad charts<br />

deaiined fer genara! planning pwpOaaa for<br />

cparations wig long Isetancaa or b<br />

araas of in-flight navigation in long range, high<br />

afliiuda, hgh aped aimrrsfi.<br />

Global Posltionlng System (GPS)- S ae<br />

Navctar Global Poeltlonlng Syatam<br />

(GPS).<br />

globulsr map projoctiofiA map projection<br />

repraaanting a hem”uphera, on vrhiih the<br />

equator and a central geograpMc meridian ara<br />

repreaenfed by straight lines immaectirrg at rigM<br />

angles, theaa lines are divided into equal pat?a.<br />

All meridians, except the central ene, are<br />

repraaamed by circular arcs connecting points of<br />

equal divisien on the equalor with the pales.<br />

Exc6pting the equator, the perallets are circular<br />

arcs dividing the ad and axtrerrre outer<br />

meridians info equal psris. The exireme outer<br />

meridmn iimite the prc.jectien and is e full clrcie<br />

gnomonic chert-A charl on the gnemenic<br />

projection. Also salied graat clrsle chart.<br />

gnomonlc ,map prc]ection-A perapastlve<br />

map Prolmlon en a pfane tangent tO ths<br />

awface of a sphere having the point d<br />

pmjectien at the center of the mere. The<br />

prejwtion is neither corrformel nor equel-ar-. It<br />

IS the onfy p+cf”m on whii great skies on<br />

the sphere are reprascmtad ae straight lies.<br />

goldenrod paper-A paper, usually a shade<br />

ef yelbw w red, for bfecking out nonpriming<br />

araae d negatives er film Ieyoufa. Also caliad<br />

maaklng papar.<br />

gonlomater—An instrument for measuring<br />

angles, see al.se photogonlometer.<br />

Goode’s Intsrruptad Homoloalne<br />

projection-An aquel-area projection, bead<br />

on tha Mdiweide and ainuaeidel prejestiene,<br />

udrrg tha sinusoidal from the Equator to 4@N<br />

end 40%, and the Mollweida in higher Iafiiudaa<br />

The cceens are “interrupted” 10 anew the


I<br />

MIL-HDBK-850<br />

continents to be recentered on seversl<br />

rrsrridii, so es 10 Sttain good Overafl shape. ff<br />

isusadwidely ferrnsps decur-mnrrk<br />

daribtkma.<br />

gora-1. (surveying) An irregulmly shaped<br />

trsd 04 ksrrd, ganarsfty triangular, left between<br />

%X%’~gir%lW&r%~&&%&&%s a<br />

rsmnsnf d a systematic sursay. 2. (globe) A<br />

hDI&&s3fx3d rnep Whbh tMy bS f~r3d tO the<br />

surface of a gfoba wi!h a rraghgible amount of<br />

dtiortiin.<br />

Govornmant Open Systems<br />

Intarconrmctlon Protocol (GOSIP)-The<br />

exact sequence of bds, chsrader6, end coriml<br />

cades used to transfer deta between mrr-pufers<br />

and peripherals through a commurricdii<br />

channel.<br />

graddlon-llm range of tones (mm the<br />

brightest highlights to the dae+mar shsdews.<br />

gmdo cormctlon-(iand surveying) A<br />

rmrradion a@ied 10 a dslance mesaured on e<br />

dope 10 reduce il to a horizontal distance<br />

between W vertical lines through its erd ~ints.<br />

Also csllacl cormctlon la tnclhmtion of<br />

tape; Incllnatlon correction; clopo<br />

corroctlon.<br />

grada-The rate of slope or degree of<br />

inclination. see also gradlant,<br />

gradient sped-l%e speed of e<br />

phologmphw material determined on Ihe bssis<br />

of the esposure con~nding to a pmticulsr<br />

grsdiint ef the chsrecreristic curve.<br />

gradlerst tints-see hypsometrlc tlntlng.<br />

gradlentsw—An attachment 10 an engineets<br />

trsnsk with which m angte of irwliibn is<br />

maasumd in terms d tha fangent of the angle<br />

rather thsn in degrees end minutes. If rnsy be<br />

used as a telemeter in measuring horizontal<br />

distam.<br />

gradlont—1. A rate of rise er fall of e quantify<br />

agsinsf horizontal d~tance expressed ss a mtio.<br />

decimal. frsction, pemsrnlage, or the tangent of<br />

the angis of hclinat’km. Also called percent of<br />

slop.; alopa. 2. The rate of increase or<br />

dacraasa of one quantify with reaped to<br />

another.<br />

gradlomotar-An instrument used 10 measure<br />

108<br />

gmvify gmdienfs.<br />

graduation ●rror—lnsccumcy in the<br />

gredusbns of the scale of an inetnarrsm<br />

Gmf sea gravlnratoti balance-type gmvity<br />

rrratar designed for ooasn surveys wtridr<br />

censisfs ofamsss attheend ofafrorizorrtal<br />

arm Ihst is .sqJPorted by e fcnaien spring<br />

mtstiinal exis.<br />

gmln dlractlon-lhe afignrnsnt of psper<br />

fibers persllel to the rnuverrrerrl cm the peper<br />

machine during msnufectum.<br />

gralnad wmfaca=The roughened or irregufsr<br />

surface of an offset printing pfste.<br />

gralnlng-The mechanical roughening or<br />

grinding et an abmsive into the autfsce of n<br />

metel press plste to increase the aurfeca arae<br />

and impmve the water receptiveness ef the<br />

surface.<br />

grain-l. (phelegmphy) One of the discrete<br />

silver psrricles resulting fmm the development of<br />

an expo+ light-sensitive nrster”kd. The mndom<br />

distribution of these psr7icles in an ares of<br />

uniform ex~sure gives rise to the qpssmnce<br />

known as “gmininess.’ 2. (psper) See gmln<br />

direction. 3. (Itifregraphy) See grelned<br />

surface.<br />

granularity—llw graininess cd a devebped<br />

photographic irnsge: evident psrtiiuiarfy en<br />

enlsrgernsnts, thstISdue either to<br />

agglomamtiis d develcpd gmine or to an<br />

overfspping psffem ef grains,<br />

Graphic Karnal System (GKS)—An ISO<br />

standard for computer graphics pmgmrwnring<br />

which contains furrckns for outputting graphical<br />

primitives, controlling the apposrsnce of<br />

graphd prknifiwea with attributes, oonfrdling<br />

grsphicsl workatatkma, controlling<br />

tmnsformsticms and cmrdinete syaserna,<br />

generating and controlling groups of pnmttiies<br />

cslled segments, tieining graphicsl input,<br />

rnsnipulating groups of dev”wa-independent<br />

irrstnxfions cslfsd metafilea, inquiring the<br />

cspsbifiiies end ststes ef the grsphiis system,<br />

end hsndfing et-mm.<br />

graphic producte-A grephic pmdud msy be<br />

e~~ofemaporckrt, orihera$rrorrratenal<br />

used to produce the rnsp or chsrt.<br />

gmphlc scda-(JCS) A gmdualed line by


ntaans d wttidr dslmaes on the map, chart, or<br />

phonograph may be measured in terms of<br />

ground dtincas. Al= calisd bar scala. See<br />

also Scale.<br />

graphical mdlnl trtangulaUon-A rsdiil<br />

triangufati perfmmad by other thsn SMwi<br />

msena. A radial trisngufstion is aasurrmcf to be<br />

rrmda *h prfrrc@ points as radiil o@ere<br />

unfasa the defiiitiwe term designates olherwise<br />

(as, for esanrpfs, nadir-point ttingufatiorr or<br />

nadii-point plot emf iaosarter trisrrgulation or<br />

lsocarrter plot, and ruidit-poirrt efoffed-tamplme<br />

pki, eic.).<br />

graphlcel rectlfJcstlon-Any rectifiiat”mn<br />

technique etrpfoying a grephw method fer<br />

determining the solution as mntraefsd with<br />

rnechsnicsl technques. See also paper-strip<br />

method.<br />

gmphlc~JCS) Any and ell products of the<br />

cartogmphc ad phol~rarnrrwtric art. A grephio<br />

rney be either a msp, chart, mosaic, or even e<br />

film str@ that was producsd using certogrephii<br />

technques.<br />

graticulo-1. A netwmrk of Iinss mprassnling<br />

parsllsts of ielitude wrd rneridicms of longitude<br />

forming a msp projection. See also fictitious<br />

gratlculo. 2. A scsle at the focel plane of an<br />

optiicl instrument to aid in the meesuremen! of<br />

objects. See e.tsa retlch.<br />

Gmvatf I’vallng rod-A speaking rod,<br />

merked with rectsnglas ssch 0.01 foot high, the<br />

ractangks at the 0.1 of foot tAng bnger and<br />

those at the 0.5 being identiied by dots.<br />

Gmvstf Iavof-A dunpy level with the spirit<br />

level mcunied on top of a short telescope tube<br />

having a large object glass. Later msde with<br />

Wysa.<br />

Qrevar—See scrfber.<br />

gravkneter (gravity mater)-A n<br />

a~iemmefer designed to measure relative<br />

dfle-s in the accalerstion due to greviiy at<br />

different Iomticms.<br />

gmvlmatrlc coordlnatas-See ●stronomic<br />

coordlnatas.<br />

grsvlmatrlc detum orlontetlon—<br />

Adjustment ef the eifipedd of reference for a<br />

rticular geodetic datum so lfral the differences<br />

&vreen the gmvimetris and estrogeodetic<br />

MIL-HDBK-a50<br />

109<br />

deftect”km compenerrts and geoidsl undufstions<br />

am minimized.<br />

gmvlmatric deffectlon~ deflection of the<br />

vertical determined by methods d gmvintafric<br />

geodesy.<br />

gravlmetrlc goodosy-The science that<br />

utifiuea maesumments and cfreracferktii of the<br />

Earth’s grav”kyfmld as well es thaotiee ragatdii<br />

thw fiefd to deduce the shepe d the Esrth and<br />

in c=xbkmkm with arc meeeurernsmm, the<br />

Eatth’s size. AlfuJ called physlcel geodesy.<br />

gmvlmotrlc geold-h eppmximetien to the<br />

geoid ss determined from gnwity observation.<br />

gmvlmstrlc map-A map on which contour<br />

lines are used to represent points at wtkh the<br />

esceleralion of grevity is equsi.<br />

gravlmetrlc survey-A swrvey made to<br />

determine the acceleration of gravity st vsrious<br />

places cm the Earth’s surface.<br />

gravlmotrlc undulatlona—Separations<br />

bstween s grravimetrically determined geoid and<br />

a refweme elliiso”d d specified flattening.<br />

gravitational constant-see constant of<br />

gravitation.<br />

gravitational disturbtwrce-See gravity<br />

disturbance.<br />

gmvltatlonal flattening—llwt mtio of the<br />

dfierence between the poiar and equetorisf<br />

ncwrnal gmvifies to the equetcwial normal gmvity.<br />

Aloe called grmrlty flattening.<br />

gravitational gradient—The chenge in the<br />

grevity per unil distarrca.<br />

gravltatlonsl hermonlc-The spheriaal<br />

herrnmk used in a~mxirrwting the<br />

grmritetionel field of the Earth. Sea ekw gravity<br />

field of the Earth; coctorlel harmonica:<br />

sphorlcal tmrmonlcs; tessaral<br />

harmonics; zonal harmonlco.<br />

gravitational perturbations- Perturbations<br />

caused ty body foroes due to rro~herkal<br />

Ierrestrisl effscts, Iurricofar efkt, tides, and the<br />

effect of refetivity .<br />

gravltntlonal potantlal-1. The potential<br />

associated with the Ioma of gmvitet’km arising


I<br />

MIL-HDBK-B50<br />

from the attraction between mesa points, e.g.,<br />

the Earth’s center and a parlicla in apace. 2. At<br />

WIY POW the W* needed to mrrmve an &jact<br />

fmm that point to infii.<br />

gravitation-lha mutual interacliin of two<br />

maaaaa producing a tome between them acting<br />

abng the Yme jcimhrg their csrdera of mass. The<br />

force la pmportiinel 10 the product of the two<br />

mase.na dw’tiad ~ the square of the d-rice<br />

batwaan the two osntera r# mesa.<br />

gravity ●nomaly map-A map showh’rg the<br />

pasibns and magnitudes d gravity anomafiaa.<br />

Also, a map on wtkh contour fines ere used to<br />

represent points at wlich the gravfty anamefias<br />

are equel. .<br />

gmvlty ●tomety—The dtiemnce bat waen<br />

the c&arvad gravity value pparfy reduced to<br />

saa level, end the thsomtical grevity obtained<br />

fmm gmrrity formuta. Af.sa called observed<br />

gravity ●nomaly. See also Bouguer<br />

anomaly; free-air anomaly: gravity<br />

disturbance; Hayford gravity<br />

anomalioa/Hayford anomalles: Isoetatlc<br />

anomaly.<br />

grsvlty corer-Any type et corer thet adieves<br />

bottem penatmtion sOtely as e reeuft of gmv”hy.<br />

gravfty dots-information concerning Ihaf<br />

aocelarathn which attracts bodies and is<br />

espreaaad as observations or in the form of<br />

gmvity anomaiy charts or spherical harmonics<br />

for spatial repraaantatiorr of the Earth and other<br />

celastial bodies.<br />

gravity disturbance-The difference<br />

between the observed gravity tmd the normal<br />

gravity et the same point (the vertical gradient of<br />

the dmturbhg potential) as ofpoaad to gravify<br />

anomaly which uses corresponding points on<br />

two diffamnt 6U1’f8C6S.Bamuea tb Cr311tIifUlJCd<br />

force is the same -en tolh are taken et the<br />

same peint, it can eteo be cAM gravltatlanal<br />

dlsturbanrx.<br />

gr~vlty flold of tho Earth-The field of force<br />

erishg from a mmbinetion of the mass<br />

eftmcfion end mtetion of the Eerth. The fmld is<br />

normelly azpreseed in terms of pint values,<br />

mean ares values, etdor series tzqmaion for<br />

Ihe potential of the fiefd.<br />

gravfty flaftanlng-See grrnrltatlonel<br />

flattonlng.<br />

110<br />

gravtty lnatrument-A device for measuring<br />

the accefatakm due ta gravi!y (absofule) or<br />

grevky diffamncas tmtwaan two or rrmra -s<br />

(relative). sea also ●atstlzad gravlmolac<br />

Brown gravity ●pparstua; dynamic<br />

gravity mateq flraf ●am grsvimater;<br />

gravimotor; La Cosfo-Rombarg<br />

gravlmeten ●tebl- gravlmeter; ●tsblatypa<br />

gravlmeteq afatlc gravity rnatafi<br />

toralon bnlanco: unstable-typa<br />

gravlmator.<br />

grmrfty network-rl netwerfr of grevity<br />

stations.<br />

grmrlty raductlo*A combination of grav-~<br />

curmctiens to cbtain reduced gravity on the<br />

gad. sea alse Bouguer corrsctlon; frsaair<br />

correction; Isoatatlc correction;<br />

terrain corrrmtlon.<br />

gravity referenca st.ctlona-Stalions which<br />

serve as reference values for a gravtty survey,<br />

i.e., with respect to which the differences at the<br />

other statiens are detenninad in a relative<br />

survey. The absolute value of gravity mey er<br />

mSY m be known at the reference stations.<br />

grevlty station-A station et which<br />

obaarvations are made to datennine the value<br />

of gravity,<br />

gravity-Viewed from a frame of reference<br />

fued in the Earlh, acceleration imparted by the<br />

Earth to a mesa whiih is rotating with the Earth.<br />

Since the Earlh is rotating, tha acceleration<br />

observed as gravity is the resultant af the<br />

acceleral”km of gravitation and the centrifugal<br />

acceleration arising fmm this rotation and the<br />

use of an earthbound rotating frame of<br />

reference. It is directed normal to aea level and<br />

to its gsopotential surfaces. See afsa ebsolute<br />

gravity; center of gravity; Clalraut’a<br />

theorem; constant of gravltetIOn;<br />

direction of tho fores of grmrlty;<br />

●q uatorlal gravlt y value; squlpotontlal<br />

surface; formula for thooratlcal gravity;<br />

gravltatlon; Hayford daflactlon tamplets;<br />

Hayford effect; HalmaWs gravity<br />

formula of 1901; Halmert’s gravity<br />

formula of 1S16; Intenelty of grrivlfy:<br />

hftarnatlonal gravity formula; bosteay:<br />

Iongltude term gravity fOrmLtln; nOrmaf<br />

grevlty; observed gravfty; raduced<br />

gravity; regional gravity; ralatlva gr=vlty;<br />

raaldual grmrlty: resolution; rosolutlon<br />

limit; standard gravity; ●ubgrrwlty;


I<br />

tfrwerwtlcal gravity; Virtual gmvlty.<br />

gray ecal.-see ●top wodgs.<br />

great clrcl- cimle on the surf~e of the<br />

Eatth, the pt911s of w4tiih ~ throu@r the<br />

canter of fha Earih. Abe cafled orthodmm..<br />

great ●lllptlc ●’s-h arc defined by a pfana<br />

wllkhoontains fhatwJpdnfa and Ihacantsrof<br />

the raferanca spheroid.<br />

graet yem-Tfra parbd of one carrplete Wcle<br />

of the wquinosea around the ecfi@c, about<br />

25,S00 years. Alae called pletonk year.<br />

grwat-clmle bamlng-The inhiif diractbn of<br />

a great cirda through two terrestrial pdnts,<br />

em==~ as angufw di@a* fmm a mfarence<br />

direction. It te usually measured f- w at 1~<br />

reference duactica clockwise to 3S0°.<br />

grewt-olrote chart-A chart on wtriih a greet<br />

circle appasm as a straight Iinw ❑chart on the<br />

gnemonic prqaction.<br />

great-clink dlrectlorr-l+orfzontel direction of<br />

a great circle, expmssad as angular dkiance<br />

kern e raferanca diraclion.<br />

grwat-clrck dlctm’we-lbe length of the<br />

efrortar arc of the great circle pining two points.<br />

It is usualty azpraasad in nautical miias.<br />

gmat-wlrcle line-h land eurveying, the fine<br />

of interaadmn ef the surface of the Earth end<br />

the plane of e graat tircle of the ceiastial<br />

sphere.<br />

great4rcl* routs-(JCS) The mute which<br />

fdbwa the almrtasf arc d a great circle tefwean<br />

two pokrts.<br />

greatest ●longation-The maximum angular<br />

distance cd a bdy ef the sotar syetam hem the<br />

Sun, aB dwerved frem the Earth. The dirsdion<br />

efthebcdy eastorwastd thati Lsuaually<br />

~fiad, as the greatest dongation west.<br />

Gmwrwlch ●pparant time (GA~Local<br />

WPrent time at the Gr~nwictr nraridiin.<br />

Qreenwlch cIvII time (GC~See<br />

Unlvorsal Tlmo.<br />

Grwanwlch hour ●ngle (GHA)-Angular<br />

d~anse west of the Greenwich celestial<br />

MIL-HDBK-850<br />

111<br />

nwridii; the arc d the sa&ralii wyiator,or the<br />

angfa at the oafastii equator, or the angte at<br />

the celaatial pole, between the upper brarwh of<br />

the Greenwich ceieatial mari.iian ●rd the hour<br />

circle d a pebrf on the cdasfid sphere,<br />

rnaaaurad westward from the Greenwich<br />

oafasfid rnarirSan threugh 380°; -I hour angle<br />

at the Greenwich meridian.<br />

Graanwlch lntarvat-An interval baaed on<br />

the )Aoon’s transit of the Graa~ich -ii<br />

msridiin. as diatiiuishd frem a iccal interval<br />

based on the Moon’s transk .4 the local c9taet!!l<br />

rnatidisn.<br />

Graanwlch lunar tkna-Local lunar time at<br />

lha Greenwich rnaridiim the arc of the Aasfii<br />

equator er the angle, at tha cafaatial pole,<br />

between the lower branch of the Gmanwrs+<br />

Cataatial mwkfian and ths hour circle of the<br />

Moon, measured wesfwatd fmrn the kwer<br />

branch of tha Grwwhvich oakr.sti.slmeridian<br />

through 24 hours: Graamvkh hour angia of the<br />

Mom, expressed in time unka, p4ua 12 hours.<br />

Graanwich Mean Time (GMT)-(JCS) Also<br />

called Greenwich civil tlma; z-time: Zulu<br />

timm See ltnlveraal Tlma.<br />

Greenwtch meridian-The meridian through<br />

Greanti, England, ewving as the raferanca<br />

for Greenwich time, in centrast with tit<br />

merkfkrns. It is accepted almos4 untiersaliy as<br />

the prims meridian, or the origin d<br />

measurement of tongituda.<br />

Gmenwlch ●ldereaf data-Tha number of<br />

mean sidereai days thal have ekpaed a the<br />

Greenwich meridian since the beginning of the<br />

sidereal day that was in pmgraas at Greenwich<br />

maan neon on January 1, 4713 B.C. see also<br />

Gmanwich aldoreal day number.<br />

Gmonwich ●lderoal day number—The<br />

integral pert of the Greenwich sidereal date. It is<br />

e mearm d nurrbrirrg umsacuttidy ●uxaaaive<br />

akfereal daya beginning at the instrmts d qpr<br />

transit of the mean vernal equinox over the<br />

Greenwich nreridiin. See atao Groonwlch<br />

oldamal date.<br />

Gmwrwich sidamef tlmo (GST)-Local<br />

sidereal time at the Greenw~h meridian. Tfw am<br />

sf the celestial aquamr, or ths angie al the<br />

#astial pole, between the tqpar bmndt d the<br />

3raenwich cafeatial rneridiin end the hour side<br />

>f the varnal equinox, measured westward from<br />

ha upper trranch of the Greenwich cabstial


I<br />

meridian through 24 hours; Greenwich hcur<br />

s@e d the VWIMd F@nOX. =W- ~ t“~<br />

units.<br />

Grwenwlch time-llna basal upon the<br />

GM* marktisn as mferenm, as mnfrssed<br />

*thstbaa edWor reMof - meridian.<br />

grid smplltud~rrpfiiude relative to grid<br />

east or wwt. See also smplltudo.<br />

grfd azhntrth-The angle in the plans of<br />

P@tibn rnaaaumd cbdrwbe between a<br />

straight fiie and the central rneridiin of a ptane<br />

mcfingufar coordhale system.<br />

grid fmering-(JCS) searing measured ftom<br />

grid north.<br />

MIL-HDBK-850<br />

grfd computation-The detamrinaticm fmm<br />

a set of fables derived from formulas, of the true<br />

shape and dlmene’brrs of a grid, for the purpose<br />

of constructing such a grfd. The grid is<br />

mstherrmlimlly coordinated with its related map<br />

projacfiom they are usually compulsd<br />

corrW-renfty<br />

grid convergence-(JCS) The horizontal<br />

angle at a place between Irue north and gr”d<br />

ninth. It is pmporliinsl to the longitude<br />

difference between the pfsca and the central<br />

meridiin. See elsa convcrgenca.<br />

grid coordinate system-(JCS) A pfane<br />

rectangular oeordhale system ususlly bessd on,<br />

end rnathematbally adjusted to, a map<br />

prc@fion in order that gwgraphic p.aeifibns<br />

(fatitudes and longitudes) msY be ras~y<br />

tmrraformed into plane coordhslea and the<br />

rnmpUl~fiifrS refafing 10 them may be msde by<br />

the ordmsry mahrts of plane aurvayirrg.<br />

grid coordhratea-(JCS) Coordheles of a<br />

grid mordinste system to wtrich numbers ardor<br />

letters ●m assigned for use in designating e<br />

point on e gr)dded map, photograph, or chart.<br />

Sss also coordlneten.<br />

grid daaIlnatlon-The angular difference in<br />

dirscfion between grid rrorlh end hue north. II is<br />

measured ess or west fmm true north, Also<br />

called declination of grid north;<br />

gls.msnt.<br />

grid dhectlor@-foffxonfsJ dimctkin expreeaed<br />

as angular distance fmm grid north.<br />

112<br />

grid dlstanm-See grid Iarrgfh.<br />

grid equMOr-A fine pwpendhdar 10 a prime<br />

grid fnaridian, et the tiln.<br />

grid lntsrvaf-(JCS) The d~tsiwe represented<br />

be4ween the fines d a grid.<br />

grid Inverse-1’he computatbn d grid length<br />

and gr”idazimuths from grid coodinsks.<br />

grid JunctIona-Those Iirms daikreeting the<br />

jokringoftwoorrn ora@daY*emsmam$Por<br />

chart.<br />

grid Iatltuds-+ngular diatarrce from a grid<br />

equator. Sea else flctftloua Iatltudo.<br />

grid fangth-The dis$rmce between tw pdnts<br />

obtained by amputation from grid oocdrrdee<br />

of the points. It dtiera from the geodetic kengfh<br />

by the amount d a small correction besad on<br />

the acsfe factor for Ihs Iins. Also calfed grid<br />

dlstanca.<br />

grid lln@-CXre of the lines d e grid.<br />

grid longftude-Angular distance bstween e<br />

prime grid meridiin and sny given grid meridiin.<br />

See also ?ictltlous Iongltudo.<br />

grid magnotlc ●ngle-(JCS) Angular<br />

dtiere~e in diracfbn between grid mxfh and<br />

myr9nsfm nofih. It is rmmsured east or wasr fmrn<br />

gnd north. Afao called grlvatlon; grid<br />

varlatlon.<br />

grid merldlatine of the grid fines<br />

aslending in a grid north-south dkcfion. The<br />

reference grid meridiin is called prima grid<br />

marldlan. In polar mgicms the prims grid<br />

msridlan is usually the 180”4” geographic<br />

meriden. See also flctltkmm rn.rldlan.<br />

grid mathod+pktogremmetry) A method of<br />

pbrting ~il from oMque photogmp~ fV<br />

SWdW@sm9 e Wmpact&e C4 e map grid on a<br />

photograph ❑nd Imnsferring the detail by eye,<br />

thst is, by using the corr-ng lines of the<br />

msp grid and itrl pemp=tw e rmi plemment<br />

guides. See elm parspectlvs grid.<br />

grid north-(JCS) The rrorfherfy or zem<br />

direction Indutad by the grid datum of<br />

dirsct.ksrsl reference.


grid numbar-The numerical value of a grid<br />

Im indiiling the diafartcal of tfwt iii b ths<br />

felae origin of the grid. See alao grid<br />

coordlnsteo.<br />

grid ortgbs-l%s point, usually riser the carder<br />

of a grid zone, wfrare a parallel intersects a<br />

ncrtlh-acuth grid fine co”midenf to a msridiin.<br />

Ss0 nloo take ortgln.<br />

grid pamlle~ line parallel to e grid equelor,<br />

cormectrng all points d equal grid latitude. S0s<br />

afsc fktftloua pamllel.<br />

grid plstta-1. (cartography) See color<br />

aaparatlon drawlrtg. 2. (photogrammetry)<br />

See reeoau.<br />

grid prtme va~ical—The vertical through the<br />

grid east and west pointe of the horizon.<br />

grid rtrsrmb llne-A line meting MI same<br />

ObfiiUe Sn@S with all grid Motidiina. Grid<br />

parallels end meridiins may be considered<br />

apdal caeea C! the grid rhumb line. See alee<br />

flctltloue rhumb Ilno.<br />

gtld t~JCS) Snafl rnerkc on the neatlie<br />

of e map or chart indiiting eddiiiod grid<br />

raferertce 6yaferne trrcfuded otI that sheet. Grid<br />

ticks are aomerimse ehown on the Inferior grid<br />

fines of some rrv3ps for ease of refererwing.<br />

grid varletlon-See grid magnetic ●ngk.<br />

grid zonkAn arbifrery divisbn of the Eerfh’s<br />

aurfece deaigrrded for idemifiihn without<br />

reference to fatiiude w Ior@sle.<br />

gridded obllque-An oblique aerial<br />

pfm@mph printed with e auperimpeced grid to<br />

asaisf In the Idenfifmatic+t C4 e psrficufsr erea<br />

within the phdcgmph; used ohii for artihery<br />

epotfing.<br />

grlddad photograph (GP)—A photograph<br />

tih a pmcke geographic grid. Used for menual<br />

msssurernenl of preclaa coordinetas wfsem<br />

elevation Ie not required. Providas accepfatr4e<br />

nircreft inertial navigation system f~nt<br />

derivation es e substitute for survey or ether<br />

point pcsifkrrlng date.<br />

grid-l. (geod~ ) Two oats of perallef lines<br />

intersecting at ng “K t anglee and forming squares;<br />

e mctengular Certeaien cocrcihete system thet<br />

MI L-HDBK-850<br />

113<br />

lo aqxriqmaed on mep6, cherf6, and other<br />

sirrriiar rapresardetiersa 04 ftw asrthk surface in<br />

an accurate and cnnaics~ rmrmer te permit<br />

idantikatkxr d grourrd Iccetii with ra6pecl to<br />

other Iecatii and lhe mrrqwtefim of diractien<br />

end dwtame to other poinfc. Z A lype of<br />

cfigiial Ekwetiwr Model (DEM)thafiederivsd<br />

km LMerpoiating deva!bn values from<br />

ineguierty or regukrty qmced pointe that have<br />

X, Y. Z vefues. 3 A network oo~ d two<br />

fw”fiee of Iinas cuch tt-at ●pair 0! lines, one<br />

~~lam,ti~rnnowe Uwrrtw<br />

poi~. 4. (GIS) Program ckwekrpal at Harvard<br />

intheeatfy 197~wl@s a@aksadalfffba<br />

standard Sodean opsrefiorse that today’a t31S<br />

heva. See also ●rbttrary grid; ●ttsa grid:<br />

B?ltiah grid raferonco ●yatam; GEOI?EF;<br />

Lambert grid; ma]or grid; mllltery grid;<br />

military grid refomneo ●ycfom; Natiorml<br />

grid: overlapping grid; parsllactic grid;<br />

parspectivo grid; pohrt-deolgnatlon grid;<br />

polar grfd; ●econdary grid; tangorrt<br />

plene grid ●ystent; tranavorae Mercator<br />

grid; Unlvaroe.1 Polar Stomog mphlc<br />

(UPS) grid; Unlversel Tranavoma<br />

Mercator (UTM) grid; world polyconlc<br />

grid, praferred grid, primary grid, ond<br />

prime grid meridian.<br />

gripper edg~JCS)The edge by whch paper<br />

or other prinling maternal is drawn into the<br />

printing machine.<br />

gripper margin—See gripper ●dgo. ‘<br />

grlvation-See grid megnatlc mrgls.<br />

gress ●rror-Tfre recutl of carelessness er a<br />

mistake, Mey be detected through repelifhm of<br />

the measurements.<br />

groea model-The !otel overtep erea d e pair<br />

of eeriel photographs. See elscr rmat model.<br />

Ground Scale Distance (GSD)-For<br />

rectified irnegefy, GSD is the center-to-center<br />

ground distanm between edjectrnt pixels.<br />

ground camerc-See torreatrlal camera.<br />

ground control point-See control<br />

●tatlon.<br />

ground oontrol+JCS) A system of aocumte<br />

rnaaauremenfe used 10 determine the distencee<br />

and diracficos or dflarenoes m almfalicn<br />

between pointe on the Eerfh. Sea atso<br />

common control; control point; flaid


control; tmvorso.<br />

ground data-see ground truth.<br />

ground dlatarrca-The grea!drsb dtiance<br />

bdween fwe gmtmd pdfiirss, as oorrtmafad<br />

with ti ranger the afraigfrt.%te d=farrce<br />

between two points. A& sefled ground<br />

rang..<br />

MIL-HDBK-850<br />

ground @rrad forward (GGF)-(eeriel<br />

phdogmphy) The nel gain per phoiogreph in<br />

IIledirecfic lnefmgh fforaq%rclfie dovertep. The<br />

GGFkeuaed frrsonpufe ffrerxsrrtmrrof<br />

expoaure=3 In a aft@ of aerial phmgmphy.<br />

ground galrrod .Idawaya (QGS)- (aerial<br />

photography) The net IrAerel pin par tliihf fcf a<br />

apesifii aidebp. The GGS b used 10 sornpme<br />

the rrurrber of flight Iii- for an arm to be<br />

photographed.<br />

ground Irrtormatlon-sae ground truth.<br />

ground nsdlr-(JCS) The point on the ground<br />

verficeffy bermelh the perepesfiie senfer of the<br />

camera lens, On e true verkai phc.togreph ths<br />

coinddee wkh the prfnci@ point. Atso celled<br />

ground plumb point.<br />

ground pw’alld-The intersection of the<br />

pksne of the photograph with the plane of<br />

refemmce of the ground. See also axis of<br />

homology.<br />

ground photogrammetry-See terrtsatrlal<br />

photogrammotry.<br />

ground photograph-See tormatrfel<br />

photograph,<br />

ground plmra-The horisonfal plene paeaing<br />

through the ground nadir of a camera station.<br />

ground plumb point-See ground rradlr.<br />

ground pyramid-A rnmponerrt of an<br />

andyiicaf method for determining the pr-iae<br />

degree of photographic tilt, representing e<br />

epedk apelkl oorrfigumtian from three ground<br />

scmfml pdrds (forming a triengle) on the ground<br />

to the @q%raure etafiin of the phonograph<br />

cmfainirrg the identical points. When used with<br />

the photo pyramid, the ground pyremid permits<br />

the axecf arrafyiical dafermkratti c4 tiil In the<br />

photograph. See aleo photo pymmld.<br />

114<br />

ground ranga-See ground diatanao.<br />

ground mBolutloKThs mirimurn diatmrce<br />

which sen be defeded Mweem two edjacarrf<br />

k+aturas, or the rrsinirrwrn size of a feature<br />

axpmaad insizeot c@jeordisfMaes ontfte<br />

ground.<br />

ground mturrr-(JCS) The raffection from the<br />

terrain as diiyed arder mmrdad 65 an<br />

irmge.<br />

ground qmd+fCS) The herknfal<br />

cOMpOnMt cd the sfmad d an aircraft relative to<br />

the aarfh’a utriese.<br />

ground ●tatlon-A monumented atatiom:<br />

eeteblbfd by fiifd eurvey mathode, wtiih IS<br />

U* as a baas for ground station equipment for<br />

the procurement of shoren or ehiran contmliad<br />

photography or control defa.<br />

ground ●mvey-A eurvey made by ground<br />

methods, ae distinguished fmm an eeriel eurvey.<br />

A ground eurvey may or may nd irrslude the<br />

uea of Photographs.<br />

ground swing-An error-causing sorrdidion in<br />

electronic dietarroe meesuring whii is brought<br />

about by the reffadion of the microwave baem<br />

from the ground or water surface. The reflected<br />

beam mixes with ha direct beam et the<br />

reseiving antenna, thereby changing the pheee<br />

of the d!recf beam and causing an error in the<br />

diefarrce rnaesured. By varying the carrier<br />

frequensy, the war bewrnes Syclic, rmking<br />

poeeible mean inelrument reedinga thet ere<br />

subatanfiilly accurate.<br />

ground trec*See ground parsilol.<br />

ground track-The vertical projectbn of the<br />

flight prfh omo the surfas.a of Wre aerfh.<br />

ground trrsth-A ferm coined for<br />

dattikrformetion obtained frum actual ground<br />

rneaeurement of euriaodshurfase feeturoe 10<br />

aid in the interpretation of rerrrofefy eenaerf<br />

data. Afeo called ground data; ground<br />

information.<br />

ground-sp=co coordlnato ●yatmn-A<br />

scheme by which Fostions of tnangulafion<br />

stalks, confrd poirrta, and other ground<br />

featume are raleted by diefwrse end azimuth or<br />

by x. and y-cwrdinetes.


‘)<br />

I<br />

I<br />

g!rwd steka+surwying) A stake dtiven near<br />

n hh, ueuafty eloped with the @ of the QUSrd<br />

-ka over the hltr. The guard stake protxls,<br />

and Ba merf@p identify, the hub. .<br />

gulda marldian-An auslfiery governing line<br />

PrOiecfed north afong an aatmnornic meridii,<br />

fmm fminta esfabfiied on the base lie or a<br />

sterderd paraibl, usuelfy at krtervels d 24 rnk<br />

east or west of the princ!pal meridian, on whkh<br />

tovmahip, aaction, and qumler aecfion eomam<br />

are esfabliched. See also ●uxiliary guide<br />

meridian; prlnetpal marldlan.<br />

guld~ drafting or aoribing surface beering a<br />

map frrwge to be tnaxtd by drafthg or scribing<br />

for repmduckn. Also celled color ●operation<br />

guida; drafting guldo; scribing guide.<br />

Gunta~a chain-A measuring device used in<br />

land suweying, oorrposad of 100 metal links<br />

fastened together with rings, the length cd Ihe<br />

chain being 66 feet. Alao called four-pole<br />

chain; tour-rod chain. See else chsln.<br />

gyroazlmuth theodollta-See gyrotfloodollto.<br />

gyrooompaus-A compa6s whiih functions by<br />

virlue d the co@as genersted in e retor when<br />

ths latter’s esie is displaced from parallelism with<br />

that of the Eerfh. A gyrocornps= is<br />

independent of megnetiem and *II<br />

eulcwneticefty align itseff in the celestial matiten.<br />

However, it requires e sfesdy tmurca of motiie<br />

power and is subject to dynamic error under<br />

certein conditions. Certain aircdt corrpesses<br />

alse u gpsoo@s to gain Sfabitii, while<br />

ralyhg besiilty on the tmgnatic meridian:<br />

theaa are to be distinguished from lhe hue<br />

gyrocompass.<br />

gyromagnatlc compe8s-(JCS) A directional<br />

9Y~ whose az”mufh scale is M“nfained<br />

iii atigntit whh the magnetic meridisn by a<br />

megnefic detector unit.<br />

gyromorldlan Indicating instrument-See<br />

gyrothoodolito.<br />

gyroscopa-A device consisting of e spinning<br />

rolor and as.sAetad supporting readouts whiih<br />

mskas use d Newion’a hw of Roiation 10 give<br />

an indkdion of the errgufar velocii of the.<br />

instrumanra case with r- to an inertial<br />

reference frame. Thie instrument ie used as the<br />

basic aaneor in many direct’kn%aaking,<br />

MIL-HDBK-E150<br />

115<br />

duectii-keepirrg, and etfifude stabilization<br />

ay6tems.<br />

gyroacoplc ●ablllxetlon-Equilibrium in the<br />

attitude ancVor oouraa of e shii or airborne<br />

vehicle rnaintaind by the usa of gymecopes.<br />

Atao, the maintenance (bytheuseof<br />

gymecopes) of .s samare in a desired aftkrde<br />

*n an eirbema vehiile.<br />

gyrothacrdoiita-A heurieiiie with e<br />

gymmqxm attached or buitf in, whereby a<br />

true azimuth rdersnce can be aetabkhsd in<br />

any Waether, day or night, without the aid&<br />

Stars, Iw-ldrrmrks, er other ViaiMe stations. The<br />

az”muth obtained fmm the gyro w hwrtiai<br />

theodofiie ie assantieity the astronomic az”nuth<br />

at the point of observation. This azimuth will<br />

dfler from the corresponding geodetic ezimufh<br />

by the emount of the Laplece cerractiwi.


I<br />

I<br />

I<br />

I<br />

I<br />

H and D curva-See characteristic curve.<br />

hachurlng—(JCS) A melhod of representing<br />

def upon a map or chart by shading In shorf<br />

diifmacfad fines drawn In the direction of lhe<br />

sbpaa.<br />

hack chronometer-A chronometer used for<br />

ViSUel reference, and not usually for re~rd<br />

purposes.<br />

halatlorr-(photography) A spreading o! a<br />

photograpffic image beyond Its proper<br />

boundaries, due especially to reflection from the<br />

side of the lifrn or plate support opposite to that<br />

on which the emulsion is coated. Particularly<br />

noticeable in phonographs of brighl objects<br />

egainsf a darker background.<br />

half merk-See Indax mark.<br />

half model—The stereoscopic model iormed<br />

by the ovariap of two adjacenf right- or left-hand<br />

expesures of Wnvergenl photographs.<br />

hall aectlon-Any two quarter seclions within<br />

a secfion which have a common boundary:<br />

uSU.Wlyidenlifiad as the north hatl, south hall,<br />

east hail, or west haff of a panicular section.<br />

half tide taval—See maan tide leVel.<br />

haltfona scraen~JCS) A series of regularly<br />

spaced opaque lines on glass, crossing a! righl<br />

anglea, producing transparent apertures<br />

between Intersections, Used in a process<br />

camera to break up a solid or continuous tone<br />

image lnlo a pattern of small dots. Also called<br />

croaslfne glaes screan. See also contact<br />

acrean; halltone,<br />

helltone—(JCS) Any photomechanical prinling<br />

sudace or the impression therefrom In which<br />

detail and tone values are represented by a<br />

series of evenly spaced dots of varying size and<br />

shape, varying in direct proportion to the<br />

intensity Of the tones they represent. See aiso<br />

halftone screen: mlddletone.<br />

HaM Mar projection—A variation, by E,<br />

Hammer in 1892, on the zenithal equal-area<br />

(Larnberf) projection, made by doubling the<br />

hortzomal distances along each parallel from the<br />

MIL-HDBK-850<br />

H<br />

116<br />

central meridian. This transforms Ihe ckular<br />

shape of the Lamberl into an elliise, slrnilar in<br />

appearance to a Mollweide projacfion, but with<br />

all parallels curved except the Equator, which IS<br />

a straight Iina.<br />

hand leval-A hand-held tnstrumanf for<br />

approximate levating, If cmnsisfs of a sighting<br />

tube with a splfi fie!U of view; a trorlzomal cross<br />

hair in one-half of the fiakj biiacfa the Image of<br />

a spirit Iavel in tha other haft when the<br />

inatmment is held ievel. See also Abney Iavel.<br />

hand proof-in offset ilthography, a proof of a<br />

plata made on a hand proof press where<br />

oparatiins are manual for inking, dampening,<br />

and laking the impression.<br />

hand templet—A lemplel made by tracing<br />

the radials from the photograph onto a<br />

transparent plastic medium. Hand templets are<br />

iaid out and adjusted by hand to tomr the radial<br />

triangulation.<br />

hand-templet pioi—See bend-templet<br />

Irianguiatlon.<br />

bend-tempia! triangulation—A graphical<br />

radial triangula!’bn using any form Ot hand<br />

templel. Also called hand-ternplet pioi.<br />

hanging levei—A spirit Iavel so mounted that,<br />

when in use, its Ieval tube is lower in elevation<br />

than is points ot support,<br />

Harbor and ApprOaCh chars (HA)—A chatl<br />

which provides delaiied porlrayal of<br />

navigationally useful information supportive of<br />

maneuvering In close quaner areas to<br />

benh/anchor, channei keeping while<br />

emering/exiling port or navQating in close<br />

proximity 10 dangars associated with close<br />

shore/harlmr approach areas. Produced from<br />

1:10,000 to ?:100,000 scale.<br />

harbor chart-A nautical chart intended for<br />

navigation and anchorage in harimrs and<br />

smaller waterways.<br />

Hardcopy Exploitation Segment<br />

[HE/S)—Segment of DMAS DiSital Pmducfkm<br />

System which provides sottware upgrades for<br />

~xisting DMA photogrammetric aquipmam and<br />

#ill delivar a new computer for triangulation.


Outputs include digital elevation data and<br />

rectified and orthorecfified imagery. See also<br />

Dlgltal Production System; MARK 85.<br />

hardcopy—Producfs which are primed on<br />

papar, photograph materials or other media,<br />

and can be interpreted dlreclfy by the human<br />

user.<br />

hmnonlc coefflclente-lhe coefficients of<br />

t@OltOMStriC terms Of an infinite series used 10<br />

approximate an Irregutsr ckmed surface. See<br />

8180 spherical harmonics.<br />

harmonic component—Any of the simple<br />

sinusoidal components into which a periodic<br />

quantify may be resolved.<br />

hermonlc constents—Tha amplitude snd<br />

epochs 01 the harmonic constituents of the tide<br />

or tidal current at any place.<br />

harmonic constituent—See constltuerrf.<br />

harmonic axpreaalone—Trigonometric terms<br />

of an infinite series used to approximate<br />

irregular curves in two or three dimensions.<br />

harmonic tunctlon—Any real function Ihsl<br />

satisfies Laplace’s equation,<br />

hamronlc mollon—The projection of circular<br />

motion on a diameter of the circle Of such<br />

motion.<br />

harmonic—A sinusoidal quantity heving a<br />

hequency that is an integrel multiple of the<br />

frequency of s periodic quantily to which ii is<br />

relatel See also compound harmonic<br />

motion; gravitational hsrmonlcs;<br />

sactorlal harmonics; almple harmonic<br />

motion; apherlcal harmonics: tesseral<br />

lSSrMOnlCS; zonal harmonica.<br />

Hassler baae-llna measurlrrg<br />

aPParatuS-~ Optical base-llne measurkrff<br />

apparatus consisting of tour rectangular iron<br />

bars mounted end to and In a wooden box.<br />

Each bar h 2 metara long. The combined length<br />

of tire apparatus being 8 me!ers.<br />

tiaylord dallectlon templsts—Templels<br />

used In mnneclbn with studies for the figure of<br />

Ihe Earth and ieostasy. In obtaining elevation<br />

raadings hmm maps in connection with<br />

topographic and Isostalic reductions, femplets of<br />

plastic are used, The templets used in<br />

MIL-HDBK-850<br />

connection with defleci”bn of the varlical studies<br />

have circles and radial tines drawn u~n them,<br />

S0 proportioned wilfl refereme to scale of map<br />

and azimuth thal land elevations and ocean<br />

depths within each compartment formed by<br />

adjacent arcs ard radii can be easily averaged<br />

and the effect of the mass therein on a plumb<br />

liIIS at the station (center O! Circles), under<br />

various hypotheses, can be computed. See also<br />

Hayford gravity templeta.<br />

Heyford elfact-The direci aftacf on gravity of<br />

masses of unit deneity extending to various<br />

distances abova and bsbw sea level; it nagleds<br />

the differences of elevat”mn batwaen tha<br />

relerertce spharoid and the gaoid.<br />

Hayford gravity anomalles/Hayford<br />

anamalles—lsostatic anomalies obtained by<br />

computing the isoalatic compensation according<br />

to the Pratt theory of isostasy es developed by<br />

Hayford, using various depths tor purposes 01<br />

comparative analysis,<br />

Hayford gravity templeta—Tamplets used<br />

in connection with gravity aludies whtch are<br />

similar 10 Haytord deflection templets excapt<br />

thal no account is taken ot ~im~h, aII<br />

compartments bounded by a given pair of<br />

circles being of the same eize and shape. A<br />

given templei can be used only on maps of the<br />

scale and projection for which it is constructed.<br />

See also Hayford deflection templata.<br />

Hsytord epherold (elllpaold)-A rafsrance<br />

ellipsoid having the fOlloWirIg approximate<br />

dimensions: semimajor axis 6,378,3S8.0<br />

meters: semi minor axis-6,356,909,0 meters;<br />

and the flattening or ellipticity 1/297.00,<br />

l+ayford-Bowle method of Iaoatatlc<br />

reduction—A method of rmmputing tha effacf<br />

of topography and isostatk compansatiorr on<br />

grsvity by which the effact of topography IS<br />

compuled dirsctiy and then corracfed for the<br />

effaCl of isostatic compansalion. Tha mechani~<br />

of this method invoive the use of the Haylord<br />

gravity iamplets.<br />

Hay ford-Bullard (or Bullard) mathod of<br />

lsostatic reduction—A method by which the<br />

topographic effect of an infinita slab of density<br />

2.67 and a thicknass equal to the elavation of<br />

the gravity atalion is first computad, and then<br />

corrected for curvature of the aea Iavai surface<br />

and, fOr difference of eievation between the<br />

station and the to~graphy.<br />

117


i<br />

I<br />

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I<br />

I<br />

I<br />

I<br />

I<br />

haza-The radiance of the atmosphere.<br />

heading-(JCS) (navigation) The diretilon in<br />

whfch the fongtfudinsl azis of an aircralt or ship<br />

Ie pointed, usually expressed in degrees<br />

cicrckwise from mrffr (true, magnetic, compass,<br />

or grid).<br />

height rsnomaly-T?re difference between the<br />

height of a terrain point above the reference<br />

spheroid and the corresponding rwrmal height,<br />

rrSSaSUred along the normal piumb he.<br />

height difterantirN-Tfre difference In height<br />

between predominant height grouplnge In a<br />

homogeneous sutlace area.<br />

trelgfrt displacement—See roller<br />

dlsplacemant.<br />

halght !lndar—A stereoscopic range finder so<br />

constructed as 10 indicale vertical heights rather<br />

than slant rarge. See also stereometer.<br />

helgtrt of Instrument-l. (spirit leveling) The<br />

height 01 the line of sight 01 a leveling<br />

instrumem above the adopted datum, 2. (sladia<br />

surveying) The height o! the center oi the<br />

Ielescope (horizontal axis) of transit or telescopic<br />

afidade above Ihe ground or station mark. 3.<br />

(trigonomatrfc leveling) The nelgtd of tne cenler<br />

Of the thaodollfe (horizontal axis) above the<br />

ground or station mark.<br />

MIL-HDBK-850<br />

Sun as origin.<br />

ttellotropa-A device used in geodetic<br />

surveying Ior reflecting the Sun’s rays to a<br />

distanl point, to ati in bng-dbtams<br />

observations. Sae also aalOnOtrOpSr.<br />

hellpad-(JCS) A prepared area dssfgnated<br />

and used for take off and Iancthg ot heficoprars.<br />

(Inctudas iouchdown or hovefpoint.]<br />

hellport-(JCS) A facility designated for<br />

operating, basing, setvicing, and malnlalnlng<br />

helicopters.<br />

Helmert’8 gravity tormula of 1901—A<br />

formula for theoretical gravity developed from<br />

the gravity observations available al the lime<br />

(1901), but not ,fitted to any preassigned value<br />

of Use Earths elfipticity,<br />

Halmart’a gravity formula of 1915-A<br />

Iormula for theoreibsl gravtty based on a triasial<br />

ellipsoid and therefore includes a bngitude<br />

term. See also Iongltuda term gravity<br />

formula.<br />

hemispherical map—A map of one-haff of<br />

the Earths surface, tounded by the Equator, or<br />

by meridians.<br />

hidden finee-Line segments obscured from<br />

view in a projected image of a threa+imansional<br />

object.<br />

height of fhe tk4a-The vertical distance hferarchy-(digital) A system of cfaesitying<br />

from charl datum to the surlace water level al features acmrding 10 feature type and<br />

any stage of the t“de usually measured in feat. signifbance. For exampla, in some cases<br />

features with lower numbem are mesked out by<br />

halght-of-eye CorrectIon—That correction to higher numbared features occupying the same<br />

sextant aftiiude due to dip of the horizon. Also posit ion.<br />

called dlD COrraCtlOn.<br />

height-(JCS) The vertical distance of an<br />

object, poim, of level above the ground or other<br />

eatabfiehed referance plane. Height may be<br />

Irxfbated as follows: very /ow-bslow 500 feet<br />

but above ground level; /Ow-SOO to 2,000<br />

feet; mediu*2 ,000 1025,000 feet; frigh-<br />

25,0001050,000 feet: very high-above 50,000<br />

feet. See also altltuda; elevallon;<br />

ellipsoidal height; geoldal hefgnt.<br />

heliocentric paraflax-See annual<br />

parallax.<br />

heliocentric—Relative to the center of the<br />

High Speed Digital Chart (fiSDC)-. vector<br />

digifal chart of selected and generalized coestai,<br />

and harbor and approach charl inforrnafion in<br />

supgwt of navigation and colliiion-avoidance<br />

display systems, HSDC davebpmem waa<br />

coordinated. with the National Ocean Senrica<br />

and Is produmd using Committee on the<br />

Exchange of Digital Data formal feature<br />

encoding. HSDC is no longer supported by<br />

OMA.<br />

high altltude-(JCS) Conventionality, an<br />

attitude above 10,000 reelers (33,000 feet). See<br />

also altitude.<br />

118


I<br />

}<br />

high denelty tops (HDT, HDDT)- A n<br />

anafog racordtng Orrd pleyback system for<br />

6tOring very high rale data that Is not directly<br />

compatible whh general purpose mmputer<br />

systems. Lfsed by CIMA for source imagery<br />

under Digiial PmducIion Syalem production.<br />

Afao known as high density digital tape because<br />

the source imagery is Irarwlerred as digital data.<br />

high rod-See long rod.<br />

high tlda-See high water.<br />

high water (HW)--The highest limit of the<br />

surlace wafer Ieval raached by the rising tide.<br />

High waler Is caused by the astronomic tideproducing<br />

forces andror the effects of<br />

meteorological conditions. Also called hlg h<br />

tide.<br />

high weter full and change (HWF&C)—<br />

See eatabllahment of the port.<br />

htgh water lntervel—See Iunkldel<br />

Intervel.<br />

high water lhra-The line on lhe bank or<br />

shore to which the waters normally rise at high<br />

water. In tidal walers, the high water line is. in<br />

strictness, the {nrersect(on ot the plane of ttra<br />

mean high water with ttse shore. The high waler<br />

lin@ is the boundary line between the bed and<br />

the bank of a stream.<br />

high water Iurtltldal Interval-See<br />

Iunltldal Interval.<br />

high water springs—Sae mean high<br />

water sprlnge.<br />

high-obllque photograph—See oblique<br />

elr photograph.<br />

higher Mgh WatOr (HHW)-The higher 01<br />

two hfgh waters occurring durfng a tidal day<br />

where the tide exhibis mixed characteristics.<br />

frlgher high water Interval (HHWl)-The<br />

Interval o! time between the transit (upper or<br />

tower) of the Mmn over the local or Greenwich<br />

martdlan ati the nexl higher high water. This<br />

expression Is use when there is considerable<br />

diurnal inequality. See also hmlt1d81 Interval.<br />

higher low weter (HLW)-The higher of two<br />

low watem of a tktal day where the tide exhibits<br />

MIL-HDBK-850<br />

mixad characfarisiics.<br />

higher low water Interval (HLWl)-The<br />

inteWai 0[ tiMe betWEen the lriUWil (u~r or<br />

tower] Of the Moon over Ihe focal or Greenwich<br />

meridian and the nest h~her ~, waler. This<br />

expression is used when there is C.ons”dersble<br />

diurnal inequality. See also Iunlttda) MWmusJ.<br />

hlgheat elevatlon-That elevafkm whlcfr la<br />

the h~hest point of relief within Ihe area of a<br />

map or chart. See also critical elevatlon.<br />

high-(JCS) A height between 25,000 and<br />

50,000 feet.<br />

hill plene-lhe plane containing the posifiins<br />

of three ground marks constffuting control<br />

points. This may be, buf rarely is, a hOtizOmal<br />

plane.<br />

hill ahadlng-(JCS) A method of representing<br />

refief on a map by sfepicfing the ShadOw5 that<br />

would ba cast by high gruund if t!!ht were<br />

shining fmm a cerlahr direction, Also calted<br />

hlllwork. See also sheded rellef.<br />

hltlwork-See hill shasflng..,<br />

hlStOrlCSd ctrart-A chart based on data from<br />

previous years 10 determine probable<br />

oceanographic palterns for a specified time.<br />

Also called flref approximation chert.<br />

hletory overlay—A specially prepared matte<br />

plaatic material which shows the sources of all<br />

sounding dala used in a bathymetric<br />

compilation.<br />

holldey-(JCS) An urrinlentional omission in<br />

imagery coverage of an area. See also gap.<br />

hologrammetry—lhe arl or science of<br />

interpreting the threedimensbnal holographic<br />

image and obtaining reliable measurement by<br />

means of hobgraphy.<br />

hologram—The hologram offers a<br />

reconstnr~ton of the ax femal appearance of an<br />

object with unique threedirnensional propart’km.<br />

This is accomplished by illuminating Ihe object<br />

with coherent light.<br />

hornogeneoue area-An area which has<br />

uniform radar reflecting p9wer at all points.<br />

119<br />

homogeneous eurtace area-A grouping


of features having the same general surface<br />

composition.<br />

homoloaouri Images-The images o{ a<br />

single object point Shal appears on each of two<br />

or more overleppimg pholograpfm having<br />

dittarant perepecuve c%nters.<br />

homologous photographa—Two or more<br />

ovartapplng photographs having ditferam<br />

camera stations.<br />

hotnolooous reye-The two perspective rays<br />

corresponding to a pair 01 homobgous image<br />

pdsts.<br />

homologous—Ttre condilion whera an Image<br />

of a given object pokrt or series of such polnls is<br />

common 10 two or mora projections having<br />

diffarenl perspective centers.<br />

tsomolographlc (homafograph[c) map<br />

proJsrctlon-An equal-area map projection.<br />

This term ia found in the designations givan<br />

Some particular map projections, such as lhe<br />

Mollweide homalographic projection.<br />

horizon camera—-A camera used in<br />

conjunction with another aerial camera 10<br />

photograph the horizon simultaneously with Ihe<br />

olher photographs. The horizon photographs<br />

indicate the tilts of the othar photographs.<br />

horizon closure—See error of closure,<br />

definffion 6.<br />

horizon coordinate system—See horizon<br />

system of coordinates.<br />

horizon photograph—1. A photograph of<br />

the horizon takan simullansously with anolher<br />

photograph for the sole purpose o! obtaining an<br />

Itiicafion of the orientation of the other<br />

pho!o~raph at the time of exposure. 2.<br />

(surveying) A corwlnuous matched Sal 01 horizon<br />

photograph defining obstructions 360°around<br />

a given station.<br />

horizon prkzm—A prism which can be Insenerl<br />

In the optical path of an instrument, such as a<br />

bubble saxtant, to permit obsewation of Iha<br />

visible horizon.<br />

hortzon profile-A pfot of vertical angles<br />

agahtst Ihe norlzomal anglas taken 360” around<br />

a point wtth annotation. See also horizon<br />

photograph; frorlzon aweep.<br />

MIL-HDBK-850<br />

horizon sweep-( surveying) A preliminary<br />

reconnaissance technique where the Instrument<br />

is pointad inH\ally al the farthest v’biilde known<br />

poim and recording clockvrba anglas to tarka,<br />

spiras, buitdtigs, signals, etc., tor purposes of<br />

idenllflcat”km and eubsequem use. Sea ateo<br />

horizon profile.<br />

horizon system of coordlnatee-A aet 01<br />

celestial coordhates, usually altiiude and<br />

azimuth or azimuth angle, basad on Ihe<br />

celestial horizon as tha primary graat clrcte. Also<br />

called horizon coordinate system.<br />

horizon traca-An imaginary fine, In the plane<br />

of a photograph, which represents the image of<br />

the true horizon tt corresponds to the<br />

intersection of the plane ot a photograph and<br />

!he horizontal plane containing tha internal<br />

perspective cemer or rear nodal point of the<br />

lens. See also true horizon.<br />

horizontal angle-Angle in a horizontal<br />

plane.<br />

horizontal axis—The axis about which the<br />

[alescope of a theotilie or transit rotates when<br />

moved vertically,<br />

horizontal bridging—See brldglng.<br />

horizontal circle-A graduated circle affixed<br />

to lhe lower plate of a transtf by which horizontal<br />

angtes can be measured.<br />

horizontal closure error—See srror of<br />

closure, definition 8.<br />

horizontal control dstum—A geodetic<br />

reference point which is the basis for horizontal<br />

control surveys, and of wttiih tiia quamifies ara<br />

known: latitude, longitude, azimuth of a tine<br />

trom this pint, and two constanta which arc the<br />

parameters of the reference ellipsoid. Tfre<br />

horizontal conlrol dstum may extend ovar a<br />

continent or be limited to a small area. Also<br />

called horizontal datum; horizontal<br />

gsodstlc datum.<br />

horizontal Controf point—Sae horizontal<br />

control station.<br />

horizontal control staflon—A station whose<br />

position haS been accurately determined in xand<br />

~grid Coordinates, or Iatituda snd longitude.<br />

Also called horizontal control point.<br />

120


horizontal conirol survey net-See<br />

survey net, delinifkm 1.<br />

horizontal controf-A network o/ stations of<br />

known geographic or grid fmsitions referred to a<br />

cvmn horizontal datum, wh”ch control the<br />

horizontal posirbns of mapped features with<br />

respect to parallels and mariduns, or northirrg<br />

and casting grid Iirrae ehown on lhe map.<br />

HOdXOntal control Irwtudes basic (marked) and<br />

Supplemanrary @nnsrrtsed) stallona.<br />

horizontal copiane-See baeal coplane.<br />

horizontal datum—See datum, definition 2.<br />

horizontal deformation—in relative<br />

ortenfalion, the cumulative model warpage<br />

atfecfing the horizontal datum from z-motion<br />

error, brldglng error, and swing error.<br />

lIOrlZOntal dlrectlon—Obse Ned frorlzorrtal<br />

angles at a triangulation station reduced to a<br />

common iniiial direction.<br />

horizontal extension—See extension,<br />

definition 2.<br />

hortzontel geodetic datum—See<br />

horizontal control datum.<br />

horizontal lntenelly—The intensity of the<br />

horizontal component of the magnetic field in<br />

the plane of the msgneilc meridian.<br />

horizontal lhw-A line perpendicular to the<br />

veriic.al.<br />

horizontal parellax—1. (astronomy) The<br />

geocentric parallax of a body on the observer’s<br />

trorfzon. This is equal 10 the angular<br />

semidiameter of the Earlh as seen Irom the<br />

body. 2. (phologrammelry) See absolute<br />

stereoscopic parallaz.<br />

horizontal pase point—See supplemental<br />

poaltlon.<br />

horlzorttal photo~raph—A photograph<br />

taken with the axis of the camere horizontal.<br />

horlzontaf plane-1. A plane perpendicular<br />

10 tha diradion of gravity: and plane tangent to<br />

the gsoki or parallel to euch a plana, 2.<br />

(surveying) A plane perpendicular 10 the plumb<br />

line wittsjn which, or on which, angles and<br />

MIL-HC)BK-850<br />

distances are observed. For any plenknatric<br />

survey il is assumed that all plumb fines therein<br />

are parallel, and all horizontal pfanas therein are<br />

parallel<br />

horizontal retraction—A natural error In<br />

SUweYiW which is the raautt of the horizontal<br />

bending of fighl rays berween a target and en<br />

obsewing Instrument. Usually cauaed by the<br />

dttterences In density of the air along the path of<br />

the light rays, reauffing from temperature<br />

variations. See also terreatrlal refraction.<br />

horizontal stadla—A method of measuring<br />

dk4aWeS wherein the stadia rod is held in a<br />

horizontal position and the stadia hairs of the<br />

irratrurrrenl are vertical during obsarvatkms.<br />

horizontal taping and plumbhrg—A<br />

method whereby the tape is field horizontally,<br />

and the posilione of M pertinent ~raduations are<br />

projected to the ground with plumb bobs.<br />

horizontal/vertical brldglng—See<br />

brldglng.<br />

horizontal/vertical exIenalon—See<br />

eXtenSIOn del,ini.,on 2.<br />

horlzontallzlng tha model—See leVellhg,<br />

definition 2.<br />

horizontally comrolled photography—<br />

Cartographic aerial photography obtained<br />

simultaneously with racardlng of distanca<br />

measurements between the taking aircratf and<br />

aach of Iwo or more geodetically positioned<br />

ground stations. Shoran or ehiran are normally<br />

used as lhe dklance measuring equipment.<br />

The resuft is precise relative horizontal<br />

positioning o! each photograph which has<br />

associated recorded distances. This positioning<br />

information is used as horizontal control data in<br />

Ihe mapping process.<br />

horizon—(JCS) fn general, rhe apparent or<br />

visible junction of the earlh and sky, ae seen<br />

Irom any specffic positbn. Also called the<br />

aPParent, vlslble, or local horizon. A<br />

horizontal plane passing through a point of<br />

vision or perapectlve center. [me apparent or<br />

visible hor”uon approximates the true horizon<br />

only whan the poim of vision is very cbse to eee<br />

level,] See also apparent horizon; attltuda<br />

Indlcaror; calestlal horizon; felee<br />

horizon; geocentric horizon; geoldal<br />

horizon; geometrical horizon; radar<br />

horizon; eenslble horizon; trua horizon.<br />

121


I<br />

Hormbow Irwol attachment-A level used<br />

In rnn~nction wilh a micrometer in a Ielesmpe<br />

whereby Ietiude observations by the Horrebow-<br />

Talcoff method can be made.<br />

Horrebow.Talcott method of Iatltude<br />

deWrmlrtatlon—See latitude<br />

delarmlnsition; zenith. telescope<br />

method.<br />

hot spot+pholography) A small area 01<br />

undesired brilliancy o! Illumination in the image<br />

projected by a prfmer or a reader.<br />

Hotlne Obllque Mercator—A mapping<br />

prmjecfion devebped spacilicaliy for LANDSAT<br />

Imagery, dividing the Earth info five zones o!<br />

Iafiiude, Wtihin each zone, oblique strips<br />

cm’respondng to indwktual LANDSAT spacecraft<br />

paths are projected onto a plane. The axk of<br />

projection surresponds approximately 10 the<br />

path of scene cemers.<br />

hour angle difference—See merldlan<br />

angle dltrerence.<br />

hour angle system (of coordinates)—A n<br />

equatorial system 0! curvilinear celestial<br />

coordinates which has the Equaior and the local<br />

meridian as primafy and sewndary reference<br />

planas, respectively. The position of a celestial<br />

body iS Qfven by ifs hour angle end declination.<br />

hour angle-The hour angle of a celestial<br />

body la the time elapsed since ifs upper transit.<br />

II k tfre engle between the observers<br />

(eslronomic) maridlan and the declination circle<br />

01 the body, measured positive westward from<br />

the meridian. See also Greenwlcn hour<br />

anQle; IOcal hour angle; sidereal hour<br />

angle.<br />

hour circle-Any great circle on the celestial<br />

sphere whose plane {s perpendkwlar 10 the<br />

plane o! the celestial equator. Also called circle<br />

of decllnatlon; circle of rlghl aacanalon.<br />

See also celestlal merldlen; coluras.<br />

hub-A temporary traverse station marker,,<br />

usualfy 01 wood, The stake is driven flush with<br />

ihe ground with a tack or small nail on top 10<br />

mark the exact point of reference for angular<br />

and linear measurements,<br />

Hull Integrlly Test Site Charfe (HITS)—<br />

Charfs which provide detailed bathymakic and<br />

environmental data for submarine test dive<br />

MIL-HDBK-850<br />

areas.<br />

Huygen’s prlnclple-A general princlpla<br />

applying to all Iorma of wave motion which<br />

states that every point on the instantaneous<br />

position of an advarcirq phasa fmnf (wave<br />

front) may be regarded as a source of<br />

secondary spherical wavelets. The poeiffon of<br />

the phase front a momam Ialar Is then<br />

determined as the envelops ot all of the<br />

secondary wavelets (ad Inflrrlfum). This principle<br />

is extremely useful In undarsfanding effecls due<br />

to refraction, reflecfbn, dfiracsion, and<br />

SCaltWin!J of all types 0( radiatiin, including<br />

sonic radiadon as well as electromagnetic<br />

radiation and applying aven lo ocean wava<br />

propagation.<br />

Hydrographlc Information Handllng<br />

System (HIHAN)—HfHAN is a<br />

sottware/hardware sysfem under development<br />

by Ihe Datacfrment Stennis Spaca Center (NRL)<br />

which will aufomate the preprocessing, merging,<br />

integration and preparation of hydrogrsphic data<br />

from a variety of sources.<br />

h ydrog rsphlc charf-(JCS) A nautical chart<br />

showing depths of water, nature of bottom,<br />

COnlOUrs,Of bottom and Wasliine, and tidasand<br />

currents m a given eea or sea and iand srea.<br />

Also called marine map; nautlcssl cfrarf.<br />

hydrographlc datum—The plane of<br />

reference of soundings, depth surves, and<br />

elevations of foreshore and offshora featuras.<br />

Also called charl datum. See also<br />

International low watar; low water<br />

datum; National Geodetic Vertical<br />

datum of 1929; eoundlng detum; tidal<br />

darum.<br />

hycfrographlc detail—Tfse featuras elong lhe<br />

shore and the submerged parts of bodies of<br />

water. Also called Irydrographlc teature.<br />

hydrographlc dlgltal data—Dafa In dlscrate<br />

numericaf form derfvad from tha measurements<br />

and descrfpflon of the physical features of the<br />

oceans, seas, lakes, rivers and ofhar wafers,<br />

and their adjoining coastal araas (with patt@ular<br />

reference to navigational ussge.)<br />

hydrographlc feature—See hydrographlc<br />

datall.<br />

hydrographlc reconnalssanca-A<br />

reconnaissance of an area of wafer to<br />

defermine depths, baach gradients, the nature<br />

122


of the bOffOM, and the location of coral reefs,<br />

mokfl shoals, and man-made obstacles.<br />

hydrographic sextanl—See surveying<br />

Saxtallt.<br />

hydrographlc 8oundlng-See sounding,<br />

defintfions 1 and 2.<br />

trydrogrephlc survey-A survey made in<br />

retetbn to any mnsiderable body of water, such<br />

as a bay, harbor, lake, or river for the purposes<br />

of determination of channel depths for<br />

navigetbn, Ioca!ion of rocks, sand bars, lights,<br />

and tx.keys; and In the case of rivers, made for<br />

flood comrol, power development, navigation,<br />

water auppfy, and weter storage.<br />

hydrogrrsphy-1. (JCS) The science which<br />

deals with tha measurements and description ot<br />

the physical features of the oceans, seas, lakes,<br />

rivers, and their adjoining coastal areas, with<br />

particular referenca 10 their use for navigational<br />

fxmses. 2. Thai part of topography pertaining<br />

to water and drainage features.<br />

hydrology+ydrology in IIS broadest extem<br />

deals with the properties, iaws, and phenomena<br />

of water of ifs physical, chemical, and<br />

physiolo@cal relations; of its distribution<br />

throughout Ihe habilable Earth; snd of the<br />

eff8d Of lhIS CirCUfalien on human lives and<br />

interests.<br />

hydrophore-An electroacoustic transducer<br />

that canvefis sound energy into electrical<br />

energy. Sea also transducer.<br />

hydrosphere-That pafl 01 the Earth that<br />

consists of the oceans, seas, lakes, and rivers; a<br />

M7?ilaf par7 of any other spatial body il such a<br />

body eXiStS. Dkwinguistred trOM lh8 atMOSfJhere<br />

and lithosphere.<br />

..,” ---.,- .,-m .. . ---- ,.. . . .. . . .. . .<br />

nB,”n”48, m,** -q”m, m”,,— u,, Sau,,,u,,bcl,<br />

eqixafione, the term assumed by the verlical<br />

mmponenf of the vector equation of motion<br />

when all Coriolls force, Earth curvalure, Iricfional,<br />

and ~efiiml ac@er81i0n tarms are considered<br />

negllgfbte compared with those involving the<br />

vertiial pressure force and the force of gravity.<br />

hydrostatic equlllbrlum-The stale ot a fluid<br />

whose surfaces of cansfanf pressure and<br />

conetam maas (or density) coincide and are<br />

horfzonfaf throughout. Complete bafance exists<br />

between the torte of gravity and the pressure<br />

force. The relation between fhe pressure and<br />

._. ——— _<br />

MIL-HDBK-850<br />

fhe geomefric heighl is given by fhe hydrosfelic<br />

equation.<br />

hygromatrlc—Relaf in~ to the retetlve humldlfy<br />

or wmparafive amounf of moisture frr the<br />

atrrme.phera. SInca the atrmsphare penetrates<br />

the pores or cells of maferfal bodiis in vsrying<br />

degrees depending upon fhe aubefances of<br />

which fhey are cmmposad, fhe amount of<br />

moistura which it comaine wili effeci the shepaa<br />

and dimensions of certain inaftumems and<br />

equipmenf used In surveying and maPpfng. For<br />

this reason 11is necessary to sefecf metartats<br />

which are not a.enaflive to hygromafrfc urnditione<br />

for the construction of fevefing rods, pfenetafrie<br />

sheels, efc., and for the construction and<br />

priming of maps.<br />

h yg roscopjc—The prope!ly of malerials such<br />

as paper and films to absorb or reiease moisture<br />

and, in so doing, to expand or contract.<br />

hyperbolic Ilne of poslflorI-A fine of<br />

position in the shape of a hyperbola,<br />

determined by measuring the difference In<br />

distsnce to two fixad points. Loran lines ot<br />

position are an example.<br />

hypariocal diatanca-The distance from the<br />

camera lens to me nearest object in tocus whan<br />

the camera lens is focused at infinity.<br />

hyperatereoscopy—( JCS) Stereoscopic<br />

viewing in which Ihe relief effect is nodceabty<br />

exaggerated, caused by the esfenslon ot fha<br />

camera basa. Afso called appearance ratfo;<br />

axaggeratad etereo; relief etrefchlng;<br />

stereoscopic sxaggeratlon. See also<br />

verlfcal exaggerelion, definition 1.<br />

hypsographlc detail-The feafures<br />

pertaining 10 relief or elevafion of terrain.<br />

hypsographlc map (or chari)-A map or<br />

chart showing land or wbmarine bottom ralief in<br />

terms of height above, or below, a datum by<br />

any me!hod, such as contours, hachuras,<br />

shading, or finfing. Also called hypsomatrlc<br />

map (or chars).<br />

hypsography—1. The science or art of<br />

describing alavations of land surfaces wilh<br />

reference to a dalum, usually sea level. 2. That<br />

part of fopogrephy dealing with rafief or<br />

elevation of terrain.<br />

hypaograph-An instrument of fhe slide rule<br />

type used fo comp,ute elevations from veflical<br />

123


—<br />

angles and horizontal dslances.<br />

hypsometer—An instrument used in<br />

determining elevations of poims on the Earlh’s<br />

w rfacs in relatiin to sea level by determining<br />

atmospheric pressure through observation of<br />

the bolting point (temperature) of water at each<br />

point.<br />

hypeometrlc map (or chart)-See<br />

hypstogrephic mep.<br />

hypeometrlc tint ecale-A graphic scale In<br />

the mergln of maps and charts which Indicates<br />

heights or depths by graduated shades of<br />

cofors. See afso hyps.ornetrlc tint Ing,<br />

hypsomelrlc tinting—(JCS) A method of<br />

showing relief on maps and charts by coloring,<br />

in different shadea. those parts whIcfI fie<br />

between selected levels. Alse called eltllude<br />

tlms; color gradients; elevatlon tlnte;<br />

gradlant tints; layer tints.<br />

hypaometry—The arf of determining, by any<br />

method, surface elevations on the Earth with<br />

relerence 10 sea level,<br />

MIL-HDBK-L350<br />

124


ke chert-A chart showing prevalence of ice,<br />

usually with reference 10 nav’@ble walerways.<br />

Ice aurvelllanca producte-Plolllrrg charts,<br />

repcrt forms, and other cworfucts used for the<br />

collection and dksemina!ion of ice posftion<br />

information.<br />

MIL-HDBK-850<br />

Icad.bar sspparatua-An apparalus ~or<br />

meeeurtw Ilnaar distance wilh great precision<br />

and acwrecy, and consisting assantialty of a<br />

Sfaal bar which is maintained et a constant<br />

tert?peratura by being surrourtdm with melting<br />

Isa. The bar is rectangular in cross section, and<br />

IS carried In a Y-shapad trough which is Iillad<br />

with matting ke and mounted on a car which<br />

rneves on a track. Bar lengths are observed wiih<br />

micrometer microscopes mou M ed on S!able<br />

supfmrfs. Also called Woodward base-llne<br />

measuring apparatus.<br />

Ideal Eartts-See aqulllbrlum theory.<br />

kdeal sea level-The theoretical sea surlace<br />

whuh is everywhere normal to the plumb line.<br />

Referance of all depth soundings to this level<br />

would rqaka them all comparable.<br />

Ideniltlcatlon poetrs-Peats of wood or other<br />

suitable rrkmerfal, appropriately marked and<br />

inacrfbed, and placad near survey stations 10 aid<br />

In their recovery and identification, AISO called<br />

supplemental poata for aurvay<br />

monumants.<br />

Idla pendulum—A working pendulum placed<br />

In the recalver in advance 01 its being used, so<br />

Ihal It may assume the same temperature as<br />

the dummy pendulum.<br />

Image corrolatlon—The matching of position<br />

and physkal characteristics betwaen imagery of<br />

the same geographic area horn dillarersl types<br />

of aenaore, between sensor imagery and a data<br />

base, or between two images frem the same<br />

aansor.<br />

Imaae dagradatlon—[photometry) The<br />

reduction of the Inherent optimum Imaging<br />

polential of individual sensor systems caused by<br />

emr In sensor operations or pmcesslng<br />

pMCt?dUrJS. Raducliorsa In quality caused by<br />

unavoidable facfom; i a., atmospherics, srmw<br />

125<br />

cover, ate., are net asaocialad with the term.<br />

Image dlrastlon—A term used 10 describe the<br />

image orientation 0! a photographic negative or<br />

positive relative to the positbrr of the emulsion.<br />

See also emulalon-to-basa; emulalon-toemulalon;<br />

right-reading; wrong-reading.<br />

Imaga dlatortlon-Any shift In’ the posllion of<br />

an Imega on a photograph which alla’s the<br />

perspective charactetistica of the photograph.<br />

Causes of image distortion hStJds lens<br />

aberration, dMerantial ahritiage of flfm or papar,<br />

and motion 01 the film or camera.<br />

Imaga enhancement—Any of aavaral<br />

processes that might improve the interpretation<br />

quality of an Image. Such processes include<br />

contrast improvement, greatar resolution,<br />

special Iillering, etc.<br />

Image motion compensation (lMC)-<br />

(JCS) Movement Intentionally Imparted to film at<br />

such a rate as to mmpansate for the fonvard<br />

motion of an eir or space vehicle when<br />

photographing ground objects.<br />

Image motion companaatlon dlatotilon—<br />

In a panoramic camera system, the<br />

displacement of images of ground points Irom<br />

their expectad cylindrical poslticn causect by the<br />

translation 01 the lens or negative wrfaca (a<br />

motion usad to wmpensale for Image motion<br />

during exposure time).<br />

Imaga motion ?actore-Those factors<br />

wherein the Image MotIon varies directly wfth the<br />

aircraft ground speed and lens focal length and<br />

inversely with the anitucle,<br />

Imege motion—lhe smearfng or blurring of<br />

imagery on an aerial ptretcgraph bacauaa ot the<br />

relative movement of the camera with raspecf to<br />

the ground.<br />

Image plane—See photograph plane.<br />

Image point-(photogrammetry) Image on a<br />

photograph mrrespcmding to a definite object<br />

on the ground.<br />

Image procasal ng—Encompasses all the<br />

various operations that can be applied to<br />

photographic or image data. These Include, but


MIL-HDBK-850<br />

are not limited to, image impression, image<br />

restoration, image enhancement,<br />

preprocessing. quantlsation, spatial filtering and<br />

olher image pattern remgntiion techniques.<br />

Image ray-straight fine from a ground object.<br />

thraugh the camera Iem, to the Imaga on me<br />

photograph. See also paMpeCilVe ray.<br />

lmageW Interpretation key—(JCS) Any<br />

diagrams. charts, tablas, lists, or sets of<br />

examplas, etc.. which are used !0 aid imagefy<br />

Intarpretere in the rapid kfanfifiition of objecls<br />

visibfe on imagery.<br />

Imagery hrterpretatlon—( JCS) The procees<br />

of location, recognition, identification, and<br />

description of objacts, activities, and terrain<br />

represented on imagery.<br />

Imagev aortia-(JCS) One flight by one<br />

aircraft tor the purpose of racording air imagery.<br />

imagery-(JCS) Collecfivaly, the<br />

representations of objects reproduced<br />

electronically or by optical meana on film,<br />

electronic display devices, or other media.<br />

lmaga-1. The parmanenl record of the<br />

likeness of any natural or man-made features,<br />

objects, and activities reproduced on<br />

photographic malerials. This image can be<br />

acquired ihmu~h the sensing ot visual or any<br />

other aegmanf 01 the elactmmagnetic spectrum<br />

by sansom, such as thermal Infrared, and high<br />

resolution radar. Sea also erect Imege;<br />

homologous Imagea; Inverted Image;<br />

latent Image; real Image; reverted<br />

Image; tharmal Imagery; Vhltial Imege.<br />

2. A visual rapresenlation, as on a radarscope.<br />

Imeglng ayeteme-(satelfite) Imaging<br />

systems carrfad on satallitas can be placad in<br />

hvo bask categories, according to the<br />

requlrernmts to be rrwt by thair applications: (1)<br />

remote sensing for interpretation is<br />

characfarized by the fact the nature of tha<br />

object imaged is of prtmary importance, and the<br />

gaomatry ie of minor Impofianca: and (2)<br />

satellite photogrammetry is charactarizad by the<br />

geometry which Is ot prfmary Interest, and the<br />

natura of the oblacr is ot minor importance.<br />

Imparaonal mlcromater—See tranalt<br />

mlcromatar.<br />

lmpoft-Tha procass of bringing data or<br />

software from one system inlo another system.<br />

126<br />

lmpoaltlon—Positioning and aeeembling<br />

negalives or positiies into printing iocaiion on a<br />

flat.<br />

lmprasaion—The inked image racefved by a<br />

aheat in a press. Commonly usad as a measure<br />

of printing production or Cawcity.<br />

In.anrf-out atallon—A recoverable but<br />

unoccupied stat’bn Irworporatad into a trrxverae<br />

by remnlng e fictiiious defkactton angle of 180°<br />

to reverse the azimuth of the course leading info<br />

it, so that[ha nest statbn minckfes with the<br />

preceding station and the in-and-out station iS<br />

ueed as the backaight lor continuing Iha<br />

traverse. In the canputatbns it is lraatad as an<br />

ordina~ station in the travarse.<br />

Incident nodal point-See nodal point,<br />

definition 1.<br />

Inctlnatlon correction—See gmda<br />

correction.<br />

Incllnatlon of the horizontal axis—The<br />

vertical angle between the horizontal aXiS of a<br />

suweying or astronomic instrument and lhe<br />

plane of the horizon.<br />

Incllnatlon-1. The angle which a fine or<br />

surface makes with the verlical, horizomai, or<br />

with another line or Suriace. 2. The angie<br />

between orbit plane and ratararwe plane; tor<br />

exampla, tha Equator is the reference plane for<br />

geocentric, and the eclbtic tor hefiicantric orbM..<br />

3. See dip, definition 2.<br />

Incllna alfJht-A sigh! made with a surveying<br />

instrument at an angle afmve or below the<br />

horizon.<br />

inclinometer—An instrument for measuring<br />

inclination to the horizontal of a ship or aircraft,<br />

or of the lines of force of the Earth’s magnatic<br />

tield.<br />

lnclualors-A topological pm~rty which<br />

providas relationships batwaen objects which<br />

are enclosed by or overlap another object.<br />

Examples of inclusion are an island surrounded<br />

by water, or a town within and a part of a taroer<br />

administrative area. See aleo topology.<br />

Indepandant raaurvey-A rasurvey which iS<br />

not depandant on the recxrfds of the original<br />

survey but is inlandecf to supersede them in


eefablishfng new land boundaries and<br />

aubdivislons. See also dependent reeurvey.<br />

Index chart-An outline charl showing the<br />

limits end identifying designations of<br />

navigational charts, volumes of sailing<br />

directions, etc.<br />

Indax contour lln-(JCS) A contour fine<br />

amenfualed by a heavier line weight 10<br />

dstingutsh H from intermediate camrfours. Index<br />

contours are usually shown as every fifth<br />

contour with their ass”~nest values, 10 facifilafa<br />

reading elevations.<br />

Index correction-l. A correction applied 10<br />

the raading from any graduated measuring<br />

device to compensate for a canstant error such<br />

as would be caused by misplacement of the<br />

Scale; lhe reverse 01 Ihe index error. 2.<br />

(leveling) That correction which must be applied<br />

10 an ObSeWed difference Of elevsflon to<br />

effminale lhe error introduced into fhe<br />

observations when lhe zero of the graduations<br />

on one or bofh leveling rods does not coincide<br />

axactly with Ihe actual bottom surface of the<br />

rod.<br />

‘Indax arror-The instrumental error which is<br />

constant and attributable 10 displacement of a<br />

vemler or some analogous ellecf.<br />

Indax ream-A real mark, such as a cross or<br />

dot, lying in the plane or the object apace of a<br />

photograph and used singly as a reference<br />

mark In cerfain fypes of monocular Inswuments,<br />

or as one of a pair to form a floating mark as in<br />

certain types of stereoscopes. In stereoscopic<br />

map plOffing instruments which utilize a stereo<br />

pair of Index marks, each mark is called a haff<br />

mark. see also floatlng merk.<br />

fndex of refracffon-See SnelM faw of<br />

refrecflon.<br />

Index prlsnx-A sextant prism which can be<br />

Krtetad to any angle mrresponding to altitudes<br />

between established WrrUs. It k the b@irle or<br />

pendulum sextant wunterpatl ot the indax<br />

mirror of a marine aexrant.<br />

Index fo photography-see photo Index,<br />

definffion 1.<br />

Indian dalum-The Indian detum is eccepted<br />

as fhe preferred datum for India and several<br />

adjacant countries In Southeast Asia. It is<br />

computed on the Everest ellipeoid with its origin<br />

MIL-HDBK-850<br />

127<br />

at Kafiinpur in Central Indii. Derived in 1S30,<br />

fhe Everest ellipsoid is the ofdeat of the<br />

eilipao”kfs in common use and &smuch too 6rrSS11.<br />

As a resuft of the fatter, the. datum Cennoi be<br />

extended too far from the origkt or very fofuo<br />

geoid aeparafions will mr. For this reason and<br />

Ihe fact that the ties bofween local friarrgulatbn<br />

in southeast Asia are rypbeffy weak, the Indian<br />

datum is probably the least salislacfory of the<br />

preferred datums.<br />

Intffan eprlng fow water—The approximate<br />

mean water faval defermfned from afl bwer bw<br />

watars at spring tkles.<br />

Indian tide plane-The datum of Indian<br />

spring bw watar.<br />

Indicated comer-A Ierm adopfad by the<br />

U.S. Geological Survey to dasignate a mmer of<br />

Ihe pubfii fend wrveye whosa focafion canno!<br />

be varified by the criferfa necessary to clase if as<br />

a found or existenl corner, but which b accepted<br />

locally as the mrrecf mmer and whose bcation<br />

is perpaiusted by such reeks as fence One<br />

intersacfions, piles of rocks, and stakes or pipes<br />

driven info the ground, which have been<br />

recovered by field investigation.<br />

Indlcafed prfnclpal point—See prlnclpal<br />

point.<br />

Indlract effect on the deflectlona—See<br />

topographic deflecllon,<br />

fndirect Ieveflng-see barometric<br />

Ievellng; thermomotrlc leVellng;<br />

wlgonometrlc Ioveflng.<br />

Indirect measurement—Any measurement<br />

secured by determining Ifs quanftfy from tfs<br />

relatlon to some measured quantify. A<br />

!echnique used in aurveylrrg whan ff is<br />

impossible to actually tape e dkitance across a<br />

river or of her such obstruction. See afao dfract<br />

meseuremenf.<br />

Indirect obsewatlon—A measure of a<br />

quantity which is a function of the quantify or<br />

quantities whose value is desired, such as an<br />

obsemed difference in elevation wifh a spirit<br />

level, used to obtain the elevation of a bench<br />

msrk.<br />

Indirect phonography—Photography In<br />

which fhe camera records an Image COaf upon a<br />

screen or similar display surface by elacfronic<br />

[television, radar, etc.) or other means.


inequality—A systematic deparfure VDM the<br />

mean value 01 a quamny. See also annual<br />

Inequality; diurnal Inaqunllty; lunar<br />

Inaquallty; parallactlc Inequality;<br />

parallax Inaquallty; phase Inequality;<br />

varlatlonsrl Inaquallty.<br />

MIL-HDBK-850<br />

Inarrlal ●zlmulh-An azlmufh which<br />

approximates the value which mulct be obtained<br />

from asfmnomic obsewafions, but which is<br />

derived from direct obeewations along the fine<br />

of sfghl with an inertial azimuth measurfrrg<br />

davfca conelafing of a north-seakkrg gymsmpe<br />

ootilned with a iheodollle. See also<br />

gyrotfreodoli.te.<br />

Inertial coordinate system—A coordinate<br />

system (n whch the axes do not rotate with<br />

respect fo the Wed sfars. and in which dynamic<br />

behavbr can be deacrbed using Newlon’s laws<br />

ot motbn.<br />

Iner?lal guidance eystem—A system in<br />

which gukjance IS parmlffed by means of the<br />

maaaurement and in!egrsfion of acceleration<br />

from wilhin the craft.<br />

Inortlal measurement unl! (lMU)—(missile<br />

guidance) A wmpacf componen! of an inertial<br />

guidance ayslem which fsas three<br />

accaleromefers mounted cm a gyrostabifized<br />

plafform. See also accelerometer.<br />

ine~lal nsvlgatlon ●ystam—A ayslem which<br />

is not dependent on man-made elecfmmagnatic<br />

signals. Newion$e sacond law of molbn is<br />

ufilized wffh a syatom conakllng of<br />

amelemmetera mounfad on gyroelabllized<br />

plaffonme, each for measuring bngifudinal,<br />

lateral, and verlkal amelerations. The double<br />

Infegratbn of ali accelerations in lhree mutually<br />

perpendicular directions pmvkfes distance<br />

traveled (Imm a known starting point) in three<br />

mutually perpendicular dlracfions. Navigation is<br />

by a highty refined form of dead rackoning with<br />

system posfficm t9ing updated fmm other<br />

navigational references In the more<br />

sophisticated ayateme.<br />

lnarflal navlQatlon-The process of<br />

meaeuring a craft% velocity, attitude (in the<br />

aubmaflne missile Iaunchlng appficalions), and<br />

displacement (incfuding changes in altitude in<br />

Ihe aircraft a@catbn) from a known etarfing<br />

poinf through sensing the acceleration acting<br />

on ff In known directions by means of devices<br />

that mechanfze Newton’s laws of motion,<br />

128<br />

Inefllal referance photography—<br />

Cartographic aerial photography obtained<br />

simultaneously with rnagnatlc tapa recordad<br />

inertial retererwe positioning data.<br />

Inferior conjuncrlon-l%o mnjuncfbn of an<br />

Inferior planet and the Sun when the planol is<br />

between the Eanh and the Sun.<br />

Inferior planeta-The planets with orblfe<br />

smatier than thaf of the Earth, i.e., Mercury and<br />

Venus.<br />

Inferior traneH-See Iowar tranelt.<br />

lnflnity—~e poinI, line, or region beyond<br />

measurable fimfis. An unaltered source of figM Is<br />

regarded as at infinity if if is a! such a great<br />

distance that rays from If can be considered<br />

parallel.<br />

Infrared dlstsnce measurement-A<br />

distance determined by measuring the phase<br />

delay 01 rnedulation algnats on a li@f beam<br />

(infrared) traveling ot a known vebcify between<br />

a dwlsnce reeler and reflector.<br />

Intrared film-(JCS) Film carrying an omukbn<br />

especially sensitive to ‘near-infrared.. Used to<br />

photograph through haze, because of the<br />

penetrating power ot inlrared fighl, and in<br />

camouflage delection to distinguish between<br />

tfving vegatathn and dead vegetalbn or artificial<br />

green pigment.<br />

Infrared—Pertaining to or designating the<br />

portion of the electromagnetic spectrum with<br />

wavelangfhs ]usf beyond the red end of the<br />

visible spectrum, such as radiatkm emitted by a<br />

hof body. Invisible to the eye, infrared rays are<br />

detected by their thermal end phefographic<br />

eHects. Their wavelength are longer fhan those<br />

of visible light and shorter Ihan thOSa Ot radio<br />

waves,<br />

h’thorlted error—The error In iniflal values<br />

used In a amputation: especially the error<br />

irrfmduced from the previous steps In a step-by.<br />

step imagration.<br />

inltlal Graptrlc Exchange Speclflcetlon<br />

(lGES)—An interim efandard tormet devebpad<br />

by the Naltonal Bureau of Standards (NIST) for<br />

exchanging graphics data between computer<br />

systems IGES Is the most wldafy used<br />

exchange formal in the world.


MIL-HDBK-B50<br />

Inlilsl monument—A physical structure which<br />

marks the Iocalbn of an Initial poinl in me<br />

rectangular system 01 surveys. See also Inltlal<br />

potnt.<br />

Inltlal operatlfrg capability (IOC)—The first<br />

affainrnerrf ol the cepabiliiy to employ effecflvefy<br />

a weapon, item of equomsrrf, or system of<br />

approved epsrclfk characferletics, and which is<br />

manned or operated by edwfuately trained,<br />

equipped, and supported operational unil or<br />

group.<br />

Inltlal point-l. That point from which any<br />

survey is inillatsd. Alao called point of origin. 2.<br />

A point wMch k esisbfished under the<br />

rectangular system of surveys and from which k<br />

lni!isled the cadastral suwey of the principal<br />

meridian end base line that controls the<br />

cadasfral survey of the Wblic lands within a<br />

given araa. See alao base line; initial<br />

monumem; principal meridian.<br />

Inner orlenta\lon—See Interior<br />

orientation.<br />

Innar plsmets—The four planets nsarest the<br />

Sun: Mercury, Venus, Earth, and Mars. See<br />

also melor planets; outer planats;<br />

aaieroid.<br />

Inserted grouping—(JCS) (radar) The<br />

incfusion of one erea of homogeneous surface<br />

material in an area of different melerial.<br />

hteet—(JCS) (cartography) A separate map<br />

positioned within the neallhre of a larger map.<br />

Three forms are recognized: (1) all area<br />

gaographwally outside a sheet but included<br />

therein for convenience of pubiicalion, ueually at<br />

the same scale: (2) a poriion of lhe map or chart<br />

et an enlarged scale: (3) a smaller scale map or<br />

chart of surrounding areas Included for location<br />

purposes.<br />

Instantaneous field of view (tFOV)—The<br />

smatieat aofid arrgie resolvable by a scanner<br />

when axpreseed in radians. When expreassd in<br />

feet, ii la the prejecfed area of the detector<br />

image on the ground and is a measure of the<br />

remlufion of a scanner or similar remole sensor<br />

with di6crete samples.<br />

instantaneous reading tape-A survey<br />

tape on which the foot mark is repeated at each<br />

sutdiiision. Thus, a tape divided into tenfhs of a<br />

foot would have fhe foot mark imprinted al each<br />

129<br />

tenth of a foot divkion.<br />

Instrument adjustment-lle process of<br />

mechanical manipulation 01 the relaiion ot<br />

componan! parts 01 an instrumerd in order to<br />

oblain the h~hesl practicsbte precision and<br />

facility in lhe designed use of ths bt5fNMsnt.<br />

instrument approach chsttl-An<br />

aeronauticef cherl designed for use undar<br />

Instrument flighf conditlorts, for rnafdrtQ<br />

irratrumsnf approach and fatdown to contact<br />

flight cotidions in the vichttfy of an aWteld.<br />

Instrument arror-A systematic error resulting<br />

from irnparfeckne in, or feuffy adjuatmanl ot,<br />

instrumanfs or dsvicea used. Also caked<br />

calibration error.<br />

Instrument parellex—1. A change in Ihe<br />

apparent position of an object wfih respect to<br />

the reference marlw of an instrument which Is<br />

caused by impenacl adjustmanf of the<br />

instrument. Aiso calied optical pareliax. 2.<br />

Parallax caused by a change in the postiion of<br />

tha observer. Also called pereonai parallax.<br />

instrument phcrtotrlangulation-See<br />

stereotrianguiat ion.<br />

instrument statlon~ee sefup, definition<br />

1.<br />

Integralad etatlon lnetrument—A n<br />

instrument combining horfzonfaf and vertical<br />

angles with electronic distance meaaurament<br />

and programmed computer capability in a single<br />

piece of hardware.<br />

lnlegratlon—(JCS) 1. A Staga in the<br />

irstelligenca cycie h which a patfern is termed<br />

through the selection and Combination of<br />

evaluated information. 2. (photography) A<br />

process by which the average mdsr pkfura seen<br />

on eeveral scans of the lime baae may be<br />

obtained on a prfnf, or the process by which<br />

several photographic images are combined info<br />

a single image.<br />

Intenelty of grevlty-The magnitude with<br />

which gravity acts, expressed in euifabfe units,<br />

usually as an acceleration, in gals: as a force, in<br />

dynes.<br />

inlaractlve-A system of alfowhkJ two-way<br />

electronic communicszfion behveen the user and<br />

the computer.


i<br />

Intercardlnal polnl—Any of the four<br />

diractkms midway between the cardinal poims;<br />

norfhaast. soufheasl, southwest, or northwest.<br />

MIL-HDBK-850<br />

Interferometer-An apparatus used to<br />

pmducs and measura interference from hvo or<br />

more coherent wave trains from the same<br />

source. Used to measure wavelengths, to<br />

measure an@sr width of sources, to determine<br />

the angular positkm of sources (as in satellite<br />

tracMng), snd for other purposes. See also<br />

radio Interferometer.<br />

Interim Terrain Data (ITD)-A DMA digital<br />

producf consisting of oomiguous data eels<br />

comprised of attributed and urraymbolizad<br />

feature Information in six thematic files (Surlace<br />

Configuration, Vegetation, Surface Materials,<br />

Surface Drainage, Transportation, and<br />

Obstaclea) and a sevemh file of Digital Terrain<br />

Elevation Data (DTED) Level 1. The data content<br />

is equivalent to the content of either Tactical<br />

Terrain Analysis Data Bases (7TADBe) or<br />

Planning Terrain Analyais Dala Bases (PTADBs).<br />

An enhanced Iranspafat!on file consisting of<br />

attributed roads (afl-waaf her fhrough Carl track),<br />

bridges, and tunnels was added to the data set,<br />

See Plannfng Tarraln Analysls Data<br />

Base; Tactical Terreln Analysls Date<br />

Baae.<br />

Interior angle trrsverse-in surveying, a<br />

closed lravarae wherein distances are maasured<br />

and only Inlerlor angle measurements are used.<br />

Intarlor orlantatlon-The determining<br />

(anafyiicalfy or in a photogrammetric instrument)<br />

of the intarior perspective of the photograph as<br />

it was at the instant of exposure. Elements of<br />

imerbr Orfemation are the calibrated focal<br />

Iangth, bcatbn of the calibrated principal point,<br />

and the calibrated lens distortion. Also called<br />

Inner orlantation.<br />

Intertor perapactlve canter—See<br />

parapectlve center.<br />

Interior to a curtre-That area lying toward<br />

the Conceva sfde of a curva and incfuded within<br />

the area of the circle of which the curve Is a part<br />

of fhe circumterenca.<br />

lnterlocklrtg angle-in till analysis of oblique<br />

photographs, the angle betwesn the optical<br />

axea of Ihe varflcal and oblkfue cameraa. Ttte<br />

dihedral angle betwaan lhe planes of the<br />

vert!cal and oblique photographs.<br />

. .<br />

intermediate contour Urse-A conlour line<br />

drawn bahveen index contours. (@ending on<br />

the wnfour interval, there are thrae or four<br />

imerrndale contours between the irrfex<br />

contours.<br />

Intermediate orbft-A cemnsf force orbft that<br />

Is tangent to the real orbii al some poim. A<br />

fictitious aatellile traveling in the kdermadiefe<br />

orbit would hava the sama position, but not the<br />

same velocity, as tha real salellita af the poim of<br />

tangency.<br />

Internal data structure-The organization<br />

within a ayslem of data and particularly, the<br />

reference linkages among data rslarrwnts. Sae<br />

also Data structure.<br />

International Gravity Standardlzatlon<br />

Net 1971 (IGSN 71)—An adiusted worldwide<br />

network of gravity measurements consisting of<br />

absolula, pendulum, and gravimeter<br />

observations. The IGSN 71 was approved and<br />

adopted by fhe International Union of Geodesy<br />

and Geophysics in 197t, and replaces the<br />

Potsdam datum as fhe international graviiy<br />

standard.<br />

International date llnS-(JCS) The line<br />

coinciding approximately with the amemerfdian<br />

Of Greenwich, modified to avoid certain<br />

habitable land. In crossing fhis line there is a<br />

date change 01 one day. Also called date Ifna.<br />

International eliipaold—A refarence elffpsoid<br />

defined by Hayiord in 1924 with samimajor<br />

axis(a) as 6,378,388.0 reefers, and flattening of<br />

li297.<br />

Internatlonaf gravity formula—A<br />

devalopmem of the formula for theoretical<br />

gravity, based on the aasumptfone thal the<br />

spheroid of raference is an exact ellipsoid of<br />

revolution having the dimensions of the<br />

international ellipsoid of reference (Madrid,<br />

1924), rotating about its minor axia once in a<br />

sidereal day; fhaf the surface of the ellipsoid is a<br />

level surface: and that gravity al the Equator<br />

equals 978.049 gals.<br />

Intarnatlonal low watar (ILW)—A plane of<br />

reference bafow maan sea Iavef; half the range<br />

between mean Iowar low water and mean<br />

higher high water multiplied by 1.5.<br />

Internetfonal ayatam of Unlt9 (Sf)-The<br />

practical international metric system of unlls


I<br />

MIL-HDBK-850<br />

adopted by Ihe Etavemh General Conference of<br />

Weights and Measures In 1960.<br />

Interoculsrr dlatance-(JCS) The distance<br />

between the centers of rotation of the eyeballs<br />

of an Irdfvldual or between the oculars O( opfiial<br />

Instruments. Afso called eye berse;<br />

Interpuplllary dletance.<br />

lnteroperablllty-Consistency between<br />

dflerent MC&G software and data sets in ferms<br />

of eccaracy, data structure, lealure coding, georetererrcing<br />

systems, daturna, epatial<br />

raaolutiina, and pracision, whch allow them to<br />

be used on cWterent kinds of equipment<br />

ayetarna.<br />

Interpolate-To determine intermediate<br />

values between given fixed values. As applied<br />

to logical contouring, 10 interpolate is to ratio<br />

vertical distances between given apol<br />

elevations.<br />

Interpuplllary dlslance—See Inter-ocular<br />

dlrstence.<br />

tntorrogatlon—Transmission of a radio signal<br />

or cembirsakm of signals intended to trigger a<br />

wansponder or group of transponders.<br />

lntOrrOgatOr.reepOnaOr-A radio Iransmiller<br />

and receiver combined to interrogate a<br />

transponder and display the resulting replies.<br />

Also called challenger. See also<br />

Interrogator.<br />

Interrogator-1. A radar set or other<br />

electronic devbe that transmits an interrogation.<br />

2. An interrogator responscrr or the transmitting<br />

component of an interrogator raaponeor.<br />

Interrupted map projection—A projection<br />

having several standard meridians, each<br />

careered over a continent, and with lobateshapad<br />

eectlons of the projection plo!led from<br />

each elandard meridian. Ttre projectbn is<br />

broken In the ocean areas between the<br />

oontlnenta, ttwa reducing the linear scale<br />

dlacrepancles ard the overall shape distortion,<br />

espaciatly toward the margins, while retaining<br />

the equal area property.<br />

Intersected point—See Intaraectlon<br />

etatton.<br />

IntersectIon etatlon-An object whose<br />

horizontal position Is determined by<br />

observations from other survey stalions, no<br />

observations balng made at the object itsetf.<br />

Where the object is observed from onty two<br />

stations, Ihe position is termed a no-check<br />

posltlon, as there & no prmf that such<br />

obsewationa are free from btunders. Interaeciion<br />

stations are either objects which would be<br />

difficult to cccupy wtih an inatntmam, or Survey<br />

SignafS whose positions can be detennlnad wtfh<br />

stdficlenf accuracy without being occupied. Also<br />

called Intersected pOlnt.<br />

tniareectlon—1. (digital rnapplng) The<br />

coexistence of end points et a apecWc<br />

geographic focation; the set of all otrjeds<br />

common to hvo or more !ntersecltng sets. 2.<br />

(surveying) The procedure 01 detarrnining the<br />

horizontal position 01 an unoccupied poinl<br />

(Intersection station) by direction observations<br />

from two or more known positions. 3.<br />

(phologrammetry) The procedure of de!enrtlnhrg<br />

the horizontal position of a poim by Intersecting<br />

lines of direction oblainad photogrammetricelly.<br />

The fines of directkkn may be obtalnad direcfly<br />

from vertical photographs or by graphic or<br />

mathematical rectification of tilted photographs.<br />

See also reeectfon.<br />

lntervalometer—A liming device for<br />

automatically operating at specified intervals -<br />

cenain equipment such as a camera ehufter for<br />

the purpose of obtaining a desired end iap<br />

between successive photograp!rs.<br />

imervielblllty test—Any of iha saveral tests<br />

used to determine the possible visiMfiiy abng a<br />

sight fine in a proposed survey net. tts purpose<br />

is to determine the existence of obstructions<br />

along a proposed fine of sighf frum wtrich tower<br />

and signal rtrqtsiremants may be developed.<br />

tntemialblltty—Function which calculates area<br />

or Ilne-of-sight which can be .aeen- from a<br />

specific location or locations. Also termed<br />

vlewehed modeling or vlewahed<br />

mapping.<br />

tnvar leveling rorS-See preclae Ievetlng<br />

rod.<br />

mvar pendulum—A quarter-meter pendulum<br />

made of fnvar.<br />

Invar acala-A measuring bar made from<br />

Invar, Normally, one Side la graduated In the<br />

metric system and Iha othar side in the Engllsh<br />

system.<br />

Invar tape-Any survey tape made of fnvar.


’<br />

lnvswhsble ponduium—A pendulum so<br />

desQned and equipped wiih means 01 support<br />

Ihsl ii can be ueed In only one position.<br />

MIL-HDBK-850<br />

lnvar—An alloy of nickel and steel having a<br />

very bw meffiifsnf of thermal expansion. Invar<br />

is used in the construction of Jaderin wires<br />

(base-line fnaasurfng apparatus), subtense bars,<br />

precise Iavelirrg rods, tepes, and pendulums.<br />

See also Lovar.<br />

lnventoW sufvey-A survey for the purpose<br />

01 mllecfkrg and mrrelaling engineering data of<br />

a particular type, or types, over a gfven area. An<br />

invenfo~ survey may be recorded on a base<br />

map.<br />

Inventory-Existing wurce matarials,<br />

intermediate and final products ‘kfentiiied by<br />

type of geographic mverage, and currency.<br />

Inverse chswf-See transverse cherf.<br />

Inverse computation—See Inveree<br />

position computation.<br />

Inverse cylindrical orfhomorphlc charl—<br />

See transverse Mercator chart.<br />

Inverse cylindrical orfhomorphlc map<br />

projection-See Iraneverae Mercator<br />

map projection.<br />

Inversa equator—See transverse<br />

equetor.<br />

Inverse latitude—See transverse<br />

Iatltude.<br />

Inveree IongltudeAee trenaverae<br />

longitude.<br />

Inverse Marcator chart-See transverse<br />

Mercator chart.<br />

Inverse Mercator map projection—Se e<br />

traneverssr Mercator map projection.<br />

Inveraa merldlan—Sea transferee<br />

merldlan.<br />

Inveree parallal-See tranaverea<br />

parellel.<br />

Inversa poeltlon computation—The<br />

derivation of Iha length, and the forward and<br />

back azimuths of a line by mmputstfon baaed<br />

on Ifre known positions of Ma ends of the fine.<br />

Also tailed Invarea; Inveree computation;<br />

Inverse posltlon problem.<br />

Inverse poeltlon problem—See Invaree<br />

position computation.<br />

Inverse rhumb llne-See Iranaverae<br />

rhumb Ilna.<br />

lnverae—See Inverse poaltlon<br />

computation; trsnaverae.<br />

Invereora-(photography) Me&hankal devices<br />

used to maintain Wrrecf conjugate distances<br />

and collinearity 01 negative, lens, and easel<br />

planea in autofocusing optical instruments, such<br />

as copy cameras and rati(fiera. See also<br />

Carpantler inversor; Peeucelller<br />

Cerpentlar invarsor; Pesucelller<br />

Inveraor; Pythagorean right angle<br />

Inversor.<br />

Inverted lmsge-An image thal appears<br />

upside down in relation to Ihe object.<br />

Inverted atere%See psaudoscoplc<br />

stereo.<br />

Inverting telescopsr-An instrument wifn the<br />

optics so arranged that the Itghl rsys entering<br />

me objective of the lens meet al tha cress hairs<br />

and appear inverted when viewed through the<br />

eyepiece without allering the orfentafion ot the<br />

image. See also arectlrrg telescope.<br />

lnvertlng—See trensli, definition 3.<br />

lonoephere—(JCS) That part of the<br />

atmosphere, extending from aboul 70 to 500<br />

kilometers, in which ions and free electrons exfat<br />

in sulficiem quamitles to reflect elecfromagnatic<br />

waves. See also atmosphere.<br />

Ionospheric correction—The mrretiton<br />

made to electromagnetic measurements<br />

between sateltiies and ground stations to<br />

compensate for the effect of the ionosphere.<br />

lrradlanceRadiant flux incident per unit area.<br />

Irregular error—See random error.<br />

Irregufar llne-A complex line which cannof<br />

be easily described by a mathematical<br />

polynomial.<br />

12


lsanomal—A line connecting polnls of equal<br />

variations fmm a normal valua.<br />

Ieentreplc- equal or constam entropy wl!h<br />

respect to either space or time.<br />

Ialande—(digital mapping) Polygons which are<br />

completely enclosed wlthln anofher polygon.<br />

MIL-HDBK-850<br />

Isobaric charl-A chart showing isobars, Also<br />

called constant pnsssura chart.<br />

laobar—A fine alOng which the amrospheric<br />

pressure Is, or Is assumed 10 be, the same or<br />

constanL<br />

lsobath—See depth contour.<br />

Iaocenter plot—See I.eocenter<br />

triangulation.<br />

Isocenter triangulation—l?adial triangulation<br />

utilizing isocenters as radial centers. Also called<br />

}socenter plot.<br />

Isocenier-1. (JCS) The point on a<br />

photograph interested by the biseclor of the<br />

angle between the plumb line and ihe<br />

phonograph perpendicular. 2. The unique poinl<br />

wmmon to the plane of a photograph, ita<br />

prircipal plane, and the plane of an assumed<br />

truly vertical phonograph taken Irom the same<br />

camera .stafion and having an equal principal<br />

distance. 3. The point of intersection on a<br />

photograph of the principal line and the<br />

isometric parallel. The isocenler Is significant<br />

because if is the cenler of the radiation Ior<br />

dkplacemenls 01 images due 10 lilt.<br />

laochron~A line on a chart connecting all<br />

points having the same lime o! occurrence of a<br />

particular phenomencm or of a particular value<br />

of a quantity.<br />

laocllnal—A line drawn on a map or chart<br />

joining points of equal magnetic dip. Also called<br />

Isocllnlc line.<br />

iaOCllnfC charl-A chart of which fhe chief<br />

feature is a system 01 isocfinic lines, each for a<br />

diiierent value of the magnetic inclinal’on.<br />

Isocllnlc line-See Isocllnef.<br />

isodlff-One of a series of lines on a map or<br />

chart cvnnectfng pointa of equal correction or<br />

dtilerence in datum, especially useful in<br />

readjustment of suweys from one datum to<br />

anolher. Sae also Isolat: Isolong.<br />

Isodynamic llne-A line connecting points of<br />

equal magnilude of any force.<br />

laogal—A cwrtour line of equal gravhy values<br />

on the surface of the Eatih.<br />

lsogonal—A line drawn on a map or chart<br />

joining points of equal magnetic declination for a<br />

given time. Aleo celled Ieogonlc line. Sae<br />

also agonlc IIne.<br />

Iaogonlc chart-A chart of which lhe chief<br />

feature is a system of isogonic Iinaa, each for a<br />

different value of the magnetic clacllnation.<br />

Iaogonlc llne-A tine drawn on a map or chart<br />

iining poims of equal magnetic declination for a<br />

given lima. The line connecting points of zero<br />

daclinalion is the agonic tins. Lines connecfhrg<br />

poinle of equal annual change are isopora, and<br />

are depicfed on Magnetic Variafien charm for<br />

the current 5-year epoch.<br />

190gram-See Isopleth. ‘ -<br />

Ieog rlv chart-A chart with fines connecting<br />

points of equal grivalbn.<br />

lsogrlv—A fine on a map or chart which joins<br />

peinls of equal angular difference between grid<br />

north and magnetic north.<br />

lsolat-An isodiff connecting points ot aqual<br />

latitude corrections.<br />

Isollne-1. A line representing the intersection<br />

of the plane of a vertical photograph wfth the<br />

plane 01 an overlapping oblique phonograph. II<br />

Ihe vertical photograph were tiff frae, the iaollne<br />

would be fhe isomatric parallel of lhe oblique<br />

photograph. 2. A line along which vafues are, or<br />

are assumed 10 ba, constant.<br />

iaolong—An isodiff corrneciing points of equal<br />

longitude corrections.<br />

Isomagnetic chart-A charf ahowing the<br />

configuration of the Earth% magnetic tiefd by<br />

isogonic, isoclinic, or isodynamic lines.<br />

Iaometrlc (conformal) latltude—An<br />

auxlllay latitude used in fhe mnfonnal mapping<br />

of the spheroid on a sphere. By transfonrrirrg


geographic Iatiiudes on the spheroid info<br />

Isometric Isstffudes on a sphere, a conlormal<br />

MSP PmiSCtiOn (the Mercator) may be<br />

celculafed, using spherical formulas, for the<br />

pkoffing of geographic data.<br />

Ieometrlc paraUal-The intersecting fine<br />

befwaen the plane of a photograph and a<br />

horlzonfal pfane having an equal perpendicular<br />

distance from the same perspective center.<br />

MIL-HDBK.850<br />

lSOp@rhetrlC cunre-A lktO on a map<br />

prOjOCflOnabng which lhere is no varlalbn from<br />

exact scale. There are two boperimetric curves<br />

passing through every polnl on an equal-area<br />

map projectbn. This characteristic gives thal<br />

class of pmjectforrs some preference for<br />

engineering maps.<br />

lsopleth-A line of equal or constant value 01 a<br />

gfven quantity, wfth respect to akher space or<br />

lime. Also called fsog ram.<br />

Isoporlc chert-A chart with fines connecting<br />

points of equal magnetic annual change.<br />

lsoDor-A line found on maarretic charis<br />

sho”wirrg pointe 01 equel ann~al change Also<br />

called magnet ic Isoporlc line.<br />

lsopycnlc—A line connecting pints of<br />

density, particularly of ocean water and<br />

at mosphare.<br />

Lsoradlel—A radial from lhe isocenler.<br />

equal<br />

laoatsay—A condition of approximate<br />

equilibrium in the outer part of the Earth, sucn<br />

that the gravitational effect ot masses extending<br />

above the surface of the geoid in continental<br />

areas IS a~roxirnataly counlarbalanced by a<br />

deficiency of density in the malerlal beneath<br />

those masses, while ths effect of deficiency of<br />

density In ocean waters is counterbalanced by<br />

an excess of denstfy In tha material under the<br />

oceans. See also depth of Isostatlc<br />

compermatlcan; Haylord.Bowle method<br />

of Isoststlc raductlon; Hsyrord-Bullard<br />

(or Bullard) mathod of Lsostatlc<br />

rsductlon; Irsostatlc adjustment;<br />

Isostatlc compensetlon; Iaostatlc<br />

corroctlon;<br />

Iaoatrsay.<br />

Pratt. Hayford theory of<br />

laoetstlc adjuatmen!—The natural process<br />

by which the crust ot the Earth adjusts 10 restore<br />

or meinlain Ifs state of equilibrium. See also<br />

lsDataay.<br />

134<br />

Isosiatlc enomaly—Tfr6 ditlerenca batwaen<br />

an obsawed value 01 gravity and a Wworetkal<br />

value al the point ot observation which has<br />

been corrected Ior alevalicrn of me station<br />

alxrve the geoid, and for Ihe effect of<br />

topography over the whole Earfh, and Ior its<br />

iaostatiw compensation.<br />

Ieoatatlc compensation—The departure<br />

trom normal density ot material in the bwer part<br />

of a column of the Earth% crust which balances<br />

(compensates) fend masaea (topography) above<br />

sea level and deficiency of mess in ocean<br />

waters, and which produces the condffion of<br />

approximate equifibr’wm of Earth’s crust. See<br />

also Isostesy; topographic daflectlon.<br />

lSJStatlC corrsctlon—The adjustment made<br />

to values of gravity or to deflections of the<br />

vertical observed al a point to take account ot<br />

the assumed mass deficiency under<br />

topographic features Ior which a topographic<br />

correction is also made.<br />

Iaoatatlc gsold—An ideal geoid derived from<br />

Ihe spheroid of reference by the application of<br />

computed values of the deflection of the vertical<br />

whkh depend upon the topography and<br />

isostatic compensation.<br />

lsoatere-A line connecting points of equal<br />

atmospheric density.<br />

Iaot lmlc-Pertaining to a quality whch has<br />

equal value in space al a paflicular time.


JBcob’s etaff-A single staff or pole used<br />

for mounting a surveyofs compass or other<br />

instrument. sometimes used in place of a<br />

tripod.<br />

Jaderln wlras (ba80 epparatua)-An<br />

apparatus used for base tine<br />

measurement. It consists of sepaala steel<br />

and brase wires, esiended under constant<br />

tenslorr over relerance tripods in the line of<br />

the base. The coefficients of expansion<br />

and tengfhs al a certain temperature of the<br />

two wires having been found, the<br />

temperatures of the wires themselves may<br />

be deduced from the dillerence O! the<br />

measurement of the same distance by the<br />

two wires. With these temperatures known,<br />

the length of the base may be accurately<br />

obtained.<br />

MIL-HDBK-850<br />

Jet Navlgatlon Chart (JNC)--A<br />

1:2,000,000 scale, coordinated series of<br />

multicolored charts, designed to sa!isty long<br />

range navigation 01 high. altitude, hlghspeed<br />

aircratr.<br />

Jolnlng—Connecting two or more separately<br />

~lgltized or stored maps. The junction<br />

between two such maps Is sometimes<br />

visible as a resufl of imperfections or<br />

inconsistencies in the data.<br />

Joint Operatlone Graphic (JOG)—The<br />

standard 1:250,000 scale Depaflmenl of<br />

Defense cartographic product which may<br />

be produced in any 01 the following three<br />

versions to meet the vafidated unified and<br />

specffied commands and mifitery<br />

dapariments area requirements: the JOG/G<br />

(Series 1501 ) Is designed 10 meet ground<br />

use requirements: JOG/A (Series 1501 Air)<br />

Is designed to meet air use requirements:<br />

ard JOG/R (Series 1501 Radar) is the Air<br />

Target Malerial version in support of radar/<br />

intelligence plannicg and operations<br />

requirements.<br />

Jullan calendar—The calendar established<br />

by Julius Caesar in 46 B.C. II is based upon<br />

Ihe assumption thal the true length of the<br />

tropkal yaar was exaclly 365.25 mean solar<br />

days.<br />

J<br />

‘135<br />

Juilan day-The number of aach day, as<br />

reckoned consecutivaty since the ba@nning<br />

01 the presem Jufian period on January 1,<br />

4713 B.C. The Jufian day numbar derrottts<br />

the number of days Ihal has elapsed at<br />

Greanwich noon on Ihe day designated,<br />

sinca this epoch day. Sea also modlfled<br />

Julian day.<br />

junction b8nCtI mark-A bench mark<br />

selected as the oomr’tmn meeting point for<br />

ilnas of tavela or Iinisa 01 levels.<br />

junction detail—A sketch or working<br />

diagram stwawirsgthe details of the various<br />

levelings at a junction.<br />

junction tlgura-A triangulation figure in<br />

which three or more triangulation arcs<br />

meet, or two or more arcs intersect.<br />

}unctlon—1 .[di@lal) The point (node) where<br />

two or more line segments join together.<br />

2.(leveiing) The place where two or n’vxe<br />

fines of levels are connected.


MIL-HDBK-850<br />

K including inexact, heuristic, and subjective<br />

K-factor-see base sffltude ratio. knowledge. The resutts 01 knOWk?dQe<br />

engineering.<br />

Ksslman lllterlng-The<br />

vartance eslimatbn<br />

recursive minimum<br />

of an unbiased Krasovsky epherold (elllpsold)— A<br />

stochastic varlabte. An a pfiod estimate ar’@<br />

SXWattanCe are linearly oombined with new<br />

data to form an updated estimate and<br />

reference ellipsoid having the iollowing<br />

approximate dimensions: semimajor axis<br />

6,378,245.0 malara; fattening or elfipficlty<br />

covanance.<br />

lt298.3.<br />

Keplers lawe-Tfre fhree laws govarnlng<br />

the mollons ot planets In thalr orbits: (1) the<br />

orbits of the planets are eltipses, with the<br />

Sun at a common focus; (2) as a planel<br />

moves in its orbit, the line adjoining the<br />

planet and Sun sweeps over squel arees in<br />

equai imarvals 01 limes; (3) me squares 01<br />

the periods of revolution of any Iwo planets<br />

are proportional to the cubes of thair mean<br />

dislances from the Sun. Also called<br />

Kepler’s planetary Iawa.<br />

Kepler’. plenetary lswa—See Keplar’a<br />

Iawa.<br />

key ftat-The principal or mastar layout or<br />

flal used as a positioning guide for skipping<br />

up other flats. Also called layout guide.<br />

See SISO fist, dafinhion 1: layout.<br />

key—A data elemenl in a data base used by<br />

the application software to locate a specific<br />

data record or group of records.<br />

kilobyte (KB)-A unit of memory<br />

representing 210 (1 .024) byles. Commonly,<br />

a kilobyle may reprasem 1000 byies. A K is<br />

used as a suffix when describing memory<br />

siza, aa in 640K.<br />

klsa plate-A prass plate used to make an<br />

addi!ion or corracrion 10 a previously printed<br />

sheel. Also called touch plate.<br />

Kllmech-Varlomat compilation method<br />

(rellef)-A process by which reproduction<br />

material of targe-scale sheats Is<br />

photographically filtered to relain only index<br />

comours. Tha indax camours are then used<br />

aa the ralief compilation for a medbm-scale<br />

aheel.<br />

knowledge baaed ayatem (KBS)—A<br />

somputer systam thal embodes knowledge,<br />

136


I<br />

I<br />

I<br />

length equetton—A condillon equation<br />

whkt! expresses the relatbnship between<br />

the flxad kanglha of Iwo lines whch are<br />

connected by triangulation.<br />

length 01 degrea-The length of a degree<br />

of Iatfiude measured along a meridian or<br />

tonglfude. The IerrQth varies somewhat wiifr<br />

the degrees of Ialttude. Those near the<br />

pole are longer and those near the Equator<br />

are efrorler. The tengsh also varies WMI<br />

different selections of sphemlds.<br />

level controf-A aerles of bench marks or<br />

other points of known elevation,<br />

established throughout a project.<br />

level correction—That correction which is<br />

applied to an observed difference of<br />

elevation tO correct for the error imroduced<br />

by the lacf that the line of sight through the<br />

Ieveting instrument is not absolutely<br />

horizontal when the bubble is centered in<br />

its vial. Sea atso Ieval constent., ., .<br />

level Nne-1. A line on a level surface;<br />

therefore a curved fine, 2. A tine over which<br />

bVeling operations are aCCornplished. See<br />

also dupllcete level Ime; ltne of<br />

levels; multtple level Ilne:<br />

slmulteneoua level Ilne; epur Ilne of<br />

Ievela.<br />

Ievet nel—See eurvey net, detlnition 2.<br />

level rod-See Ievellng rOd.<br />

lev~~r~eu:~ce—See equlpotentlal<br />

Ievet trier-An apparatue for use in<br />

measuring the angular value o? the<br />

divlsbna of a apiriI level,<br />

Ievellng error of cloeure—See error of<br />

closure, definition 4.<br />

leveling lnatrument—An Instrument used<br />

tor determining dltferences 01 elevations<br />

between points, See also Abney level;<br />

dumpy level; Egault level;<br />

enslneer”a level; firel.order level;<br />

Flacher Ieval; Gravett level; hand<br />

MIL-HDBK-850<br />

137<br />

L<br />

level; hanging level; Iet}tude Ieval;<br />

Lenoir level; Iocator’a hand level;<br />

mllltary level; pendulum level; plate<br />

level; praclaa level; reverelble level;<br />

●alf-levellng level; ●plrlt level;<br />

Stampfer level; ●trldlng tavel;<br />

teleecope level; tlttlng Ieval;<br />

Troughton level; U.S. Geological<br />

Survey level; wye [Y) Iavel.<br />

Ievallng rod-A straight md or bar, deelgned<br />

for use in measuri~ a vertical distance<br />

between a potnt on tha gruund and the line<br />

01 collimatbn of a leveling instrument which<br />

has been adjusted to a horizorrfat posttlon.<br />

Also called bvel rod; rod, See aleo<br />

Barlow Ievellng rod; Boaton Ievellng<br />

rod; double-target leVellng rod;<br />

foot-meter rOd; Gravatt Ievellng rOd;<br />

Invar Ievellng rod; long rod; Molltor<br />

praclsa Ievellng rod; New York<br />

Ievellng rod; Pemberton Ievellng<br />

rod; Phlledelphla Ievellng rod;<br />

preclsa Ievellrrg rod; range rod; salt.<br />

raadlng Ievellng rod; ahorf rod;<br />

alngle-target leveling rod;<br />

Stephenson Ievellng rod; tepe rod;<br />

targat Ievetlng rod; U.S. Englnear<br />

praclsa Ievellng rod; U.S.<br />

Geological Survey precise Ievellng<br />

rod.<br />

leveling the model—See Ievellng,<br />

detinilion 2.<br />

line map-See planlmetrlc map.<br />

line of apsldas—Tha major axis of an<br />

elliptical orbit extended indeflmtely in Lmth<br />

directions. Also called apse Ilne.<br />

Ilne of collimation—(oplics) The line<br />

through the second nodal palm of the<br />

Objedive lens of a telescope id the center<br />

of Ihe reticla. Aleo called almlrrg tlna;<br />

fine of eight: polntlng Ilne; ●lght<br />

Ilne.<br />

Ilne of constant trcale-Any line on a<br />

photograph wtrich is parallel to the trve<br />

horison or 10 the ieomatric psrallel. Also<br />

called Ilne ot equal acala.<br />

Ilne of equal acala-See Ilne of


I<br />

,!<br />

I<br />

I<br />

I<br />

I<br />

I<br />

!<br />

I<br />

I<br />

I<br />

I<br />

I<br />

I<br />

constant scale.<br />

MIL-HDBK-850<br />

Ilne of iorca-A fine indicating the diraclion<br />

in whti a force acts, as in a magnetic fietd.<br />

focal magrretlc disturbance-See focal<br />

magnetic anomaly.<br />

IabellnQ+digftal) The process of aasignlng<br />

atfrihstes to potygons.<br />

Laborde map projection—Similar to the<br />

transverse Mercator projection, except that<br />

lhe Laborde projacts a spheroid rather than<br />

a sphere omo a plane. This contormal<br />

pmjectbn is best sufted for regions which<br />

are elongated In a direction which M at a<br />

considerable angle to the msridian. [USAF<br />

special Fl!@f Charts are based on lhis<br />

projection.]<br />

LaCoete. Romberg grsvlmeter—A longperiod<br />

spring suspended cantilevered<br />

weight system adapted to the<br />

measurement of gravity differences,<br />

ladder grid numbers—Those grid numbers<br />

which identify fhe grid lines wilhin the<br />

neafline.<br />

Lambert nzlmuthal equal-ares map<br />

propsctfon -See Lamberf zenlthal<br />

equef.area map projection.<br />

Lambert azimuthal polar map<br />

projection—A Lamberf equal-area map<br />

projffclion wiih the pole of projection al the<br />

pole of the sphere, and lhe radii o! the<br />

circles which represent the geographic<br />

parallels corresponding to the chords of<br />

those parallels.<br />

Lambert bearing-A bearing as measured<br />

on a Lambert contormal chart or plotting<br />

eheel. This approximates a great-circle<br />

baaring.<br />

Lamberf csmtraf equlvafent map<br />

projection upon the ptene 01 the<br />

merldlan-An azimuthal map projection<br />

having fhe pole of the projection on fhe<br />

Equator. Also called Lamben equal<br />

erea marldlonal map projection.<br />

Lambe~ Conformal Cfrafi-A chart on tne<br />

Lamberf carformal projection.<br />

Lambert cortformel conic map<br />

138<br />

prolecf ion—A contormal map projection<br />

of the so-called conical fype, on which all<br />

geographic meridians are repreaenled by<br />

straight fines which meet in a common<br />

pint outside the limits of the map, and the<br />

geographc parallels are rapresantad by a<br />

series of arcs 01 cimfes havi~ this common<br />

@nt tor a tamer. Meridians and psratleb<br />

infersect al tigfsl angles, and angles on fhe<br />

Earih are correctly raprassmed on the<br />

projection. This projection may have one<br />

standard parallel along which the scale is<br />

held exact; or Ihere may be two such<br />

standard parallels, both maintaining exact<br />

scale. At any fmint on the map, the acsle is<br />

the same in every direcfbn. It changes<br />

along the meridians and is constant along<br />

each parallel. Whera thare are two<br />

standard parallels, the scale between those<br />

parallels Is too smafl; beyond them, too<br />

large. Also called Lamberf conformal<br />

map projection.<br />

Lambert Conlormal map projecllon-<br />

See LamDert conformal conic map<br />

projection.<br />

Lambert equal.area meridional map<br />

pro)actlon—See Lambert central<br />

equivalent mep projection upon th9<br />

plane of the merldlan.<br />

Lambeti grid—An informal deaignatlon for a<br />

coordinate system based on a Lambed<br />

conformal map projection.<br />

Lambert zenlthal equal-area map<br />

projection—An azimuthal map projaclion<br />

having the pole of the projection at the<br />

center of the area mapped. The azimuths<br />

of great circles rad!atlng from this tamer<br />

(Wle) are truly represented on the map:<br />

equal distancea on thoss greal circles are<br />

represented by equal linear rfbtancea on<br />

the map, but the scale along those great<br />

circle Ilnes so varies with distance Irom the<br />

pole of the projection, that an equal-araa<br />

projection Is produced. Al= called<br />

Lambarf azimuthal equal-aree map<br />

projecffon.<br />

Iamlnate-1. The procese of ptasewing a<br />

map sheef or other graphic by sandwiching<br />

between two sheets of clear Symhetic<br />

malerial (polyethylene polyester plaslic).<br />

The laminating equipment uses heat and<br />

pressure but no adhesive. 2. (relief model)<br />

See p)estlc block.


land boundary-A line of demarcation<br />

fmtween two parcels of land.<br />

land effect-See coastal refraction.<br />

land mass slmulat~r plate-See<br />

fsctorad transparency.<br />

land survey-The process of determining<br />

boundaries and arsas of tracts of land. The<br />

term csdastral survey Is someflmea<br />

used to dasignaia a land survey, bui in this<br />

country lls use sfwuld be restricted to the<br />

SUfVeyS Of public lands of the United<br />

S!atea. Also called boundary survey;<br />

property survey. See also cadastral<br />

survey.<br />

land-line adjustment—Posltionlng lhe<br />

public land fines on a topographic map to<br />

Indicate their true, theoretical, or<br />

epproximata location relative to the<br />

adjacent tarrain and culture.<br />

landmark-l. An object crl enough Interest<br />

or prominence in relation to iis surroundings<br />

to make ii outstanding or to make it useful<br />

In determining a location or a direction. 2.<br />

Any monument, material mark, or fixed<br />

object used to dasignate the location of a<br />

land bmndary on the ground.<br />

LAN DS,AT—The generic name for a series of<br />

aarfh obsewlng satellites, fimt launched in<br />

1972 by NASA. IANDSAT serves as<br />

plaffomns for several sensors, including the<br />

Return Beam Vidlcon (FiBV), Ihe<br />

Multispectral Scanner (MSS), and the<br />

Thamatic Mapper (TM). Originally named<br />

ERTS, for Earlh Resources Technology<br />

Satellite.<br />

Iandacape map—A Iopogrephic map made<br />

to a relatively large scale and showing all<br />

datails. Such maps are required by<br />

archnecfs and landscape gardeners tor use<br />

in planning buildings 10 fit the natural<br />

tolmgraphic teatures and for landscaping<br />

parka, playgrounds, and private eslates.<br />

These are generally maps of small areas,<br />

and scales vary from 1 inch -20 feet to 1<br />

foot = 50 feet, depending on the arrwunl of<br />

detail.<br />

Laplace azimuth mark—An astronomic<br />

azimuth mak at a Laplace Station.<br />

MIL-HDBK-850<br />

139<br />

Laplaca azimuth-A geodetic azimuth<br />

derived trom an astronomic azhrsutn by use<br />

01 Ihe Leplaca equation:<br />

Laplace condltlon—The Laplace condition,<br />

expressed by the Laplaca equatbn, arises<br />

horn the facf Ihal a deflacf”bn of the vertical<br />

in the plane of the prima varfkel Ml gtva a<br />

differanca between astronomb and<br />

geodetic bngitude and bafwean<br />

astrurromic and geodetic azimuth; or,<br />

conversely, that the obsewed differences<br />

between astronomic and geodatc valuaa of<br />

the Iongilude and of the azimuth may both<br />

be used to determine the dellacfion in the<br />

plane of the prima varticel.<br />

Lapface control-Con!rol and correction of<br />

astronomic azimuths through observations<br />

of Ihe deflection of the plumb line in the<br />

prime vertical (comparison or astronomic<br />

and geodetic Iongilude).<br />

Laplace equation—l. The equation which<br />

expresses Ihe relationship between<br />

astronomic and geodetic azimuths In tarms<br />

of astronomic and geodetic bngiludes and<br />

geodetic latitude. 2. (~tenlial) A pariial<br />

differential equation of the sacred-order<br />

which is satisfied by the Newlonian<br />

potenlial of every finite body at all exterior<br />

points.<br />

Laplece station—A triangulation or traverse<br />

station at which a Laplau azimuth is<br />

determined. Al a Laplace atafion both<br />

astronomic longitude and astronomic<br />

azimuth are dalermined.<br />

Iarge-scale map—(JCS) A map having a<br />

scale of 1:75,000 or larger. Sea also map.<br />

Iaaar Ierraln profile recordar—An<br />

electronic instrument that emits a<br />

continuous wave laser beam from an<br />

aircratt 10 measure vertiial dbtartcas<br />

between the aircraft and tha Earths<br />

surface.<br />

lasar—A devica producing coherent energy<br />

beams in the spectrum of Iighl or near-iiiht<br />

frequancias. A .Iaser-equipped Geodimetar<br />

makes it possible 10 measure greater<br />

distances.<br />

Iatant Image-The invisible image produced<br />

In radiation-sensitive materials which


ecomes visible upon processing.<br />

Intoral chromsstlc absrrratlon-A n<br />

aberration which affects the sharpness 01<br />

knages off Ihe lane ask because different<br />

cobrs undergo different magnificaliorm<br />

lateral geln-(JCS) The emount o! new<br />

ground covered taterally by successive<br />

phomgraph!c runs over an area.<br />

Ietensl magnlflceflon-The ratio of a<br />

length in the Image, perpendicular to the<br />

lane azie, 10 a mrresponrlng length in the<br />

object.<br />

MIL-HDBK-850<br />

lateral rafmctlon—lhe horizontal<br />

mmponenl of the refraction of light through<br />

the atmosphere.<br />

lateral ●hlff-The offset of the position of<br />

the peak of an anomaly with the mass of<br />

magnetization (or gravitation),<br />

Ieteral tltt-See roll, definition 2,<br />

Intltudo bmwf-(JCS) Any latitudinal ship<br />

des’@ated by ascepted units of linear or<br />

engutar measurement, which circumscribes<br />

the Earth. Also called band; Iatltudtnal<br />

band.<br />

Iatltude correction—The amount of the<br />

adjustment of observed gravity values to an<br />

ati!trarily chosen bese Iatltuda. Also,<br />

correction to Iattiude In a traverse course,<br />

Ietltude datarmlnatlon, zenlthtaleacope<br />

mathod—A precise method<br />

of determining astronomic Ialitude by<br />

measuring the difference of the meridional<br />

zenith disfances of hvo stars of known<br />

declination, one north and the olher soulh<br />

of zenith. AlSO called Horrebow-lalcott<br />

mathod of Iatltude determination.<br />

Iafltude dlffarence-(plane surveying)<br />

Length of fhe projection of a traverse<br />

muree onto a meridian. Also called<br />

norshlng; aouthing.<br />

Iafltuda ●quation—A condition equation<br />

which expresses the relationship between<br />

the fixed latitudes of two points which are<br />

mnnected by triangulation or traverse.<br />

Iatltude fector—The change in Ialilude<br />

140<br />

along a celestial fine of position par one<br />

minute change in longitude.<br />

Iatltude level—A sensitive spirit level<br />

attached to the telesmpa of an instrument<br />

employed for observing astronomic tatituda,<br />

in such manner that when Ihe Ieleempa is<br />

clamped in position, the level measurea, in<br />

a vertical plane, variations in the direti~on of<br />

Ihe Iina of mliimation.<br />

Iafitude of the ilna43ee dlfferance of<br />

Iatltuda, definition 2.<br />

Iafltude-1. (general) A finear or angular<br />

dktarrce measured mx’fh or south of the<br />

Equator on a sphere or spheroid. 2. (pIana<br />

surveying) The perpendicular distance In a<br />

horizontal plane of a poimfrorn an eastwest<br />

asis of refarance. See also<br />

dlfferonce of iatltude, definition 2. 3.<br />

(on a sphere) The angle at the mnfer of a<br />

sphere between the plane of the Equator<br />

and the fine to the fmint on the surface of<br />

the sphere. 4. (traverse) The norlh-eoulh<br />

component of a traverse course. S.<br />

(photography) The ability of an emulsion to<br />

record a range of brightness values. See<br />

also argumerrl ot latitude; assumed<br />

Iatltude; astronomic Imltuda;<br />

authallc (equal-aree) Ialltude;<br />

celestlal ialltuda; clrcla of Iatltude;<br />

difference of Ietltude; flctltlous<br />

Iatllude; galactic Iatltude;<br />

geocantrlc Iatllude; geodeflc<br />

Iatllude; geographic Iatltuda;<br />

geomagnatlc Iatltude; grid latitude:<br />

ieometric (conformal) Ia:ltude;<br />

latitude correction: mlddla Iatltude;<br />

obllque latitude; parallal: parametric<br />

Iatltude; rectifying Iatltude;<br />

terraatrlal Iatltude; traneverae<br />

Iatltude; varlatlon of latitude.<br />

Iatltudlnal band—Sac latitude band.<br />

Iatltudlnal curve-This term denotes an<br />

easterly and westerly property line adjua!ed<br />

to the same mean bearing from each<br />

monument to the next one In regular order,<br />

as dktinguished from the long chord or<br />

great circle that wou!d mnnecf the initial<br />

and terminal points.<br />

lattlce—(JCS) A network of intersecting<br />

positional lines printed on a map or chart<br />

from which a fix may be obtained.


law of propegistlon ot error—The<br />

probable (standard) error of the sum of two<br />

or more quantifies is equal 10 the square<br />

mot of Ihe sum 01 the squares of their<br />

probable (sfandard) errors.<br />

law of unlversel gravltaIlon—S e e<br />

constant 01 gravitation.<br />

Ieydown-often used to designate a mosaic<br />

temporarlfy assembled from uncropped<br />

prfnts.<br />

layer tlnfs—See hypsometrlc tlntlng.<br />

layered data-Themelically separated data.<br />

The geographic equivalent of fhird normal<br />

form.<br />

Iayer—(digllal mapping) A logical separation<br />

of data base information according 10<br />

theme. Many geographical information<br />

systems arxf CAD/CAM sysfems allow the<br />

user fo choose and work on a single<br />

thematic layer or any combination of<br />

fhamatic layers at a time.<br />

!.<br />

layout guide—See key flat.<br />

Ie yout—Tha planned posif ionlng of<br />

reproduction material to lit the requirements<br />

and limitations 01 lithographic plales, paper,<br />

and finishing. Also called lay. See also<br />

flat, definition 1.<br />

lay—l. See IayOCft. 2. To assemble a<br />

photomosaic. Often referred to by the<br />

mefhod ueed In assembly, such as wet<br />

Icy, sfaple lay, efc.<br />

lead llne-A long, graduated chain or line af<br />

fhe end of which Is aftached a lead welghf,<br />

used to measure depths of water, Tha lead<br />

line Is usually used when making soundings<br />

by hand In water less fhan 25 fathoms<br />

deep.<br />

leap secorfd-The sfep adjustment made fo<br />

UTC to compensate for the approximately 1<br />

second that tha fime Irensmitled by UTC<br />

elgnals gains on UT1 or UT2 each year.<br />

Normally, UTC is decreased by exactly 1<br />

second (I.e., fhe Ieep second) a! 24h on<br />

the Iaat day of December and/or Juna. See<br />

alsO fJTO; UT1; UT2; Coordinated<br />

Unlvarsal Tlma.<br />

MIL-HDBK-850<br />

141<br />

Ieap-trog mefhod—A rapid meana of<br />

obfaining alevafions of stations akrng a<br />

mule bervveen two base stations, or 10<br />

obfaln a cbsed foop of altimeler elavationa.<br />

The ayetem uses four barometers operating<br />

in pairs. One pair of barometers remains al<br />

fhe base atalion whlla Iha ofher pair IS<br />

advanced 10 the first station at whti tima<br />

beromaler and weafher candtiione are raad<br />

and racordad airrruftaneousty. Ttfe original<br />

base sfaticrn pair are advanced to the<br />

aacond alafion and the process rapaated.<br />

Thla method does rwl produce raiiibla<br />

aievations. The two-base mefhod ka<br />

considered batter.<br />

Iasst count—(micmmafer or varnlar) The<br />

finesf reading fhal can be made directly<br />

(wilhouf estimation) from a vernier or<br />

micrometer.<br />

least equares—The theory of Ieaet squares<br />

slates that in a sef of redundanf<br />

observations, the most probable adjusfed<br />

values of the obsawalions ara obtained<br />

whan the sum of fhe squares of fhe<br />

adjustments to fhe observations fo obtein<br />

mathematical compatibility is a minimum.<br />

A Ieasl squares adjustment imposes lhis<br />

@2nCfitiOnon a set of redundanl and<br />

Inmmpatlbla obsawafions so that the sel of<br />

equafions may be solved uniquely for fhese<br />

most probable values. See aiao<br />

arfjuafment of observations.<br />

Iaft bank—That bank 01 a slream or river on<br />

fhe Ie!t of the observar when he is facing in<br />

fhe direction of flow, or downstream.<br />

Legendre polynomial—A special case 01<br />

the associated Legendre tursct’on in which<br />

fhe function becomes a Pd)VWSIal.<br />

Legendra”a ttaeorem-A mathematical<br />

fheorem stafing fhaf ffra Iangfhs of fhe<br />

sidas of a spherical triangle (very short by<br />

comparison wilh fhe radiue of the aphare)<br />

ara equal to fha Iet’)gfhs of fha<br />

corresponding sides of a plana frtartgle in<br />

which fhe plane anglas are derlvad by<br />

reducing each of fhe spharlcsal angles by<br />

approximately ona-third of the spherical<br />

axcass.<br />

Lehmann’ts mathod-Sea triangle-of -<br />

error mathod.


length corracflon-(taping) The difference<br />

bahveen the nominal length of a laps and<br />

ils effective length under conditions of<br />

afandardiiafion, The standard length of a<br />

fape is usually expressed by a number o!<br />

whole units (the nominal length) plus or<br />

minus a small distance which is tha length<br />

correction defined above.<br />

MIL-HDBK-850<br />

Lenolr laval—An krsfwmerrf which has the<br />

telescope passing through steel blocks,<br />

one near each end, whose upper and lower<br />

tamrs are plane and closely parallal; me<br />

bwer faces real upn a brass circle; the<br />

UPPar facas SUPPOII a apiril level, which is<br />

reversed in tavelirrg the instrument.<br />

lens axis—See optical axla.<br />

tans calibration-See camera<br />

calibration.<br />

Iarrs component—See lens element.<br />

Ians dlaforliorr+JCS) Image displacement<br />

caused by lens irregularities and<br />

aberrations.<br />

lens alemenl—One lens 01 a complex lens<br />

system. In a photographic lens, the Ierms<br />

from element and rear element are<br />

often used. Also called lens component.<br />

Ians epaed—See relative aperture.<br />

Ianaatlc compaas—A type of compass<br />

equipped wfih a lens which permits the<br />

observer to read the far aide of the<br />

movable dial.<br />

lens-A disk of optical glass, or plastic, or a<br />

combination of (WO or more such disks, by<br />

which rays of fight may be made to<br />

Kvrverge or to diverge. Such disks have<br />

two surtacas, which may both be spherical,<br />

one Plane and ona spherical, or various<br />

other cmnbinallons [cyfirrdrical, paraboloid,<br />

or hyperboloid). See also achromatic<br />

lens; anastigmailc lens; aplanatlc<br />

Iena; apochromatlc lens; aapherlcal<br />

Iana; aallgmatlzer; coated lens;<br />

Compensating lasts; converflble<br />

Ians; cylindrical Iena; eyepiece:<br />

Freanel Iena; Metrogon Iena:<br />

narrow-angle Iana; negative Iene;<br />

normal-angle Iene; objective lens;<br />

po.sitlve lens; process lens:<br />

142<br />

apherlcal lens; auperwide-angle<br />

Iene; thick Iena; tfrln Iana; wldean@e<br />

Iene.<br />

Level O topology—A topological surface<br />

which comains a set ot entily points and<br />

edges. Edges mnrain onty coordinate and<br />

aftritrute information.<br />

Level 1 topology—A topological aUIfaC8<br />

which Cunsiars of a eel of entity poinfs and<br />

edges that meet at nodes. Edges contain<br />

stan node, end node, next edga, and<br />

previous edge information,<br />

Lavel 2 lopology—A topological surface<br />

which consists of a set of edges and entity<br />

points, when projected on a planar surface,<br />

the edges maet only at nodes. Edges<br />

contain start node, end node, and next and<br />

previous edge information, Edges meet<br />

only at nodes.<br />

Level 3 topolog y—A IopoloQical surf aca<br />

which is partitioned by a set ot mutually<br />

exclusive and coliecfively exhaustive facea.<br />

Edges conlain left tace, right face, start and<br />

end noda, and next and previous edge<br />

information. Edges meet oniy at nodes.<br />

level constant—The amount by which the<br />

actual line 0! sight lhrough a leveling<br />

instrument (when the bubble ia centerad in<br />

ils vial) departs from the tmfy horizontal line<br />

through the center of the instrument,<br />

computed in millimeters per millimeter of<br />

siadia interval. When leveling rods<br />

graduated in yards instead 01 meters are<br />

used, the level constant, C. woutd be<br />

expressed in milliyards per milfiyard of<br />

stadia interval. Also called C-conetant.<br />

Iavellng—1. (survaying) The operations of<br />

measuring vertical distances, diraclly or<br />

indirectly, 10 determine elevations. See also<br />

aatrogeodetlc Ievellng;<br />

astrogravlmetric Ievellng; barometric<br />

Ievellng; dltterentlal Ievellng; direct<br />

Ievellrrg; firs!-ordar Ievellrrg; flylrrg<br />

Ievela; geodetic leveling; profile<br />

levallng; reciprocal Ievellng;<br />

aacond-ordar Iavellng; aplrlt<br />

Ievellrsg; atadla trigonometric<br />

Ievellng; thermometric Iavellng;<br />

third-ordar Ievellng; fhree-wire<br />

Ievellng; trigonometric Ievaflng;<br />

verrlcef engulatlon; water Ievellng.<br />

2. (photogrammetry) In absolute


I<br />

1<br />

,:, >4, ,,, ,.,.<br />

orientation, the operalion of bringing the<br />

model datum parallel to a relerence plane,<br />

usually the iabletop of the stereoplotlirrg<br />

instrument. Also called horlzontallzlng<br />

the modal; Ievellng the model. S e e<br />

also aerolevellng; oriermatlon,<br />

delhifion 7.<br />

laval-A partition within an MC&G data<br />

WbIYmuP that is an aggregation of data<br />

elements distinguishable by data<br />

chsractaristics (e.g, resolution, scale,<br />

accuracy).<br />

Ilbrary attribute—(dlgltal mapping)<br />

Properties of a Iiirary. These propartiea are<br />

comalned in the Library Header Table, the<br />

Library Attribute Table, and olher tables<br />

related to them.<br />

Ilbrsry negallve mold—A negative mold<br />

which has been esiended to a size<br />

compa!lble with the printed plastic map and<br />

forming equipment, and which is kepl in file<br />

lor subsequem castings.<br />

Ilbrary-(digital mapping) A collection of<br />

Covarages contained wi!hin a specilied<br />

spatial errtem. all of which share a single<br />

coordinate system and scale and have a<br />

wmmon lhematic definition.<br />

llbraIlorr-A real or apparem osclllamry<br />

motion, particularly the apparent oscillation<br />

of Ihe Moon, which resulks in more than<br />

half of the Moon’s surface being revaaled<br />

to an observer on lhe Earlh, even though<br />

Iha same aide of the Moon is always<br />

toward the Earih because the Moon’s<br />

periods of rotation and revolution are the<br />

same.<br />

lllt—See selecflon ovarley.<br />

Ilmbl. The graduated curved part of an<br />

instrument for measuring angles, as that<br />

pars 01 a marine sexlanl carrying the<br />

altitude scale, or arc. 2. The circuiar outer<br />

edge of a celestial body. See also lower<br />

Ilmb; upper limb.<br />

Ilmlt of rellable pholo coverage—A label<br />

placed along a dashed line separating<br />

reliable photo compilation trom map<br />

Computation on a chart. The Iabei is always<br />

placed on the photo compilation side of the<br />

Iimlf line.<br />

MIL-HDBK-850<br />

143<br />

line copy—Any wpy suitable for<br />

reproduction withoul using a screen. Copy<br />

mmposed ot lines as dk.tinguished horn<br />

wntirwous tone copy.<br />

Ilne of levele-A continuous series of<br />

measured differences 01 elevation. The<br />

indtitiual measured differences may be<br />

Singla observations in Ihe case of single-run<br />

leveling or fhe means of repeatad<br />

obsewat”ons ifl the case 01 double-Nfl<br />

Iavaling.<br />

Ilrre of noda*The straight line wnnectirrg<br />

lhe two points of inlersaction of the Scfiplic<br />

with the orbit of a planet, plarsetoid or<br />

wmet: or the line of irrlereecfion of Ihe<br />

planes of the orbit of a satellite and the<br />

aquator of its primary.<br />

Ilne of posltlon-A line indicating a series<br />

of possible positions, determined by<br />

observation or measurement.<br />

line of slghl—1. The straighl line between<br />

two points. This line is in the direction of a<br />

great circle. but does not follow the<br />

cuwature cd the Earth. 2. The line<br />

exlending from an instrument along which<br />

distant objects are seen, when viewed with<br />

a telescope or olher sighting device. Afso<br />

called almlng ilne. 3. (optics) See Ilne<br />

of collimation.<br />

Ilne of soundlnge—A series of soundings<br />

obtained by a vessel underway, Usually at<br />

regular intewals.<br />

Ilne patterrt-A photographic negative<br />

wntaining parallel lines of equal-sized<br />

widths, which are equaily epaced. Line<br />

patterns are used for printing tones of a<br />

color or to present a pattern of coverage for<br />

a chart feature. Sea also area patlern<br />

screen.<br />

line rod—See range rod.<br />

line thlnnlng (generalization)-1.<br />

(vector) Reducing the quantity of<br />

coordinates necessary to pmray tha basic<br />

shapa at a feature by using a aerias of<br />

rules. 2. (rasier) Process wheraby a<br />

finear Ieature is represented in a grid by a<br />

wntinuous series of cells, each 01 which<br />

touches along its sides and comers, no<br />

more fhan two other cells belonging lo the


fearure.<br />

MIL-HDBK-850<br />

Ilne tr_A tree intersected by a surveyed<br />

iina. reootiad in Ihe fietd notes of the<br />

eu~ay,’ and marked wiih two hacks or<br />

notches cut on each of the sides lacing Ihe<br />

line. Afeo calied alght tree.<br />

lln~route map-A map or overlay for eignal<br />

comrrrunicstion operations that shows me<br />

actual routes and types of conslrucfion of<br />

wire urcuits in the fiafd. II also givas the<br />

iocalions 01 switchboards and telegraph<br />

stalions.<br />

Iineage-lnforrnalion about the data source,<br />

parlkxdarty Iha original scale and accuracy.<br />

lineal convergency—The length by which<br />

meridians approach one another when<br />

extended from one parallel 10 another.<br />

Ilneer bulldlng fronlege—in air<br />

photographic interpretation, the side<br />

elevation of structures of homogeneous<br />

area.<br />

linear distortion-The failure of a lens to<br />

reproduce accurately to scale all distances<br />

in the ob)ect,<br />

Ilnear error of closure-The straight-tine<br />

dis:ance by which a Iravarse fails 10 close.<br />

Ilnaar error—A one-dimensional error (such<br />

as an error in elevation) defined by the<br />

normal distribution hrnction,<br />

Ilnear feature—A feature that is portrayed<br />

by a fine that does no! represent an araa,<br />

Afeo called line featura.<br />

Ilneftt magnlllcstIon—The ratio of a linear<br />

quantity in the image to a corresponding<br />

finaar quantity in Ihe object. If may be<br />

lateral marmiiicailon or Ionam.rdinal<br />

magnification.<br />

Ilrrear parallax-See absolute<br />

etereoacoplc parallax.<br />

llneerlzetlon—The process of redefining a<br />

ael of nonlinear equations 10 a set of<br />

approximate linear equalions to facifitale<br />

solution computations.<br />

Ilnes of Communlcatlons (LOC)— (JCS)<br />

All the routes, land, waler, and air, which<br />

144<br />

connect an oparating military force wilh a<br />

base of operations, and aforrg which<br />

supplies and reinforcements move.<br />

lines on a apherold-Any direct Iine<br />

befwean two positions on a apherokf,<br />

represanled by two points on tha Earth.<br />

Such a fins may be one of mathematical<br />

definition, or it may raautt Irom a direct<br />

survey between the fmirds on the Earth.<br />

See afso curve of alignment;<br />

geodesic Ilna; normal aectlon Ilne.<br />

Ilnlng pole—See ranga rod,<br />

link and nods-A data em.rcture<br />

characterized by data in whti one or more<br />

finks are related to one or nxore features.<br />

The beginning and end points of each fink<br />

are identified by node identifiers either<br />

expfbiffy or implicitly.<br />

link of levels—Sea Ilrtk, definition 1.<br />

Ilnk—1. (levefing) A fine, a pan of a line, or a<br />

combination of lines or parts of lines of<br />

levels, whtch, taken as a unit, make a<br />

continuous piece of leveling directly from<br />

one junction banch mark 10 another<br />

junction bench mark without passing<br />

lhrough or ovar any other junction bench<br />

marks. Also called link of Ievals. 2. A<br />

unit 01 finear meesure, one one-hundredth<br />

of a chain, and equivalanl to 7.92 inches.<br />

See also chain. 3. A fine between two<br />

consecutive nodes.<br />

Ilquld hand compass—A type of hand<br />

held compass wherein the cornpaas card is<br />

damped through the action of a liquid.<br />

List of Llghta—The DMA publication which<br />

identifies and describes lights and fog<br />

signals in foraign waters of tha worfd. This<br />

information is also accessible on fhe<br />

Navigation Information Network<br />

(NAViNFONET).<br />

Ilal of dlracIlorr%A listing of objacts<br />

observed al a triangulalbn station, together<br />

with the horizontal dlractions in terms of arc<br />

01 the circie, referred to one 01 the objects<br />

observed as a zero initial.<br />

hat-See x-tilt.<br />

Iltho copy—See Iflhographlc copy.


Ilthograpfrlc copy—A graphic reproduced<br />

by the lithographic precess. Also called<br />

Iltho COpy.<br />

Ilthographlc drafting—See Iuschlng.<br />

lithography—A planographlc method of<br />

printing based on the chemical repulsion<br />

between grease and waler to separate the<br />

printing from rronprinting areas. See also<br />

offset Illhogrephy;<br />

photolithography.<br />

lithosphere-The solid part of lhe Earth or<br />

other spSflal body. Distinguished from the<br />

efmosphera and the hydrosphere.<br />

local adjustment—See station<br />

ad]uatmen!.<br />

local apparent tlma—The apparant solar<br />

time for fhe meridian of the observer.<br />

local sefronomlc tlma—Mean time<br />

reckoned from the upper branch of the<br />

bcal maridian.<br />

Iocel attraction—See local magnetic<br />

anomaly.<br />

Iocsl chart-A large-scale aeronautical charf’<br />

designed tor contact fiighl in a congested<br />

area.<br />

local clvll time—See local mean time.<br />

local coordinate system—A right-handed<br />

rectangular coordinate system of which the<br />

z-esis coincides with the plumb fine through<br />

the origin<br />

local datum—The point of reference of lhe<br />

oeodetic control used exclusively in a small<br />

iirea. Usually iden(ifiad by a pro-per name.<br />

local horlzcm—See epparenl horizon.<br />

local trour angle-Anguler distance wesl 01<br />

the bcal celestial meridian; the arc of Ihe<br />

celestial equator, or the angla at the<br />

celestial POle, belween the upper branch 01<br />

the local celestial meridian and Ihe hour<br />

circle of a point on the celeslial sphere,<br />

measured westward from Ihe local celestial<br />

meridian through 360”.<br />

MIL-HDBK-850<br />

145<br />

local lunar time-The arc oj the celeslla)<br />

squalor, or the angla at Ihe celasiial pie,<br />

between the bwer branch of the kx.al<br />

calestial meridian and lhe hour clrcfe of the<br />

Moon, measured westward from the lower<br />

branch of the bcal csfestlal mertcfian<br />

through 24 hours; focal hour arrgla 0! the<br />

Moon, exprasaad in lime unffs, PIUS 12<br />

hours. See also Greenwich lunar time.<br />

IOIX31 magnatlc anomaly-Abnormal or<br />

irregular variation of the Earth’a rnegnafii<br />

field extemfing over a ralalivaly small araa,<br />

due to local magnetk inlluencas. Also<br />

called anomaloua megnetlc varlatlon;<br />

local attraction; local magnatlc<br />

disturbance; magnetic anomaly.<br />

local mean time-l. (JCS) The time<br />

interval elapsed since tha mean WI%<br />

transit of the observets amemaridian. 2.<br />

The arc of the celestial equator, or the<br />

angle at the celestial pole, between the<br />

lower branch of the local celestial meridian<br />

and fhe hour circle of the mean sun,<br />

maasured westward from the lower branch<br />

of the bcal celestial meridian through 24<br />

hours: local hour angle of fhe mean sun,<br />

expressed in time units, plus 12 hours.<br />

Called local cIvII tlmo in United stales<br />

terminology irom 1925 through 1952. See<br />

also local aawonomlc time:<br />

Universal Time.<br />

local merldlan-The meridian through any<br />

particular place or observer, serving as the<br />

reference for local time. Also called<br />

reference meridian.<br />

Iocel eldereal time-The local hour arwle<br />

of the vernal equinox, expressed in time<br />

units. Locel stiareaf lime at the Greerrwich<br />

maridlan is called Greenwich aldereal<br />

time.<br />

local tlma-1. Time based upon the local<br />

meridian as reference, as contrasted with<br />

that based upon a time zona mesidlan, or<br />

the meridian of Greenwich. 2. Any time<br />

kept locally.<br />

local vertbal—The direction of the<br />

acceleration of gravity, aa opposed to tha<br />

normal 10 a reference eurlace.<br />

Iocatlon survey-The establishment on the<br />

ground of points and fines in positions


MIL-HDBK-850<br />

which have been previously determined by<br />

COwlation or by graphical melhods, or by<br />

desrmption obtained from data supptied by<br />

documents O( record. such as deeds,<br />

maps, or other sources.<br />

locators hand levef-A hand IWld type of<br />

tavel used to measure approximate<br />

ditferencee in elevation<br />

Iocklng angla-in tilt analysis of oblique<br />

photographs, the complement of the<br />

interloc+ring angle. The depression angle 01<br />

the oblique when the lilt of the WMllCal<br />

photograph is zero.<br />

Ioglcal conalatancy-(digilal mapping) The<br />

correctness 01 the relationships encoded In<br />

the data Wrmfure of Ihe daIa sel.<br />

Ioglcel contouring—A procedure, based on<br />

the Iacta that contours are spaced equally<br />

along a untform slope, which permits the<br />

sketching of contours from field notes with<br />

considerable ascuracy arrd without Ihe<br />

need of running a ievel line for every<br />

mntour. Contour lines are interpolated by<br />

spaciW them proportionately between spot<br />

elevations established af every poinl where<br />

there is a change in slope.<br />

lonQ chord+ roule surveying) On a Simple<br />

wrve, the chord, or straight line, that<br />

extends from me poin\ of curvature to the<br />

poirrf ot Iangerwy; on a compound curve,<br />

the chord Ihat extends from lhe pint of<br />

compound curvature to the point of<br />

wrvature or to the point of tangency. In a<br />

description of a circular land boundary, the<br />

iengfh arrd bearing of fhe long chord is an<br />

important factor.<br />

long Ilne ezlmuth (LOLA) surveye— A<br />

measurement by use of phoforecording<br />

thaodolites and airborne strobe lights of<br />

bng azimuth lines nol visible between<br />

ground afafions.<br />

long rud-A level rod, usually a Philadelphia<br />

md, permitting readings of 13 teet when<br />

fully extended. Also called high rod. See<br />

also ahorr rod.<br />

Iong-parlod constltuant—A tide or tidal<br />

current constituent with a period fhat IS<br />

independem of the rotation of the Earth but<br />

whfch depends upon !he orbital movement<br />

of the Moon or of the Earth. The period is<br />

146<br />

usually longer than a day and in general a<br />

halt-month or larger.<br />

Iong-period perturbations-Periodic<br />

perturbations in Ihe orbft of a plane! or<br />

satellite which require more than one orbital<br />

period to execute one completa periodic<br />

veriation.<br />

Iong-renge chaft-See long-range<br />

navlgallon chart.<br />

long-range navigation chart-Any one of<br />

a series of small scale, 1:3,000,000 or<br />

smaller, aeronautical charls designed for<br />

long fllghls using dead reckoning ar’d<br />

celestial navigation as the principal means<br />

of navigation. Also called Iong-ranga<br />

chart.<br />

Iongltude difference—See departura.<br />

definition 1.<br />

Iongltude equation—A condition equation<br />

which expresses the r.elalkmshiP beween<br />

the fixed longitudes of two points which are<br />

connected by triangulation or traverse.<br />

Iangitu”de tactor—The’ “change in Iongltude<br />

along a celestial line of posilion par one<br />

minule change in latitude.<br />

Iongltuda of the Moon% nodes—The<br />

angular distances along the ecliptic of the<br />

Moon% nodes from the vemat equinox; the<br />

nodes hava a retrograde r’r’miion, and<br />

complete a cycle of 360” in approximalety<br />

19 years.<br />

Iongltude signal—A sign indicating a time<br />

event, observable al different stations, and<br />

used in comparing local times 01 those<br />

stations, end determining the dtiererrce of<br />

their longitudes.<br />

Iongltude term gravity formula—A n<br />

additional term in the formula tor theoretical<br />

gravity which expresses the variation with<br />

bngitude due to a triezial ellipsoid of<br />

reference. See afso Halmert% gravity<br />

formula of 1915.<br />

longltude—A linear or angular distame<br />

measured east or west Irom a reference<br />

meridian (usually Greenwich) on a sphere<br />

or spheroid. See also assumed<br />

longltude; asironomlc Iongltude;<br />

Celeetlal longitude; circle of


longitude; dllkversce of Iongltude;<br />

flctltloue Iongltude; galactlc<br />

longitude; geodelic Iongltude;<br />

geographic Iongltude; grid<br />

Iongltude; merldlan; oblique<br />

Ionoltude; Ierreatrlal lon~llude;<br />

traneveree longitude.<br />

Iongltudlnel chromatic aberraf ion—A n<br />

aberration which affects the sharpness of<br />

all paris of an image because different<br />

colors come to a locus at dillerent<br />

diafarrcas fromlha fens.<br />

Iongltudlnaf msgnfflcatlon—The ralio of a<br />

length inlhe Image. parallel to the axis, to<br />

a Corresponding length inlhe object.<br />

Ionglludinaf eeperetlon—Time separation,<br />

fongltudlnal fill—See pitch, definition 2,<br />

look anglea-The alevation and azimuth at<br />

which a particular satellite is predicted to be<br />

tound at a specffied lime. See also alerta,<br />

loop closur-(leveling) The ditlerence<br />

be fWJeenthe rod sum on the run OU1and<br />

the rod aumonlhe run back,<br />

loop error of closure—See error of<br />

closure, definition 5. ,<br />

loop traverse-A closed traverse that starts<br />

and ends al fhe same station. The traversa<br />

provides neffher inherent validafionot<br />

SlafliI)g posilion and azimuth, nor validation<br />

against systematic distance error, See also<br />

connecflng traverse.<br />

Lorac—Afrade name fora hyperbolic radio<br />

bcation system. [This term is derived from<br />

the words ‘long-range accuracy.”]<br />

loran charf-A plotting chart on which loran<br />

groundwave fine of positions and sky wave<br />

wrrecfkm values have been printed, for<br />

use in loran navigation.<br />

toran flnea-unes of constant time<br />

difference between signals from a master<br />

and a slave loran station,<br />

loran fabfea—Publications containing<br />

tabufardsta forconstmcling loran<br />

hyperbolic fines 01 position.<br />

MIL-HDBK-850<br />

147<br />

LORAN-C Secondary Phssaa CorrectIon<br />

Tabla-Tabufafed secondary phase<br />

corrections tor LORAN-C in a given service<br />

area lor each appropriate transmfffer pair or<br />

station. These correctbns account tor<br />

overtand radio wave phase ratardatbvr.<br />

foran-C—A long-range radio navigation<br />

pcsllfon fixing system using a cornbinaibn<br />

of time difference of reception and phase<br />

difference of signals from fwo stations to<br />

provide a fine of posll”mn.<br />

foran-(JCS) A long-range rado navigation<br />

pesition fixing system using the time<br />

ditlerenca of reception of pulse type<br />

transmissions from IWO or rrmre fixed<br />

stations. [This term is derived fmm the<br />

words ‘fang-range navigation.-]<br />

Iorhumb llna-A line along which the rates<br />

of change dl the vaiues of two families of<br />

hyperbola are constants.<br />

Iorop photography—A general term<br />

referring 10 any photographs taken with a<br />

long total length (in excess of 100 inches) -<br />

camera with a narrow-angle lens, me lerrn<br />

is derived from lhe words ‘tong-range<br />

oblique photography,-]<br />

lost corner—A corner whose position cenrml<br />

be determined, beyond raasonabie doubt,<br />

either from traces of the original marks or<br />

from acceptable evidence or testimony that<br />

bears on the original position, and whose<br />

location can be restored only by raference<br />

10 one or more interdependent comers.<br />

Lovsw tapa-A newer version of lhe Invar<br />

tape used in surveying operations. Lovar<br />

tape possesses properties and cost factors<br />

between fhal of the less acurrata steel<br />

tape and Ihe more arxurate fnvar tape.<br />

Lovar—A steel alloy having a few coefficient<br />

of expansion used in construction of<br />

precise Lovar tapes. See also fnvar.<br />

low tfde—See low water.<br />

low water (LW)—The lowest limit of tha<br />

swlace water level reached by the bwering<br />

tide. Low water is caused by tha astronomic<br />

tide-producing forces andlor the eHecfs o?<br />

meteorological conditions, Also celled low<br />

tfde.


I<br />

I<br />

!I<br />

low water datum-An approximation of the<br />

plane of mean low waler, adopted as a<br />

standard datum plane for a limited area,<br />

and retained for an Indefinite period, even<br />

Itmugh If might dltter slightly horn a bettar<br />

datermlnatlon 01 mean low waler from later<br />

obsewalions.<br />

low water tull and change-The average<br />

Interval of time between the Iransil (upper<br />

or lower) of the full or new Moon and the<br />

next low water.<br />

low water inequality-See dlurnaf<br />

Inequality.<br />

low water lfrtervel-See Iurtitldal<br />

Interval.<br />

low water llne-The line defined by the<br />

bourtdary of a body of waler al ita lowest<br />

stage (elevation). in tidal waters, ftre low<br />

water line is, strictly, the intersection of the<br />

plane of mean low waler with the shore.<br />

low water krnltldal interval-See<br />

turzltldal Interval.<br />

I<br />

low wster aprlnge datum—An<br />

approximation of the plane of mean low<br />

water Sprirros, Wad as a datum in local<br />

I<br />

araas, and ‘retained for an Indaiinile period,<br />

even thouoh It mloht differ sliohllv from a<br />

batter det


Ioxodromlc curve-See rtrumb line.<br />

lunar celestiel equator—A great circle on<br />

the celestiaf sphere in the plane of the<br />

Moon’s equator, i.e., in a plane<br />

perpendicular to the Moon’s axis of<br />

rotat ton.<br />

lunar chart-A charl showing the surlace 01<br />

the Moon.<br />

lunar cycla-Any cycle related 10 the Moon,<br />

particularly the Callippic cycle or Ihe<br />

MeIonic cycle. See also saros.<br />

lunar day—The interval between two<br />

successive upper transits of Ihe Moon over<br />

a local meridian. The period of Ihe mean<br />

lunar day, approximately 24.S4 solar hours,<br />

Is derived from the rotation of the Earth on<br />

its SXiS relative to the movement of the<br />

Moon aboul the Earth. Also called tldaf<br />

day.<br />

lunar declination—Angular distance 01 the<br />

Mcen expressed in degrees north or south<br />

of the ceieslial equator; it is indicated as<br />

posllive wnen norm. and negative when<br />

south of lhe equa!or. Also called<br />

declination of the Moon.<br />

lunar dla!ance—The angle between the line<br />

of sight toward Ihe Moon and the line o!<br />

sight toward another celestial bedy at Ihe<br />

point 01 an observer on lhe Earth.<br />

lunar aartfselde than—A chart showing<br />

that portion of lha Moon% surtace visible<br />

from” the Earlh,<br />

lunar ecllpae-The phenomenon observed<br />

when the Moon enlers Ihe shadow of the<br />

Earth. A lunar eclipse is partial if only part ot<br />

ifs surface is obscured; and tolal if the<br />

entire surface is obscured.<br />

lunar equation—A Iaclor used m reduce<br />

observatbms of celestial bodies to the<br />

barycenter of the Earlh-Moon system.<br />

lunar faralde chart-A chart showing that<br />

portion of the Moon’s surface rwt visible<br />

from the Earth.<br />

Iuner Inequellt y—1. Variation in the<br />

Moon’s motion in its orbit, due to attraction<br />

MIL-HDBK-850<br />

149<br />

by other bodies of the solar system. Sae<br />

also evectlon; parlurbatlon. 2. A<br />

rninu!e fluctuation ot a magnetic needle<br />

horn fts maan pcsltiin, caused by Ihe<br />

Moon.<br />

lunar Interval-The dltferance in lime<br />

behveen the transit of tha Moon over the<br />

Greenwich meridian and a local meridian.<br />

The lunar interval equals the diflemnce<br />

between the Greenwich and total intenfala<br />

of a tide or current phase.<br />

lunar month—See aynodlcal month.<br />

Iuna r nods-A node of the Moon’s orbii.<br />

tunar parallax—The horizontal parallax or<br />

the geocentric parallax of the Moon.<br />

lunar aatelllte-A man-made safellite that<br />

makes one or more revolutions about the<br />

Moon.<br />

Iuner tida-Thai part ot the tide caused<br />

solely by the tide-producing forces of the<br />

Moon as distinguished trom that parl<br />

caused by the tortes Of the Sun.<br />

lunar Urns-l. Time based upon the<br />

rotation of Ihe Earth relative to the Moon.<br />

2. Time on the Moon. See also<br />

Greenwich lunar time; local lunar<br />

time.<br />

lunatlon—See aynodlcal month.<br />

I u ne—Thai part ot the sutlace of a sphere<br />

bounded by halves of two great circles.<br />

lunlcentrlc—See ealenocentric.<br />

.Iu nlaolar effect—Gravitational elf acls<br />

caused by lhe a!lraction of fhe Moon and<br />

of the Sun.<br />

Iunlsolar perturbation-Perfurbafions of<br />

artificial satellite orbits due to the attractions<br />

of the Sun and the Moon. Tha mosf<br />

Imporlanl effects are secular variations in<br />

me mean anomaly, in the right ascension<br />

01 the ascanding node, and in the<br />

argument of perigee. All other orbital<br />

elements, except the mapr semiaxis,<br />

undergo long periodic changes.<br />

Iunlsolar preceaalon—lhat component ‘of


I<br />

general precession caused by the<br />

mnbined effect of the Sun and Moon on<br />

the equatorial perturbance of !he Earth,<br />

Woducing a westward rrmtion 01 the<br />

equinoxes along the ecliptic.<br />

MIL-HDBK-850<br />

Iunltldal lntenraf-The interval between the<br />

Mmn’s transit (upper or lower) over the<br />

bSal Or Greenwich rneriilan and lhe<br />

folbwing hqh or low water. The average of<br />

all hl~h water Inlervals tor all phaSeS 01 the<br />

Moon, Ihe mean high waler Iunllldal<br />

interval, is abbreviated 10 high waler<br />

intarval. SimUarly, the mean low water<br />

Iunllicfal interval is abbreviated to 10Wwater<br />

Interval. The h~h water or bw water interval<br />

is daacribed as bcal or Greenwich<br />

according to whether the reference is to the<br />

transit over ihe local or the Greenwich<br />

meridian. Also called establishment.<br />

. . .. . ,<br />

150


I<br />

I<br />

1,<br />

MAD Operrstlonal Effecflveness Charm<br />

@fOE)-Deiailed information on geomagnetic<br />

fiald Intensftlea In ocean areas, Used in plannlng<br />

tactical AntiSubmarine Watfare (ASW)<br />

oparallons. Magnetic anomalies are color coded<br />

to assist in setting sensitivity on Magnatic<br />

Anomafy Detaction (MAD) equipment.<br />

MAD Plannlrrg Charta (MADPC)—<br />

Intormatlon on geomagnetic total-field<br />

Intenaffkrs for selacfed ccean areas. Used as a<br />

planning base for An!lSubmerine Warfare<br />

(ASW) op’atlons. Magnetic anomaliea are color<br />

coded to assist in datermlning the effectiveness<br />

of Magnetic Anomaly Detection (MAD)<br />

equipment for a given erea,<br />

magazine—(aerial camera) A component in<br />

the aerial camera sysfem. If serves to ho!d the<br />

exposed and unexposed film and includes the<br />

film drive mechanism and film tlanenlng device<br />

(platen).<br />

magenta contact scmcm—A contact film<br />

screen composed of msgema dyed dots 01<br />

variable density used for making hafflone<br />

negatives.<br />

msgnatic amplltude-Amplilude relative to<br />

magnetic .eaat or west. Sea also amplitude.<br />

msgnetlc annual change—The amounf of<br />

magnetic secular change undergone in 1 year.<br />

Also caflad annual change; annusl<br />

mEgnetlc change; annuel rate; annuaf<br />

rate of change. See also mag netlc<br />

sacular change.<br />

MagnOtlC annual varlatlon—The small<br />

regufar fluctuation in the Earth’s magnetism,<br />

havfng a perbd of 1 year.<br />

. .<br />

magnsmc varlatlon.<br />

Also called annual<br />

mrrgnatlc anomaly-See local magneilc<br />

anomaly.<br />

magnatlc azimuth—At the point of<br />

obsewafion, the angle between the vertical<br />

ptene through the observed objecf and the<br />

vertical plane In which a traely suapanded,<br />

SymfnStfiCally magnetized needle, influenced by<br />

no tranSleM arltficisl magnetic disturbance, will<br />

come 10 rest. Magnalic azimuth is generally<br />

MI L-H DBK-850<br />

151<br />

M<br />

reckoned from megnalw ncrlh (O”) clockwise<br />

through 360”, Such an azinufh shoufd be<br />

marked as being magnetic, and the date of ifs<br />

appfiiability should be given. Magnetk ezlrrwfhs<br />

are frequently measured wffh two Wlfd T-O<br />

Iheodolites in rxmnactiin with compass rose<br />

surveys.<br />

magnetic bearing-l. (navigation) Bearing<br />

relative 10 magnetic north: mmpaaa bearing<br />

correcfed for deviafbn. 2. (swwaylrsg) Bearing<br />

relative 10 magnefic north or south, and staled<br />

in an east or weat dtrectbn. The compasses<br />

included with the engineer transit and the 1minute<br />

theodolite can be used fo read magnetic<br />

bearings. Also called compass baarlng.<br />

magnetic chart-A speciaf purpose map<br />

depicting the dislributbn of one ot the magnalic<br />

elements, as by bogonlc lines, or of fts secular<br />

change.<br />

magnetic compasa—A compass depending<br />

upon the anraction of Ihe magnelism of the<br />

Earth for its directive tome.<br />

msgnetlc dally veriaUon-The transient<br />

change in the Earth% magnetic Iiekd associated<br />

with the apparenf daily motions of the Sun and<br />

Moon. In most places the solar dally variation<br />

follows approximately a consisfenf pattern,<br />

affbough with appreciable and unprediiabfe<br />

changes in form and amplitude.<br />

magnatlc declination-(JCS) The angle<br />

between fhe magnetic arnj geograpfskef<br />

meridians at any place, axpressed in degrees<br />

east or west to indicate Ihe dlrectbn OJmagnetic<br />

noflh from true nonh. In naufkal and<br />

aeronautkal navlgaflon the term msgnetlc<br />

variation Is used instead of magnatlc<br />

decllnaflon, and Ihe angfe is termed<br />

varlatlon 01 the compass or megnetlc<br />

varlatlon. Magnetic decfinatlon Is not<br />

otherwise synonymous with magnetic variation,<br />

which refars to regular or irmgufar change with<br />

lime of the magnefic declination, dip, or<br />

intensify. [Because of bcal attraction, Ihe<br />

magnetic declination of two close fXJnt6 may<br />

differ by severaf degrees.] See also Magnetic<br />

varlatlon.<br />

Imagnetfc<br />

devlatlon—See Oevlatlon.


magnetic dlp circle-An instrument for<br />

measuring the magnetic dip by the use of a<br />

needle and a graduated vertical circle.<br />

magnetb dip needle-l. A dip circle or the<br />

needle thereof. Also called dlp needle. 2. A<br />

needle arranged 10 diacbae an intense bcal<br />

arvxnsfy of the magnetic d!p am useful In the<br />

recovery of lost iron survey monuments.<br />

megnetlc dip-see dip, definition 2.<br />

magnetic dlracflon-Horizontal direction<br />

exprassed as angular distance from magneliC<br />

norih.<br />

MIL-HDBK-850<br />

magnetic disturbance-1. Irregular, large<br />

ampliiude, rapid time changes ot the Earth’s<br />

magnetic field which occur at approximately Iha<br />

same lime all over the Earth. Also called<br />

magnatlc storm. 2. Sometimes used 10<br />

dascrlbe spalial changes in tha Earths magnetic<br />

field. See also local magnellc anomaly.<br />

magnellc diurnal variation—l. The daily<br />

variation. 2. The rrlmple harmonic component<br />

of the daily varial~on having a period ot 2.4<br />

hours.<br />

msrgnetlc elemanta—The declination, lhe<br />

horizontal Intensity, the vertical intensity, the<br />

total intensity, tha inclination or dip, tha strength<br />

of Ihe force toward geographic north, and the<br />

ahength of the force toward geographic east.<br />

magnallc equator-(JCS) A line drawn on a<br />

map or chart connecting all points al which the<br />

magnetii InclinWlon (dip) is zero for a specilied<br />

epoch. Also called eclhrlc Ilna; dlp equator.<br />

See also geo-magnetic equator.<br />

magnetic flald lntanally—The magnetic<br />

force exerted on an imaginary unit magnetic<br />

pole placed at any spacifled point of space. II is<br />

a vector quantity. Its direction is taken as tha<br />

direction toward which a north magnelic pole<br />

would tend to rrswe under lhe inlfuence of the<br />

field. Alao called magnetic flald; magnetic<br />

field atrangth; magnetic force; magnetk<br />

Intanslty.<br />

magnatlc field strength-See magnetic<br />

field Intensity .<br />

magnstlc field-See magnatlc field<br />

Intanalty.<br />

152<br />

magnetic force—Sae magnellc field<br />

Intenalty.<br />

magnetic lncllnallon—Saa dip, definition 2.<br />

magnetic lntenalty—Sae magnetic field<br />

Intanalty.<br />

magnatic Iaoporlc llrte-Sea Ieopor.<br />

magnetic latltuda—Saa dip, definition 2.<br />

magnetic lines of force-imaginary lines ao<br />

drawn in a region containing a magnetic fiefd to<br />

be everywhere tangent to the magnetic fiald<br />

intensity vector if in vacuum or nonmagnetic<br />

material, or parallal to the magnelic induction<br />

vector il in a magnetic medium.<br />

magnatic lunar dally varlatlon-A periodic<br />

variation ot the Earths magnatic field that k in<br />

phase with the transit of the Moon.<br />

magnetic meridian—At any point, the<br />

direction of the horizontal component ot the<br />

Earths magnatic field. Not to be confused with<br />

geomagnetic merldlan.<br />

magnetic momenl—The quantity obtained<br />

by multiplying the distance between two<br />

magnetic poles by the average atrenglh of the<br />

poles.<br />

magnetic north-(JCS) The direction<br />

indicated by the north-seeking pola ot a freefy<br />

suspended magnetic naedle, influenced only by<br />

the Eartha magnetic field. Sae also compaaa<br />

north.<br />

magnetic observation—Measurement of<br />

any of Ihe magnetic elemants.<br />

magnetic pole-Either of the two placas on<br />

the surface of the Earth where the magnatic dlp<br />

is 90°. Nol to be contusad with geOnSt3gnatiC<br />

pola. Also called dip pole.<br />

mngnetlc prime vertlcaf-The venical circle<br />

through the magnatic easl and west poims of<br />

the horizon.<br />

magnetic aecutar Changa—lncreaea or<br />

decrease of intensity andtor change of direction<br />

ot tha EarIh’s magnetk field over a period of<br />

many years [usually given as avaraga gammas<br />

per year for Intensity values and minutes per


,<br />

1.<br />

I<br />

year for directional values].<br />

magnellc solar dally varlatlon—A periodic<br />

variation of the Earths magnetic field that is in<br />

phase with solar [bcal) lima.<br />

maonotlc atrstlon-A rnonumenled station al<br />

which a series of magnetic observations have<br />

been msda, h usually consists of a bronze<br />

marker se! in stone or concrete at which, in<br />

addition to latitude and longitude, the magnetic<br />

value Is irrdiiated.<br />

magnetic storm—Sae magnatlc<br />

dlalurbance.<br />

magnetic aurvay-A survey conducted to<br />

meaaure the strar?glh anct/or diraction of the<br />

Earth’s magnetic field al spacific poinls on or<br />

near the surface of the Earth.<br />

magnetic tape—Ferrous-coated tape,<br />

Selective polarl.zation of the suriace permits lhe<br />

sequential storage of digital data. Commonly,<br />

magnetic tape rafers to reel-to-reel tape as<br />

opposed to tapa enclosed within cartridges.<br />

magnatlc varletlon charl—A than depicting<br />

isogonk fines, or lines 01 equal magnelic<br />

declination, for a given time.<br />

magnetic varlallon—(JCS)l. In navigation,<br />

at a given place and time, the horizontal angle<br />

betwean the true corfh and magnetic north<br />

measured east or west according 10 whelher<br />

magnetic north lies east or west of true north,<br />

Also called vatlatlon. See also magnetic<br />

declination. 2. In cartography, the annual<br />

change In dlrecflon of the horizontal component<br />

of the earfha magnelic fjeld.<br />

magnatlam—The ability to attract magnetic<br />

material, notably Iron and steel. Also called<br />

terreatrlal magnetlam. See also blue<br />

magnellam; geomagnetiam; horlzontaf<br />

Intarmlty; red magnetism; vertical<br />

Intenalty.<br />

magnato-optlcaf disc—A mass storage<br />

media which cunsists of a transparent rigid<br />

substrate, which is coated with a recording layer<br />

composed of rare earth and transition metals.<br />

Wrffing isachieved by using a Iasertoraiee the<br />

tempsratureof asmallaraaof the recording<br />

layer. This terrporarily fowersthe coercivity (the<br />

strength of the magnetic state), allowing the<br />

direcfionot the magnetic field to be reversed by<br />

a small external magnetic field applied by fhe<br />

MIL-HDBK-850<br />

153<br />

drive’a magnetic head. Erasing is accomplished<br />

by the same process, except theeppliad<br />

megneticfiaJd isreveraed indirection. Reading<br />

of magneto.opticai materiat can be patlonned<br />

either magnetically or optktlfy.<br />

magnetometer sunrey-A suwey wherein<br />

the Earth’s magnetic field lsmapped by the use<br />

of a magnetometer. See also magnetic<br />

aurvay.<br />

magnatometer—An Instrument used In the<br />

smdyof geonzegnatlsm for measuring a<br />

magnetic alement. See atso flux-gate<br />

magnatomater; flux motar; nuclaar<br />

praceselon magnetometer; optical<br />

pumping magnetometer; theodo.<br />

Iltefmagnetometer; varlometer.<br />

magnification-(optics) The ratio of the size<br />

of an object to the size of ifs magnified image.<br />

Also called power of a lens. See also<br />

angular magnlflcatlon; dlopter; letWfSl<br />

magnlflcatlon; Iktear magnification;<br />

Iongltudlnal magnitlcatlon;<br />

unldlmenalonal magnification.<br />

magnltylrrg power—The ratio of lhe apparent<br />

length of a linear dimensional seen through an<br />

optical instrument, and by the unaided eye.<br />

Thus, an instrument witha magnify ing power of<br />

three makes anobjecf appear lhrea timasas<br />

high and three times aswida. Alac called<br />

dlamatar. See also dlopter.<br />

magnitude—l. Relative brightness of a<br />

celestial body. Also called stellar magrsltuda.<br />

2. The intensity of a shorf-parbd magnetic<br />

Fluctuation, usuafy expressed in milfigausaesor<br />

gammas. 3. Relating to amount, aize, or<br />

greatness.<br />

mehr scheme slatlon—A station through<br />

whfch the main computations and adjustments<br />

of thesurvay data arecarried andserve for the<br />

continued extansionof the survey. Also cslled<br />

primary station; prlnclpal atatlon.<br />

malntalnablllty —Tha capacity for making<br />

updates in an efficiant and cast-affetilve<br />

manner to a data base or software.<br />

major axla-The longest diameter ot an<br />

ellipse or ellipsold.<br />

major datum—See preferred datum.<br />

major grid—The primary grid or grids on a


I<br />

,<br />

maporchafl. See also overlapping grid;<br />

secondary grid.<br />

major planet&The tour largest pianels;<br />

Jupffer, Saturn, Uranus, and Neptune. Also<br />

called giant planata. See also asteroid;<br />

Inner planeta; outer planata.<br />

make llna-An accurately scaled line denoting<br />

thesiza lowhlch origlnalcopy is to be enlarged<br />

or reduced. Also called make size. See also<br />

scale of reproduction.<br />

make ready-The adjustment of feeder,<br />

grippers, aida guide, pressure behvean plate<br />

and bfankat cyflnder, impression plate, and ink<br />

fountain prior toa press run.<br />

make size-.see make Ilne.<br />

man.mada faaturea—Sea culture.<br />

manauverlng board—A polar coordinate<br />

pbffingshaet devised to facilitate solution of<br />

proble-ms involving relative movement.<br />

manually dlpltlzed—The process of<br />

convetilng an analog map or o!her grap~lc<br />

overlay into numeric Iormal with the use 0: a<br />

digitizing tablerfableland manually lracing the<br />

inpul wtfh a cursor.<br />

manually ancoded—The process of data<br />

input, including tabular and attribute information,<br />

info a computerawrrpalible format through the<br />

use of direct operator Interaction wilh collection<br />

arrd/or storage system peripherals.<br />

MIL-HDBK-850<br />

manuacrlpl—The original drawing of a map as<br />

compiled or Conehucted frown various data,<br />

such as ground surveys and phonograph. See<br />

also multluse manuscript.<br />

Map and Charf Data Inlarchange<br />

Format (MACDIFj-A project undertaken by<br />

the Province of Ontario, Canada, and the<br />

national governments of Canada and the USA<br />

to develop standards for format, Wucrure, and<br />

ceding of di@fal map and charf Information.<br />

MACDIF providas a coding scheme for encoding<br />

a diglfal description of map or chart data.<br />

map accuracy apaclflcatlons—<br />

Specifications which set up slandards to which<br />

the finished map must adhere. See also U.S.<br />

NaIlonal Map Accuracy Standards.<br />

154<br />

map accuracy standards—See U.S.<br />

Nallonel Map Accuracy Standarda.<br />

map adjuslmant—An adjustment of the<br />

horizontal position of maps to mntrol points or<br />

10 a specific grid plotted on the map projection<br />

at compilation scale.<br />

map catafog—A publication giving both<br />

graptilcal and word descriptions of all maps.<br />

charts, and related products issued by a<br />

producing agency. U contains information such<br />

as the fine, scale, adition date, edition number,<br />

prica, and classification of all publications<br />

issued.<br />

map charf-See combat Cfrarf.<br />

map controlled—Utilization of a msp, rather<br />

than geodetic or photogrammetric data, for<br />

purposes of positioning map detail.<br />

map exchange agraament—An approved<br />

agreement between a United Stafes mapping<br />

organization and a foreign mapping<br />

organization to furnish each olher specified<br />

mapping, chariing, and geodetic dale as<br />

published, or on a request basis. See also<br />

cooperatlvs mapplrw agreement.<br />

mep index—(JCS) Graphic key primarily<br />

designed to give the relafionshtp between<br />

sheets of a series, their coverage, availability,<br />

and W’ther information on the series. SaO ako<br />

map.<br />

map matching guidance-The guidance of<br />

a rocket or aerodynamic vehicle by means of a<br />

radarscope film previously obtained by a<br />

reconnaissance flight over the terrain of the<br />

route or from a radar simulation system. snd<br />

used to direct the vehicle by afiining ifaeff wifh<br />

radar echoes received during flight from Ihe<br />

terrain below. See also stellar map<br />

matching.<br />

map matchlna—The simultaneous electronic<br />

or mechanical optical scanning of an observed<br />

map imacje obtained fmm a space vehicle, and<br />

a reference map image, while the reference<br />

msp image Is beina oriented and scaled until a<br />

close comparison between the hvo is found. An<br />

inspection of the scale and oriantatlon of the<br />

reference map indicates the position of the<br />

vehicle. See also rmlaa Doppler maP<br />

matching. “


map nadir—Point on a map or manuscript<br />

vertically beneath the perspective center of the<br />

camera lens al the instant of exposure.<br />

map of standard format—A map with<br />

dimensions, iayout, Iettaring, and symbolization<br />

In accorUanca with the epacificaliorss tOr the<br />

sartas.<br />

map paraflal—See axla of nomology.<br />

map point—A supplemental conlrol poinl<br />

whosa horizontal position can be obtained by<br />

scaling Ihe coordinates from a map or chart on<br />

which the point can be identified.<br />

map projection—An orderly system of lines<br />

on a plane representing a corresponding syslem<br />

of imaginaw lines on an adopled terrestrial<br />

datum eurlace. A map projection may ba<br />

derived by geometrical mnstrucfion or by<br />

mathematical analysis. See also Altoff equelaraa<br />

map projection; Altsers conical<br />

aqual-map projection; aphylactlc map<br />

pro]action; arsthallc map projection;<br />

azimuthal aquidletaru map projecIlon;<br />

azimuthal map projection; Bonne mep<br />

.projaction; Casalnl map projection;<br />

Caaslni.Soldner map projection;<br />

cortformal map pro)ectton; conic mep<br />

pro]actlon; conic map projection wllh<br />

two ●tanderd pareilels; cylindrical equelaraa<br />

map projection; cylindrical equalspacad<br />

map projactlon; cylindrical map<br />

projactlon; doubly azimuthal map<br />

projection; aqual-araa map projection;<br />

equatorial map projection; globular map<br />

projection; gnomonlc map projection;<br />

Goods’a Interrupted Itomoloelna<br />

projection; Hammer projection;<br />

homalographlc map projection;<br />

interrupted map projactlon; Laborde<br />

map projection; Lambert azimuthal<br />

polar map projection; Lembsrf central<br />

aqulvaient map projection upon the<br />

plana of tha meridian; Lambart<br />

conformal conic map projactlon;<br />

Lamban zanithal aquai-araa map<br />

projactlon; Marcator map projactlon;<br />

meridional orthographic map projection;<br />

modlflacl Lamberr Conformal map<br />

projection; modiflsd polyconlc map<br />

projection; Mollweida homalographic<br />

map projection; nonparapectlve<br />

azlmulhal map projection; oblique map<br />

projection; obliqua Mercator map<br />

projection; orfhambadlc map projection;<br />

MIL-HDBK-850<br />

155<br />

orfhographlc map projactlon;<br />

perapactlva map projactlon; parapecllve<br />

map projection upon a Iangant cyllnttar;<br />

polar map projection; polar orfhographlc<br />

map pro}ectlon; polar ataraographlc<br />

map projection; polyconic map<br />

projection; polyhadrlc projection;<br />

rectangular map projection; rectangular<br />

polyconlc map projection; ●lmple conic<br />

map projection: alnuaoldal map<br />

projection; skewed map projection;<br />

ateraographlc horizon map Prolactlon;<br />

staraographlc map projactlon;<br />

atereographlc meridional map<br />

projection; traneveraa map pro)ectlon;<br />

trenaverae Marcator map projection;<br />

tranavarea polyconlc map projactlon;<br />

Warnar map projection.<br />

map reference code+JCS) A code used<br />

primarily for encoding grid caordinatas and othar<br />

information parlalning to maps. This cods may<br />

be used for other purposes whan the ancryptkm<br />

of numerals is raquired.<br />

map revlslon—See raviaion.<br />

map scale—Sae scale, definition 1.<br />

mep series-(JCS) A group of maps or charts<br />

usually having the same scale and cartographic<br />

specifications, and with each sheet appropriately<br />

iden!ifisd by producing agency as belonging to<br />

the same aerias. Also called eerlea.<br />

map sheet—(JCS) An individual map or chart,<br />

either complete in ttself or part of a serias. Also<br />

called aerles.<br />

map atrbefltuIe-A hasty reproduction of<br />

aerial photographs, photomaps, or mosaics, or<br />

of provisional maps, or any Othar P~U~ used<br />

in place of a map, when the precisa<br />

requirements of a map cannot be met.<br />

map teat—The accuracy of topographic<br />

mapping can be tesled by running Iravema and<br />

level lines across selectad areas 01 any map<br />

sheet, and comparing geographic pOMiOna Of<br />

map features with those determined by travaraa<br />

end comparing interpolated elevations ot points<br />

Irom the map with thosa determined by tha Iaval<br />

line.<br />

map-controlled moaalc—A tecfsnique of<br />

constructing mosaics by using topographic<br />

maps as the basis for comrol and orientation<br />

purpxes. The method may be ueed in


I<br />

I<br />

preparing both controlled and semicontrolled<br />

mosaics although Ifs use is preferred with Ihe<br />

latter.<br />

MapGrafix-A vector, Macintosh-based<br />

9eoOraPtic infOM’IaliOn system developed by<br />

ComGrafix, Inc.<br />

Maplnfo-A vector, personal computer based<br />

geographic Information system developed by<br />

MapInfo Corporation.<br />

mepping cemera—A camera specially<br />

designed for oceans. The production of<br />

photographs to be used in mapping. The<br />

modifier mapping or surveying indicates that<br />

the camera is equipped with mechanisms to<br />

maintain and to inclcate me Imerior orientation<br />

of the photographs with sufficient accuracy for<br />

mSp@W pummsea. A mapping camera may be<br />

an aerial mapping ~mera or terrestrial mapping<br />

camera. Also called euweylng camera.<br />

mapping photography—Aerial phonography<br />

obtained by precisely calibrated mapping<br />

cameraa and conforming to mapping<br />

specifications, as distinguished from aerial<br />

photography tor other purposes, Also called<br />

aerial cartographic photography;<br />

canographlc photography; Chat’flng<br />

photography; auwey photography.<br />

ITIapplnQ, charslng, and geodesy<br />

(MC& G)—MC&G comprises the collection,<br />

Iransronnation, generation, dissemination, and<br />

storing of geodetic, geomagnetic, gravimelric,<br />

aeronautical, topographic, hydrographic,<br />

cultural, aml Ioponymic data. These data may<br />

ba used for military planning, training, and<br />

operations inciudrng aeronautical, nautical, and<br />

land navigation, as well as for weapon<br />

orianfation and target positioning. MC&G alao<br />

includes the evaluation of topographic,<br />

hydrography, or aeronautical features ior their<br />

aftad on military oparatione or intelligence. The<br />

data may be presarrfed In the rorm of<br />

topographic, planimetric, reliet, of thematic<br />

maps and graphics} nautical and aeronautical<br />

charla and pwblicatlons; and in simulated,<br />

pholographlc, digital, or computerized Iormats.<br />

map-1. (JCS) A graphic representation,<br />

usually on a plane sutiace and al an<br />

established scale of natural and artificial<br />

features on the surface of a part or the whole ot<br />

the Earth or other planetary body. The features<br />

are posffioned relative to a coordinate reference<br />

system. 2. To prepare a map or engage in a<br />

MIL-HDBK-850<br />

156<br />

mapping operation. See also admlnlatrellve<br />

map; base map; battle map; boundary<br />

map; cadaatral map; choraogrephlc<br />

map; compiled map; contour map;<br />

controlled map; county map;<br />

dlstrlbutlon map; domeatlc map;<br />

englnaerlng map; axparlmental map;<br />

tllght map; flood control map;<br />

tluoraacant map; foreawy map; general<br />

map; general-purpose map; gaologlcal<br />

map; gravlmatrlc map; gravity ●nomaly<br />

map; hemlapherlcal map; hypaographlc<br />

map (or chart); Iandacapa map; larg.S<br />

scale map; Ilne-route map; medlumacale<br />

map; morphographlc map; natlva<br />

map; operation map; orftrophotomap;<br />

orthoplctomap; OUtllne map;<br />

photocontour map; photorevlsad snap;<br />

photocontrol index map;<br />

photogmmmetrlc map; photomap;<br />

physlographlc plclorial map; plCtOgraM;<br />

plctomap; planetabla map; planlmatrlc<br />

baea map; planlmatrlc map; plannlng<br />

map; plaatic raliaf map; port plan;<br />

provisional map; quadrangle; radar<br />

Intelllgenca map; radar map;<br />

reconnalaaanca map; red Ilght readabla<br />

map: rellef modal: road map; routs<br />

map; shaded-relief map; sltuatlon map; ‘.<br />

sketch map; small-scale map; source<br />

map; rxpeclai-purpose map; apeclal )obcover<br />

map; standard accuracy map;<br />

standard content map; atate baae map:<br />

atrataglc map; Tactical Commandara’<br />

Terrain Analyals; tactical map; tOpICal<br />

map; topograpttlc map; Topographic<br />

Map of fha United States; traffic<br />

circulation map; wall map; waather<br />

map.<br />

Marcfr equinox—See vernal aqulnox.<br />

margin data—See marginal data.<br />

margin lntormatlon—Sea marghtal data.<br />

merglnal data-(JCS) All explanatory<br />

inlormalion given in the margin of a map or<br />

chafl which clarifies, defines, illustrates, antior<br />

supplements the graphic portion ot the shaat.<br />

Also called border data: bordar<br />

information; margin Information.<br />

margin—(JCS) In cartography, the area of a<br />

map or chart iylng outside the border.<br />

marine map—See hydrographlc chart.


I<br />

. . ... .<br />

MARK 90-MARK 90 is the second of two<br />

development phases of the Defense Mapping<br />

Agemy’s Oigital Production System (DPS). Its<br />

mission is 10 provide DMA with end-to-end<br />

softcopy production capabilities. MARK 90<br />

Imorporafes the Data Integration. Source<br />

‘ A@isiiion, Hardcopy Exploitation, and the<br />

Universal Rectifier Seaments 0! the MARK 85<br />

.-.<br />

Dhase with new Production hfanagemenl, Data<br />

servicas, Source Preparation, Dali Eslracfion,<br />

and Product Generation Segments. See also<br />

Dlgltel Production Syalem; MARK 85.<br />

mark—1. A call used when simultaneous<br />

observations are being made, to indicate to the<br />

second person the moment a reading is 10 be<br />

made, as when the time of a celestial<br />

observation is to be noted: or the momen! a<br />

readrng is a prescribed value. 2. (suweying) A<br />

dafinile object, such as an imprinted metal disk,<br />

used to d8signale a survey poinl and<br />

SOtI’IelhSteSrefers to the enlire suwey<br />

rnanumanl. Mark is used with a qualifying Ierm<br />

such as station. ralerenca, or bench. See<br />

a150 bench mark; reference mark; atatlon<br />

mark; wltnees mark. 3. (phologrammelry)<br />

See !Joallng mark; Index mark.<br />

MIL-HDBK-850<br />

maps lo obtain more accurate register of<br />

marine sextant—A sextant designed primarily preprinted line wO* to the IandfO_ Of the<br />

for marine navigation. .._ “.. –..<br />

mokf. BY maskirm. differanlial haa!ina is<br />

achieve~. Also ~lled screen Ing. -<br />

marine smrrvey-See oceanographic<br />

survey.<br />

maak—1. In pholomechanisal processing, to<br />

block out an area by means of actinically<br />

MARK 85- MARK 85 Is the first of two<br />

opaque material, to prevent exposure in the parf<br />

development phases of the Defense Mapping blocked out. Also, the cavaring material tfseif<br />

Agen@s Digital Production System (DPS). Ifs when ao appfied. 2. A clear stable baaa plastic,<br />

mission was to improve hardcopy production coaled with an opaque stratum which can be<br />

methods, generate improved production<br />

paeled oft bafween Photographkslly etched<br />

management and dala base management outline Images, thus Lrroduclng an open-window<br />

s.apeblliiies, and provide initial soflcopy<br />

nagalive of the dasired area. This process of<br />

production capability. The six segments include: masking is offen identified by the trade name of<br />

Hardcopy Exploitation (HELS), Source<br />

the material used. 3, A continuous tone pdtive<br />

Acquisition (SA6), Data Integration (C)KS), or negative made lmm an orighal negative or<br />

Feature Exfract”krn (FE/S), Universal Rectifier positive for tha purpose of afrering the image<br />

(UR/S), ana Digital Comparator (DC/S). See produced from the orighal. Used to aller<br />

also Dlgltal Production System; MARK contrast, correct color portrayal. or praduca<br />

90.<br />

pictotone or picfofine imagas.<br />

Maraden charl-A chart showing the<br />

distribution of meleorolooical data, especially<br />

over fhe oceans. -<br />

masa attraction vertical-The normal to<br />

any surlace of constant geopatential. On the<br />

Earlh this vertical is a function only of the<br />

distribution of the mass and is unatfecfed by<br />

forces resulling from the molions of the Eatih;<br />

e.g., the dkreclion 01 a plumb bob cm a<br />

nonrotating Earih.<br />

master film poaltlve-A pasilive made trom<br />

an original negative for the purpose o! making<br />

additional negatives.<br />

master gfass negative—See calibration<br />

plate.<br />

master model—The developed original terrain<br />

model which bears, in miniature, the same<br />

spatial relationships as the actual ground it<br />

represents. Also called orlghsal modal.<br />

masfsr plot+JCS) A portion of a map or<br />

ovarlay on which are drawn the outlines of tha<br />

araas covared by an air photographic Sorlia.<br />

Latitude and longitude, and map and aonie<br />

information ere shown,<br />

master print—( mosaicking) A photograph<br />

which is reoresenlative of the mosaic araa usad<br />

as a guide “during the developing Process to<br />

insure -. the tonal match of subsaauem Orinta.<br />

mestar projectlo*The originally computed<br />

maaklng paper—See ~oldenrod paper. and constructed map prajacfion lmm which<br />

copies are made: one such projectbn serves as<br />

maeklng—A means of controlling plastic the masler for copies circling the globe whhln<br />

expansion locally during Iormlng of plastic reliaf tha same saf of standard parallels.<br />

157


1<br />

1<br />

,<br />

,<br />

I<br />

I<br />

maefer etatlon-Thai station in a given<br />

system of transmitting stations that controls the<br />

transmissions of the other stations (the slave<br />

stations) and maintains tha lime relationship<br />

befweenthe pulses of tha stations. Insatelliie<br />

surveys, positions can be upgraded<br />

mttsiderabfy by trenslocation. See also<br />

tranalocatlon.<br />

match Unee-tl aerfesot grease pencil lines<br />

drawn ona photograph, radiating horn the torn<br />

edges of lhe print onfolfsa adjacent areas to<br />

serve as a registration guide when laying the<br />

individual prfrrf In tha moaalc.<br />

match strlp+S.ee tlo srtrlp, detinilion 1.<br />

matching—The act by which detail or<br />

lntormalbn on the edge, or overlap araa, of a<br />

map or chart k compared, adjusted, and<br />

ccwrecled to agree wilh the exisling overlapping<br />

chart. Also called edge matching.<br />

MIL-HDBK-850<br />

matrix dam-Data which consists oi a matrix<br />

of evenly spaced rows and columns of data<br />

points. The position within the rows and columns<br />

represents the geographic position, while (he<br />

data point is the value 01 some spatial variable<br />

al Ihal posfiion., An example is DTED, which<br />

provides elevations al nominal 100 meter<br />

horizontal intervals.<br />

Snatte print—Prim made on pholographtc<br />

paper with a dull finish which Is more suitable Ior<br />

pencil or ink annotations than a gfossy print.<br />

maximum elevaflon figure—(JCS) A figure,<br />

shown in aach quadrangle bounded by ticked<br />

graficule fines on aeronautical charts, which<br />

represents the height in thousands and<br />

hundreds of feel, abova mean sea level, of the<br />

highest known natural or man-made feature in<br />

that quadrangle, plus suitable factors 10 allow for<br />

Inaccuracy and incompleteness of fhe<br />

topographical heighting information.<br />

MC&G utlllty software environment<br />

(MUSE)-Software programs which perform<br />

general purpose operations on Mapping,<br />

Charting & Geodetic (MC&G) data that are<br />

applicable to a broad range of eys!ems and<br />

usara rather than a single, special purpose.<br />

Some examples Includa datum and projection<br />

transformafkxrs, coordinate conversions, and<br />

symbol libraries.<br />

mean anomaly—See anomaly, definition 3.<br />

158<br />

mean center of Moors-1. A central point<br />

for a lunar coordinate system. 2. The pint on<br />

the lunar surface intersected by the lunar radius<br />

that is directed toward the Earths tamer when<br />

the Moon is al the mean ascendiW node and<br />

when the node coincides with the mean perigee<br />

or mean apogee.<br />

mean charf-Any chart on which Ieopleths of<br />

the maan vaiua 01 a given oceartogrephk<br />

element ara drawn. Also called mean map.<br />

maan deviation—See averaoe devlallon.<br />

maan dlatance—See aemlmajor axla.<br />

mean dlurnel high water Inequalliy<br />

(DHQ)—Half the average dflerence between<br />

the heights of the two high watara of each tidal<br />

day over a 19-year pariod, or a computed<br />

equivalent period, obtained by subtracting the<br />

maan of all high waters from the mean of the<br />

higher high wafers.<br />

mean diurnal fow water Inequellty<br />

(DLO)—Hail the average difference between<br />

the heights of the two low waters of each t’kfal<br />

day over a 19-year perbd~or a computed<br />

equivalent period, obtained try aubtracfkrg tha<br />

mean 01 Ihe lower bw waters from the mean 01<br />

all low waters.<br />

mean equinox of date—See mean<br />

equinox.<br />

mean equinox—A fictitious equinox whose<br />

poailion is thal of the vernal equinox at a<br />

particular date with the effect of nutafiin<br />

removed. Also called mean equinox of<br />

date.<br />

mean error—The algabraic maan of all errors<br />

derived by comparing observed or computed<br />

quantifies wilh all fixed values of common<br />

dimensional parameters in an integral<br />

observation system or mmputalion modef, A<br />

mean error


I<br />

of the terrain above mean sea level of an area<br />

to be photographed.<br />

mean high water (MHW)—Tfre average<br />

height of all the high walers recorded over a 19year<br />

period, or a computed equivalent period.<br />

mean high weter Iurmldal interval-S 88<br />

Iunltldal Inlewal.<br />

maan high water springs (MHWS)— The<br />

average height of all high walers recorded<br />

during syzygy over a 19.year period, or a<br />

mmmled equlvalant period, Also called hlgn<br />

water aprlngs.<br />

mean higher high waler (MHHW)—The<br />

average height of st! lhe daily higher high walera<br />

recorded over a 19-year period or a computed<br />

equivslenr period. It is usually associated with a<br />

tide exhibffhrg mixed characteristics.<br />

mean hlghar high water eprlngs<br />

(MHHWS)—The average height of all higher<br />

high walers recorded during syzygy over a 19year<br />

perbd, or a mmpuled equivalent period.<br />

mean low water (MLW)—The average<br />

height ot all low waters recorded over a 19-year<br />

period, or a computed equivalent period.<br />

mean low water Iunltldal Interval—See<br />

Iunltldal Interval.<br />

maan low water eprlngs (MLWS)—The<br />

average height of all low waters recorded during<br />

SYZY9Y over a 19-yeer Period. or a comPuled<br />

equivalent period.<br />

mean lower low water (MLLW)—T he<br />

average height of all the fewer low waters<br />

remrdad over a 19-year period, or a computed<br />

equivalent period. It is usually associated wilh a<br />

tide exhlbffing mixed characteristics.<br />

maan lower tow wster springs<br />

(MLLWS)—The average heighl of all lower low<br />

watem recorded duffng syzygy over a 19-year<br />

perbd, or a computed equivalent period.<br />

mean map—See mean chart.<br />

mean of tha errors—The average value of a<br />

set of errors.<br />

mean place—See mean posltlon.<br />

MIL-HDBK-850<br />

159<br />

mean poeltion—The position of a afar<br />

mrrected for sacular variations including pruper<br />

motion, bul unmrrec!ed for short term<br />

variations. AISO calied meen piaca.<br />

mean ranga (Mn)-Tha difference in height<br />

balween mean h~h water and mean low water,<br />

measured in feat or meters.<br />

mean refraction—The refraction effect on<br />

vartical engles given usually in the plane of a<br />

vertical circle for average condkiins 01<br />

temperature and barometric preaaure.<br />

mean rivar level-The average height ot the<br />

sutiace 01 a river at any poinf for all stages of<br />

the tide over a 19-year period, or a mmpufed<br />

equivalent period, usually determined from<br />

hourly height readings. Unusual variations 01<br />

river level due to discharge or N@f may be<br />

excluded in computation,<br />

mean sea level (MSL)—[JCS) The average<br />

height of the surfsce ot the sea for all stagas of<br />

the tide, used ae a reference tor elavationa.<br />

[Usually determined by averaging height<br />

leadings observad hourly over a minimum<br />

period ot 19 yaars.] Aiso tailed sea level<br />

datum.<br />

mesn sidereal flm~Sidereal time adjusted<br />

for nutalion, 10 eliminate slight irregularities in<br />

the rate.<br />

meen solar day—The interval of Ilme from a<br />

transit ot the mean sun across a given meridisn<br />

to its nexl successive transit acrosa the same<br />

meridian.<br />

maan solar tima—Time measured by the<br />

diurnal molion of a fictitious body, termed the<br />

mean eun, which is supposed to move<br />

uniformly in the celaatial equator, completing the<br />

circuit in 1 tropical year. The mean sun may be<br />

considered as moving in ihe celestial equator<br />

and having a righi ascension equal 10 !he mean<br />

celeslial longitude of the true sun. Also called<br />

meen flme.<br />

mean ephere depth—Tha uniform depth 10<br />

which the water would covar the Earth ii the<br />

solid aurfacea were smoothed off and were<br />

parallel 10 the surface of the geoid.<br />

mean equare error—The quantity whose<br />

sauara is eaual to the sum ot Ihe sauares of lhe<br />

individual e;rors divided by the numtkr of thosa


I<br />

I<br />

I<br />

I<br />

errore.<br />

mean sum--see flctltlous sun.<br />

mean tide level (MTL)-The reference<br />

plane midway between mean high wafer and<br />

mean bw water. Also called half tide level;<br />

ordlne~ tide level.<br />

mean time-see mean solar ilme.<br />

MIL-HDBK-850<br />

meender corner—A corner eslablishedat the<br />

infersecfionot standard, township, orsecfion<br />

Iineswifhtha maanclar line near banksol<br />

navigable straams or any meanderable body of<br />

water.<br />

meander llna—A traverse of the margin of a<br />

parmsnenf natural body of waler, along Ihe<br />

locus of the bank or shoreline at the elevation of<br />

maan or ordinary high watar, upon which bank<br />

or shoreline a riparian right may be predicated,<br />

measured ang le—An angle as read directly<br />

from an Instrumental observation and without<br />

any application of corrections for focal<br />

conditions. A measurad angle which has been<br />

wrrecfed for local conditions only at the point of<br />

observation is considered as an obsemed angle.<br />

mechanical arm templet—See spider<br />

templet.<br />

mechanical-tampfet plot—See<br />

mechan\cel.temp\et triangulation.<br />

mechanical-temfslet trlanoulatlon—A<br />

graphkal radtal triangulation u~ng slotted,<br />

spider, or any form of mechanical templel. Also<br />

called machanlcal-templet plot.<br />

mechanical-templet—Any templel which is<br />

manipulated and adjusted mechanically In<br />

laying out a radial triangulafiin,<br />

madlum.scale map-(JCS) A map having a<br />

scale larger than 1:600,000 and smaller than<br />

1:75,000. See stlao map.<br />

megabyte (MB)—A unit of memory. One<br />

megabyte equale 1,04S,576 bytes or<br />

approximately one million byfes.<br />

mamorlal—A durable article deposited in the<br />

ground at the position of a corner 10 perpetuate<br />

that position should the rnonumenl be removed<br />

or destroyed. The memorial is usually deposited<br />

160<br />

al Ihe base of the monumem and may cortsisf<br />

of anything durable such as glass or storwware,<br />

a marked stone, charred stake, or a quantify of<br />

charcoal.<br />

Mendenhall pendulum—An hrvariabla<br />

pendulum, one-quarter meter in length, with a<br />

vibration period of one-half second, composed<br />

of a Ienticular-shaped bob on a thin atam,<br />

swung in an airiight casa from whch the air haa<br />

been largely exhausted.<br />

menauratlon—1. The act, procaas, or arf of<br />

meaauring. 2. That branch of mathematics<br />

dealing with the determination of Iangfh, area,<br />

or volume,<br />

Mercator bearing—See rhumb baarlng.<br />

Mercator charr-A charr on the Mercator<br />

projection. This Is the charl commonly used for<br />

marine navigation, Also called equatorial<br />

cylindrical orfnomorphic chars.<br />

Mercator dlrecflon-Horizontal direction of a<br />

rhumb line, expressed as angular sfkstarwe from<br />

a relerence direction. Also ca}led rhumb<br />

dlrecllon.,<br />

Mercator equal-araa map pro)ectlon-<br />

See sinusoidal map projacflon.<br />

Marcalor map projection—A conformal<br />

map projection of the cylindrical type. Tha<br />

Equator is represented by a stra”ghf line true to<br />

scale; the geographic meridiana are represent ad<br />

by parallel straight Iinespwperdicmlar to the fine<br />

representing the Equaloc lhey are spaced<br />

according to their distance apart at the Equator.<br />

The geographic parallels are represented by a<br />

second system of straight fines perpendkxlar to<br />

the family of lines representing tha maridiana<br />

and therelora parallel with Iha Equator.<br />

Conformality is achievad by mathematical<br />

analysis, the spacing of the parallels being<br />

incraased with increasing distance fmm Ihe<br />

Equator to conform wlfh tha expanding scale<br />

along the parallels rasuffing from the meridians<br />

being represented by parallel fines. Also called<br />

equatorial cylindrical orfhomorphlc map<br />

projection.<br />

Mercator track-See rhumb Ilne.<br />

Mercury datum—A worldwide geodafic<br />

system derived from an analysis of data from<br />

astrogeodelic, gravimetric, and salellite sources.<br />

Results of this analysis provided a best-fitting


wortd ellipsoid used in tracking Project Mercury<br />

manned apace misskms and as the relerence<br />

dafum for the efecfronic navigation syslems—<br />

Omega, ioran, and loran C. See also Fischer<br />

ellipeold of 1960.<br />

mercury barometer—A barometer in which<br />

atmospheric pressure is balanced against the<br />

weight of a column of mercury. See also<br />

aneroid barometer; cistern barometer;<br />

alphon barometer.<br />

merge-To take two or more maps or data<br />

sets and ~tne Ihem fo~elher into a single,<br />

Coharem map or dala base wilhout redundant<br />

Information.<br />

merg lng—The process of joining two or more<br />

Oveffapping data sets.<br />

marldian altltude—The altilude of a celesliel<br />

body when ii is on the celestial meridian ot the<br />

obswvar.<br />

merldlen angle difference-The dillerence<br />

between two meridian angles, particularly<br />

between Iha meridian angle of a celestial body<br />

and the value used as an argument for entering<br />

a table. Also called hour angle dlflerence.<br />

merldlan angle-Anguler distance east or<br />

west cd the bcal celestial meridian; the arc of<br />

the celestial equator, or Ihe angle al the<br />

Calestial pole, between the upper branch of Ihe<br />

Icetl celestial meridian and the hour circle of a<br />

C8fWflal body, measured eastward or westward<br />

from the focal celestial meridian lhrough 180°,<br />

and Iabelad ‘E- or “W 10 indtcale the direction<br />

of measuramant,<br />

merldlan d18tance-1. (astronomy) The hour<br />

angie of a caieslial body when Ciose 10 bul not<br />

axacrly on tha astronomic meridian. 2. (plane<br />

surveying) The perpendicular distance in a<br />

horizontal plane of a poinl from a meridian of<br />

reference. The difference of the meridian<br />

diStarSCeSOf the WTds Of a line is called the<br />

departure of the line.<br />

marldfan extanslon—That porfion of a<br />

Meridian ahown above the top construction line<br />

of a projection,<br />

meridfan Ilna-(plane surveying) The line of<br />

imeraacllon of the plane of the celestial meridian<br />

and the plane of the horizon. It is a horizontal<br />

direction usad In surveying. Ila astronomic<br />

azimuth is O“ or 180”.<br />

MIL-HDBK-1350<br />

161<br />

merldlen obaervatlon-Measurement of fhe<br />

altitude ot a celestial body on tha celeaffal<br />

meridian 01 Ihe obsewer, or the altitude so<br />

measured,<br />

merldlan paeaege—See merldlan Wanslt.<br />

meridian teleOCope-A porfebfe Instrument<br />

so designed fhat if can be used as an<br />

astronomic transft, or quickly oonverfed for use<br />

as a zenlfh faiescope.<br />

merldlan fransfr-l%a passage of a ceieetial<br />

body across a celestial rnaridan. Also called<br />

marldlan paasaga. Sea also cufmlnaflon;<br />

frenslt, definition 1.<br />

merldlan-A north-south referanc.a line,<br />

parficuiariy a greal circle through fhe<br />

geographical poles ot the Earlh, horn whch<br />

longitudes and azimuths are determined; or a<br />

plane, normal to the gaoid or spheroid, defining<br />

such a line. Sae aiso aatronomlc merldlan;<br />

auxiliary guide meridian; celestial<br />

meridian; cantral merldlan; convergence<br />

ot marldians; doubla meridien distance;<br />

ecllptlc merldlan; fictt!lous merldlan; .<br />

geodetic merldlen; gaographfc<br />

meridian; geomagnetic marldian;<br />

Greenwich meridian; grid merldlarr;<br />

grslde meridien; gyro merldien; IoCai<br />

merldlan; magnetic meridian; meridional<br />

difference; marldlonal part; meridional<br />

plane; obliqua meridian; photograph<br />

merldlan; prime fictitious meridian;<br />

prime grid meridian; prima meridlen;<br />

prime obiique merldlan; prime<br />

tranaverae marldlan; prlnclpal meridian;<br />

standard marldian; table of merldlonel<br />

parts; time meridlen; transverse<br />

meridian; true meridian.<br />

meridional difference-The difference<br />

belween the meridional perfa of any We gfvan<br />

parailels. This differeme is tound by subtraction<br />

if the two parallels are on the same aide of the<br />

Equator, and by addition if on opposite aidea.<br />

marldional dlsfanca-The dislance between<br />

latitude iines as determined from the mid-<br />

Iatilude of a map projection.<br />

meridional intervai—Tha valua of the<br />

dislance between meridians of a projacfion al<br />

chart scaie.<br />

meridional of fssfs—Smali distances appiiad


to the lengths of meridians In order to create Ihe<br />

carves of the lop ard bottom latitudes 01 a<br />

projection.<br />

meridional orthographic mep<br />

prolecllon—A map projection having the<br />

plane of the projection parallel to the plane 01<br />

some selected meridian; the geographic<br />

parallels sutd the cenlral meridan are straight<br />

lines, the outer mertiian is a full circle, and the<br />

other meridians ara a= of ellipaea.<br />

meridional part-The length of the arc of a<br />

meridiin between the Equator and a given<br />

parallel on a Mercator chart, expressed in unitS<br />

of 1‘ of bngltuda at the Equator.<br />

merldlonel plana-Any plane containing the<br />

polar axis of the Eamt. See also astronomic<br />

merldfan plene; geodetic meridian<br />

plane.<br />

mete date basbl. Information about<br />

irrformation, e.Q. a tisf or catalog of directories.<br />

2. Information abouf data, e.g. a directory of<br />

data storage focef ione. See also Data baee<br />

and Deta dictionary.<br />

MIL-HDBK-850<br />

metedata—lmormalion about inforrnat(oh:<br />

more specifically, information about the meaning<br />

of other data.<br />

meteorological chart-Any chart showing<br />

meteorological (weather) information.<br />

meter rod—See precise Ieveflng rod.<br />

metee-and-bounda survey—A method of<br />

dascrlblng the boundaries of tracts of land by<br />

gtifng the bearing and length of each<br />

succesaiva fine. Much of the land in the<br />

nonpublic land States has been eurveyed and<br />

described by fhie method. This melhod is also<br />

used in the surveys of the public lands 10 define<br />

the boundaries of Irregular tracts, such as<br />

claims, grants, and reservations, which are nonconformable<br />

to the rectangular system of<br />

subdivleion.<br />

method of reperltlone—The determination<br />

of Ihe angle between two marks by<br />

accumulating, on fhe horizontal circle of a<br />

repeating theodolile, the sum of a series 01<br />

measurements of tha horizomal angle between<br />

the two mafia.<br />

Matonlc cycf%A period of approximately 19<br />

years, or a computed equivalent, durin9 w~ch<br />

162<br />

all phase relationships bafween Moon, Sun. and<br />

Earlh occur, and atter the lapse of which the<br />

phases of fhe Moon refurn 10 a particular date in<br />

the calendar year. Durfng any cycle, new and lull<br />

Moon will recur on approximately the same day<br />

in the calendar year.<br />

metric camera-A specially constructed end<br />

calibrated camera used to obtain geometrically<br />

accurate photographs for use In<br />

photogrammetric hwtruments.<br />

metric mapping euppon date (MMSD)-<br />

Camera model parameters which albw proper<br />

geographic positioning of features scan on<br />

image~ based on sensor position and pointing<br />

angle relative to the aarth’s geoid.<br />

metric photography—The recording of<br />

events by means of photographs, either singly<br />

or sequentially, together with appropriate<br />

coordinates, to form the basis for accurale<br />

measurements,<br />

Metrogon lens—The trade name o! a wideangle<br />

lens for aerial cameras used in mapfring,<br />

charting, and reconnaissance photography. See<br />

also trlmetrogon camera.<br />

mlcrofeafurea—Features of relief, drainage,<br />

and Iandlorms wtilch can be Idanlified on<br />

photographs, but are too small to appear on<br />

maps<br />

micrometer mathod—Tba delerminafion of<br />

the astronomic azimuth of a line by measuring<br />

indirectly with an ocular micrometer attached to<br />

a theodolite or Iransit the horizontal angle<br />

between a selecled slar at its elongation and a<br />

suitable ground mark (light) placed close to the<br />

verlical plane which passes through the star,<br />

and applying that angle to the azimuth of the<br />

star computed tor the epoch o! Ihe observation.<br />

micrometer—An auxiliary device to provide<br />

measurement of very small angles or<br />

dimensions by an insfwment such as a<br />

felescope. See also tilar micrometer; ocular<br />

micrometer: transit micrometer.<br />

mld.1atitude—1. Sea mfddle Iatltude. 2.<br />

(cartography) The one parallel that is a! the<br />

same scale as Indlcaled on a Mercator<br />

project ion.<br />

Middle ldtltude-One-half of the arithmetical<br />

sum of the latitudes of two places on the same<br />

side of the Equetor. Middle Iatltuda is labeled


I<br />

b .!.<br />

‘N” or “S” to Indicate whether it is north or south<br />

of the Equator. Aiso called mld-latltude.<br />

mlddhz crrdhtate-Tl?e distance trorn the<br />

mickile poirsl of a chord 10 the middle point 01<br />

lhe mrreaponding circuler arc,<br />

middle point (MP)-Thai point on a circular<br />

wrve which is equidistant from Ihe two ends of<br />

the curve.<br />

mlddletone-in haMtone, any neutral tone<br />

intermediate between the highlights and<br />

shadows of an ori~inaj and the resulting<br />

reproductbn. Ateo, !he tones in a reproduction<br />

between the highlights and Ihe shadows.<br />

mileage chart-A chart showing distances<br />

between various points.<br />

millta~ city map—See city products.<br />

SSZlllti3W geOgmphy—(JCS) The specialized<br />

field oi geography dealing with natural and man.<br />

made physical features Ihal may affecl lhe<br />

planning and COnducl 01 mililary operations,<br />

MIL-HDBK-850<br />

MllltItry grid reterence syslem (MGRS)—<br />

1. The alphanumeric posilion reporting system<br />

used by U.S. Military. 2.(JCS) A syslem which<br />

uses a standard-scaled @d square, based on a<br />

point of origin on e map projection of the Earths<br />

surface In an accurate and consistent manner 10<br />

permit either position referencing or Ihe<br />

~mpu!at~n Of direction and dislance between<br />

gnd positions. See also mllltary grid.<br />

mllltary grid—(JCS) Two sets 01 parallel fines<br />

Interaectisg at right angles and forming squares;<br />

tha grid is superimposed on maps, charts, and<br />

other SImllar representations of lhe Earth%<br />

auriace In an accurate and consistent manner 10<br />

permit Iderrtlficatlon of ground Iocallons with<br />

reapecf 10 other locations and Ihe computation<br />

of diection and distance 10 olher poinls. See<br />

81S0 mllltary grid reference system.<br />

Mliltnry Inetallatlon map (MIM)-D M A<br />

maps constructed rrom one or more standard<br />

series maps and overprinted with information<br />

such as fire zones. training areas and range<br />

Iaciliiles. M [Ms are constructed only for major<br />

camps, posts, and areas which are used<br />

extenaiWly for training and research. Produced<br />

at 1:50,000 acals.<br />

mlllta~ level—A compact ruggedized version<br />

of the dumpy level developed specifically for<br />

163<br />

military use. It k primarily used for thfrd-ordar<br />

levelin~, but has a samnd.order capability.<br />

m)ln.?ry stsndard (h91L.STD)-in<br />

acmrdance with the basic policy of the<br />

Department of Defansa, Defense<br />

Standardization and Spacifi@ion Program,<br />

military standards are issued Ior the<br />

comprehensive presentation of engineering<br />

praclices (including test IrSefhods), procedures,<br />

processes, codes, safety requiremema,<br />

symbols, abbreviations, nomenclatures, type<br />

designations and characteristics Ior siandard<br />

equipmams or items, either singly or In tamifies.<br />

Military standarda ara afso used fo cover overall<br />

characlaristics of famifies o! end hems or major<br />

components. These characteristics Irmlude, as<br />

applicable, envelope dimensions, performance<br />

ratings, primary structural features, and data<br />

required Ior interchangeability of components.<br />

mlllemap-A quantitative disirlbution map on<br />

which there are 1,000 dots, representing the<br />

quanlity depicted; each dol therefore represents<br />

1/1 ,000 of the Iotal, and is located as accurately<br />

as possible accordfW 10 the available evidence.<br />

mllligal—A unit of accalera!bn equal to<br />

1/1 ,000 of a gal, or 1/1 ,000 centimaler per<br />

second per second, Thk unit is usad in gravity<br />

measurements, being approximately onemilliontfl<br />

of the average gravity at fhe Earths<br />

surlace, Such maasuremenf includas the<br />

componant of camrifugal acceleration in the<br />

direction of the gravitational acceleration.<br />

milllgause-Unit 0! magnetic !orca equsl to<br />

0.001 gauss (oersled) or 100 gammas.<br />

mine eurvey-A survey to delannine the<br />

positions and dimensions 01 underground<br />

passages of a mine; also, of the natural and<br />

artificial features (surface and underground)<br />

relaling to the mine. The data include both<br />

horizontal and vertical positiorsa, lengths,<br />

directions, and slopes of tunnels; topographic<br />

and geologic characteristics of the particular<br />

vicinity; ownarshtp ot the land and ot the mine.<br />

mineral survey-A survey made to mark the<br />

iegal boundaries of mineral deposits or orebaaring<br />

formations on the pwbfic domain, whera<br />

the boundaries are 10 be determined by Ilnes<br />

other than the normal subdivision of the pubflc<br />

lands.<br />

Mlnlmelfy Redundant Topology (MINI.<br />

TOPO)—Ttre internal digital spatial data


atnxcture of lhe DMA Digital Production System.<br />

MINI-TOPO consists of two overlapping data<br />

structures: cartographic and spatial. The<br />

cartographic structure contains all attribute<br />

hdomxstbn, relatlonahlps between Iaatures and<br />

feature components, and ties to the underlying<br />

apatiil structure Ieval. The spatial structure<br />

aasocistes the cartographic !aalures 10 lheir<br />

exact geographic placement. Also known as<br />

the Mapping, Charting, & Geodesy Feature<br />

Data Exchange Structure (MCGFDES).<br />

mlnlmum bounding rectangle (MBR)—<br />

The smallest possible rectangle, with Norfh-<br />

S.oufh and Eaat-West sidas, which encloses an<br />

araa of Intaresl.<br />

minor axla—~he shortest diameter of an<br />

elfipse or alfipeoid.<br />

minor control plol—See radial<br />

trlangultstlon.<br />

mhtOr conlrol—See photogrammetrlc<br />

control.<br />

minor planets—See astaroid.<br />

minus angle—Sane ‘hirgle of “depieasion.<br />

minus declination—See decllnatlon,<br />

definition 3.<br />

mlntis sight-See foresight, definition 3,<br />

minute of standard length—The length of<br />

1 mhrute of bngilude at the Equator. The length<br />

ia variable, depandlng on the dimensions 01 the<br />

particular elfipaoid (spheroid) used as a<br />

raferance surface.<br />

mirror Image—See revened Image.<br />

mlscellaneoua Chat’t-A charf other than a<br />

regutar navigational chart; a special chart.<br />

mismatch—A condition which occurs when<br />

detail ia displaced and perfect matching cannot<br />

be achievad.<br />

ftIISSlle launch alte data card— A<br />

standardized form containing launcher geodelic<br />

Irrfomraflon which has been produced on the<br />

CUfreM wortd geodelic system. Used in<br />

conjunction wfth the missile target dala card.<br />

mlselle target data—Precise geodetic target<br />

MIL-HDBK-850<br />

164<br />

positioning data required 10 suPport strategic<br />

and Iactical weapon syslems. See also polnl<br />

position data.<br />

mlaslng triangla-(pendulum) A lri~ngle<br />

which represents the failure ot the two sides of a<br />

knife edge to reach a periecf intaraecfion In a<br />

geometric line.<br />

mistake—See blunder; arror,<br />

mock-up—See atyla sheet.<br />

model coordlnatee-(photogrammatry) Tha<br />

space coordinalea 01 any point imaged in a<br />

stereoscopic model which define Its posffion wffh<br />

reierenca to tha air base or to the Instrument<br />

axes.<br />

modal datum—1. (photogrammetry) That<br />

surface in a stereoscopic modal corweived aa<br />

having been reconstructed as part of the model<br />

representing the sea level datum of nature.<br />

Often modified to designate the Iypa of<br />

phonography used, such as ccmvergam model<br />

datum, and transverse model datum. 2. For<br />

relief maps or models the datum may or may<br />

not be sea level but is consistent within a relief<br />

map saries.<br />

model marriage—The rejoining of seclions of<br />

a model, aller the carving operatfon, to the<br />

original nealline limits 01 a relief model.<br />

model acala-(phologrammetry) The<br />

relationship which axisls between a dk.tanca<br />

measurad in a stereoscopic model and the<br />

corresponding distance on the Earth.<br />

modellng—The developmem of the model<br />

surface by the application of modeling clay<br />

between fhe step edges of the step cast, A<br />

preparato~ step in producing relief models.<br />

model—Sea alrborna Iandlng modal;<br />

assault Iandlng model; aesault models;<br />

flat modal; gross modef; half model;<br />

maater modef; neat modef: perapactlve<br />

spatial modef: relfef modef;<br />

stareoscoplc image; etereoscoplc<br />

t’nOdel; strategic planing model; tactical<br />

plannlng models; terrain modal; warped<br />

MOdel.<br />

modlflad facslmlle chart-A naufical charl<br />

published by a foreign hydrographlc agency and<br />

reproduced by DMA, Specific atxfhorkty to<br />

reproduce is contained in a bilateral agreement,


Ii<br />

which will alSO identify any qualllicalions to the<br />

permission to reproduce.<br />

modlfled Julfen stay-An abbreviated form<br />

of Ihe Julian day which requires Iewer digits and<br />

translates the beginning of each day from<br />

Greenwich noon fo Greenwich midnighl:<br />

obfained by subtracting 2400000.5 from Julian<br />

daya.<br />

modlfled Lambert conformaf chart— A<br />

chart on the modified Lamberf mnformal map<br />

projection. Also called Ney’a chert.<br />

modified Lambert conformal map<br />

projactlon—A modification of the Lambarl<br />

conformal projection for use in Wler regions,<br />

one of fhe standard parallels being at latitude<br />

89°5958- and fhe ofher at Iafi!ude 71° or 74”,<br />

and the parallals being expanded slighlly to<br />

form complefe Concanlric circles, Also called<br />

Ney’a map protection.<br />

ISSOdlfled polyconlc map pro]action— A<br />

map projecfiorr obtained from lhe regular<br />

polymnk projection by so allering the scale<br />

afong the central meridian thal the scale is exact<br />

along fwo standard meridians, one on either<br />

side of the cenlral meridian and equidistam<br />

therefrom. Also calied rectangular polyconic<br />

mep projection.<br />

modufatlon arror—in electronic distance<br />

measuring equipment, the difference in<br />

modulating frequencies obtained from crystals,<br />

between fhe actual frequencies of the crystais<br />

and the frequencies required for a correct<br />

distance measurement<br />

modulatloh—A variation of some characteristic<br />

of a radio wave, called the carrier wave, in<br />

accordance with Inslanlanaous values of<br />

another wave called the modulaflrrg wave.<br />

Thase variations can be amplitude, f~equency,<br />

phase, or pulse.<br />

molr6-An interference pallern resulling from<br />

the overlaying or oveprinling of halflones or<br />

tints whose screen angles are not sufficiently<br />

separated to make the patlern inconspicuous or<br />

fo preclude a pattern accuracy.<br />

mofd afteraflons—The slight modification of<br />

the fandforms of the mold, often necessary in<br />

local araaa in order to obtain proper register due<br />

to unequal afretch required to accommodate the<br />

Iandtorrns on a plaslic relief map.<br />

MIL-HDBK-850<br />

165<br />

molded aerial phonograph—A vertkal aerial<br />

phonograph, usually annotated with mlfiiafy<br />

symbols, which has been iormed to show terrain<br />

configuration.<br />

Molitor preclae Ievelfng rod—A spaaking<br />

rod of T-shaped cross section, with graduation<br />

marks shaped as friarsgles and rectangles, the<br />

smallesf div~ton baing two milfimetere. Read by<br />

estimation to singla milfimetara. Equipped whh<br />

thermometer and circufar feval.<br />

Mollwelde homalographlc map<br />

projection—An equal-area map pro)ecflon<br />

showing the Equa!or and geographic pSralfelS<br />

as alraighl lines, and tha geographic merid!ana<br />

as elliptical arcs, with the exception of fhe<br />

central meridian, represented by a straight line,<br />

and the meridian 90” from the center, shown as<br />

a lull circle.<br />

moment of lnerfla-The quanfity obtained by<br />

mu kiplying the mass of each small part Of a<br />

body by the square of ils dktance from an Ssis,<br />

and adding all tha resuffs.<br />

momentum-uanlity of motion. Linear<br />

momentum is’ tire quantity obtained by<br />

multiplying the mass of a body by Its finear<br />

speed. Angutar momentum is fhe rJJan!ilY<br />

obtained by multiplying tha momant of Inarfia of<br />

a body by its angular speed.<br />

momenl—A Iendancy to cause rotation about<br />

a point or axis, as of a corrfroi surface abour ~s<br />

hinge or of an airplane about its center of<br />

gravity; Ihe measure of fhis tendency is equal to<br />

the producf of the force and the perpandsular<br />

distance belween Ihe point of axis of rotation<br />

and the fine of action of the force.<br />

monochromBfor—A dispemlve devka fOr<br />

isolation of narrow ~tilons of the spectrum.<br />

monochrome—A single hue or color.<br />

monocomparator—A precision instrument,<br />

consisting of a measuring system, a viewing<br />

sysf em, and a readout sysfem designed for the<br />

measurement of Image coordinetea on a eingfe<br />

phonograph.<br />

monoscoplc [mono) lmaglng—A eingle<br />

image taken of the iargaf.<br />

monoscoplc rev falon—Exfracfion ‘of Image


identifiable feature data from a single image.<br />

No eflorf is made to compensate for relief<br />

displac#nerd or till. Existing cenler line data<br />

(CLD) Ieature and elevalion data are registered<br />

with the imagery. New CLD Ieatures may be<br />

added and existi~ CLD features may be<br />

delated or rrmdiiied spatially or atlribulionally.<br />

MIL-HDBK-B50<br />

month—The period of the revolution o! the<br />

Moon around the Earlh, The month is<br />

designated es sidereal, tropical, anomalistic,<br />

nodical or dracontic, or synodlcal, according 10<br />

whether the revotutkm Is relative to lhe stars, the<br />

vernal equinox, the perigee, the ascending<br />

node, or the Sun. See also anomalistic<br />

month; calendar month; nodical month;<br />

eldereal month; aynodlcel monlh;<br />

tropic.al month.<br />

monumemed bench mark—See<br />

permanent bench mark.<br />

mmm’mtt-l. A structure used or erected to<br />

Marl( the posttion of a eurvey station:<br />

permanence is Implied. See elso artlflclal<br />

monument; natUral monument. 2. A<br />

physical structure, such as an iron post, marked<br />

stone, or tree in place, which merks the Iocelion<br />

,0!, a mrner point established Dy a Caoastral<br />

survey. Objecis, to be ranked as monuments,<br />

shoukt have certain physical properties such as<br />

visibility, durability, and stability, and they must<br />

defhra Iocafiin without resorting to<br />

measurements. Monument and corner are<br />

nof synonymous, although the two terms are<br />

often used largely in the same sense. See also<br />

corner.<br />

Moon posltlon camera mathod—A means<br />

01 determining geodetic position, that is<br />

unaffected by deflection of the vertical. by<br />

photographing the Moon against a star<br />

background.<br />

morphographlc mep—A small-scale map<br />

sfrowing physiographic features by means of<br />

standardized pictorial symbols, based on lhe<br />

appearance such features would have if viewed<br />

oblquety from the air.<br />

moseicklng board-A smooth-surfsced<br />

material, usually tempered Masonite, to which<br />

the mosaic is fastened with a suitable adhesive.<br />

mosaic—l. (JCS) (photogrammelry) An<br />

assambly of overlapping aerial photographs<br />

which have been matched to form a continuous<br />

phofographc representation of a portion of Ihe<br />

166<br />

Earth’s surface. Also called eerlal mosaic.<br />

See also controlled mosaic; map.<br />

controlled mosaic; orthophotomoselc;<br />

scale- retio moselc; eemlcontrolled<br />

mosaic; strip moeelc; uncontrolled<br />

mosaic. 2. (cartography) See panel base.<br />

most probable valua-That value of a<br />

quantity which is mathematically determined<br />

from a series of observations and ia more nearly<br />

free trom the ettects ot errors than any other<br />

value that might be derived from the same<br />

saries ot observations. Derivation ot the rrrmst<br />

probable value is made after blursdare and<br />

systematic errors have been removed from the<br />

data.<br />

moving averaga—See conaecutlva<br />

mean.<br />

multlplex—A name applied 10 anaglyphic<br />

double-projection stereoplotlars with the<br />

Iollowing characteristics: (1) the stereornodel is<br />

projected from dia~aitivea reduced from aerial<br />

phonograph negatives; (2) the projection system<br />

illuminates the eriire d!apositive format area:<br />

and (3) lhe stereomodel is measured and drawn<br />

by observation of a floating mark<br />

multlband photography—A remote sensing<br />

syslem which produces more Ihan one image of<br />

a single area in which each image shows a<br />

dillerenl wavelength band of the<br />

electromagnetic spectrum.<br />

mullibeam survey-A hydrographic survey<br />

conducted wilh an array ot sevaral or many<br />

transducers mounled on the sounding vessel,<br />

designed 10 take simuiieneous soundings on a<br />

wide swath ot the ocean bottom.<br />

multicolor—Two or more cmbrs. Also called<br />

polychrome. See also process color<br />

printing.<br />

multinational data bese—A standardized<br />

data base operated and maintained under the<br />

control of two or more participating mamber<br />

nations,<br />

multiple level llne-Two or mora single lines<br />

of spirit leveling run between me sama terminal<br />

points, but along different roulas.<br />

multlple-camera assembly—An assembly<br />

01 two or more cameras mounted to maintain e<br />

fixed angle between their respective opfical<br />

axes.


I<br />

I<br />

I II<br />

MUIIlple-lenS camera—A camera with two or<br />

more lenses. with the axes of tha lenses<br />

SYSlamaliCally arranged al fixed angles in order<br />

to rover a wide field by simultaneous exposures<br />

in all cframbars.<br />

I’ttUltlple-lene photograph—A photo- graph<br />

made with multiple-lens camera,<br />

multlple-etege rectlficellon—A technique<br />

empbylng standard equipment to rectily oblique<br />

phOIOS by applying a series Of projections to<br />

eflecl the desired projective transformation.<br />

multlplex control—See photogrammelrlc<br />

control.<br />

multlplex triangulation—See atereotriangulation.<br />

multlepectral aenslng—Employment of one<br />

or mora sansors to obtain imagery from differenl<br />

poriions (bands) 01 the electromagnetic<br />

spactrum.<br />

multlspect ral—Remole sensing in two or<br />

more spectral bands, such as visible and,<br />

inlrared Sae also Infrared; remote sensihg.’<br />

multluse manuscript (MUM)—A manuscript<br />

compilation that, as a minimum, establishes the<br />

contours, spot elevations and includes the<br />

horizontal position of the significam planimetric<br />

features. II is suitable for use in completing a<br />

topographic map, or an aeronautical or nautical<br />

charl; and the integrity of its horizontal and<br />

vertical accuracy is retained in all end products<br />

made from it.<br />

MIL-HDBK-850<br />

167


I<br />

I<br />

I<br />

I<br />

nadir polnl—See photogrepn nadir.<br />

nadir redfsf-A radial from the nadir point.<br />

rmdlr-polrst plot—See nedlr-polm<br />

trlangukrtlon.<br />

MIL-HDBK-850<br />

nadir.point trlan@ailon-Radial lrian.<br />

gulation in which nadir points are ulilizad as<br />

radial centers. Also callad nedlr-pOlnt<br />

plot.<br />

nadir+JCS) Thet poim on the celestial<br />

sphera directly beneath the observer and<br />

directly opposite the zenith. See also<br />

ground nadir; map nadir;<br />

phOtOpFaph nadir.<br />

nanoteala—(geomagnetiam) A unit 01<br />

magnetic field intensity generally used in<br />

describing the Earths megnelic field. It is<br />

defined as 10-9 Iesla = 1 gamma. See also<br />

gamme.<br />

narrow-angle lens—A Ians whose total<br />

length /s equal approximately 10 twice Ihe<br />

diagonal of tha format.<br />

National Geodetic Vertical datum 01<br />

1929—Known as ‘sea level datum of<br />

1929. prior 10 Seplembar 1973, this dalum<br />

was established by constraining the<br />

cumbined interconnected United States<br />

and Canadian networks 01 Iirst-order<br />

leveling, es it existed in 1929.<br />

national data baae—A data base<br />

designed, operated and maintained by any<br />

nation for purposes specific 10 that nation.<br />

national mao accuracv stendards—<br />

Sasr U.S. “Nallonal Map Accuracy<br />

Standards.<br />

native ma~A map of any counlry<br />

produced by that country’s governmental or<br />

private agencies,<br />

natural detail—The features on the Earth,<br />

such as streams, lakes, Iorests, and<br />

mountains; exclusive of the works 01 man.<br />

Also called natural feature. See also<br />

Culture; hydrographlc detail;<br />

N<br />

168<br />

hypaogrephlc datall.<br />

natural error—Errors arising Irom variations<br />

in temperature, humidify, wind, gravity,<br />

refraction, and magnetic declination.<br />

natural leature—See natural devail.<br />

natural monument—A natural feattsra,<br />

such as a stream, boulder, tree, etc., which<br />

serves to mark the location of a survey “<br />

station or land corner. Sae also<br />

monument.<br />

nautical broadcasta—Radio navigational<br />

warning broadcasts to shipping on Urgent<br />

dangers to navigation, advanced<br />

information on changing navigational<br />

conditions, and special warnings<br />

disseminated by ollicial U.S. Government<br />

proclamations alfecting shipping. This<br />

information is also accessible on the<br />

Navigation hflorma!ion Syslem<br />

(NAVINFONET).<br />

nautical chert—See hydrographlc<br />

chart.<br />

nautical mile—Typically, a measure of<br />

distance equal 10 1 minute of arc 01 a great<br />

circle. See also International Nautical<br />

Mile.<br />

Naval Operating Area Chart<br />

(OP ARE A)—Naulical charw produced<br />

and Overprinted with prescribed OPAFIEA<br />

boundaries, submarine transit lanes,<br />

aeronautical and olher information for fleet<br />

exercise areas.<br />

Naval Range Charts—Detailed<br />

balhymelry, grid, and range boundaries;<br />

information on range acoustics; and<br />

seismic instrumentation.<br />

Navigation InformalIon Network<br />

(NAVINFONET)—The DMA data base<br />

which contains the information to produca<br />

the following publications: Notice to<br />

Mariners. Summary of Corrections, Lisl of<br />

Lighls and Fog Signals, II also provides<br />

users access 10 upto-dale marine<br />

information via commercial<br />

telecommunications services.


navigation chari-See aeronautical<br />

chart; hydrographlc chart.<br />

Sravlgallon alghi—An auxiliary device used<br />

in the Iaking of aerial photography to show<br />

nol only the vertical Iiekf of view buf also<br />

the path ahead and behind the aircraft.<br />

Navlgatlonal Flhmstrlps (NFS)—Filmstrips<br />

depicting cartographic data as<br />

photographed from lithographic copy<br />

arrwng the JNC and TPC series for A-7<br />

aircraft, ONC and JOG series for HH-53<br />

aimraff. and all 4 chart series for Remoie<br />

Map Reader (RMR) equipped (F-14 E).<br />

Used In akcraft equipped wi!h a moving<br />

map display system to provide in-cockpit<br />

display of aircrafl horizontal position relative<br />

to the chart data.<br />

navigational planets—The tour planels<br />

commonly used ior celestial navigation:<br />

Venus, Mars, Jupiter, and Salurn.<br />

nsvlgarlonal triangle—The spherical<br />

triangle solved in compuling altitude and<br />

azimuth or greal circle sailing problems.<br />

The celestial triangle is Iormed on the<br />

celestial sphere by the great circles<br />

connecting the elevated pole, zenilh of the<br />

assumed position of Ihe observer, and a<br />

celestial body. The iarrastrial triangle is<br />

formed on a spherical Earth by the great<br />

circles connecting the pole and two places<br />

on Earth, either the assumed position of<br />

the obsamer and geographic position of the<br />

body for calastial observations, or the<br />

points of deparlure and declination for<br />

great circle sailing problems. The<br />

expression navigational lrtangle<br />

aPPlies to either the celestial or terrestrial<br />

trlangte used for solving navigation<br />

problems.<br />

NAVINFONET—See Navlga!lon<br />

Informssllon Network.<br />

NAVSTAR Globat Poaltlortlng System<br />

(GPS)—A navigation and positioning<br />

system, mnsisling of 24 saleltites, with<br />

which Ihe three-dimensional position and<br />

the velaclty of a user at a poinl on or near<br />

tha Earlh can be determined in real lime.<br />

Its raterance syslem ia WGS 84. The<br />

users receiver will require tracking of a<br />

minimum of four of the salelli!es trom any<br />

tocation at any time to eslabtish position<br />

MIL-HDBK-850<br />

169<br />

anct velocity.<br />

Navy Navlgatlon Satellite System<br />

(NNSS)—A set 01 tive or six saleltites in<br />

polar otitl with which three-dimensisnat<br />

position of a user can be determined. See<br />

also brosdcast aphamarls; Dopplar<br />

navlgatlon; praclae ephemarta.<br />

near-certainty error (3.5 elgma, 3.5u)—<br />

The 99.76 percent error kderval based on<br />

the bivariate normal distribution function.<br />

See also circular near-cartalnty error;<br />

circutar error probable.<br />

neat model—The portion of the gross<br />

overtap of a pair of phonographs that is<br />

actually utilized in photogrsmme!ric<br />

procedures. Generally, tha neat model<br />

aPPnJximaleS a rectangte whosa width<br />

equals the air base and whose tength<br />

equats the width between tlights. SeO atso<br />

gross model.<br />

neatllnes—(JCS) The lines that bound the<br />

body 0! a map, usually parallets and<br />

meridians [but may be conventional or<br />

arbitrary grid lines]. Also catled shaet<br />

Ilnes.<br />

negative altltude—Angular distanca below<br />

the horizon.<br />

negative component In color mlxtura—<br />

A componenl that is mixed wilh the sample<br />

light in order to desaturate it sufficiently to<br />

obtain a match with a mixture of the other<br />

two components.<br />

negetiva corrections—Changes mada<br />

directly on a negative or a scribed surface.<br />

See also negative engraving.<br />

negative dellactlon angle—See<br />

detlectlon sngle, definition 1.<br />

negetlva engraving—The operation of<br />

making corrections and additions to<br />

negatives. This term shoutd not be applied<br />

to the process 01 scribing on coaled<br />

plastics,<br />

negativa forming—in relief model making,<br />

Iorming into a negalive motd,<br />

negatlvs lens—A lens diverging a beam ot<br />

parallel tigh! rays, with no raal focus being


obtained. Also called concave<br />

dlverglng lens.<br />

lens;<br />

negative mold—Tne cast resulling Irom<br />

casting over a masler relief model.<br />

negative ecrlbhrg—See scrlblng.<br />

negative lltling—See tung.<br />

negative-l. In black and white<br />

phol~raphy an Image on film, plate, or<br />

paper in which the normal tones of the<br />

SUbjeCt are reversed. In color phcdography,<br />

an image on film, plale, or paper, In which<br />

cobra appear as lhelr complements. 2. In<br />

Cartographic scrtbing, a scribed sheet is<br />

essentially a manua[ly produced negative.<br />

See also dupllcate negative; orlglnal<br />

negetlve.<br />

network enalysls—Analytical Techniques<br />

mrrcemed with the relationships between<br />

Imetions on a networlc such as the<br />

cakulafion of optimal routes through road<br />

networks, flow capacities of network<br />

systems, or the best Iocalion for facilities<br />

aiOW networks.<br />

net—See euwey net.<br />

neutral date—Digital Geographic<br />

Information Ihal is inlended 10 supporl<br />

numerous applications but must be tailored<br />

for a specific application.<br />

neutral filter—A filler Ihal reduces lhe<br />

Infenslty of light reaching the film or plate<br />

without aflectlng fhe tonal rendition Of<br />

mlora In the original scene.<br />

Naw York Ieveflng rod—A two-piece rod<br />

wilh movable target. For heights greater<br />

than 6 1/2 ieet, the target is clamped at 6<br />

1/2 teet and raised by extending the rod.<br />

Graduated to hundredths 01 a foot and<br />

raad by vernier to thousandths.<br />

MIL-HDBK-850<br />

new ch&srt-A chart constructed to satisfy the<br />

needs of navigation in a particular srea. If is<br />

laid ouf in conformity with a broad scheme<br />

10 meet future needs in fhe adjacent ereas,<br />

new edl{lon-Confeins changes of such<br />

importame to map or chart users lhal all<br />

previous printings are made obsolete,<br />

170<br />

new survey—See resurvey.<br />

Newton’s laws—l. (gravilalion) Every<br />

parlicle of matter in the universe attracts<br />

every other panicle wiih a !orce proporilonal<br />

to the product of Ihalr masses and inversely<br />

as the square o! the distance between<br />

them. 2. (motion) (1) Every body continues<br />

in its state of rest, or of uni{orm rndion in a<br />

straight line, unless it is compelled to<br />

change Ihaf stale by a force impressed<br />

upon il. (2) The rate of change of<br />

momen!um is propofilonal to Ihe Iorce<br />

impressed, and takes the dkecfion of the<br />

slraignl line in which the force acts. (3) To<br />

every aclion Ihere is an equal and opposite<br />

reaction; or, the mufual actions of two<br />

bodies are always equal and oppositely<br />

directed.<br />

Newton’s rings—An interference effect<br />

arising from close, bul nol quite pertecl.<br />

conlact between Iwo surfaces, manifested<br />

b~ irregular concentric rings of color.<br />

Newlonlen constenf of gravltetlon—<br />

See constenf of gravitation. .,<br />

newton—The newton is the mefric (S1) unit of<br />

force. A force of 1 newion (N) acting on a<br />

mass of 1 kilogram imparts an acceleration<br />

of 1 reeler per second per second. .One<br />

newton equals 1 kilogram per meter per<br />

second per second. See also dyne.<br />

night efiect—(JCS) An ellecl mainly caused<br />

by variations in the slate of polarization of<br />

rellacted waves, which sometimes result In<br />

errors in direction finding bearings. The<br />

ellect is mosl frecfuenf al nightfall.<br />

no-check poslfion—See IntersectIon<br />

station.<br />

nocturnel arc—See aatronomlc arc.<br />

nodal Iine—in a tide area, tha fine about<br />

which the Iida oscillates and where fhare is<br />

little or no rise and fall of fha fida.<br />

nodal plane—A plane perpendicular 10 tha<br />

optical axis al a nodal poinl.<br />

nodal point of emergence—See nodel<br />

point, definition 1.


nodal point of lncldence—Sae<br />

point, definition 1.<br />

nodal<br />

nodal point-l. (optics) One 01 Iwo points<br />

on the optical axis 01 a lens, or sysiem 01<br />

lenses, such Ihal a ray emergent from the<br />

sacord pmint is parallel to the ray incidenl<br />

at tha first, Ttris first nodal point is also<br />

referred to as the front nodal point,<br />

Incident model point, or nodal polnl<br />

01 Inclcfenca; and !he second poinl as<br />

the rear nodal polrtt, emergent nodal<br />

point, or nodal polnl 01 amarganca.<br />

Also celled nods. 2. (astronomy) See<br />

node, definition 1. 3. (hydrography) See<br />

amphldromlc point.<br />

noda cycle-The lime required (or the<br />

regression of the Moon’s nodes 10<br />

complete a circuil of 360= of longitude: a<br />

period of approximately 16,6 years.<br />

node-1. (astronomy) One of the two poinls<br />

of intersection o! the ortil of a planet,<br />

planetoid, or comet with the ecliptic, or of<br />

the orbit 01 a satellile wilh the equatorial<br />

plane 01 the orbh 01 its primary. Also called<br />

nodal point. See also ascending<br />

node; dascendlng nods; ecliptic<br />

node; equatorial node; line of<br />

nodes; Iongltude of the Moon’s<br />

nodes; lunar node; regression 01<br />

tha nodes. 2. (oplics) See nodal<br />

polnl, definition 1. 3. A unique poinl<br />

representing the Iocalion ot a teature, 01<br />

the location of an intersection or connection<br />

of some number o! tea!ures. Alternatively,<br />

a node is any isolated point, or the junction<br />

of any two or more edges, or the erid<br />

points of an edge.<br />

nodlcal morr!h-The interval of lime<br />

banvean two successive passages ot Ihe<br />

Moon through the same noda of its orbit,<br />

aPPrOximalelY 27 days, Also called<br />

dracontc month.<br />

nodlcal period—The interval between two<br />

successive passages 01 a salelfile or planel<br />

through the ascending node of its orbit.<br />

nolaa lavel—The magnitude of random<br />

errors in a particular type 01 measurement,<br />

nominal focal length—(JCS) An<br />

approximate ValUe Of the focal length,<br />

rounded off to some standard figure, used<br />

MIL-HDBK-850<br />

171<br />

ior the classification of lenses, mirrors, or<br />

cameras.<br />

nominal orbli—Tha true or ideal orbit upon<br />

which a space vehicle is expected to msval.<br />

nomogram—A diagram showing, to acafe,<br />

the relationship between several variables<br />

in such manner that tha value of ona which<br />

corresponds to known vefues ot the others<br />

can be determined graphically.<br />

Non-Submarine Contact (NSC) Llate—<br />

Lists which contain a tabulated fist of<br />

wrecks and other obstructions which might<br />

be construed as submarine by sonar.<br />

nonautomatic rectlflar-Any rectifiar which<br />

requiras compulalbn of the elemenls of<br />

rectification, each of which must be<br />

manually set on its corresponding circle or<br />

scale on the rectifier.<br />

nongrevilationsl parturbatione—<br />

Perturbations caused by surface forces due<br />

to mechanical drag of the atmosphere (in<br />

case 01 low flying satellites),<br />

eiecvOmaQnelism, and radialion pressure.<br />

nonmonumented bench mark—See<br />

temporary bencn mark.<br />

nonperspectlve azimuthal map<br />

projection—A projection not based on<br />

perspective lines of sigh! from a single poim<br />

of view.<br />

nonselective filtar—A lilter Ior which<br />

transmittance is sutrslamially independent<br />

of wavelength.<br />

nontiltlng-fens rectltler—A clesa of retillier<br />

wherein the lens is constrained to rnova in<br />

the direction o! its fixed esis.<br />

nontfltlng-negative-pfane rectlfler— A<br />

ClaSS ot rectifier which Conlalns a nomiltfng<br />

negative carriar. In this class of racfffiars,<br />

the negaliva carrier plane remains<br />

horizomal.<br />

normal dlstrfbutlon !unctlon—A<br />

mafhemaficaf funclion describing the<br />

behavior of one-dimensional random errors.<br />

normal equation—One of a set of<br />

simultaneous equafions derived from


MIL-HDBK-850<br />

observation, condition, or correlate<br />

equations, and expressing a condilion [or a<br />

feast squares adjustment. In a least<br />

squares adjuslmem, values oblained Irom<br />

the solufion of normal equations [either<br />

directly or through the correlale equations)<br />

are applied to the observation or condition<br />

aqualions to obtain the desired corrections.<br />

normal gravity !leld-A mathematically<br />

derived gravity Iiald used in geodesy 10<br />

closely appros.imale the Earth’s actual<br />

gravily field.<br />

normel gravity—A reference gravity field<br />

that k malhemaiicalfy defined tora<br />

normalized earlh which has gravitational<br />

symmetry. It is commonly taken as the field<br />

01 a rotating level ellipsoid bul may be<br />

arbNrarily defined.<br />

normal orbll—The orbit 01 a saletli!e<br />

considered with nodislurbing effects<br />

presemdue loother celestial bodies, or to<br />

some physical phenomena. Also called<br />

unperturbed orbit.<br />

normal section szlmuIh—Tne angle<br />

between lhe geodetic meridian 01 [he<br />

observer and the plsne comaining Ihe<br />

ellipsoidal, normal of the observer. and<br />

measured clockwise from the north in a<br />

plane parpendicularlolhe elfipsoidaf<br />

normal of the observer.<br />

nOMSal section llne—A line on the surface<br />

01 lhe ellipsoid connecting two points on<br />

that surface, and traced by ap!ane<br />

containing the normal al one point and<br />

passing through the other poim.<br />

normal tension—(tapin@ The tension to be<br />

aPPfied 10 a law 10 compensate for the<br />

shortenlngeftecl of sag in order to bring<br />

the tape to standard Ieng!h. Thai pull at<br />

wh!ch the tension correction and sag<br />

exaClly balance each olher,<br />

normal waler level—The mosl prevalenl<br />

water level in a watercourse, reservoir, lake,<br />

or pond. generally defined by a shoreline of<br />

permanent land-type vegetation. Along<br />

Iarge bodies of water, wave aclion may<br />

relard vegetation beyond the normal<br />

shoreline.<br />

normal-angle lens—A fens having an<br />

angle of coverage from 60°to 75”. A lens<br />

172<br />

whose local length is equal approximately<br />

10 Ihe diagonal 01 the formal,<br />

normal—1, Aslraighl line perpendicular to a<br />

surtace or to another line. 2. A condition of<br />

being perpendicular to asurtacaorline.3.<br />

In geodesy, Ihe straight Iina parPandicUlar<br />

Io the surface of the reference ellipsoid.4.<br />

The average, regular, or expected vafue of<br />

a quanlity.<br />

North American datum of 1927 (NAD<br />

27)—The datum which defined the<br />

geodetic positions in the United States and<br />

adjoining countries was derived lrom a<br />

readjustment of the geodetic data as<br />

available up lo 1927. II is based onlhe<br />

Clarke 1866 ellipsoid. See also horizontal<br />

datum.<br />

North American datum of 1983 (NAD<br />

S3)—The newdalum, which replaces NAD<br />

27, is geocentric and based on GRS 80<br />

parameters. llscoverage includes Alaska,<br />

Canada, CONUS, and CentralAmerican<br />

countries Irom Mexico to Panama. Total<br />

number 01 redefined horizontal stations<br />

exceeds 250K. . . . ..<br />

North Slar— See Polaris.<br />

north declination—See decllnatlon,<br />

definition 3.<br />

north geographical pole—The<br />

geographical pole in the Northern<br />

Ilemisphere, at latitude 90” N.<br />

north geomagnetic pole—The<br />

geomagnetic pole in the Northern<br />

Hemisphere.<br />

north magnetic poLs-Tne magnetic pole<br />

in the Northern Hemisphere.<br />

norlh poinl—See celestlal merldlan.<br />

norlh polar circle—See Arctic Clrcla.<br />

northbound node—See ascending<br />

node.<br />

norlhlng—1. (JCS) Northward increasing grid<br />

values on a map. See also talae<br />

northing. 2. (plane surveying) See<br />

Ialilude difference.


norfh-The primary reference direction<br />

relative to the Earth. See also compass<br />

north; grid north; magnetic north;<br />

true north,<br />

No!lce to Mariners—Speci!ic narrative and<br />

graphic correction dala for all DMA, USCG<br />

and NOS nautical charfs, publications and<br />

new information required to navigale. This<br />

information is published weekly. It Is also<br />

accessible on the Network (NAVINFONET)<br />

as inmrporaled in the summary 01<br />

corrections.<br />

numerlcel map—See dlgltal map.<br />

nutatlon In right ascension—Se e<br />

equallon of the equinox.<br />

nutatlon-1. The oscillation of me axis 01<br />

any rotating body, as a gyroscope rotor. 2.<br />

(aslronomy) Irregularities in the<br />

precessional motion of Ihe equinoxes<br />

because of varying positions of the Moon<br />

and, to a lesser extent, ot other celestial<br />

bodies with respect to the ecfiplic.<br />

MIL-HDBK-850<br />

173


1<br />

ob)ect orlontad-A design and programming<br />

mehdobgy tbt seeks to mim”k the way we<br />

form models of the worfd, end embodies thrae<br />

main propatlias. e.g.. enoapsulafbn,<br />

inheritance, and polymorphism.<br />

ob)actlvo bns-fn telaacopaa and<br />

microscopes, the optical corrpnenf tikh<br />

receives light from the cbjj and forms the first<br />

or primary image. In a camera, Ihe image<br />

formed by the objedve lens is the final image.<br />

In a lalaecqrs or micmacope used viauelfy, the<br />

image formed by the eb@tive Imm is megnifisd<br />

by the eyepiece.<br />

oblete .Illpsold of rotatiort-An ellipsoid of<br />

tmtotion, the atmrter axis of wh~h is ha axis of<br />

rotation.<br />

oblique alr photograph-(JCS) An air<br />

photegmph taken with the camera axis directed<br />

betwaen ha horiiomal and verilcel planes.<br />

Commonly relerrad 10 es an oblique: (1) high<br />

obllqua- one in vhksh the apparant herizon<br />

appears; end (2) low obllquene in which<br />

the apparent Im’izon dees net appear.<br />

obllque ●scension-The arc of the celestial<br />

equator, er the angle at the cslast’kil pele,<br />

between the hour circle c4 the vernal equinox<br />

and the hour cimfs through the intersection of<br />

the celestial eqmtor and the eastern horizon at<br />

the instant a point on the eblique sphere riSSS,<br />

measured eastward from the hour circle of the<br />

vernal equinox through 24 hours.<br />

oblique chart-A charl on an ebfique map<br />

projactiin.<br />

oblique coordinetea-Magnitudes defining s<br />

peinf relative to two interacting<br />

~nps~dsulw lines, called axes.<br />

oblique cylindrical orthomorphic map<br />

projection-See obllquo Mstcator<br />

projection.<br />

obliquo equetor-A great circle the plane of<br />

Wzh is perpendicular to the axis of an obfique<br />

projection.<br />

obllqua gratlcul*A fbfitious graticule baaed<br />

upen an cblique map projection.<br />

MIL-HDBK-850<br />

o<br />

obliquo ldtudo-Angular distance from an<br />

obliiua equator. See alse fictitious Iatltud*.<br />

obllque lon!#tude-Angufar dtience<br />

between a prima oblique maridiin and eny<br />

given oblique msridiin. See abo fictitious<br />

Iongltudo.<br />

obllquo map projection-A map projection<br />

with en axis inched at en angle between O“ and<br />

90”.<br />

oblique Mercator projectlorr-A conformal<br />

cylindrical map pmjsctien in wliih points on the<br />

surface d a sphere or efliisoid, such as the<br />

Earth, are conceived as developed by Mercator<br />

princi#ss en a cylindrical fengenl abng an<br />

obtique grast circfe. Atae called oblique<br />

cylindrical orfhomorphlc projection.<br />

obllquo maridlabA great ckcle<br />

perpendicular 10 an oblique equator. Tha<br />

reference obfique meridian is txilled prime<br />

obliqua meridinn. See “alw fictltiouc<br />

meridian.<br />

obllque’ parallel—A circle or line parallel to an<br />

oblique aqustor, connecting all points of equal<br />

oblique latitude. See also fictitious parallel.<br />

oblique plotting Instrument—An instrument<br />

for plotting from oblique photographs.<br />

obllque pole-One of the two peints 90” from<br />

an oblique equator.<br />

obllqua rhumb line-l. A line making the<br />

same clique angle with all fctitious mstitans<br />

of an oblique Mercaler pmjactibn, CZb~qua<br />

parsliela and meridians msy be corraidarad<br />

spec’wl cases of the diqua rhurnb iina. 2. Any<br />

rhumb line, real or fm’nious, makhtg an ebfique<br />

angle with its meridiins. In this ssnae the<br />

expraesiert is used to distinguish such a rhumb<br />

line fmm parallels and meridians, real or<br />

fiilitious, whiih may be included in the<br />

expression rhumb Ilno. see al= fictitious<br />

rhumb line.<br />

oblique sketchmnetor-A type of sketchmsster<br />

in which obtique pfretegrsphs are<br />

utilized.<br />

174


.<br />

obltqua sphese-The cdestial ephem as it<br />

-m !0 BfI observer bsfween the Equator<br />

and the pole, wltera caiaatial bodie4 appair 10<br />

rise obliie!y to the horizon.<br />

obllqulty of tho acllptic-Tire acute angle<br />

bafween the ptane d the ecfiplk (the pkene of<br />

the Earth’e orbff) and the ptena of the cefesfiaf<br />

equator.<br />

oblffemtsd corner~n obfifereted camar ia<br />

one al whine point there are m ramaining<br />

traces of the rnmsument or tts a~aaoriea, but<br />

whoaa location his bean perpatustad, or the<br />

pckt for whiih may be mcovomd beyond<br />

reasonable dcwbt, by the acts and taafirmny of<br />

tha intersected Iandownars, compatant<br />

aurvayom, or other quafiii &cal .sulktorii&, w<br />

witnesam, of by awns acceptable recent<br />

evidence.<br />

obsarvntion equatlort-An adjustment<br />

aquet”bn wherein variables representing<br />

cerredkms to approxknetions of the unknown<br />

pammetera, as well as vstiebles rapmsenting<br />

adjustments to the observelions, remain in the<br />

~tbps. + 1S8S Squrima adjuatnremt<br />

emp~YW3 th?s type cd equstiom is said to be by<br />

the obaafvatron equations methed, m variation<br />

of parameters method, as opposed to the<br />

condiion equations method.<br />

obs*rv@lon-See obsarvad value.<br />

obswvod ●ffltuda-Carected sexienl<br />

ahilde; angutar d~enca to the center of a<br />

celestial bxly ebove the horizon, mrmcled for<br />

instrumental ermm. pamosrel error, dip.<br />

relredion, and eemidiemeler end paellex if<br />

neceesery. See also truo dfitude.<br />

observed angla-An engle obtained by direct<br />

instrumental cbeervaticm A measured angle<br />

Wfsiih hes bean corrected for bud condiiiens<br />

only et tha point of obsenfation, is cmaeidemd<br />

an observed engla.<br />

obaarvod gravity ●nomafy-See gravity<br />

●nomaly.<br />

obaorvad gmvfty-The value of grsvlty at a<br />

station ee determined fmm e gravity metar, a<br />

pandulum, or an instrument timing free falling<br />

bodies. The gmvity ok4eind is eilhar relattie or<br />

ekolute according to the apperatua used to<br />

make the maaauramanle.<br />

MIL-HDBK-850<br />

obaorved valua-A value of a quantify that is<br />

okieined by instrumental maeaumment of the<br />

qusniity. The term observad valus La often<br />

a@iad to tha value of a quantify tied horn<br />

inefrumenfel nreeaunmrant nftar corradons<br />

have hsen applied for eyefamatic errors by<br />

some methcd d adjustment.<br />

obaolata cfsatt-A chart which does not<br />

contain the tahst nevigafionsl information,<br />

occuftatlon-1. (astronomy) The<br />

di~pearenca of a cefesfiel body behind<br />

amtfwr body of larger eppmenf size. When tha<br />

Moon paasas between the obaasvar and a star,<br />

the sf.sr is said to be occuttad. 2. (aufvaying)<br />

Name appfiad to a geodetic survey technique<br />

which employs the primiple c4 ocdtafion where<br />

repeated cbeervations are made on an<br />

unknown position, accurstefy timed with aimllar<br />

obsewations at another unkmwn sfatiin, snd<br />

msfhemsticelly reducing these date to<br />

detemrine the exact geodetic poailii d the<br />

unknown stations. See elm star occultation<br />

method.<br />

occupy -(aurwying) To sat a surveying -.<br />

instrument over a point for the purpose of<br />

making observations,<br />

ocaanographlc ststlon—An observation<br />

point in ocean fmm wiich meemgrephii<br />

obearvet”ws am taken.<br />

oceanographic survey-A study or<br />

examinat”mn of renditions in the ocean or any<br />

part of if, with reference to animal or plant ~da,<br />

chemical elements present, ie~atum<br />

gradients, etc. Also selled msr’hm survey.<br />

oceanography-1. The study of the W,<br />

emtxecing and integrating all krmwiedge<br />

pertaining to the me end ifs physical<br />

boundaries, the chemistry and phyaica of sas<br />

water, and marine tsioJOgy.<br />

oceanology—Sea oceanography.<br />

octant- type of sextant having a nsnge d<br />

90” and an arc d 4S”.<br />

ocular mlcrometar-A filer micrometer so<br />

ptacad that its wire nmves in the prir+el focal<br />

plane of a taleacopa Also callad ●yaplaoo<br />

mlcromatar.<br />

175


odograph+ mschenk-sl instrument<br />

containing e ctiskrwe measuring efemsnf which<br />

is moved or hanad by art amount proportbnal to<br />

the octual d~ traveled e mmfmes<br />

ekmswrf whiih provides e fixed reference<br />

direcfbrt; and en iraegratorwltioh provkJea for<br />

lhe resolution of the direction of motion kito<br />

Oowwnts ~ for the sunrrnalbn or<br />

integration of the dIa4anm conpments.<br />

off soundlng~Any area where the depth of<br />

water oannor be measured by a soundhg lead,<br />

g.afmralfy ooneidsred to be beyond the 1O@<br />

fathom line. Oppoaiie of on aoundlngs.<br />

otf-llnKTranamlaakm of information between<br />

a mmp~er ~ a pebheml unit before or after,<br />

but not durbrg procasshg, in contrast to on-line<br />

processing.<br />

offlco computations-Oomputalions based<br />

on tiefd measurements, including all cskulationa<br />

raialive to the raduction d field suwey notes to<br />

grsphz form for any type of survey or for the<br />

continuation of fiefd work.<br />

otfeet II-A supplementary line close 10 and<br />

roughly parallel with e main tine, whiih is<br />

referred by measured offsets. Where tha line for<br />

such dafs are desired is in awh paaitiin that if is<br />

dticuft to measure over if, the required data ere<br />

obtained by running an offset line in a<br />

mnvenient location and meaauring offsets fmm<br />

it to aatient points on the other line.<br />

offset lithography-An indirect method of<br />

printiig wheraby the ink imsga is trsnsfamd<br />

from tha press piste to an intermedda surface<br />

of a rubar blanket, and trom that to the paper<br />

or other stock. Also called ottseti ottsat<br />

prlntine. See alao Ilthography;<br />

photolithography.<br />

owed praaa— A we= which mntsina on exira<br />

cylinder, rubber mvamd, upon which the image<br />

is printed firer and then reprinted<br />

from this cyfirrdar onto the papar.<br />

or ‘ottssr,”<br />

off sot prlnthr~ee offset lithography.<br />

MIL-HDBK-850<br />

desired, thus k.calrng the aemnd line or point<br />

with raferanoe to the War or survayad Iii. An<br />

offset is also e job in a survey a ahw Ime, fha<br />

line having approximatafy the -e direction<br />

both before and after passing the pg. Offsats<br />

ara measured from a aurveysd line, or fries to<br />

the edges d an kraguisr-shaped body d water,<br />

ortoarry bgulerfine ~kiadaaired to<br />

locale. 3. (printing) see otfset llthogr~phy.<br />

OK sheet-The first press irrrpreaskrn fran<br />

each mkor, a mlor corrbinatiorr, approved for<br />

accuracy d re@ter ●nd cola.<br />

Omsiga-A kong-mnge hypettrolii rravigat’bn<br />

system designed to pmvida worfdwikte rxwaraga<br />

for navigation.<br />

omnldlractlonal radar predlctlort-A radar<br />

prad!!ion wtriih is interxfed to be vefid tmm<br />

any dirsotion of approach. The Radar<br />

Significance Analysis Cde on the Series 200<br />

Air Targat Chad is an exsrrqrfe of<br />

omnidirectional radar pradiii~. Each mdd<br />

ares represents an analysis of relative radar<br />

intensify from all dkecfions.<br />

omnigaln. radar prediction—A radar<br />

prediction containing some informatbn aboul 811<br />

radar responsive features within the prsdidad<br />

aras. Thii ia eocon@ii by prfwtiiing all<br />

significant radar retume m relative intaneifiss<br />

baaed on Ihe predicted probabiiii d the return<br />

ramsining on the mdsrso~a at decreased gain.<br />

Ganaralfy, tha mora intsnse the return a~<br />

cm the predktiorr, the more likely it will ramsin on<br />

tha mdsrsrqm as the gain is dacr-sad.<br />

on soundhrga-hy eras where tha deplh of<br />

water can b msaaured by a sounding lead,<br />

generdfy cmraidarad to ba within the Ior2fathom<br />

fine. Opposite of otf soundlnga.<br />

o n-llna-Transmission of informet.km between<br />

a co*er arrd a tamninal or dIa@ay devioe<br />

whlla pmmasing is occurring, in contrast to df-<br />

Iiia proceaaing.<br />

one-projector molhod-see one-awl ng<br />

method.<br />

offast-1. (c.etiogmphy) In pmjecticm one-swing trtathod-The technque<br />

rnnatruction, that mrwdl dktance added to tha employed in relstive orientation for clesrfng y.<br />

Iangfh of the meridians on each side of the parallax by mahttalning one projector of a pair in<br />

central mendmn in order to detarmine the top a fixed position and making all adjustments with<br />

latitude of rhe constrtiad chad. 2. (surveying) the aemnd pro@for in ralaliofrtrMp to tha fket.<br />

A short line perpendicular to a surveyed fine, Also died ono-proJactor ms.thod; ●lngk<br />

rnaaaured to a fine or poinl for Wish data are proJector mathod. y-swing method;<br />

176


I<br />

I<br />

1<br />

one-to-one (1:1) copy-See contact<br />

Size.<br />

opacNy-See donslty, defintilon 1,<br />

opaqu~l. Not transmitting fight. 2 No!<br />

transmitting the particular wavelengths (whbh<br />

MSY w ~Y ~t bS visible) whiih affasf given<br />

photosensitive metariefs. Thus, e substance<br />

msybacpaque toaernscobrs end notto<br />

others. Ii sway be visually @nsparent, yet<br />

adiniselfy opaque. 3. A matetfal epplbd to<br />

emas of a negative to make il opeque m those<br />

eraas. 4. To appfy e materiel w bbckeut.<br />

open ●d traverse-See opm trevarsa.<br />

open eystsm (OS)-t. Any system thal<br />

interacts wiih KS envimnmant through inpul end<br />

output. An epan system is eble to edspt or<br />

edjust to shsnges in the environment in order 10<br />

continue its axisiense. 2. In sorqnrters, en<br />

epan sysiem has detailed published oparaling<br />

inetrudiom, hsrdware end software daacriptiorrs,<br />

end interface diagrams enebhng users and thti<br />

party vendors 10 add to or rrmdify the system to<br />

adspt i! to the usats apacifc needs, See also<br />

GOSIP.<br />

open tmversKA survey traveme which<br />

bsgins from e station of known or edcptad<br />

position, but does not and upon s known or<br />

edOfJfd station. Also called opan end<br />

traverse.<br />

open window Pr=oss+csflography) A<br />

method of preparing sobr separation negatives<br />

or positives W peeling an opaqua stratum from<br />

its base in the desired areas. It is normally used<br />

for prepering large areas covered by vegemtion<br />

~ OPen WSler. * else sneak, definition Z.<br />

operation map-(JCS) A map showing the<br />

bc.stbn and strangfh of friendly forces invofvad<br />

in an operation If may indtcete predicted<br />

movement and katien of enemy forces.<br />

Operational Navlgetion Chart (ONC)-<br />

Ths stenderd worfdwiie small-scale<br />

(1:1 ,000,000) aerenautbel chart serbs. It<br />

oontains sartographm data with an eerrmsufbsl<br />

overprint depicting obstrucfioms, aarodromes,<br />

etc., designed for medium attiiude high-speed<br />

visual and radar nevlgetion, Also used for<br />

mission pfanning/ensfysis and intelligerrse<br />

briefings.<br />

MIL-I-IDBK-850<br />

oporatlotml grid-A grid in currant<br />

oparafionsl use. Genaralfy this weuld be the<br />

prafermd grid but oc.ukl be a pmvbusty<br />

pwmioed grid.<br />

opemtfonal llbrarlaa-A DMA approved,<br />

sefesfive date file sonskting of axim sc@se of<br />

originafs, dupkale copies. oompufar fxinted<br />

catalogs, etc., obtainad from any daeignelad<br />

DoD Iitsary or from other nsfioneliy designated<br />

brariis within the non-DoO aganoies. and<br />

maintained in a DoD MC&G agansy for he dtrecf<br />

use in accor@ing assigned production<br />

mbsions. General reference pubfbatbns sush<br />

as dbfibnsries, gbseariee, atlases, pariodiils,<br />

etc., are axsluded from cxwtfmla e@ad to<br />

oparstiorml libraries.<br />

oporatlonel system-A system that has<br />

bean devebpsd, verified, and is being operated<br />

under the auqkes of a unified er specified<br />

commend.<br />

OPpOsltl O*l. The situatien of tvm celestial<br />

bcdas having either celestial longitudes or<br />

sideraal hour sngles differing by 180-. The term<br />

is usualiy used only in’ relalion to the position of<br />

a pfanet or moon frcfn the Sun. 2. The eituation<br />

of two periodic quantities differing by half a<br />

cycle,<br />

optical axle-(.fCS) In a lens element, the<br />

straight fine which passes !fsmugh the ~ars of<br />

curvature of the lens surlacae. In an s@ical<br />

system, the fine formed by the coinskhg<br />

principal axes of lha series ef optical elements.<br />

Also sallad axis of lens; Iena SXIS;<br />

prlnctpal ●xis.<br />

optical baee-llne maasurlng ●pparstua—<br />

A bass apparatus oompoaed ol bare wfvxre<br />

lengths are defined by distances between fines<br />

at or near their ands, wfrich are cbserved by<br />

suitabfy mounlad and adjusted mkmxoopas. In<br />

using any optkal bsselina measuring apparatus,<br />

the -Ions of the bars are c=xrfrdfed bv<br />

mic&cOpas on stsbfs aup+x.rtt whims Ads<br />

fines may be brought into coincidence with the<br />

fiiucisl marks on the bare, eithw by adjusting a<br />

bsr or a micmscepe.<br />

optical canter-The peinl of intersection of<br />

lines which represent within the lens tbse rays<br />

whose amergant directions are parallel to their<br />

reepactke “midant dkecbne. lhb point lies on<br />

Ihe eptical axis. An clique ray, even if it pssaaas<br />

through this point, undergees a bngitudinal<br />

77


d~lacemenf increasing with the thickness of<br />

the tens.<br />

optical cormlatlon-The process of<br />

ekcfronicatfy relsting a stored @refoWaPhk film<br />

~! of a geographc arm with a reaftima opticsl<br />

_ =Wird by phofogrephc or telsv”b<br />

sensors. H is used to provide poeitiiing<br />

information to CUTeCl or check air nevic@On<br />

and guidence eyaerns.<br />

optkal danalty-A consnon logarithm of<br />

mciprod of tmmmiftance.<br />

optlcd ffst-A surfeoe, usuelfy of glass,<br />

ground end peliihed pfans within a fraction of e<br />

wavelength of fight. Art eptbel eternent or gfase<br />

blank with en cptical fiat is used to 1ss1 the<br />

flatness of other suriaces, Atso called fist;<br />

optical plan..<br />

optical parallex—See Instrument<br />

perellex, definition 1.<br />

optlcel psth-The path followed by e my of<br />

light thrwgh en eptical system.<br />

optical plnne-See optical flat.<br />

optical plummst —See vertlcel collimator.<br />

opticel rectificetlohl%e process of<br />

projecting lha image af e fitted eerial<br />

photograph onto a horiiorrtal reference pfans to<br />

eliminate ths imags dbplscements ceused by<br />

tin of the aerisl csmers eI the time of exposure.<br />

optical square-A emall trend instrument<br />

urd in setting oft e righl engle. One form of<br />

eptiml squsre uses two plane minors placed at<br />

an angle of 45° to eech other. In use, one<br />

otjacl is alghted dhct, and another object is so<br />

pfsced thal ifs fwice-reffected imege appaars<br />

directly in fins with the first object. The lines to<br />

the point of observation from the w observed<br />

objects wifl then meet in a right engle. In<br />

mother form IX optical square, e single pbne<br />

mintrr is so ptsced thst d makes en engle of 4S”<br />

with e sighting line; one ~jecf is sighted direct,<br />

and the dher so plead tfrd its rafiected image<br />

is seen alse in tha sighting line.<br />

optical ●ystarn-All the parts of a compound<br />

lens end acoassory o@icsl perts which ere<br />

designed to corrtribule to the formation of an<br />

imege on s phomgrsphn emulaiin, w of e<br />

visual image, or of an image on a projection<br />

screen.<br />

MI L-HDBK-B50<br />

optkal vemfsr-A mkroscope with vernier<br />

Iii ruled on e gleas elide pfscad in the fccel<br />

plane conunon 10 the cbjective end the<br />

ey@ace, where if is corrpered wdh the image<br />

of the grsdusted circle.<br />

optical Wodg-ee wedga.<br />

optical-machanbal soanner-A system<br />

ufifizing a rc4ating - ard a dahxfor in<br />

conjunction with knses and prisms to record<br />

raflerled ardor emitted eldromagrdic energy<br />

in a scsnni~ mods IIkenS the ffigtrf peth.<br />

optical-projection lnatrumenta—A ckss of<br />

instruments which provide pmjectsd kwgae d<br />

photographic prints or &her opeque meleriel<br />

superfmpeaed on a mep or msp manuscript.<br />

Often ussd fer transferring detsil from nesrverticd<br />

photographs or other seurce material.<br />

optimum ground ●lovatlon—<br />

(phetogrammatry) The efe.ation of an assumed<br />

herizentel surfem in Ihe eraa photographed that<br />

would be pmjeckf at Ihe optimum distance in<br />

the pfotting instrument.<br />

orbitei aftitude-The mean altitude above<br />

Ihe surfece of the psrent bedy of the orbii C4 e<br />

astellile.<br />

orbital elemOnts-A set of sk parameters<br />

defining the orbii et a body eftrected by a<br />

central ferce.<br />

orbltsl Irrclirratlon-lhe direction thet the<br />

path of an ofiiing body tekaa. In the case of an<br />

Eerth setetfiie, ths psth may be defined by the<br />

angle of irdinstii of the peth to the Equator.<br />

orbital mode-A methed for determining the<br />

peaition of en unknown station posifien men<br />

the unknewm podtiin arrmt be viewed<br />

aimutfenmusly with known pdf!k.ns. The arc of<br />

the ssteliite otbit is axtrapoleted from the<br />

ephemeris of the setellife determined by the<br />

known stetions wtich permits the determination<br />

of the position of the unknown stetbn<br />

dependent completely en the =tellife’s orbital<br />

parameter.<br />

orbltel motion-Continuous motion in .x<br />

clcssd peth about and as a dkd resuff of a<br />

source of gravitational aftractbn.<br />

ortrltal path-One of the trecks on a primary<br />

178


txrdy% surface traced by a stmelfite that orbits<br />

etmul ff eeveref fff in a dkaction other thsn<br />

normel to the primary ~s asis of roferien.<br />

Each track ie diepleced in a dirscbn epposite<br />

end by an amount equal to the dagraee d<br />

rorstion between each sslsllite ortid.<br />

erbftal perfod-The irrtervel betrmsrr<br />

~0 PSSSSgSS of a eatel~de through the<br />

same poinf in its erbff. Also csfled portod of<br />

●atellite.<br />

orbftal phr~l%e plane of the eliii<br />

defmad by e oentral force ortrit.<br />

orbftal voloofty-The vebohy of en Earth<br />

seteflife cf other orbiting body et any given @rf<br />

ill fts Otid.<br />

orbft-The psth of a body or particle under tha<br />

krffuenca 04 a gravitational or other force. For<br />

ErMMPfS, IIrs Otbh d e oalastiil bafy or ealel~de<br />

is its peth refstffe to another body around whiih<br />

ff revotves. Tha term orbft is commenly used to<br />

designete a cfosed pelh. See alse centml<br />

force orbl~ intermediate orbit; nomlrml<br />

orbit; normal orbit; oaculatlng orbit;<br />

perturb-d orbit; polar orbit; sbatlonnry<br />

orbit; two-body orbit.<br />

ordinates—in a system of ractangutsr or<br />

Obf@e mordinstes, the finear distance of a<br />

pOim maasud hum the *Qordsl or X-exis,<br />

end parallsl to the y.esis. Also cafbd total<br />

latitudes; y+oordlnate.<br />

orientation Inset-See Inset.<br />

orientation pohrt-+t picture point selected in<br />

ame.s carvnen 10 vwticel photogrs.phs and their<br />

cwrespondng diiuas wh~h serves to<br />

aetebfii the relstienshii between the vertical<br />

and the cbhque. Tvm such points ere usually<br />

selected in asch vartiil photograph and<br />

Wensferred to the metching cbfique photo.<br />

orlsntstlon-1. The act of astsbkhitg correct<br />

miefbmshii in dmactii with mferanca to the<br />

points of the COmpnes. 2. The state of bahg in<br />

correct rafelbnship in direction with reference to<br />

!he points of the compass. 3. A msp is in<br />

eriarrtation wtmn the map ayrrbob ere pamllel<br />

wifh their oomespwtding ground features. 4. A<br />

surveyor% wand is in oriematbn Wlhe horizontal<br />

circle reada W vrlwn Ihs fine c4 coffimstiin is<br />

pedal Io the dirdion ff had at en asrfier (initisfJ<br />

posftion of the Instrument, w to a stendard line<br />

of reference. If the fine of reference is e<br />

M[L-HDBK-850<br />

IIWlidii, tha CkJe *II skw ezimulhe &ermd<br />

to thsl meridiin. 6. A photograph is in<br />

Orianfatien when h Cumcrty preeetis the<br />

i=x=r~e ~W ~ the umund or hen images<br />

en the phdegraph ~ in the same drection<br />

from the poird ef observation es do the<br />

~-i MSP _fs. 6.<br />

Phdogremmatric oriantetii is the racrastion &<br />

nehrel terrsh feetums at a miniature scale by<br />

the optical projection of m~ing<br />

photographs. The modal ls formed when all<br />

oorrespondii light rays horn the rw projacters<br />

interaad fn space. Sss afso sbsoluts<br />

orfentatlon; ●erolawellng; ●strogaod.tlc<br />

datum orlentatlon; basel orismtatlon;<br />

●mpiricat orlentatlon; ●aterlor<br />

orkmtatlon; grevlmetdc datum<br />

orkrntetlon; Interior orlontation;<br />

preliminary orientation; relativ~<br />

orlentatlon; alngle astronomic atatlon<br />

datum orientation.<br />

orlgfnal copy—l%e photographs, atlwork.<br />

scribed II?detil, typed matter, erdor other<br />

meterials to be p~assad for re~cduction. Also<br />

cded Orlglnel .<br />

orlghnl tnodOl=See maater modal.<br />

orlgirml negetlv*Thet negative developed<br />

from the film wtriih wss in e tamers megazine<br />

al the irrstent of exposure. Syrrurynrous with a<br />

first-generation photogmphic product.<br />

original eurvOy-See survey.<br />

orlgfnel-See orlglnal copy.<br />

orlghr—The reference poeifien from which<br />

engles, coordinstss or dtianws are reckoned.<br />

See also fafse origin; grid orlght.<br />

orthochromatic-(photography) 1. Of,<br />

pertaining to, or producing tonal values (of fight<br />

or shade) in a phetogmph, corraqending to the<br />

tones of nsture. 2. Designating an emulsbn<br />

sensitive to blua end green fight, M ncd to md.<br />

orthodromc-Sae greet clrolo.<br />

orthogonal mep proIectlon-See<br />

orthographic map proJactlon.<br />

orthogonal-At rfght angles ractangufdy:<br />

meeting, crossing, or fying at right englas.<br />

ofihogrephlc chert-A chart on the<br />

179


‘1<br />

(<br />

‘1<br />

orthogrrqhic proj@ion,<br />

orthographic map proJoctlon- A<br />

perapadtie azimuthal projecikm in whkh the<br />

projecting has, emawrting fmm a pairl al<br />

itinity, are perpandiilsr 10 s tangsrrt pfane.<br />

This pmjectii is usad chirtRy in navigational<br />

aatmnorrry for intamerrv erting cmrd@tas of the<br />

caksfii equator and horizon systems. Ako<br />

celled otihogonal map projoctlon.<br />

o~hom9trlc correction-A aystemat’c<br />

wrracfion whkh mual km ap@d to measured<br />

dfierence observed through Ievefing.<br />

orthometrlc .lovstloAn elevation to<br />

wtrii the orthcmetric Oorr@ien has beam<br />

applied.<br />

orfhomorphlc chert-A charl on vdich very<br />

small shapes are eorrectfy rsqmssenlad.<br />

orfhomorphk mep projection—See<br />

conformal mep projection.<br />

orfhophotograph-A phetogrephic copy,<br />

prepared from a perspective photograph, in<br />

which Ihe d rspkamants of images due to tift<br />

and relief have been removed.<br />

orthopttotomap-A photomsp made from an<br />

assembly cd orfhophotographs. It may<br />

incorporate special cartographic tmetment,<br />

phetogmphc edge enhancement, color<br />

=W@iono Or a mmbinatkm of these.<br />

orthophotomoealo-An ecaembty of<br />

orlhopho!egrephs forming e uniform scale<br />

mosaic.<br />

orfhophotoscope-A phelomaohanical<br />

device, used for producing orthophetogrspfas.<br />

orfhoplctomep--A pictomap made from an<br />

Orfhepholornap base.<br />

erfhorectfflcatlon-’f%e process of rerrmving<br />

imege displacement rmuead by tifl end tamain<br />

rafief. Tift, howevar, is not relevant in radar<br />

images.<br />

orfhost#rooocopy-A ccmkliiien wherein the<br />

horizontal and vertksl dstancas in e<br />

6teraoecmpic model appear to be at the rame<br />

ecale.<br />

osclllatlort-A double motion. one in each<br />

MIL-HDBK-850<br />

1<br />

dkactbn, of a pendulum. An osdflatbn is<br />

Corqlosad of fwe wccasive vbratbna.<br />

osculating ●lemont~The elaments that<br />

defins en osculating orbii. See eteo oeculatlng<br />

orbit.<br />

oaculatlng ●lllpaO-An eliiiee thet Is tangent<br />

at a point (called tha ●poch of oaculatlon) to<br />

a real Ohit.<br />

oaculatlng orbit-l%a ellipse that a ratellffe<br />

weukf felbw aftar a specifii time Y (the epoch<br />

of 06Cufatti) if aU fercs@ cAher than oenfml<br />

inverse squere forcae cee~ to act frem time<br />

Y’ on. An -feting orbd is tangent to the msd<br />

pcsturbad erbif and hsa the same vekcity at fhe<br />

point of tangency.<br />

other grids-t3rids other than tha Univarael<br />

Tmnsvarsa Mercator (UTM) and Universal Pofar<br />

Star~raphic (UPS), such as Caylcm Bett, Indii<br />

Zerre 11A,West Melaysisn RSO (Metric) Grid,<br />

etc.<br />

oufer Orl.sntsrtiOn-See ●xtcrrlor<br />

orientation.<br />

outer planet—The planets with orbiis terger<br />

than that of Mars; i.e., Jupiler, Saturn, Urenus,<br />

Neptune, and Pluto.<br />

outlier-A rnaasurament which dose net fd the<br />

remainder ot rnsasuremenls of the same<br />

quantity, where the reason for the discre~ncy<br />

cannof be assessed.<br />

oufllne ma~(JCS) A map which represents<br />

just sufficient geographic information to permit<br />

the correletien of addiiiensl data pfsced upon it.<br />

ovorcharglng—Appfy ing axcessive edrMenal<br />

infonnetien (semrsufiql or navigstionaf) to a<br />

map or chari resufling in cluttar.<br />

overhang+eerial photography) The addlt”mnal<br />

exposures beyond the boundary of an area to<br />

ba photographed, usualfy two ezpaeur~ at the<br />

ends d each strip 10 assure corrplste<br />

stereoscopic covarage.<br />

ovorlapplng grid-A mapr grid from a<br />

neighboring sraa prirneri~ intended to facilitate<br />

mifitary surveying amf fire-control. Sss eko<br />

major grid: secondery grid.<br />

ovorlapplng mosn-See coneocutlvo


moan.<br />

...<br />

ovarfapplng polr-(photogrammatry) Two<br />

photegraphrr taken a! dfferant exposure<br />

afatione in * a manner that a portion d one<br />

photograph almve the same terrain as ehown<br />

on a portion of the Mhar pMogmph. Thii term<br />

oovere the ganarat caaa and does trot iqrfy Ibt<br />

the phdographs wera taken for afar~ic<br />

examination. Sea dae atoraoscoplc pair.<br />

ovmfap-1. (JCS) In photography, the arrmurd<br />

by wh~h one photograph includes the aerrra<br />

area oovered by another, cuctomsrify aspresaed<br />

as a parcantaga. The overlap between<br />

auccaaabe ak photograph an a ffight line i6<br />

called forward ovorlap or forward fap. Also<br />

called and kap. The everfap between<br />

phetegm@ in djacen! prelfel fight Iinee is<br />

sailed side overlap or aide tap. 2. (JCS) In<br />

03rtogrephy, that prtierr of e map or chart<br />

whii ovetiaps the area covered by anethar of<br />

the same sar”w. 3. An area included wfthin two<br />

surveys of raoord, n4@I by record are daacribad<br />

as having one or more wmrnon boundary tines<br />

with ne inclusion of idarrfical parts.<br />

overlay—1. (JCS) A printing or drawing on a, s<br />

transparent or se.rnkancparant rnedum et the<br />

same esale as e map, chart, etc., to show<br />

derails not appearing, or requiring apacial<br />

emphads, on the Griginal. 2. (digfia!) A data<br />

layer, uaualty dsafing with enfy one as+ed of<br />

related information, WMch is U+ to supplement<br />

the data base, digital, image overfays. e.g.,<br />

overlaying a raster bee map with a vector<br />

afrmefine map. Overlays are registered to the<br />

base, by e common ceerdinate system. 3.<br />

(iiihograp~) Additional data, ore pattern,<br />

printed after the olhar Iaa!urea, so as to<br />

‘overlay’ them. See el= corractlon overtay;<br />

history overley; redaracope overlaya;<br />

●olectlon ovorlay.<br />

overprint-l. (JCS) Inforrmfiin printed or<br />

aterrqmd *n a map or chart, in eddiiion to<br />

that origindfy printed, !0 chow data of<br />

irrwdmca or special uea. Also called ●urprint.<br />

2. A feature of n corrpoalfe map image<br />

irwidantaliy printed co as to interfere with<br />

another feature.<br />

overrun control-@CS) Equipment anabling a<br />

camem to continue operaling for a<br />

pradalermined number of frames or sacends<br />

after normal cutoff.<br />

ovoreh~ot+ transparency or a print of a map<br />

MIL-HDBK-850<br />

wr@albn ueed for recording aupplemantaf<br />

mformat’mn.<br />

OWOI’E129 dlWt-A chml whoee naatline6 hava<br />

been extemled dlghtly, thereby ktoraesing the<br />

ahaat eize to include a amatl fend area m order<br />

to evoid p~fishiig a aqxwate graphii d that<br />

area.<br />

. . . . .-.<br />

181


panchromatic-(photography) SensKwe 10<br />

Iiiht of afl cofors, as a film or pfate amufaion.<br />

pancmtlc ●yste*A variabla power optical<br />

systam. Aiao celled zoom system.<br />

panel baa.-(cartography) The completed<br />

aaae@y d piacas of film poaittvaa onto a grid<br />

of Prq-hn tbhii is useds a ba~ for<br />

~mpt~tion. Al- called film moealc; panel.<br />

panelln~l. (cartography) Cutting a film<br />

poahive c4 a mep, in whiih some diatortien is<br />

irwdvad, into savetal pieces end cementing<br />

them in pfsce, on e projection constructed on e<br />

stable-base rnerkm, in such e WY that the<br />

error IS d~ribufad in small amounts thmughouf<br />

the area rather than being localized. 2.<br />

(surveying) The placement of panels on a<br />

oonlrd station to facifiieie station Hentifzation<br />

on aerial phdography.<br />

MIL-HDBK-850<br />

panel—l. (cartography) See panel baee. 2.<br />

(photogrsmmslry) An element of e target used<br />

for rnntrol station idcmtikation on aerial<br />

photography. Perrels are rnsde of cloth, plaslks,<br />

pfywood, or Masonite, and are poeitiinad in e<br />

symmetrical pattern centered on the aration.<br />

See 81s0 target.<br />

panoramic camera-A camera whiih takes a<br />

partial or complata panorama of the terrain.<br />

Some dasigns uillize a lens wfich revofves<br />

about an axis parpendicuiar to the optical axis:<br />

in c4her designs, the wnera itaaff is revolved by<br />

cfockwork to cbtain a panoramic field of view.<br />

See also frame camera.<br />

panoramic diatortlon-The displacement of<br />

ground points from their expected perspective<br />

pmilions, caused by the cylindrical shspe of the<br />

negative film surface and the scanning action of<br />

tha lens in a pmoramk camera system.<br />

panoramic photograph—Photography<br />

obtained from a panoramic camera.<br />

pantograph—An insfrurnarrt for copying<br />

mSPS, drawings, or o!har graphics at a<br />

pradetarminad scale. Pantographs capabla of<br />

edjuafnranf for several scales are known as fbmd<br />

ratio pantographs. See elso two-dimensional<br />

pantograph.<br />

P<br />

papar-strip method-(recf~-tkn) A<br />

graphiil mathcd d mating a poinkby-pdnf<br />

racfificatiort bssd on the irwarianca Ofthawoaa<br />

ratb. A rnodiketii ef lhw tacfmiqus parrnife<br />

Insp dafSil to be rw-b?ad hom an obGqus .eafial<br />

~~09R@I ~f@d on the projectivii d atrai@rt<br />

parafiactlc aberration-sae differential<br />

●barratlort.<br />

paraiiactlc ●ngle-l. (eafroriomy) The angle<br />

between e ~s hour atde and its varfkal<br />

circla. Afao called pormion angle. 2.<br />

(photogrammetry) Alto catted angufar<br />

parallaz. See angle of convergence.<br />

pamllactlc ormr—An emor caused by<br />

personal or Itirument perallax.<br />

paraliactlc grid-(photogmmmetty) A uniform<br />

pattern of rectangular lines drawn or engraved<br />

on some trsnsparenf material, usually glass,<br />

and pIscad either over the piratographs of e<br />

ateraosapk pair or in the optiil system of e<br />

stereoscope, in oder to provtie e continuous<br />

floating mark system.<br />

Derellectlc hreauellty—A sacondarv eti”-t in<br />

&lar perturbation-s in the Moon’s Ionf@de due<br />

to the eliiptichy of the Earfh’s orbit.<br />

parallax age-See age of paraliax<br />

Inequality.<br />

parallax bar—See ●teraometer.<br />

parallax dlffemnca-lhe dfierenos in tha<br />

absolute stamoacopic paralkaxas of two painta<br />

imagad on a pair of photograph. Cuatomarity<br />

used in dalermirdort of the difference in<br />

elevation of objects.<br />

parallax in ●ltftuda-Geocentric parefiax at<br />

any aftiluda. The expression is used to<br />

dtitrrguish the pamllax et the given eftitude from<br />

Ihe horizontal parakex when the body is in the<br />

horizon.<br />

parallax hraquallty-The variation in the<br />

mnge of tide or In the speed of tidal currents<br />

b-use of the continual change in the distence<br />

of the Moon from the Earfh. The range of Ma<br />

182


Srdtqaad dtiddcurrmfs.tand tohcmeaaaa<br />

he Moon apfmnrchaa perigee and 10 dac$fase<br />

Saifqmmchas apogee.<br />

pmslhx-1. (JCS) In photography. the<br />

~rant di+lecemer$ of the poaitiin of m<br />

object m ralstii to a rdarenca point due to a<br />

change m the point of observation. 2. The<br />

appararrf d~lacemant bafwwan objacfs on the<br />

Earth’s surfaca due to thaii diiemnca in<br />

elevation. Also called ●ngufar parallax; want<br />

of corr~spondmrco. Sea also ●bsoluto<br />

●tarooaoopic parallax; sga of parallax<br />

Inequality; ●nnual parallsx; ●quatorid<br />

horlzontd parallax: ?deo parallax;<br />

goocentrlc p~rdlax; horizontal parallax;<br />

Inatrurrmnt parallax; lunar parallax;<br />

raaldusrl parallax solar parallax; yparallax.<br />

parallel of attftude-A circle of the calestisl<br />

sphere pamllel to the horizerr cmnacting all<br />

points of aqual attiiude. AISAJcalled<br />

dmucantrtr; dtltuda circle; circle of<br />

●qual dtltuda.<br />

pamllel of decfinatlon-A circte of the<br />

celest’ml sphere parallel to ths cslastial equator.<br />

Also cslled celastlal parallel; circle of<br />

equsl docftnatlon.<br />

parallel of latltude-See drda of<br />

Iongltudo.<br />

parallel plate-An optical disk with optically<br />

fist, frarattsl tmrfa~ used aspacielly in epticd<br />

micmmeters. Atso called pfene plate. See<br />

also optical ffat.<br />

pamllel sphere-The celestiel sphere as it<br />

appaers 10 an observer at the pole, where<br />

cdeetial bodias -r to nxwa psrallal to ths<br />

horizon.<br />

parallal-A circle on the surface of the Earth,<br />

parallel 10 tha pfane of the Equator and<br />

contracting all points of equsl Letitude, or a circla<br />

paeltel to the primery grast circle d a sphere or<br />

sphamid; also, a closed cwve approxinmling<br />

such a circla. Also callad Inverao oarallal.<br />

Sae al- ●stronomic parallal; tillptlc<br />

parallal;<br />

parallel:<br />

parallel;<br />

parallel:<br />

parallal:<br />

pamllal;<br />

flctltloua parallal: gaodatic<br />

goographlc paralld: grid<br />

ground parallel; Iaomatrlc<br />

oblique parallal; photograph<br />

prlnclpal parallal; standard<br />

tranaveraa parallal.<br />

MI L-HDBK-850<br />

paramoterlxa-l%e act or process of<br />

deMX?MIg a geornatric ailustim with a<br />

rmlhamstical model canteining edjuetabla<br />

mtsants.<br />

paramatar—in general, any qusntify of a<br />

pmtrfam that is nd an hrrfaparrderrt variable.<br />

More apacifiilly ths term Lsoften ussd to<br />

dstinguhh from dependent variables quantifies<br />

tiih msy be as@nad arbkrary vahmw for<br />

P@~s of tfv? problem a! fmnrt.<br />

pammatrlc ●quatlOne-A eat of aquatiins in<br />

which the independent varisfias or cxmrdirAes<br />

are aach axprti in terms d a paramsfer.<br />

parametric krtltuds-l%e angle at the @ntar<br />

of a a@em whiih is tangent to the aU@soid<br />

along the gsodetic equator, betwean the pfane<br />

of the equator and the mdlua to the pdrtf<br />

intersected on the sphere by a straight line<br />

perpandiiulsr to the plane of the Equator and<br />

passing through the pdnt on the ellipsoid whose<br />

parametric falitude is defiisd. Parametric<br />

Islituda is an ausiliafy tstitude used in problems<br />

of geodesy and cartography.<br />

paraxlal my—A ray whoaa psth lies very nasr<br />

the axis of a lens and whiih intersects the lens<br />

surface et e point very cioss to its vertex end at<br />

nearly normsl incidence,<br />

partial tlds-%s conetltuent.<br />

pasa point-A point whose horizontal atior<br />

varrioel position is dsterminad from phorogmphs<br />

by photogmmmetric methods and whiih Is<br />

intended for use in the abadute orientation of e<br />

medel. Also cdlsd photogrammetrlc pcdnt.<br />

See also annex point; supplemental<br />

elevation; ●upplamontal position.<br />

paaelva aatelllte-A selellhe” which contakrs<br />

no pver syces 10 sugmen! output POwen a<br />

setelhte wfwch is a pessive raflsctor. Sea also<br />

■ctive satalllta.<br />

paaa-1. A single circuil c4 the Earth by a<br />

satelliie. See also orbit 2. The period of time<br />

a sstelliie is wiihin telemetry range d a deta<br />

acquisition stat”kxr. 3. (rnansuretion) Orre<br />

COmpl?t? -t of pointings or maasuramants on<br />

a sp~~lc Plate, reeeau, or other rn.adii<br />

contammg photograph~ imagery.<br />

patch-(digital) A small ares d irrformetii<br />

eplii into a data base or eofiwere in otdar to<br />

33


I<br />

I<br />

I<br />

update, corrplefe, or density the date content.<br />

psth—l%e project-km of the orbffal pfans d the<br />

mtetliie m the, Earth’s surfaoe: the bcue CI ti<br />

satellite eubpomt.<br />

MIL-HDBK-850<br />

PC ARC/lNFO-A vector data, rafatienal<br />

geegrsphii infonnetii syetam for a peraonel<br />

SUWtdW. Produd by Environmental systems<br />

Reeaemh Institute 8$ e Iew-and GIS.<br />

PC-1OOO camore-A trade name for a<br />

Qacdetk stellar sarnare having a focal length of<br />

1,000 mm.<br />

Peeus.allicw Invbraor+ cf.ms of inveraor<br />

pnwiding a mectumicel eelutiin for tha linear<br />

end angular elements of rectifiition, Also called<br />

scissors Nrvorsor.<br />

Poaucolller-Cerpantler lnvarsor— A<br />

modified Cepsnfier invemor coupled to the<br />

finkage system of a Paeucalfier invarecr to<br />

provide e mechanical means of sofvhg the<br />

linear and engufar elements ef rectif@atian.<br />

peel—(negative engraving) A t~hnique of<br />

removing the opaque stratum from hs<br />

W+K@K! bese. Peeling between etched<br />

ouihne Images prcdume a negative; psefing<br />

oulskje of the etchd outfine images pmdwes a<br />

positive. See also mask, definitbn Z.<br />

pbepslght slldade-A type of aliiede<br />

ocmeisting of e peep sight mountsd on a<br />

straightedge.<br />

peepslght compass—The sights of s<br />

%~~ f- by Mendeti with sfiis for a<br />

stghtlng medium rather than a telescope.<br />

peg sdjuetrnont-A method of adjusting a<br />

Iaveliig Inalrument of the dumpy level type, to<br />

make the fine of solfimetion pereflef with the axis<br />

of the spirit level, and employing two stable<br />

marks (pegs) the length et one instrument sight<br />

epert, Also called 11/10 peg ●djuetmamt.<br />

peg test-A method et testing the mlfirnstion<br />

adjustment of a Ievefing instrument.<br />

Pemborton Icvellng rod-A speaking rod<br />

marked wffh affemate mws of circular and<br />

dlernond-shaped dots, running diegonq!ly<br />

ecmse the rod. Read to hundredths ef a foot.<br />

pendulum ●lidade-A telescopk elidede in<br />

184<br />

which a pendulum dev”- replecee the<br />

mnventional bubbfe for mtabfiehing a horizontal<br />

reference fine from whiih verficaf angles may be<br />

measured.<br />

pendulum mstrolabe-An astronomic<br />

instrument ushg e constant attitude for poeitii<br />

datarmimdii. fts distinctive feature is a mirror<br />

~~~ On t~ of e pandufum tO fOrrn the<br />

arbfii horizon.<br />

pendulum lovef-A Ievefing instrument in<br />

whiih the line d eight is euferrmticelly<br />

maintained hcrisordnl bf mswms d a bdf-in<br />

pendulum &v&e. Afm callad ●utomatic<br />

Ievof.<br />

pendulum—1. In general, a body sc<br />

suspended es to swing frardy to end fro under<br />

the influence ef gravity and rnementum. 2. A<br />

verl”-1 bar so stswc+&5 from Mow by a stiff<br />

spring as to vibrate to and fm under tha<br />

combkd actien of gravity and the r@oring<br />

force of the epring. See else compound<br />

pendulum; dummy pendulum; ?roeswlnglng<br />

pendulum: Idle pandulum;<br />

Invar pendulum; Invarlabls pandulum;<br />

Menderthall pondutum; quarts . . .<br />

pendulum; rsmalver; rekstlve pendulum:<br />

reversible pendulum; simple pendulum;<br />

working pendulum.<br />

percent of enlargemenVreductlon—The<br />

fecfor by which an original is to be enlarged or<br />

reduced in rapmducfion. A 50 pement finesr<br />

enlargement et a 4- by 54nch eriginal weuld be<br />

Ginchss by 7 l/2-inches, whifa a 50 percent<br />

reduction of the -me original would be 2-i~hes<br />

by 2 l/2-inches. See alse ecale of raproductlon.<br />

parcant of alop*See gradlant.<br />

periapala—see perlcenter.<br />

parleatron-That point of the orbit of ons<br />

mersbsr of a deuble star system at whii the<br />

stars are nearest togelher. Cpposite et<br />

epeatron.<br />

pericenter—fn en elfiiticel orbii the peint in<br />

the orbit whiih is the nearest dIsfanca from the<br />

focus where the affreofing mass is Ioceted. The<br />

perkecder is al one end of the mmpr asie of the<br />

ortital ellipse. Oppeeite et apoapsls;<br />

epocentar; ●pofocue. Aieo csllsd<br />

porlapels; perlfocua.


I<br />

perlcynthlon-See perflurre.<br />

perlfocus-See perlcentor.<br />

perigee-to-porigae porlod-Se e<br />

mnomdlstlc period.<br />

perlgaa-lhrr pint et whiih a sslelh orbii is<br />

the last distance frum the centar of !ha<br />

gravitational fmtd of the earth. Opposite of<br />

spogee.<br />

MIL-HDBK-B50<br />

Perlhalion-l%e fminf in the atiiii orbii of a<br />

planet wtkh ie the rtaerasi to the Sun, when the<br />

Sun is the cantar of attraction. Opposlta of<br />

●phailon.<br />

porllune-The point of cbsesl approach of an<br />

orbiing tmdy to the Mwn. Opposite of aplune;<br />

apocynthlon. Also cd(ad perbynthlon.<br />

period of saialflte-See orbital parlod.<br />

I perlodlc ●rrors-in a cernplsta set of<br />

Obearvaticms thera corresponds to every<br />

.:, . A<br />

igdiwidual error mother error which is nwesasriky<br />

more or’i-” atpal and opposite. In a limited<br />

series the carrcallsriert may not be quite axed,<br />

but the error of the mean of n observations<br />

-Y be 6xp6cted IO ba I/n of that of a single<br />

measure, or less.<br />

perlodlc parturbationa-Perfurbe! ions to the<br />

orbii of a plane! or satellite which change<br />

direcric.n in regular or perkrdii fashw in lime,<br />

such that tha average effect over a long period<br />

d time is zero.<br />

pfwlodlc tarme-in tha mathematical<br />

SZfJfaSSbn of an orbti, tenna which vary with<br />

time In both magnitude and direction.<br />

pertod-1. The inlarvel needed to cornolate e<br />

~cia. 2. The interval batwean pesesgas “at a<br />

tbrad point d a given phase of e eirr@<br />

hsrmonk weve; Ihe reciprocal of frequency. Sae<br />

also ●nomaliatlc parlod; nodlcal period;<br />

orbltel period; alderoai pariod; aynodlc<br />

period.<br />

pormanwrt bsnch mark (PBM)-A bench<br />

mark d es nearly permanent character as ft is<br />

pmctiila to establish. Ueuslly designated<br />

simpfy as e bench mark or BM. A permanent<br />

bench mark is intended to msintein its elevet”on<br />

wkh raference to an adopted datum wifhoul<br />

185<br />

changa ovar a long period of time. Also catted<br />

monumwtted bench mmrk.<br />

perpondicuiar ●quatlott-(traveme) A<br />

rmndiin equation to reduca to zem the<br />

algebraic sum of the pmjaotibrrs 0( the separate<br />

Ii cd a traverse ~ pqmdcarlera to a<br />

faed line with vdich the travaree fcnrre a cbsad<br />

figure.<br />

parparrdlculer-A perpandiiuler line, pfene,<br />

etc. A distinction is sometimes made between<br />

pe~ndabr and normal, the fermar applying<br />

to a fine at right angiea to a etrdght he or<br />

pfana, and the kdtar referring to a ~me a! right<br />

angies 10 a curve or cutved surface.<br />

personal equation-lhe time interval<br />

between the serrcory @rception of a<br />

phenomenon and the mo!er reaction thereto. A<br />

personal equation may be either pceittie or<br />

nagetiie, es an observer may anticipate tha<br />

occurrence of an event, er wait until ha actually<br />

eeee it occur before reeking a record. Ths is a<br />

systermtic error, trasted ae the constant type.<br />

personal ●rror—An error caused by an<br />

imtiiiduet’s personal habits, hk inability 10<br />

perceive or measure .iimenaionsl values exactly,<br />

or by h!s tendency to reecr mentally and<br />

physically m a uniform manner under aimitsr<br />

conditions. i! may be a eysterndc error, il it<br />

occurs regutsriy or a blunder tf il occurs once. A<br />

cerlein amount of mimr paraoml errer can be<br />

included with random armrs.<br />

paraonal parallax—See Inetrumont<br />

paraiiax, definition 2.<br />

perepecthre ●xis—See axis of homoiogy.<br />

porspectlve contar—The point of origin or<br />

termination of bundles of perspective rays. The<br />

two suh poirris usustty associated with e survey<br />

photograph are the intarior parapactive cantar<br />

and ihe exterior perspective center. In a perfect<br />

Iena-camsre system, perspective rays fmrn the<br />

interior perspective cent er to the phclographz<br />

images ancloss the same engfes as do the<br />

mrraspcnding rays from tha exterior perspective<br />

center to the objects photegrephed. In a Ians<br />

having distortion, this is true only for a particular<br />

zone of the photograph. In a perfectly adjusted<br />

Ians-cwmrra system, the axterbr and interior<br />

perspective centers correspond, respectively, to<br />

the fronf smd rear nodel points of the camera<br />

Ians. Also celled canter of projection.


porspectlvo chm’t-A chari on a perapacfive<br />

Pr@actiin,<br />

perspective grid-(JCS) A network of firms,<br />

drawn or superimposed on e Photograph. 10<br />

represent the pers+ecfive of a syafernrdic<br />

natwwk d fines on the ground or datum plane.<br />

~~h~~ad Canadian grid. Sea al= grid<br />

parapectlvs map projoctlon-A map<br />

project’km produced ~ efrdght fines radiiting<br />

from a aslacfad point and passing lhreugh<br />

poirrfs on the earth’s surface to the projection<br />

surface. Alee called geomctrlc map<br />

pro)actlon.<br />

parepactlvo plane-Any ptane ccmlaining<br />

the perspective canter. The intersection ef a<br />

perspective pfana and the gmurrd will ahvays<br />

-r as a straight fins on an ae~I<br />

photograph.<br />

MIL-HDBK-850<br />

parspectlva proJactlon-The projection of<br />

points by sfreighl firma drawn through them from<br />

aoma given peint to an intamaction with the<br />

plans et projection, Unless etharw.iea indicaIad,<br />

tha point of pjection is understood 10 be at a<br />

finite distarwe from the plane of projection,<br />

parspectlva ray—A line joining a perspactiva<br />

canter end e peirrt objact. See else Image ray.<br />

perapectlve apatlal modat-Crptical<br />

raconatrucfion of an area of tarmin shcwing<br />

depth by viawing a pair of aarial photographs<br />

through a atersoacapa.<br />

parspactlva view—A three-dimensional<br />

representation generated with a reference to a<br />

app~iawer location on or abeve Ore surface<br />

perspectlva-l%a appearatwe to the eye of<br />

objects in rasped to their relative distance and<br />

pesifion.<br />

perapectlvity—The corraepondence batwaen<br />

the points, lines, or pkwras of two geemelric<br />

configurations in perspective. Usually raf erred to<br />

as linear pe-ivii because the true<br />

parapdive center must be recoverable befora<br />

angular percpedvhy can be included.<br />

perturbation-in celastial mechanics,<br />

dtierencas of the actual orbii from a central<br />

188<br />

fercs odid, arising from some axlar’rd fo=<br />

such es a thkd @ altrac4ing the other two; a<br />

rasisling nrerlum (atmosphere): failure of the<br />

Parerrt bodytoad aaapdrrtmaaa, and so<br />

forth. See alse gravitational pwturbatlons;<br />

long period parkurbatlons; Iunlsolar<br />

porfurbatlone; nongravltatlonal<br />

perturbatlona; perlodlc perturbations;<br />

●ocular perturbatlona; short parlod<br />

perturbations: torrastrisl parturbetiorm.<br />

perturbed orbff-Tfra otbit of a aatelfiie<br />

differing fmm Ms norrnaf orbii due to various<br />

d=turblng affacfa such as nonaymmefrical<br />

gravltstkmal affecls, atmoapherk drag, radiil’on<br />

pressure, acd se forth. Sea alao perturbation.<br />

perfurtrlng factom (forces)-in celestial<br />

mschanii, any force that ads on lha orbi!ing<br />

body to change its ortit from a cen!ral ferce<br />

orbit.<br />

phase age—Saa ago of phase<br />

Inoquallty.<br />

phaao angle-l. Tha phase difference of two<br />

periodically recurring phenomena of the sama<br />

fr~uency, expressed in angular maasura. 2.<br />

The angle at a celestial body between the Sun<br />

and Earth.<br />

phase inequality—Variations in U-m tide or<br />

tidal currents a-iated with changes in the<br />

phase of the Meon. At new and full Mom<br />

(springs) the tide-prcducing forces ef the Sun<br />

and Meon ad in ccmjuncfion, reaulthg in greater<br />

Ihan average tide end tidal currents. At first and<br />

teat quarters of the Moon (naepa) the tideprcducing<br />

fore= cppoaa each other, resufting in<br />

smaller than everaga tide and tidal curranm.<br />

phase-l. (general) Of e petiedic quanlify, for<br />

a ~flicubr Valua of the indapendenf variable,<br />

the fradional part of a period through which the<br />

independent variebfa has advanced, measured<br />

from an arbiinwy reference. 2. (surveying) The<br />

apparent dkplacernanl of en ob)~t or s’wnal<br />

caused by ona aide being rrwre atrengfy<br />

illuminated than the other. The resuftant error in<br />

pointing is aim’iar 10 the armr cauaed by<br />

observing an accantric signaf. 3. (astronomy) A<br />

atege in e cycle of r-rring aspects, =u6A by<br />

a ~~e~tb Varieticm of the illumination of an<br />

object. The Moon passes through ifs phases,<br />

new Meon to full Moon and back to naw Moon,<br />

as its position relative to the Sun and Earth<br />

changes.


MIL-HDBK-850<br />

Phlladolphla Iovallng rod-A two-piece<br />

fer@ rod, with gredut”m marks an efyfed that<br />

itmayalso beuaadaa aapaekingmd. For<br />

heights grader ttren 7 feet the target is clarrpd<br />

at 7 feet, and raised @ exfend@I the md. A6 a<br />

Wget md, h is mad try vam’mr to trowandths of<br />

a foot ae a Sp6atring d, to haff-trrmdredfhx of<br />

a foot.<br />

photo sltltuda-f-teighl of an aircrafl above<br />

the mean elevation d the terrain to be<br />

photographed.<br />

photo Index-l. An index map made by<br />

assembling the indwidual aerial photographs<br />

into their p- ratetiie pdfions and copying<br />

the assembly phofegmph=lly at a reduced<br />

scale, Atau called Index to photography;<br />

photo plot; plot map. 2. See ●ortia plot.<br />

photo plot-See photo index, definition 1.<br />

photo pymmld+ component of an<br />

enalytbal mathcd of precise detemninalicm of<br />

phokrgrephic tilt which repraeants e spacifii<br />

,.> .,,<br />

-<br />

spatial mrrfieuration formed by three control<br />

points of known posifii on tha phofegraph<br />

(forming a trkmgle) rmd the e~re station.<br />

When used with the ground pyremkl, b permits<br />

the exscf peeitiin of the exposure station to be<br />

determined and, by analytical tmhniques, the<br />

I exact lilt of the ptwlograph.<br />

pyramid.<br />

Ses also ground<br />

photo revlslon-The process of making<br />

chmgee on a map baaed upon infcmnation<br />

obtained from a study of aerial photographs.<br />

photo ecafe-See ecale, definif”mn 1.<br />

Photonlldade--A ohofottremmetric instrument<br />

,. . . .. . .<br />

having a telescopic elidade, a ptateholdar, and<br />

e hinged rulhg arm mounted on s tripod frame.<br />

It Ls uaad fer pbfting fines of diradkrn end<br />

measuring vertical angles to selected Iaetures<br />

aPrin9 on diiue and terrestrial<br />

photographs.<br />

photoangulator-See ●ngulator.<br />

phstobss*The dffitance batwaen lhe<br />

princ”@alpoints of two adjacent prints of a series<br />

of vertical aerbl photographs. If is usually<br />

measured on one prim after tranafenfng the<br />

principal point of the other print. Sae also bee.<br />

line. defintfion Z.<br />

1s7<br />

photocomposelo mechanicelfy i- one<br />

or mare knagea by afap-and-mpeat axposums<br />

in pradetanninad poaitiine on n press pbte er<br />

wmlpa by means of e photoCortylOaing<br />

mechme.<br />

photocorrtour map-f%sentially, a<br />

t~raphic rrmp upon which the plsn”metric<br />

detail is dapkfad photographically in ke cured<br />

*i. ff ~ ueuaffy prepared from cwvergenf<br />

photography efflmugh cmwantionel verikel<br />

photography can be used.<br />

photocontour process-A pmoesa<br />

davabpad to combine, in a pholocontour map,<br />

that information normslfy portrayed on a<br />

lopegraptk dmwing end an earial photograph.<br />

The tyatem ususlly k mmposad of three<br />

elements (1) e cunventiorrsl ateraopbffer for<br />

oonlduring; (2) a mcfiiier for fill rectifiithr of the<br />

aerial Pholograph& and (3) e zone printer to<br />

eliminate relief displacement. It is deaignad to<br />

utilize convergent phetographe etthough normal<br />

vertical phetegraphe can ba r.diiiied ee well.<br />

photocontrol basa-See control bneo.<br />

photocontml dlegram—Any selected base<br />

MSP Of phOIO index cm wtkh prc$msed ground<br />

control netwerks, te imluda prcpaed posilioms<br />

for psss points, ere defineakd. See also<br />

photocontrol index mep.<br />

photocontrol index map-Any eetaofed<br />

base map or photo index on W)ch ground<br />

amtrot and photo “klentifiad ground poinfa are<br />

depicted end identified. sea also<br />

photocontrol djagmm.<br />

photocontrol point—sea plctum control<br />

point.<br />

photogonlomeler-An instrument for<br />

messuring angles from the true perspective<br />

center to points on a photograph.<br />

photogremmetrlc cmrrem-A general term<br />

trpplicabJe to eny camera used in any of the<br />

several trranchaa of photogrammetry.<br />

photogmmmetrlc compMatlorr-See<br />

compilntlon, definifien 2.<br />

photogrammettlc control point-A<br />

horizomal centml point which hes been<br />

~afablished by phofogrammafric triangulation.


photogrammotrlc conWf-(JCS) Control<br />

esf8blished by pfrotogramnrstric metfnde as<br />

distinguished hum mntrol Easfablished by gnxnd<br />

methods. Ales called mirror control;<br />

multlplax control.<br />

photogrammotrlc mep-A topogrephc map<br />

pmduoed from aerial photographs and gmdetii<br />

control data by rmene d phdogrammetric<br />

instruments. Also called steraomsrtrfc map;<br />

storeotopographlc map.<br />

photogramm.strlc pofnt—see paaa polni.<br />

photogrammotrlc pyrsmld-An rmafyficel<br />

methcd f~ thm pradsa determirratien of<br />

phetograpiic tift, sonsiating d a ground pyramid<br />

and a pfrofo pyramkt, whish represent a spatkd<br />

configuration formed by Ihree control points of<br />

krwwn posflic.n on the photogmph (forming a<br />

triangle) and the exposure station. See also<br />

ground pyramid; photo pymmld.<br />

photo grammetrlc rsctlficetlon—S e e<br />

roctlficatlon.<br />

photogrammntric suwey—A survey utilizing<br />

either terrestrial or aerial photographs.<br />

photogrammatrlc triangulation—See<br />

phototrlangulstion.<br />

photogrammotricatly dlgltlzed-tligitized<br />

from esrial phofogmphs and geodatic control<br />

data by mamns cd photogrammetrk instruments,<br />

previding threedim-ienal oootdkuatec.<br />

photogrammotry-1. (JCS) The eeience or<br />

art of obtaining reliebfe mamurerrranta from<br />

ptrotogmphic images. 2. The preparation of<br />

sherrs and maps from eerial photographs using<br />

stewxcopic aquipment end methods. See also<br />

aarlal photogramm@ry; ●nalytical<br />

photogrammetry;<br />

8teroophotogramms4 ry; terreutrlaf<br />

photogrammetry.<br />

photograph cerrter-The center of a<br />

KdIOtOOmph as indited by the im99aS of the<br />

fducb-l rriark(s) of the samera. In e perfectfy<br />

adjusted camem, the photograph center and<br />

the principal point ere identical.<br />

photograph coordlrtmtos-A system of<br />

coordinates, eiiher rectangular or polar,<br />

describing the ~shion of a ~int on a<br />

MIL-HDBK-850<br />

188<br />

photograph.<br />

photograph merldla*The imepe on a<br />

photograph d any horizontal line in the +ecf<br />

6PW= which is Parefial to the prkipal plane.<br />

Since ati -h fines msst.at infinity, the irmgs of<br />

the meeIing point is at the infemectkm of the<br />

vmti~tititi~-anddl<br />

phOtOQ~ maridiarrs pass through that point.<br />

photograph rtadir-The point at tvhiih a<br />

vertical line through the perapedve canter of<br />

the csnrara Iena piemac ths pfane of the<br />

photograph. Also called nedfr Polnc<br />

photographic plumb poln~ plumb pofnt.<br />

photogmph paralfal-The image on a<br />

photograph of any horizontal fine in the object<br />

_ - is Parpetiiutar to the ptinciil<br />

plane. All photogmph parellels are parperrdiiular<br />

to the prirwipal Iina.<br />

photograph parpandicular—The<br />

perpandiculer from Ihe interior pe~ive<br />

center to the plene of the phcdograph,<br />

photograph plsrre-The pkme in the camera<br />

in vhich ttw @ate W. fiim.is heLd. It is rrd excclly<br />

lhe primary tmd plme of the lens, bul k e<br />

plans pfaced so es to secure the best Mama<br />

of shsrp fetus on ell parts of the pbte or film.<br />

Also sailed Image plane.<br />

photograph plumb point—See<br />

photograph nadir.<br />

photographic covaraga-(JCS) The extent<br />

to which an area is mvared by photogm@ry<br />

from one rnkion or a eeriee of rnisaimre or in a<br />

peried of time. Cmerage in thm sense conveye<br />

the ideal of avaitdility of photography and ia not<br />

a synonym for the word photography.<br />

photographic datum-The affective datum<br />

for each phetegraph. It ia a horizontal pfane at<br />

the avarsge elevation d the tan’sin, on wliih<br />

d=tances rrreaaumd will be al the average aeele<br />

of the photograph.<br />

photographic ●xposure-The time of<br />

exposure multiplied by irradiance or illuminance.<br />

photographic lntarpratatlon-The<br />

examination of photegraphc imege6 for the<br />

purpose of Identifying objects end deducing<br />

thek eignifke.rrce. Also celled<br />

photolntarpratation. SSe dse Imagary<br />

interpratatlon.


i<br />

I<br />

photogmphlc readhrg-(JCS) The simple<br />

r-nifhn ~.. d natural or marr-rnda features<br />

horn photogrepha not invohfing tiger-f<br />

inlerpretat”mn techniques.<br />

photogmphlc reduction-lhe production of<br />

e naget”we, diepoaMie, or print at a scale<br />

smaller hut the wigiml.<br />

photogmphlc scsle-(JCS) The ratio of e<br />

dialarrca measured on a phofegmph or moaak<br />

to the cormaponding distance on the ground,<br />

claaaiied as follows very large-scale-l :4,999<br />

and Iergec Iarge-ade-l :5,000 to 1:9,999:<br />

m9diUm4iCSl*i :10,000 to 1:24,9W, amsllseals-1:25,000<br />

to 1:49,999; vefy amall-ac@3-<br />

1:50,000 and sndler. Sss also acde.<br />

MIL-HDBK-850<br />

photogmphle 8UNay—A survey<br />

acoompfiahad from either aerial photographs or<br />

terraatrial phctegraphs, or from a combination of<br />

both.<br />

photographic zanlth tube (PZT)-The<br />

moat praciae instrument for meridian<br />

ebaervationa. No corrections are required for<br />

.- Ievel, azimuth, cdlimatkm, or flexure. Each<br />

cbwvation gives a nreesure d both the time<br />

end the Iatilude.<br />

photography—The art er preceaa of<br />

producing images on sensitized material<br />

through the eden d light. The term<br />

photography in aometimas incorrectly used in<br />

pleca of tho term photographs. See also<br />

analytical photography; composite air<br />

photography; continuous strip<br />

photography; control point<br />

photography; convargenl photography;<br />

cross-fllght photography; diract<br />

photography; fan camsra photography:<br />

horizontally controlled photography;<br />

Indlract photography; Inortlal reference<br />

photography; Iorop photography:<br />

mapping photography; motrlc<br />

photogmphy; multibrmd photography;<br />

positional camara photography; procefia<br />

photography: radar photography;<br />

radamcope photography;<br />

mconndasanca photography: ●horan<br />

controlled photography; spilt vorftcal<br />

photography; aupplamantal<br />

photogmphy: tarraln profile<br />

photography; trlcsmora photography.<br />

photograph—A general tarm for a positive or<br />

negative picture made with a camera on<br />

aanshiuad nmteriaf, or p+fnfs from such e camera<br />

original. Soa also ●arlal photogmph;<br />

●rnotated photo-graph; eqrrlvdont<br />

vertical photograph; homologous photograph;<br />

horizon photogmph; horfxontal<br />

photograph; moldod ●erial photograph;<br />

multlple-kta photogmpft; oblique dr<br />

photo-graph; erffrophotograph; psnommle<br />

photograph; plnpolnt photograph;<br />

termatrld photograplv varticd<br />

photograph; wing photo-graph.<br />

photoidontlflcatlorr-(mrrveyirrg) The<br />

datacfiorr, idant#kafien, and marking d ground<br />

suwey afatiena on aasial photogmpha. Positive<br />

idenfifkation and kbcatkm is required if survey<br />

data are fo be used to ccmtml phetcgrammatric<br />

compilation. Atse called control-afatlon<br />

Idontiflcatlon.<br />

photolnterpretatlon kcy-t?eferenca<br />

materiels designed to facilitate rapid and<br />

sccureta idenfiiicatic.n and iha delarrninatierr of<br />

the aignifiinca of objacf6 or oondiiions from an<br />

analysis of their photo imagea.<br />

ptrc40hrtorpretntion-Sae photographic<br />

Inierpratatlon. . . . . . . . .<br />

photolntarpretrzmeter-A device, used in<br />

conjunction with e pocket ateroosc+a, fOr<br />

making vertbl and horizontal meoauramsmta.<br />

photolithography—A Mhographii prweaa in<br />

which phetographk products are used to<br />

prcduce an image on the PrhN”mgsurface. See<br />

also Ilthography: offaot lithography.<br />

photomap backup-A photomep printad on<br />

the bock of a line map of the same area and at<br />

the same scale.<br />

photomapplng—The pmcass of making<br />

~W Or charfa ,from Various -S of<br />

photographs, @h reference to other source<br />

mOpa, clxwfs, or aufveya.<br />

photomap-(JCS) A reproduction of a<br />

photograph or phelomoaaic upon wheh the grid<br />

lines, marginal data, contours, place names,<br />

boundaries, and other data may be added.<br />

photomochanlcal—Perfainin~ to or<br />

designating any rapmducfkm prose.% by a<br />

wtiinslion of photographic and machanlcal<br />

operations.<br />

189.<br />

photomvlaed map-A topograph~ or


pkrnirrudric map whiih km bean rwiaad by<br />

pholoplenimetric meNv2cis.<br />

photosphoro—11’re irstanaafy Lvight portion of<br />

the Sun v“bble to the u’taidad eye.<br />

photothaodollte-A gmurrd swvaying<br />

instrumsnf combining e aurvay csrnam and a<br />

transit; used for massring the angular<br />

orientation of the csrmere et the moment of<br />

espoeure. Also csllad oamers trandt.<br />

pfrototopography-The science of surveying<br />

in tikh the detail is pidfad entirefy fmm<br />

pfmtographs taken at suitable ground stat”ksns.<br />

See also terrestrial photogrammetry.<br />

phototrlsngrrlation-The process for the<br />

errtanaicn of horizenlel ertribr vartiil mntrd<br />

whereby the massuremenls of angles er@or<br />

dstsncaa on overlapping photographs ere<br />

reislad into e epal’ml solution using the<br />

perspective principles of the photographs,<br />

Ganemliy, thk prrxess involves using seriel<br />

photographs and is called aorotriarrgulatlon,<br />

aerial triangutatlon, or photogremmetrlc<br />

trlangulstlon. See else smnlytlcal nedlrpoint<br />

triangulation; analytical<br />

phototrirrngulatlors; analytical radial<br />

trtanguletlon; Arundel method; brldglrrg;<br />

cantllovar artamsion; direct radial<br />

trlangulatlon; axtenslon of control;<br />

graphical radial trlnnguiatlon: handtemplet<br />

trlengulatlon; Iaocantar<br />

trlangulatlon; machanlcat tomplet<br />

triangulation; nadir-polrrt trlangulatlon;<br />

radial trlanguletlon; slotted-tamplet<br />

triangulntlon; aplder-tamplat<br />

triangulation: atoraotamplat<br />

triatrgulatlon; ●teraotrisnguiation: atrlp<br />

radial triangulation; templat method.<br />

phototrig travarsa-A vertkai-angle traverse<br />

ernpbying phototrig methods; e procedure for<br />

detmrrining aievet”mns trigonomakicsily, wherein<br />

horizontal distances are delermkred phot~<br />

gmmmslrkelly and vertical angles ere eilher<br />

measured instrumentally in the fmtd, or ere<br />

obtained fmm measuramants on terrestrial<br />

photographs.<br />

phototypaaattar-A type satting unit<br />

@JmPri~n9 k Sepemte and indepandant unifa,<br />

the keyboard unit and the photographic unit.<br />

Composition is accanpliiad at the krryboard<br />

wrii, as.swrtislfy an eiectrk typawritar, which<br />

l?rod~- e lypawrtien proof copy end a<br />

perforated tapa. The tapa is then fad al any<br />

MIL-HDBK-850<br />

190<br />

convenient time theraaffar to the photographic<br />

IWit * pmducaa a right-reading fdm positive<br />

Suhable for rrticklp Wcrrk<br />

physkal characteristic-(target) The visibie<br />

nmtarisi aspects of a target or installation,<br />

inctucfing, but nol timirad to, dimensions,<br />

atruduml metariaks, fxadorninrmt haigM,<br />

wrrfigumtim, and orientation of ifs various.<br />

~wma 6M se buildings, SINCWSS,<br />

runweys, end aaaodatad facilities and sarv-.<br />

phyalcaf gaoderiy-See gravlmetrlc<br />

gaodasy.<br />

phyaiographlc pictorial mep-A map with<br />

relief dapktad by the syslerrmtic ap@iition of a<br />

atsndardizad sat of mnventionel pictorial<br />

symbols, baaed on lhe cirnpiifii appaamnca of<br />

the physical fasturas they represent, as viewad<br />

obliquely from the air at an angle of about 4S”.<br />

piano-wiro tapa-Piano wire used instead of<br />

e metallic ribbon tape when il ia edviaable to<br />

mnt ml hydrography try precise traverse rs!her<br />

than by a weak axlenskrn of triangulation,<br />

pictochrome procese—The process<br />

employed tO prdme Pktomsps. Consists of<br />

three tonal separations pholograph~ily<br />

exirsclad from a photornmaic, blockout masks,<br />

drstfad symbols, and names date.<br />

pictograrn-A msp of distribufkma. eapecidiy<br />

mmrrvxfiiies in which small pkforial<br />

represantstive synrbofa (e.g., aacke, bridra,<br />

barrels) ere located over the arm of producl”kn.<br />

pictoline precosa-+ photographic masking<br />

prmass utiiiiing a rotating vacuum frame 10<br />

produce an edga-emhencad line image from a<br />

continuous tone image.<br />

pictomap-(JCS) A topographic map in which<br />

the photographic krragery of a sandard moaa”ks<br />

has been convartad into interpretable cdcrrs end<br />

ayrnbois by means of e pktomap pmcass. Saa<br />

also pictochroma procosa.<br />

pictoriai symbolization-(JCS) The u= of<br />

symbols whch mnvey the visual character d<br />

the features they rapraaent.<br />

plctotone process-A photo- lithographic<br />

method from which film for rapmductim and<br />

transfer 10 printing platen is danvad fm the<br />

printing of monochrome pholornrspa and<br />

piclomaps. The prmaas provides e random


I<br />

grsnutar-like affect which Viaibfy sharpens ths<br />

dafinttkn ol fea:um6 and aepsmtion of l-,<br />

and, in many instances, M euperkr 10 Iudftons<br />

printing.<br />

pktum control polrtte-%pplemenhsry<br />

horizomet and Vwfkal Wntrol pointtl that ●a<br />

raquired for the inutwdiete control of msppirrg<br />

operatkna In a gkfen ems. Thaee P“Ms are<br />

eatsbiii by field awvey pardaa irr apedfIs2<br />

Icealbm and are prac&ly idantifiad on the<br />

~~1 ~wk for the projscf. Also CSIM<br />

photocontrol point; plcturo pohrt.<br />

plcturo ●kmsmt (plxol)-See plxd.<br />

pktum plmw-A plane upr whiih can be<br />

projactads system of lines or rays fmrn an<br />

~tohrrnani rnagsrcbr picture.in<br />

PamPtitie drawing, the system of reys is<br />

urdersfoad 10 converge to a single point. In<br />

phelogrsmrnetry, the photograph is the picture<br />

plene.<br />

plctum point—See control poino picture<br />

control points.<br />

MIL-HDBK-850<br />

pkA chart-Special dlS1’tS, CWerirrg Ihe<br />

ocesns ot the world for esch rrrenth of the year.<br />

is6usd on one sheet for 3 rrmnths at s lime on e<br />

qusrtsrty besii. They show mstserdogic,<br />

oceanogmphc, and hydregrsphw data for use<br />

in conjunction with cenventionel charts. Thsly<br />

articles of profeasicmd inleresl to the sesfarer<br />

are published on the backs.<br />

pilot sheet-A sample of a new series, made<br />

as a frial in anfi@mtion of a msp aeriae, to<br />

disckea the problems which occur in the verieus<br />

stag= of compilation, drafting, and<br />

repmductbn. It is Ister used as a guide in<br />

developing the ssrias. Atrm celled prototype.<br />

Soe else ●xperlmentel map.<br />

ollot’a treoe-(JCS) A rwmh wariay 10 e mav<br />

~de by the pitot of’ a phottiraphlc -<br />

reconnaissance aircrafl during or knmadistety<br />

after a sortie. It shows the location, direction,<br />

number, and order of photograph runs made,<br />

together with the camera(s) used on each run.<br />

pilot-Saa eoliing dlreetiorm.<br />

plnholee-Tiny clear spots on negative imsg=<br />

caused by dust. air bubblas, or undiasotvad<br />

chemkata.<br />

plnpolnt photograph-(JCS) A mingle<br />

191<br />

pho@r~h or a ster~ir of e specifc objecf or<br />

tergat.<br />

plrtpolnt target-(JCS) In mtillery and naval<br />

gtalfmsl@p@, atsrgetkwsthensa matwain<br />

d-meter. Sea else ●roe brgo~ prooiee<br />

Inatallatlon poeltlon.<br />

plrr+.survaying) A metal pin used for nmrking<br />

taped measuramonts m the ground. A set<br />

consists at 11 pine. Also sasllad cftsinlng phu<br />

surveyor’s smow; taping ●rrow; taping<br />

pin. See else turrrlng point pin.<br />

pttch-1. (JCS) The -lien of an airueff or<br />

stip ebmd &a bteml exis. 2. (J@ In air<br />

photography, the csmere mtstiin ebouf the<br />

trsnsverae axis cd the aircraft. %<br />

(phetogremtry) A rotation of the camera, or<br />

of the photograph coordinate system, about<br />

either the phdogreph ysda or the exterior ysxia.<br />

in some phofogrammetrk inslrumants and<br />

in anslyiiil Spplkations, the eyrrbl phi (+) my<br />

be used. Also called longftudlrtel tilt: tip<br />

(wbiih is an obsolete term): Y+llt.<br />

plxOl-A pkfure element, smallest unil of<br />

inforrrdion in e grid.oall map .or scanner imsge.<br />

Also known ee PEL.<br />

place nama-See toponym.<br />

place—See posltlon, definition 2.<br />

plan position Indicator (PPI)-1. (JCS) A<br />

cathode-my tube cm which radar returns are w<br />

displayed as to besr the same relat”~atip to<br />

Ihe trsnsmitfer as ths cbjscfs giving rise te<br />

them. 2. A csthoderay indicator in which a<br />

signal eppeara on a redial line. Distance is<br />

inckatsd mdially end bearing as an artgla.<br />

plan range-(JCS) [n air photegmphm<br />

wnnsisasnce, the horizontst diaranca fmm<br />

the pint below the ahcmff to en cbject on the<br />

ground.<br />

plarw coordlnatoa—See plan.<br />

rectangular coordinates.<br />

plene curve-See plane dtlptlcel ●rc.<br />

plane .Illptlcal arc-Arry pert of the line<br />

formed by the irrtersecfien of a phe end an<br />

ellipsoid. Ah csbd piano curve.<br />

plane parallel plate-See parellel plats.


1<br />

plan. polar coordinator-A system of poier<br />

ooordiiaa in whiih the pdrrts sfl Ii in one<br />

plsne. In the Iarnirrobgy of anatytii gaemstry,<br />

the d~lanoa from the origin to the poinf is ffre<br />

rnegmtude of the rartkrs veclor and the polar<br />

dislmrca is the vectorial arrgfa.<br />

plan. rutangulsir coordinatea-A system<br />

Ofcoodnat en in a horizontal pfene, used to<br />

describe the positions of points with respect to<br />

an origin. Also salted plans coordirmtos.<br />

plane survay-A survey in whiih the surface<br />

c4 the Emth is conaidsmrf e pfsne. 1% arnsll<br />

simas, precise msulte may ba oMalnsd with<br />

plsn-aurveylng methods, but the ascuracy and<br />

precision of such rasufrs till dacraasa as the<br />

sras surveyad irrcrassaa in size.<br />

plamstable MAP-A msp co~ilad by<br />

plantable mathcds. Tfra term includes map<br />

made trj complete field mapping m a base<br />

projection ard field corrtwring on a pfenimetric<br />

base map.<br />

planatablc tmvars~ graphical traverse<br />

accompfiihed by @antstable. methods: .<br />

MIL-HDBK-850<br />

plsnotsbla-A fiild device fer ptotthg the fines<br />

of e survey diracrty from obesrvationa. It ccmsistn<br />

essenfkdly” of a d~awing board rrwunted on a<br />

tripod. with a Ievefing device dsaignad as psrf of<br />

the bosrd and tripod. See else elidade;<br />

Phlleddphla Ievellng rod; stadia.<br />

planetary ab.arratlon-The angular<br />

dispfscement of the gaomatric direction<br />

betwasn the ob@f end the obsarvar et ths<br />

instant d light emission, from the gaawrmiric<br />

direction at the instent of observation.<br />

planetsry conffgurstlone-Apparenl<br />

positions d ths pfanats relative to asch other<br />

and to other bodies of the solar svstem. –.<br />

fmm the Earth.<br />

ss saen<br />

planetary geometry-l. Mathematical<br />

traatnwrd of the shspe and figure of e plenet.<br />

2. Methemsfical treatment of relationships<br />

between M or morn plsnets ardor their orbits.<br />

planetary praoesslon-That component of<br />

general Pr=aesion auaed by the effect of ofher<br />

plenats on the aqustorial profubarenca of the<br />

Earth, producing an aaatward motion of the<br />

equinoxes efong the ecliptic.<br />

192<br />

plarrstold-Sea ssterold.<br />

plmmt-A celestial body of tha solar system<br />

ravdviig around the Sun M a naarfy ckcular<br />

orMaarn* bdymvoMmgamunda fir.<br />

See afao ●stwold; Infortor plmmts; Inner<br />

plarmta; melor plarmts, nmrlgatlonal<br />

planets; outor planets; prlnclpel<br />

plarmts; 9uperlor planete; torrastrl.sl<br />

planet.<br />

plana-saa aatronomlc rrrerldlart plan.;<br />

bssal piano; colllmstlon plane; ●pipolsr<br />

plmra: focal plane; gsrodetlc martdlan<br />

plnna; ground plan.; hlfl plan.;<br />

horlzontd plmra; marldlonel plan.;<br />

nodal plane; orbital plane; pampectlva<br />

plane; photoWaph plane: plcturo plane;<br />

prlndpal plane; tangent plane; v-rtlcal<br />

plan-.<br />

planlmetar—A machanicd integrator for<br />

msssuring the area of a plane surfece. Saa also<br />

poler planlmeter.<br />

planimetrlc map+JCS) A map representing<br />

only the horizontal positiin of festums. Also<br />

called Ilne map. See also topographic<br />

map.<br />

planlmetrlc-baao map-A map prepared<br />

from aerisl phofogrsphs by phologrsmmatric<br />

rrwlbds, as a guide or basa fer contouring.<br />

planlmetry-1. The science of maasuring<br />

plane surfaces; horiiontsl measurements. 2.<br />

Parts of a map which mprsaent everything<br />

excapt retisf; that is, works of man, and natural<br />

featurss such as weeds and wstar.<br />

planlspher*A representation, on a plsrre, of<br />

the celestial sphere, esgecialky csre en a polar<br />

projection, with mesns provided for making<br />

certain rnsaeuramanfe. such as affiiuda and<br />

azimuth. Also, a msp rapreasntafion, on a<br />

pkma, C4 the Earth’s sphara.<br />

planlapherlc astrolabe-An astrolabe<br />

consisting c4 a full graduatad circle tih a<br />

centrally mounted aliiads end accasamy<br />

adjustable pletes on which ara engraved<br />

s4eraogmphic projactiins of tha heevens and c4<br />

the sphere for focel latitudes,<br />

Planning Tarrein Anafysla Dets Baso<br />

(PTADB)-Ar 1:250:000 ~le hsfdcOfly, -<br />

gwgmpmc mrormataxi cystam corwatmg 0; a


set of aalected tingle thamaf!! Iemein<br />

itiormetbrr everfeye.<br />

plennlng chart-A chsrt tiIgnd ap&fiilly<br />

Ior p4srtning flight Operetiins.<br />

ptennlng nrs~rnall-scele rrditary map used<br />

for gemersl planning puqrosee.<br />

MIL-HDBK-850<br />

plestk bfook-Tha bkck of bonded Ct3/hlfOSS<br />

Sc9ta?te sheets, mdr Sheet equal M rftiiese to<br />

Ihaoontcxc irdervet ettheadeoftha relief<br />

rnedel, from which the Ierrein bees is art. Alse<br />

mllsd Iamlrralo.<br />

plastlc rdlof map-A topographic msp<br />

printed on pisatic and molded into a threedirrwnsbnsl<br />

form. The plesfis medum is<br />

gerrerdyfo mmdtryha elarldvslwurn worm<br />

tarrein model to atileve the Ihresdiiensional<br />

representetic.n.<br />

plato coordinates-l%e x- end y+oordirmtes<br />

of control points sppeming on e phc.togrsphc<br />

plate.<br />

plate lavtd-A spirit level ettached to the plste<br />

-, of a surveying instrument for leveling the<br />

grsdwlled affile or, indirectly, mekhlg me Verlical<br />

axis truty verticsl.<br />

plsto reductlo~ling of mntmi peint<br />

imsgea on a delisr plste.<br />

plate-l. (Iiitrogrephy) A lhin metal, pla~ic, or<br />

fMp@ til, thst cawrise the printing im9ge and<br />

* eurbce is treeted to make onfy the<br />

irmge erase ink rscsptwe. Alm cellad press<br />

plate. See aim color plate: combination<br />

plate. 2. (photography) A tranqwant medium,<br />

UMI& 9=, mtrrd wtih a phof~raphkc<br />

emulsion. SW elsrr diaposltivo: stellar<br />

plate.<br />

platforrrt-The vehicle that holds a sensor. If is<br />

uauslty a aateliiie, but may be a plane or a<br />

halimp4er. Senaers can be meunbsd on tripods<br />

for oartain uses, such es examining<br />

etrrctrornsgnet’k radiation frem various types C4<br />

vegelelion,<br />

Pletonlc year-sea great year.<br />

plat-A dmgrsm drswn to ecsla ahowing lend<br />

boundaries end euMiviaiirre, together with all<br />

data essential to !fre description and<br />

idarrtifkation of the several urtita shown thereon,<br />

193<br />

ard including one or more sertificatas indiifing<br />

dueepprovaL A@atdfiers fremarnapift thatil<br />

doaarrnr nsmamrily show ecMtioM 1cultural,<br />

dtinsge, and refief bturoe. sea aim<br />

eedeetrel map.<br />

plot map-see photo Index.<br />

piofflng chart-l. (JCS) A chsrf designed for<br />

the graphical processes of rravigafien. 2. A<br />

sherf designed prirrwity for pbttii end deed<br />

rackonirrg or fines of position fmm caledial<br />

ofxwvalbrre or radio eida. Reiit#, cdtwe, and<br />

drainage are ehovm M nacesmry.<br />

pbttfng sssl+The refstirxrshii of the size of<br />

the ~iislien to the size d the ground ares it<br />

represents.<br />

plot-(JCS) 1. A map, chsrt, or grsph<br />

reprewnting dsta of any sat. 2. To represanl<br />

en a disgram or chsfi the pmitiin or course of s<br />

target “n tarms of angles snd d~s from<br />

known pmitiins bsste a pxitiin on e map or<br />

chsrt. 3. Ths visusl dkpby of a tingle<br />

gaogrsph=l Iocaticm of an airborne objad at a<br />

patiiculer instant of time. 4. A portbn of a msp<br />

or overlay on whiih are drawn the cutfirm’a d the<br />

mess covered by one or nmrs phetogrsphs.<br />

Sss else master piot.<br />

plumb bob-A con”-1 device, ususlly of brass<br />

and suspendsd by a mrd, by masns of whiih s<br />

pint csn bs projacled vertically into ape= over<br />

reist”wely short dktanses.<br />

plumb line-l. The line ef fotce in the<br />

geo@enliel field. The continuous curve to<br />

whiih Ihe directien of grsvity is everywhere<br />

tangential. 2. A mrd with a piumb bob at one<br />

end for determining the dksct@n d grsvify.<br />

plumb point-See photograph nadir.<br />

plurtge-See transft, definition 3.<br />

plus rmgle-see ●nglo of .Ievatlon.<br />

plus de.sllnatlon-See decllnatlon,<br />

definition 3.<br />

plus dlstnnea-Frscfionsl pert of 100 fest<br />

used in designating the location of a point on a<br />

survey Iina as .4 + 47.2,” meening 47.2 feet<br />

beyond SIalion No. 4 or U7.2 feel fmm the<br />

inkiil point, measured along e specified line.<br />

See also plus ●tetlon.


I<br />

plus polnt~ inWmadiite point on a<br />

travar’xa area bcalad & 8 plus didarca from<br />

the begirming cd the coume.<br />

phIS sight-sea backslght.<br />

plus atatiort-An infermadiite point on a<br />

traverse, not et en even tape length distance<br />

horn the initial point. See elm pfrm dlatance;<br />

taping station.<br />

MIL-HDBK-850<br />

Point Podtlonlng Deta Baas (PPDS><br />

sets of geodefbalfy cordmllad photographs and<br />

acxmrnpanying dsta Ihsi emble trained<br />

pa=nnel using appmpriah hardware end<br />

software 10 derfve precise coordinates for any<br />

feature identifiable within the PPDB.<br />

point ●nomdy—lhe value of the grevity<br />

anomety at a epactfii Iocat”kxr es obaarvad or<br />

predbfad.<br />

point bas.-A manuscript titch conieins<br />

redml centers, picture p@nfs, peas points.<br />

mnfrel mints. and lie mints fmm the<br />

photog~phe used in the mdiel vienguletion<br />

tiettiod. ”--”’ ‘“” ‘ “’ “ “ ‘<br />

point taature-An objet! whose Iocalien can<br />

be described by a tingle eel of coordhstee.<br />

point mrsrk@r-A device used for idenlifykrg<br />

@rfs on deitiv= by either meting e snwll<br />

hole in the emufeiin or meting a small ring<br />

emund the dafeil point itself Also celled snap<br />

marker. See also point-transfer dovlca.<br />

point of catilnty-in a simple two-point<br />

infereecfion problem, thet poinI where the two<br />

intersecting ray6 cross end Ihe polnf is<br />

mnfi~ by the intersection of e thitd or check<br />

raY Pfsemg through the earns point.<br />

pohtt of compound curvature (PCC)-<br />

The point on a line survey where e circ.uler curve<br />

of one radius is tangent to a circular curve of e<br />

different radius, both curvee lying on the seine<br />

aide of their ccmwnon tangent.<br />

polrrt of contact—Any level trurfece abng e<br />

tannin pmfib recorder (TPR) flight line fhrrf can<br />

tra flown over both before and after the<br />

chenglng or adjustment of a TPR positional<br />

camera magazine, a chart roll, or a recading<br />

pen.<br />

194<br />

point of curveturo (PC)-Thtr point in a line<br />

survey where e tengerd ends and e circuler<br />

cuwe bagkra. See ●lso Point of tangancy.<br />

point of cuep-Tha poinl of tengencf of two<br />

curves, the direction d tha tienabn d said<br />

Curvaa being of Lqpoailo aim Such se the<br />

vertaxd aYofareilrucd frecJr orepoint on the<br />

*of n corwex—a2mav elana. hbyatsoba<br />

applied to the pint d fsmgency d a straight line<br />

and a curve where the duectbn of axtenaicm of<br />

the iii and curve are d oppeaite dgn.<br />

point of InflectIon-The point at whch e<br />

reversal d dkection d curvature telree @ace.<br />

pohrt of Irsteraactlon (Pl~The point where<br />

thetwotangents dacimuiercuwe maat. Abo<br />

celfed VOrtOX Of cUW*.<br />

point of orlgln-See Inltlal point.<br />

point of revoree curveturo (PRC+The<br />

point of tangency common to two curves, the<br />

curves lying on the cpposile side of the<br />

common Irmgcmt.<br />

polrrt of aymm@r’y-The point in the focal<br />

plsne of e cemere aboul whiih all lens<br />

distortions are symmetrical. If the lens were<br />

perfectly mounted, lhe poin! of symmetry weuld<br />

coincide wilh the prkipal point.<br />

point of tang.ncy (PT)-The point in a fine<br />

euway w%we e circular cuwe ends and a<br />

tangent begins. The point of terr~ncy and point<br />

of curve ara both points of tangeney, their<br />

dtierenf daaignelione being determined try the<br />

direction of pmgmss along the fine; the point of<br />

curvature & reeched first.<br />

point of vorflcal curve (PVC)--The point of<br />

chenge hom a line of uniferrn dops to a vertical<br />

cuwe.<br />

point of var’ficd Intaroactlon (PVl)-The<br />

point c4 intereactlon d two lines, each having<br />

different uniform slopes.<br />

point of vertical tangent (PVT)-The point<br />

of chenga from a vertical curve to a line of<br />

uniform elope.<br />

pohtt podtlon deta (PPD)-The collective<br />

resuh of an anelytbl triangulation effort thet<br />

provides evaluated geodetic poaifbns c4


*toidemifbbkr ground pokrte of raaeau<br />

wwwacfims. Theaa podtkms are ttre raautfd<br />

en evaluated adjustment 04 the points to a<br />

apacifii ffu3fhamatical surface and era<br />

ew- in tame d Mfde, kmgiiude,<br />

sievetiin, and poailionel accuracy for aech<br />

point.<br />

potnt poaftlonlng-(surveying) The proceee<br />

cd aafablishhg indapedant survey fmaitii.<br />

See also shorl ●m; short ●rc gaodatk<br />

adjustment; translocs!lon.<br />

point poaltiorr-(Doppler) The geocentric or<br />

geodetic podfiin c4 a point determined from<br />

satellite tracking date by a Dof#ar receiver and<br />

the sefefiiie(s) aphemeridas.<br />

point the lnatrument-Turning the survey<br />

instrument to where the cross hske (verttil,<br />

Irorizorrtel, or both) are aaurefety aligned with<br />

the tsrgei.<br />

point-decignetlon grid-(JCS) A system of<br />

lines having no relelicn to the sctual acele or<br />

orienfeiion, drawn on e mep, chsrf, or air (aerief)<br />

ohotoarach diviilna if into saueres co the!<br />

“r. .<br />

point-matching mathod-(rectifiilion) The<br />

techn”que d ufiiiuing en eutofocus rectifier for tiff<br />

removel by the menuel matching of projected<br />

image points 10 hose pbtted in their correct<br />

horizorrfel posifiin on a film templef.<br />

point-tranafor davlca-A stereoscopic<br />

imlnmrrant ueed to make corresponding image<br />

points on overtopping photographs. Also celled<br />

tranmwfbor. See also point marker.<br />

polntor-(digitel) The eddrsss cd e record or<br />

ohsr dete gro~ings contained in another<br />

record.<br />

polntlng ●ccuracy—The exectneas, in<br />

surveying or photogremmetry, with whmh the<br />

line of eight or flcding merk cen be directed<br />

toward a tergef or imege point.<br />

polntlng arrora-Errors whch reflect the<br />

accuracy with whiih the flcating msrk d e<br />

sferaoplotfing aysfam csn be located on a sherp<br />

model point. ~eea errors gerrarelfy folbw a<br />

more or leas random dkfribufiin but chew a<br />

,<br />

MIL-HDBK-B50<br />

aysfenmtic trend with progreaelve wwfring time<br />

on fha instrument due to eye fatigue and its<br />

affect on ateraOaec@c parceF4”m.<br />

pointing llna---sea Ilno of oollimatlom.<br />

pointlrr~lm (menaurafii) Pfacing the reticle<br />

orindex markdap+sdakn rnaafaairlg<br />

inslrurns~. b es ● carpanstor, wiffdn the<br />

aymmatrrod oentaroroarter dgrsvityd ●poinf<br />

being meaewed to ds4errnirra its position<br />

ralettve to the position d other points in some<br />

system d mrdinsfas. 2. (aler eocompibtiin) A<br />

geneml term appfied to the movement of the<br />

tracing table d a elereopbtfing instrument to<br />

apecifii conbd ar#or picture pdris on the<br />

datum during orientation d n ctemorrrodal. 9.<br />

See lint of sight, definition 2.<br />

point—A positiin on a reference system<br />

detemrined by a survey. See elso<br />

amphldromb point; anglo point; ●nnex<br />

point: antlsolar point; ●strogravlmatrlc<br />

points; cardlnel points; check point;<br />

control point: datum point: datall<br />

points; distant points; fix: lm*90 POlnC<br />

Initial point; Intercardlnol point; mep<br />

..&nis crm br.. more reedily Icceied.%... .~, . . ., ,polnt;. “middle point; nodal” point;<br />

orientation polnc pass point: plus pdnt;<br />

point-in-polygon—A geographic information prlnclpal point; sublunar point:<br />

system (G IS) routine whk=h 8ssss.%s whether a subaatellite point; subsolar pointi<br />

fminf falls within e polygon.<br />

eubstollar point; tle polrrt; turning polrrt;<br />

wing point; witness point.<br />

195<br />

polar axia-The primery axis d diractien in ●<br />

system of pofar or spherid cmrdhatw..<br />

polar bearing-in a system of paler or<br />

ephericsl coordinates, the angle formed by the<br />

intersection of the referenca meridiind plane<br />

end the meridmnal plene containing the point.<br />

polar chert-1. A charl of pobr areas. 2. A<br />

chart on e poiar projection. The prelections most<br />

usd for pdsr chsrls ere the grrornenic,<br />

stereographic, azimulhsl equidistsnl, trensveree<br />

Mercator, and nwdifi.sd t.ambert conformel.<br />

polar clrcla-Eifhar the Arctic Circle (north<br />

polsr circie) or the Anlercfic Circle (souih polar<br />

circle) .<br />

polar coordlnatee-(JCS) 1. Coordirmtas<br />

derived from Iha distance and smguler<br />

measurements from a fued point (pole). 2. in<br />

artillery and neval gunfire aupporl, the direction,<br />

d=lanca, and vertiil cmrrectiorr from the<br />

observer/spotter position to the target.


I<br />

I<br />

I<br />

I<br />

I<br />

I<br />

polar diamotor-Tha dmnvster of the Earth<br />

between the poles.<br />

MIL-HDBK-850<br />

polar dlstanoa-ltrrgular distance from a<br />

ceisatiml pole; the arc of an hour circle between<br />

e os4eatisl pele, usually the atavatsd pole, arrd a<br />

point on Iha oefeetial @am, maasumd fmm<br />

the cslastisl @s though ltW. Ses also<br />

codecllrmtlon.<br />

Polsr grtd+l grid system utifizod for aerial<br />

nsvigstiin bt tha pofar regbns. It cOnsi@s of a<br />

r@CISIWdW grid wfth X- end y-axes aligned with<br />

tha W—lSO” and the 90”E-sooW msridians<br />

respectively. When plotted on a tmmvarea<br />

Mat’cater map pmjactkxr of the pebr ragions, ff<br />

represents a system of transversal nraridiins<br />

ard persUats whoes plea era at the<br />

intersections of the Equator errd the 0“—1 80”<br />

meridian.<br />

II polar map projection-A map pmjacfion<br />

wnlered on * pole,<br />

I<br />

I<br />

I<br />

L<br />

polar motion-Sea wwlation of the pole.<br />

polar orbit-An Earth satelfiie orbit thst has<br />

an incfinsticm of about 90” and, harm, passes<br />

over tha Earth’s poles.<br />

polar orthographic map projection-A<br />

-P P(@*ti hs~ing the plane of the<br />

propctm parpandculsr to the axis of rotation of<br />

the Earth fpsrallel with the pfana d !he<br />

Equator); in this pmjaction, the geographic<br />

psrsllals era full circles, true to smle, arrd the<br />

gsogrsphii maridiins am straight lima.<br />

polar planimeter-An instrument wad in<br />

rnaaauring eraas fmm a drawing. The<br />

instrument rota!as about e pla, harce its<br />

nama.<br />

polar mdius-l%a mdiua of the Earth<br />

maasurad abng Its axis of mfatiin.<br />

polar Satelltte-fmy sstelfiie thal passes over<br />

the north arxf south pales ef the Earth: i.e., one<br />

that has an incfimstion of about 9W with respscf<br />

to the EartNs Equator.<br />

polar ●tarsogmphlc mep projection- A<br />

stereographic pmjactiort having the center of the<br />

projsdkan bcetad et a pofa of ths sphere.<br />

Polarls correction-A correction to be<br />

196<br />

eppfied to the observed Sltiilxie of PolSris 10<br />

*sin the Iatitda.<br />

Polarls-Tha aacsmd-msgnituds dsr, Alpha, in<br />

the oomsteltatibrr Ursa Mii (Littte -r). Abo<br />

celled Nofih Stm polestar.<br />

polarlsstion flftar-Any of the manufactured<br />

plestii tbars Wfictr plane pelsrizes Ordinery fiiht<br />

when i passes tfrougfr the fi~er. Ueuefly<br />

idetrtifii ty e trade rumta.<br />

polarl~tlo~optics) Ths act or pmcaas<br />

modfyrng tfght in such ● way that ths vkwatii<br />

ara restrktsd to ● eingle plane, Acourdhg to the<br />

wave theory, ordinmy (urpotarised) fiihf vibrstee<br />

In all planes perpandicutsr to the drdort of<br />

PmP8!@~0n. On passing thrwgh or contacting<br />

a#aru.m9nww4urn (==h=PokmXd ora Katr<br />

call) erdinsry tight becomes plane polstfzsd, that<br />

is, its vibrations am fiisd to a single plans,<br />

pcdastrodlat-A machenkal counter for<br />

determining the azimtnh and altitude of Polaris<br />

M eny time.<br />

pole of the Milky Way-The pole in the<br />

galactic system of coordinates,<br />

pOl-st=r—See Polaris.<br />

pole-1. Either of the two points of intersection<br />

of the surfece of a ~here or spheroid and ifs<br />

axis. 2. The origin of e system of polar<br />

coordinates. See alse ●verage terrestrial<br />

pole: cehsstlal pole; doprossed pola;<br />

ecliptic pols; slevatsd pole; flctltlous<br />

pole; galactlc pols; gaomsgrmtlc polo;<br />

magnetic pole; north geographical pole;<br />

north geomagnetic POIS; north magnetic<br />

polo; oblique PoI*; south geogrsphlos)<br />

pola; south geomagnetic polo; ●outh<br />

magnstlc polo; torrsstrlal polo:<br />

transverse pole.<br />

polhody-A chart depicting the motion of the<br />

terrastr”ml pole as a function of tires. See also<br />

varlatlon of the poles.<br />

polyart-A plastic based printing substrate with<br />

excellent wet strength.<br />

polychromo- See multicolor.<br />

polyconk chart-A chart on the polyconic<br />

map projection.


)<br />

I<br />

j,’ :<br />

polyconlc map projectlorr-A map<br />

Pro&tiin hsving the central geographic<br />

meridmn repasented by a etraight line, along<br />

wllibh ha Z+racirrg fw fines ‘gtlw<br />

gaegmpMi parallels LeWo&%%%%ths<br />

diatanoea bafwam the Psrofkriq the PSlldkk<br />

areraPmaantadbY arosofdrdea Which ammt<br />

corrwrdrio, bti wtreee centcsa lie a the fii.s<br />

repraeartting the central meridian, and wtuxe<br />

radii are datarrnirrad by the lengths of the<br />

efaments of oonee which ere tangent abng tha<br />

parellals. All meridians except the cantrel ones<br />

are cuvad. The projacfii is neither cotiormal<br />

nor equal area, b~ it has been widely used fc+<br />

MSPS of srnafl areas beoauae of the ease wth<br />

wtriih k can be conafruoted.<br />

polygonlzatlorr-The process of connecting<br />

logathar Iinaar faatura information to form<br />

@ygona.<br />

polygon—Thematically common areas<br />

WW* of contiguous faces.<br />

MIL-HDBK-850<br />

polyhedrlc projection-A projection used for<br />

a farga-scale tcpgraphii map whereby a small<br />

quadrangle on the apha@d is proj=tad onto a .,<br />

plane trapezoid. Scale is made true ekhar on<br />

the central meridian or along the sides.<br />

PrJrre pr18i’n-A prism thst deviams the axis<br />

180° and inveris the image in the plane in whwh<br />

the reflection takes place. It may be descr!lmd<br />

as two nght-angla prisms cemented togathar.<br />

Porro-Koppe princfple-Tha principle<br />

applied in some photogremmetric instruments to<br />

eliminate the effect of canera-lens distortion.<br />

The phetographb poaifiie or negathve is<br />

observed through a lens or OPfkal system<br />

identkal in diatoriion charecteristbs to the<br />

camera objective whiih meda the eriginal<br />

exmarra. In effect, this mathd of obervatien<br />

isareverse we d the camera, with the feed<br />

ptane becoming the object whiih is imaged at<br />

infhify by parallel bundles of rays emerging from<br />

the lens. The chief ray et =h bundle assumes<br />

its oomact diractien, and the cme c4 rays is<br />

idetiid IO thet WIVXS vertex was the incident<br />

node of the camera lens et the instant of<br />

e-sure. The parallel bundles may be<br />

observed & msena d a bkeoc@o system<br />

focused at infirrfty and made rotatable ebeut the<br />

imldant node of the lens. This melhod of<br />

afimlnatlng lens dtiortbn Is utlfiied kr<br />

photogrammatric inatrumenls of both the<br />

monoacopk type, such as the photogoniomeler,<br />

197<br />

and the ate raoacc@typ usedfOr<br />

aferrseplotting.<br />

port plm--A spaciakpurpoaa large-scale map<br />

d a port ems showing piers, milrcd axtarrakma,<br />

repair fecilkiea, pild offii, cuatemheuaa, ad<br />

other a@oabfe norrnavi@enal Ieafur=.<br />

portsblo m.rtomrttlc tldo gs~A smell<br />

automatic tide gage, designed for use where e<br />

ahal series cd ebaarvationa is rracaaaary for the<br />

raduction of seundings 10 a cernrrmrr datum.<br />

posttlon angta-Sea parallactlc ●ngle,<br />

dafkrifii 1.<br />

poaftlon plottlng ahaat-A blank cheii,<br />

usually on the Mercator prejacfbn, ehewirrg only<br />

the graticule md a compass rose, so that fhe<br />

chari can be used for eny bngituda. Sea also<br />

universal plotting shoot.<br />

positional accurscy+mrtography) A term<br />

used in avalualirrg the evarall refiatrilii of the<br />

positions of cartegraphii features on a rrmp or<br />

charf relative to their true pcdtiin, or 10 an<br />

established standard.<br />

posltlonel camera photography-<br />

Photegraphy obtaind with e camera afigned<br />

with the TPR radar beam, uaad for correlation<br />

errd transfer of recerdad vertical data to the<br />

cartography photography.<br />

positional error-(cartography) Tha anmunt<br />

by wttiih e cartogmphe feature fails to agree<br />

with its true positkm.<br />

positioning camer~ camera used for<br />

cor-relation purposes in the airberne profk<br />

recorder system. It is mounted on the radar<br />

antenna arxt records the area illuminated by the<br />

radar beam.<br />

pmsltiorr-1. Data wh=h define the Ieurtbn of<br />

a point w~h ra~ 10 a reference system. 2.<br />

The place occuprad by a point m the eurfaoe.d<br />

the Earth or in apace. Abo oelled plaos. a.<br />

Ths 6Qmdinat8S which define the focden of a<br />

point on the geoid or spheroid. 4. A prescribed<br />

setting (reading) of the horizontal skcla d a<br />

direction thaodolita wfdih is to be used for the<br />

cbseryation on the initiil sfatkrn d a series of<br />

stations which are to be observed. Afao cafbd<br />

clrcfa posftion. See else ●djuatod<br />

position; apparent poaltlon; ●atrometrlc<br />

posltlon; ●stronomic poaltlon; c. f.stlal<br />

tlx; celastlal line of poaltlon; clrcla of


i<br />

posltlon; convergent posltlon; ●leotronlc<br />

Ilno of posltlon; fldd podtlort: fix:<br />

gsocorttric ststlon podtlon; goodetlc<br />

posttlon; googmphlc position; line of<br />

podtlon; mean poaltlon; point position;<br />

point pooitlonlng; pracls. Installation<br />

posltlon; prollmlna~ position; ml=tlvo<br />

podtlon; supplemental posltlon;<br />

transvores posltlon; true posltlon.<br />

podtlvo dtltude-Angutsr disttrnaa abeve<br />

the Irorixon.<br />

poaltlvo doflccfion ●tgla-See deflection<br />

●ngle.<br />

posltlvo forming--ln refief model making,<br />

forming over e posiftie mold.<br />

posftltm kms-A lens that converges a beam<br />

of parallel light rays 10a pdnt focus. Alw called<br />

converging lens; convex lens.<br />

podtlvo mold-The cast pulled from a<br />

negative mold when msking s relief medal.<br />

Posltlveln photography, an irnatye on film,<br />

plale or paper hsviig @proximsIe~ rhe same<br />

total rendilion of Iighl and shade es the original<br />

subject.<br />

potorrtlal dlsturbarrco-See disturbing<br />

potential, definition 1.<br />

potontlnl of dlsturblrrg msssws—See<br />

disturbing potsmtiol, definition 1.<br />

potontial of random maaoee—S ee<br />

disturbing potontlal, definition 1.<br />

potontlal-A scaler function, the gradient of<br />

vdiih resufts in a vector field. Use of the scalar<br />

function simplifies investigation and dmcription<br />

of the phenomenon considered. Used<br />

esfeneively for magnetic, grsvifalional, and<br />

gravity field investigations. In calastial<br />

mechenbs and geodesy, the negative of the<br />

potenlisl, sometimes called the force<br />

function, is usualty empbyad. Sea else<br />

dloturblng pcrtentlal; gravitational<br />

potontlel.<br />

power of ● Iono-%a dloptor;<br />

magnlflcetion.<br />

powor of teloscopa-fsurveying) The<br />

magnification of a telescope Men focused at<br />

MIL-HDBK-850<br />

198<br />

infinity.<br />

Pratt-Hayford theory of Ixoofaoy— A<br />

thaoty c& imstatk m~nmtiin whiih a=rnaa<br />

that every Iopogrephio excess or dsfed of mass<br />

is corrpanaatad by an equal and opposite<br />

dated or ascaaa, evenly dietrtbtstad knmadtalely<br />

babw If twfwesn grcund level or see Mfom<br />

faval ard a fmad de@h, called the depth of<br />

componoatlon, commonly 113.7 km. Alw<br />

called tormontlng dough theory. Sea also<br />

Airy theory of Ioostasy.<br />

Pra-Ship Readhroso Rovlow (PSR)-A<br />

review under the verification phase d DMA’tt<br />

modarniisdiorr pogrsm (DPS). PSR axarninae<br />

sagmanf fecfory tasting, planned tes4ing<br />

activities. and pmducfion canter readiness 10<br />

determine when to shp DPS equipment frem<br />

the mntrscfor to tha production centers,<br />

prwossion in declination—The component<br />

of general precession abng a celestial meridian,<br />

anmunting to abouf 2D.~Of arc par year.<br />

pracaxslorr In right sscenslon-The<br />

COMPOr@t of generel precession abng the<br />

celestial equator, amounting to aboui 46.1” of . . . . .<br />

arc par year.<br />

precession of tho aqulnoxes—The mnical<br />

motion of the Emth’s axis sbeuf the varfical to<br />

the plsne of the aclipt”c, caused by the ettractiie<br />

force of tha Sun, Moon, and other planets on<br />

the aqualarisl protuberance of the Earth. Sea<br />

also ganeral pracesalon.<br />

precosslon-Changs in the direction of the<br />

axis of rcrtslion 01 e spinning body, as a<br />

gyroscope, when acted upon by a torque. The<br />

direction of motkm d the axis is such that jr<br />

causes the dkacfion cd spin of the gymecopa to<br />

tend to coincide with Ihst of tha impressed<br />

torque. See also drl~ gertaral precesalon;<br />

plsnetory procsiaolon; toppls; topple<br />

axis; total drift.<br />

Proclss Bathymetric Navlgatlon Zone<br />

Charts (PBNZCs)-Charts depicting hlghfy<br />

detailed underwater topography in the form of<br />

bathymetrk curves. Detailed multibeamkwath<br />

bsthymatry allow s~merinas to precisely fu<br />

Iheir posltksre from bottom contour mstching.<br />

Also dlad Bathymetric Recovery Area<br />

Charts (BRACS).<br />

prsicloo ●phomerle+oordinatee and<br />

velocity of an artificial satellite, mmputsd for


I<br />

, . . a,. E.,-<br />

., .<br />

,.<br />

unifornr time interveb from data ac@md lrom a<br />

WOridwida treckklg nafwk The aphernaris is<br />

-Ed from ebaarvefims takan from merry<br />

statima spaced worMwide and adjusted<br />

logether ty feaa4 aqusma rrr&hods for<br />

rnasimum accuracy. Saa broadcast<br />

●phemerls; ●ph.merle; Navy Nevlgetlon<br />

Satelllto System.<br />

preclss Insfsllatlon position (PIP)-<br />

Gaodetis ODDrdiitaa of installation reference<br />

pcints raffading their maximum posa&Ja<br />

refinement by utifizing all intelligerwa sources<br />

snd qrtirmsm computer techniques of anafyfii<br />

eraa adjustment.<br />

preciaa leveling rod-A md used for precise<br />

Ievefing. Tha graduations are on an Inver rbbon<br />

whti is meintsii under constant tension and<br />

whiih, for all pmdical purpeaes, eliminates tha<br />

need for correcting br changes in length. Thase<br />

reds are usual~ graduslsd in whole end<br />

frecticmal meters. The bsck side of the md is<br />

gmduated in feet and tenlhs of feet. Also celled<br />

Inwsr Iov*ling rod; motor rod; Molltar<br />

preclae leveling rod; National Goodetb<br />

Survey first-order Iavollng rod.<br />

. .... . ..- .. . . .<br />

precise levcrl-An instrument designed<br />

spectiliy Im ebtaining presiae resutfs by dired<br />

IweJing leshniquas. 11is esaenlielty the same as<br />

an enginesr’s fevel except thst it contains<br />

micrometer esrews for more precise Ieveting of<br />

tha instrument end contains a prism<br />

arrangement wharaby tha level bubble san tm<br />

observed simuffenaously with the rod reading,<br />

precise radar ●lgnlflcent location<br />

(PRSL)-Tha horizontal and vertical values<br />

derived for a selecled ground feature that is<br />

radar aignifiinl. The ratum may be eithar<br />

positwe or nagative.<br />

Preclrilon Automatic Photogrammetrlc<br />

fntenmlometer System (PAPl)-Aulomatic<br />

intervabmeter utilizing radar in determining<br />

interval for desired aerial photography forward<br />

lap.<br />

preclslon sftlmeter—A sensitive anaroid<br />

bammater. In surveying, ff will prodwe rasuks<br />

eccurata 10 within a mater arty when the two.<br />

bass method fS =refUIfV SDDlbd. sea ebO tWObase<br />

method. - “ ‘<br />

prdslon csmere-A relative term used to<br />

daslgnate eny camera capabfe of giving high<br />

resofufian and dimensbnal results of a high<br />

MIL-HDBK-850<br />

order of ==Jr=v.<br />

preslskwr depth rocordor+ davice which<br />

naoords eourrding inferrnet”m en electmaenait “we<br />

PSPCMfor depths up 10 6.GCXt fathcsna. H<br />

provides a trigger to the sonar and pertarrns a<br />

time measuring functbn.<br />

prsclslo*The cbeeneas with which ra@rded<br />

maaaummatis rrade under aimifer condifiins<br />

era grouped tog8ther. NOTE Precision k<br />

affeded anfy by the random armra in the<br />

MESSUriW Pmce=. Accuracy is affedad @<br />

pr~isiin and unknewn andor ayatemetk errors.<br />

pmrfomlnsnt height-(JCS) In air<br />

ranna baanse, the haight of 51 peroent or<br />

rrmra of the structures wilhin an area of similar<br />

surfece materiel.<br />

preferred datum-A geedatic datum selected<br />

aa e bass for oorrsofidaticm d bcal independent<br />

daturna within a geographiil area. Abo atlfad<br />

major dstum.<br />

preferrad grid-l. The grid designated by<br />

DoD for prodtsXion cd new maps, charts, and<br />

dighal ~raphic data: and shown on the<br />

%dex to Prefarred Grid.% Datums, and<br />

Ellipsoids Specified for New Mapping.’ 2. The<br />

grid praferrad by DMA for production of new<br />

maps erd chsrts.<br />

ProllmlnaW Design Review (PDFt)-A<br />

raviaw sonducfed prior to commencing Ihe<br />

detailad design process 10 assure that fha<br />

appa.esh is feasible and sound from e design,<br />

davelapment, tesl, and adivakm point of view.<br />

prrrlimlnaW oditlon—See provlslonel<br />

crdltlon.<br />

preliminary OIevatlOn-An elavation arrived<br />

at in the offiie after tha index, Ieval, red, end<br />

tamparature camcfksns have been appfiad 10<br />

the &served diffarances of elevation and new<br />

elevations have been arrrputed.<br />

preliminary orlentstlon-An initial, rough<br />

orientattin of projecfers prier to ac=xnpfiihing<br />

retative ori.snlalion of a afareomodel. II is the<br />

appmxirnste krvefing and scaling o/ the<br />

instrument frame and projectors, based on the<br />

best aafirnefe d what hi utfirnete Orianfetians<br />

are esaumad to be.<br />

preliminary position—in Ihe adjustment of<br />

Iriangufetion, the term preliminary b epphad to<br />

99


gaographc positiina detfvad from aelwtad<br />

obeervalions for use in forming istflude ard<br />

bngitudrt oortdiiion squat”b.s.<br />

prollmhwtry surtmy-llre collection of survey<br />

data on #tiih to bees studies for a propeaed<br />

projesf. Sea clso mconrtalssetrco survey.<br />

preliminary trhttgfo-in the adjustment of<br />

lriengukstion, the term pmflmlna~ is epphed<br />

to trianglas derived from eabcfad observations<br />

for u= in forming latitude and longitude<br />

cenditiorr equations.<br />

praflmlnary-Not of the desired ascuracy and<br />

praoisiin, end ed@ed fer te~ery use with<br />

the provieo d later bektg eupemadad.<br />

MIL-HDBK-850<br />

prOproaoscing-Prelirninery transformation cd<br />

raw data required to facilitate furlher<br />

cerfegraphic prcsmeeing.<br />

pmpunch ragfttter ayetem—A melhed in<br />

whiih a system of precisefy located holes are<br />

punshed m the margins of msp or chsrl<br />

meterisde (swh ss films, vinyls, etc.) p+er to lhsiI<br />

sctusl use. Exact register of msterials cen be<br />

=~khad by piecing regisrer studs (smell<br />

plsstiz or metal pins) through the holes, thereby<br />

sssuring exact regisler of detail. See also<br />

reglstar merke.<br />

prescribed grid-The grid that is Iccally<br />

prescribed by the,counlry of cvigin of mifitsry<br />

commander.<br />

Presentation Manager-A graphical user<br />

inletiace devebpad by IBM for U% with the<br />

0S/2 operating system.<br />

press plat.-See plate.<br />

prose prrxrf-A fiihogrsphed impression Ieken<br />

from arrmmt the first cooies run en the Dress<br />

ard used f;r checking tirpeiws. Also ~bd<br />

press pull.<br />

press pull-See prsies proof.<br />

preesum ●ltlmotar-See barometric<br />

eltlmotor.<br />

preewsre dtitud~JCS) An atrnespherii<br />

prasure, expressed in terms of ellitude which<br />

corresponds lo that pressure In the standard<br />

atmosphere. See alw ●ltftuda.<br />

m.<br />

do<br />

presmtm gage-A tkfe gege that is operated<br />

8[ the bottom of the body of water being gaged<br />

ard * rasorde tidal height cknges by the<br />

dtierance in pressure due to the rise and tell of<br />

the tide.<br />

primety bench msrk-A bench meh does to<br />

a tide station to wlii the tide staff and tidal<br />

dstum origimlty - referanoed.<br />

prfmary body-The ceiestisl body or centrel<br />

fwse field aboul wh~h a eateltiie or other body<br />

orbits, or fmm whii if is esoaping, or fewards<br />

whiih it b falting. Also oetled prlmery.<br />

pdmery circle-See prfmary great circle.<br />

primary OomplletlOn-A speciaily prepared<br />

mstte pfsstii materisl usad to depicl sounding<br />

data corrected 10 true depths in bathymetric<br />

compilations.<br />

prlmery great clrola-A great circle used as<br />

the origin of measurement of a ceordinste:<br />

perliculsrfy such e circle 90° from the poles cd a<br />

system of spherical coordinates, as the Equstor.<br />

Also celled furrriemental circle: prlrna~: , -.<br />

circle.<br />

prlmery grid-The major, or principal grid on<br />

msp or cherf.<br />

prlmery key-A key that uniquefy identifies e<br />

row 04 data in a dsta base.<br />

primary row-A single row of attribute deta<br />

eeseciated with e simple feature.<br />

primary ●tatlon-See main scheme<br />

atatlon.<br />

primary tide atatlo*A place at which<br />

mntinuous tide obsewaticme are made over a<br />

number of yeers to cbtein beAc tiial data for<br />

the Iecalify.<br />

prlmery—See primary body.<br />

prime flctltlous merldlan—The reference<br />

meridmn (real or fditious) uesd an the erigin for<br />

maesuremant of ftctitieus Iortgiiude.<br />

prime grid meridian—The reference<br />

meridian of e grid. In polar regions if is usually<br />

the 1S0”4” gaogrephic meriden, used aa the<br />

origin for measuring grid bngifude.


1<br />

!<br />

prim. lnvotso morldiar+%e prlmo<br />

tmrrsvorso morldlrsn.<br />

prfms morldhwr-T)re meridian of longitude<br />

O“, used as the origin for measuremeri of<br />

bngifude. The meridiin of Greenwich, Englsnd,<br />

is dmcsf urrhrarsd~ U* for th~ puqmae.<br />

prtms oblique merldlan-The refereme<br />

ftiiliws maridii d an oblique grdiculs.<br />

prime tmrmveree merldlan-The reference<br />

meridiin ef e tranavema gmticufe. Also celled<br />

prlmo Irrversa merldlen.<br />

prima vettfcel clrcfe-lhe vertical circle<br />

through the east end west peirrfs of the horizon.<br />

fr may be trua, msgrmtic, carqx?ee, or grid,<br />

depandng -n wlich east or west points ere<br />

involved. Also csllad prime vartlcsl.<br />

prim- vorflcal plan%The plane<br />

perpendicular to tlw meridiin plene (astronomic<br />

or geodetic) ccmtaining the normel. The<br />

irrfemacfions of the ssfrenomic prima vertkal<br />

plena with ha horizon ere the east and west<br />

. . .. . . .. . . - peints, --Also called east point. -<br />

prlmo vertical-See prime vertical circle.<br />

prlmltiva-(digilal mepping) The bwest level of<br />

attribution.<br />

principal axla—See opticsl axis,<br />

principal dlutance-1. The perpendicular<br />

d~ance hem the infernal pampacttie center 10<br />

the P&ne d a particutsr finished negstive or<br />

print. This dislance is equal to the celibratad<br />

f-l length nxmctsd for bolh the enkrrgemen!<br />

or mducliin ratio ard the film or psper<br />

shrinkage or expension. h maintains the seine<br />

perspective sngles at the internal perspective<br />

center 10 @nts on the finished rregetive or print,<br />

as existed in the taking camem at the moment<br />

d exposure. Thii is a geometrical p~erfy of<br />

each psrtiiuler finished nagstive or prfrrt. Also<br />

celled ●ffactlvo focal length. 2. (multiplex)<br />

The Paqmndicubr distence horn the intemel<br />

PamPacfke canter of the projector lens to the<br />

pfsne of the emulsion side of the dispositive.<br />

prlnclpal fOcuO—See focus.<br />

MI L-HDBK-850<br />

principal point and the rwdir pint).<br />

prfncipal morldla%l. The mandian<br />

esiendad from an initiel point, w which<br />

mguler querferquarter aacfbn, section, end<br />

kxvn.ship corners have bean or are to be<br />

aafabliahad. See also ●ssxillary gulds<br />

meridian: guide merldlan. 2.<br />

(pFratogmmmatry) Saa prfnclpal point.<br />

prfnclpsl parallal-(JCS) On an obfiqua<br />

phologmph, a line p+rrsllel lo the true horizon<br />

and passing through Ihe ptirwipal point.<br />

principal planet*The larger bodes<br />

revolving about the Sun in needy circular crrbifs.<br />

The fmevm principal planets, in order of their<br />

d~:ance from the Sun, are: Mercury, Vanus,<br />

Estth, Mars, Jupiter, Ssturn, Uranus, Neptune,<br />

end Plulo.<br />

principal plane-1. (JCS) (photogremmetry)<br />

A vertical plsne whii contains the principsl<br />

point of an cbiique pfretogrsph, the perapacWe<br />

center of the Isns, and the ground nadk. 2.<br />

(optics) A plane through a prfncipsl point end<br />

perpendiiukw to the optical sxis. see also axis<br />

of homology; axis of tilt; ground<br />

parallel; ground trace; horizon trtrce;<br />

Isometric parallel; line of constant<br />

scale; line of equsl scale: photograph<br />

merldlan; photograph psratlel; principal<br />

line; principal meridian; prlnclpal<br />

parallel: vanlsrhlng Ilne; vanishing point.<br />

prfnclpal point-f. (JCS) (phetegrammetry)<br />

The feet of the mwoendicular to the photo Plene<br />

through the fxr-ie canter. Gen6mlly<br />

determined by intereectkm of the lines joining<br />

OpPOsite Coftimating or f~ucisl rnsrks. [If the<br />

fiducisl merks are not visible on tha photograph,<br />

the principal pain! may be found by drswing<br />

d-gonals between opposite c=xnera w by<br />

messuring one-hslf the distance elong each<br />

side of the photegrsph and rxmnecfing these<br />

rnsdre in the sema menner ee fiduciel merks, er<br />

by resaau merks.] Also called indicated<br />

prlnclpel pohrt. See elm photograph<br />

center. 2. (calibrated) The canter d mdial lens<br />

distortion, usually givan es x- and y- dislancas<br />

from indicated principsl p3int.<br />

prlnclpal scale-(JCS) In cartography, the<br />

scale of a reduced or genarsting globe<br />

representing the sphere or epharoid defined by<br />

the fractional relation of their respective mdii.<br />

PrhtCIPal llna-The tmce of the PrinciPal Plane AIsO CaII~ nominal ●cala. sw also SCOl~.<br />

upon e photograph (e.g., the hne through the<br />

201


prlrrclpd 8tatlon-See main schema<br />

station.<br />

princlpd vorflcai circla-l%e veti”=l circle<br />

through the north and rmulh points of the<br />

horixon, ccirrcidmg whh the celestial meridiin.<br />

prlnclprd veMcal-(JCS) On an oblique<br />

photograph, a line psrperrdiiulsr to the trua<br />

horizon and passing through lha principal point.<br />

prlrrclpd-dlst~nco ●rror-in a stereepletting<br />

system, an instmrrwmt error resulting from<br />

iW~r ~lamtbn d the aeriel csmere,<br />

diie printer, er pmjactw. The error is d<br />

I little impcxtance in a flat autfa~ ~~ ~ the<br />

I<br />

I<br />

MIL-HDBK-850<br />

effects era incrassd<br />

the model.<br />

in prcportien to the relief in<br />

prirrclpal-point assumption-lhe<br />

asaurnptkm with respect to appmxirnstefy<br />

vatiical DMefysfis tfwt radiil directiane are<br />

cmract fi *U* fmm the principsl peint.<br />

principal-point ●rror-A personal error in<br />

wfrich the principal peints in a stereoplotting<br />

+ystem are dspbced in such e rrrsnner that<br />

they have unsqusl x componems with a<br />

resultant error in vert”~l acsla. Such ermffi are<br />

ususliy irrfrcducad into the system by either<br />

irrrpmper ~“entstbn of the d~pcsitwe plste in<br />

ths printer, in the prejecror, or both.<br />

prlnclpal-polrrt radial-A radml from the<br />

principal pekrt of a photograph.<br />

prlrrclpal-point triangulation—See radial<br />

triangulation.<br />

print-A photogrsphw copy msda by projacrion<br />

or contact printing from a nagative or<br />

transparency. See 81s0 contact print:<br />

dlapoaitlvc; ●nlargomsnt: matto print:<br />

photographic raductlon; pro]ectlon print;<br />

ratio print; rtrctlfled print; transformed<br />

print.<br />

prlamatlc ●strelaba-An astrolabe consisting<br />

of a telsacope in e horizontal position, with a<br />

prism and arfifiiisl horizon ❑ttached at its<br />

objective end, uaad for detemnining astronomic<br />

positions.<br />

prlamstlc compaae-A small msgnetic<br />

~v* h?kf in the .harrd whwn in u6e ad<br />

aqwppad wffh psep.wghls and glass prism no<br />

202<br />

arranged that ths rrqrnatic bearing or sximuth<br />

of a lie can be resd at ths same tima that the<br />

Iina is Sightad over.<br />

prlarnatlc ●rror-lhef error due 10 lack of<br />

persflelbm d the two faces of an optical<br />

eJenrerrt. erMresa mhrorora .shsdagle se.<br />

prtarn-A transparent body bounded in pt by<br />

* pkm!3 faces thst ara rmt Pruwlbh used to<br />

deviate or dbparaa 8 bsenr of light. S8s also<br />

dova prlam; horizon prlarn lndax prism;<br />

Porro prlam; roflecthrg prism; refracting<br />

prism; ratrodlroetlve prism; rhomboidal<br />

prism; right-engle prlam; roof prtnm:<br />

wedge.<br />

Probeblllstlc Vertical Obatructlon Date<br />

(PVOD~ file whd cOrnbineC M6kjUd<br />

dansify functiens with discrete varticsl<br />

ebstructien dsta extrscted f~m v~~l<br />

Ohtruction Data (VOD), Digital Festure Anefyais<br />

Dats (DFAD), the DhAA Digital Verticsl<br />

Obstruct”on t% (DVOF), Powerfh Data, and<br />

intelligence dstsbssss. PVOD provides cruias<br />

missile and aircrsft missien plannsra verticsl<br />

obstruction inferrnatien which csn be used to<br />

rnmpule probability. el mission ~ss, set<br />

mean cbsrsnce heights, ad plan mission<br />

mules. PVOD is the repbcement product for<br />

VOD.<br />

probability hrterval—See confidmce<br />

interval.<br />

probable swror—1. In B measured valua, if is<br />

the moat probable value of the resultant error in<br />

the measurement. This is a plus or minus<br />

qusrrtity thst may be Iargar than lha resutranl<br />

armr or srnallar than the reeuftant arrcr, and ifa<br />

prc&3bility of bahg larger k squat to its<br />

prebsbifiiy of being smaller. 2. The 50 parcent<br />

error interval based on the bwariate normal<br />

distribution function.<br />

procosa camera—Sea copy camara.<br />

process color prlnlln~lithography) A<br />

Iechn”que tor the reprcductien of a subjsct or<br />

chsfl in full cetor rendifiin, by cerrrbining tones<br />

ef the primsry cobrs, (yelbw, msgtmta, cyan)<br />

and bbck. Sea also procaaa plates.<br />

procasa lerre-A lens for photechemical<br />

~pyln9$ enIar9in9$ or projsct~n pumcaea, free<br />

fmm aberratbns, usually of low aparfure and of<br />

eymmatrid cunafruclion.


. . .<br />

procoas photography-Lina end halftone<br />

photography m wfdch the rasufting negstive.s<br />

amf positiies are subsequently ustxl in the<br />

PrafMreibn d press p4slss.<br />

Procoaa Platm-Twr or - color press<br />

pfstes corririiad to prmtuse dhar mfors and<br />

shadea. sea also color plate; combination<br />

pfate; promaa color prlntlng.<br />

Product Gonoratlon Sogmmnt (PWS)-A<br />

segment sit DMA% DPS wfich witl ~vida the<br />

cepstidity to generate tath d~itsl producfa and<br />

reproducible msteriafa for hsrd mpy tips and<br />

charis. By utilizing digitizing cspabiiii= and<br />

graphc werkdafione, the segment wift provide<br />

for mllasfion of MC&G data fmm esicfing hard<br />

% 9rCPhii including maps, charts, and<br />

manuscripts. During product generation, the<br />

segment will esiracf e.pprqrriate dela fmm the<br />

MARK 90 MC&G databaae 10 ganarata required<br />

products. In producing cobr ~ratea for<br />

graphic products, PG/S will mnvarf the d~ital<br />

data to grspMc ayrnbols, gmaraliie and<br />

diapLemr graphii symbets, perform mbr<br />

separation, and ganarate ths reproducible mpy,<br />

See ,alm<br />

Sy8t*m.<br />

MARK 90; Dlgltsl Production<br />

product data-Data thet is either collected in<br />

a W~c PmdUti b’~ or data which is derivsd<br />

from rrsutral date for a sfmciri appiiiikm.<br />

Production Management Segment<br />

(PM/S)-Segmsnt of DMA’a DPS wh~h will<br />

irsmrpxale the MARK SS Data Integratim<br />

%gmant to provide e total pmdusfim planning<br />

and mansgamarrt capabil~ using the MARK 90<br />

prodtiim prmeases. This aagment will<br />

perform requirements, definition, long-range<br />

planning, pmgrsm development, prmfuction<br />

sshaduting, and status mportirrg. See et=<br />

MARK SO; Digital Production System.<br />

proftla tavdlng—The determination of<br />

elevat’kmts of peints at shod m-urad intervals<br />

a~ng a definitely bested line, such ae the<br />

center tine of e highway.<br />

profile-1. A vertical sacfii et the surface of<br />

the Oround, er of urrdarfyiig streta, w both,<br />

abng my faad line. 2. Ekrvatbn of the termin<br />

abng coma definifa tine. Elevations are<br />

measured al a etilcianf nun-bar of points to<br />

enable dafining the configuration of the ground<br />

surface.<br />

MIL-HDBK-850<br />

Z03<br />

Progremmere Hlarerchlcal Intemctlve<br />

GraphJcs Systam (PHIGS)--An ANSI<br />

stsrsimd wiich pMViCbS S sat d hmclkwrs for<br />

rrmdifiition d graphii &ta and the<br />

mlatii between the graphical dsta; and<br />

the dethitti, diapby, 8ild rnafifiibrr d<br />

gsomatridty related objsds, and two and three<br />

dmensionrd grsphicel data. See efao Grephlc<br />

Kernal Syetem.<br />

progress dratch-A msp or sketch showing<br />

work accorrptiied. In triangulation and tmverae<br />

surveys, sash poird as@khad is shown on the<br />

pmgrass skafsh, snd at= Iii obsarvad ovar<br />

and base fines measured. In a Ievahg survey,<br />

the program sketch shows the rode foflowwd<br />

and Iha towns pasaad through, but not<br />

necesssrity the tmatierra of the bench rnarfse.<br />

prograeslv. motio~tion in an orbit in<br />

the usual orbifsl diraclicn of calaatial bedims<br />

within e givan system. Specifiialty, motion of a<br />

mteliiie in the sema dkacfion to the direction of<br />

the primary. Oppoaife of ratrogrado motion.<br />

progrocshm proote-A aerbs of coler prints<br />

thst chow the irrdividuslfy Sewatad mbr .. ...7...<br />

printings of a jcb and th&ir p&as#ve<br />

combinations as each mbr is overprinted.<br />

projected map di8plsy (PMD)-An inftight<br />

navigstien ekt which uses e continuous sdor or<br />

btsck-and-whiie sprocksted filmstr~ amteining<br />

chsrt imagery, pojaded on a dqlay device md<br />

driven by the ainxsff’s cm?qniter. The eircraff%<br />

position is dispisyad with correlated chart imsge<br />

10 show bcation and direstim aduslty bekrg<br />

flown.<br />

projection compufatlon-The<br />

determination, from a aef of tabfes derfvad trorn<br />

formulss~ of the true shspe end dimanabrrs of e<br />

MSP Pml=tkm, for ths purpoas of constructing<br />

such e projection. See atse grfd<br />

computation.<br />

projoctlon dlstanc-lhe disterrce from the<br />

exlerml node of a prqecticm lens to the ptsns<br />

onto whiih the imege is pmjeded.<br />

projection gonerntlon-lhe transforrnsllon<br />

of a spherical surfeca, aush as lha aarth, to a<br />

plane surface. Regsrdlese d the trarrsforrnet”m<br />

methcd, Wrare is elwsya some dbfortbn in the<br />

plarra view.<br />

projection printer—An optical device for


enferging w reducing the Lmage C4 a negalfve or<br />

~~:$~:~ by Wasting if onto a<br />

projection print-(JCS) An enfargad or<br />

reduced photographic print made by projactiin<br />

of the image d a nagafive or a transparency<br />

onto e aansiliiad SIeiece.<br />

projection tablaa-oela made evaifeble in<br />

tabutar fomr far determining a definfle<br />

rebst”bnsIip wttii exists befwwn any grid<br />

intersection and arry edjaoant infarawtien d<br />

falituda and kngifude fbrw on the map<br />

projection.<br />

projactlon tkka and eroaaee-licks<br />

fMIPCI~KIJCU tO and inside the nastlino of a<br />

-P @c~ tO indi=te points threugh whkh<br />

parallels end maridans wou!d pass if they had<br />

bean extended. Small cross MS* indiitrr<br />

where the lines inlerswf within the map.<br />

MI L-HDBK-850<br />

projection transforrnatlon-The process of<br />

changing fmm one map prajacfiin to another<br />

MSP pmj~iOn. Tranaforrmticms may involve<br />

chang= in aquatkma, eltiiaeids, scale factors,<br />

cone cerrstanls,. elendard iin~,. aaandard ,, ~.<br />

parallels, origkrs, central meridians, etc.<br />

pl’o]actlon-l. (geometry) The axtension of<br />

lines or planes to Interaecl a given surface the<br />

transfer of a point from one surface to a<br />

corresponding poaitiin on another surface by<br />

greph~l or aneF@al metfrads. SW afee map<br />

prolwtlon. 2. (photography) Tha process of<br />

placing a negative or posffive photograph in a<br />

projecting camara and r~roducing ha image<br />

on a acraan ar on e sensitized photographic<br />

medium. 3. (surveying) The astansion of a fine<br />

beyond the paints wtrish determine its charscfer<br />

and pesitiin. The transfer cd a series of survey<br />

Iinas to a single thaeretkal fine by a series of<br />

fines Pwpandiiuler to the thaorafkal fine. In<br />

surveying a travarsa, a earirrs et rnawumd shod<br />

lines may be projected onto a singla kng fine,<br />

connecting two main eurvey stations, and the<br />

m lirrs is than treetad ae a measured tine of<br />

the treveree. See also prolongation.<br />

projector station—The pesifion of a projesfor<br />

unit of a steraopfoffar tien absolute orientation<br />

hea been aooompliehad. This poeifiin recreates<br />

the concliiiorts existing et the corresponding<br />

camera efaliorr et the instant of exposura.<br />

pro)actor-An optical instrument tilch throws<br />

the image ot e negetive or print upon a ecraen<br />

204<br />

or ofher viewing surface, ueuaffy at a larger<br />

asala. Sea alwr rotfwtlng projador.<br />

prolata Wpsold ot rotatlo~ae prolato<br />

spharold.<br />

prolate spheroid-An ellipsoid of rdation<br />

efongtha rnajorexie, wtrldrieafongtha arrieot<br />

sarfh rotation. Al@ celled prolate ●lilpaold of<br />

rotation.<br />

prolongation-in eurveyfng, .9 fine is<br />

prafanged when the faa wgment d the<br />

au~ay@d fine is mtanded fn the sap-m dimdorr<br />

as the segment lteeM. A pmkngatbn of a curva<br />

under such a datirWorr of exlersskn would be a<br />

lime tangent to the cwve et the pdnf of<br />

exfansian, although the term frequently is usad<br />

to mean a continuation along the curvature of<br />

the curve.<br />

prOOflng-Tha oparaticrn et pulfing proefs of<br />

pfetas for proofreading, revising, approval, and<br />

other purpce.w prior to pnxtustiorr printing.<br />

proOf-A trial print, produced by any mathsd,<br />

for examination or aditing, 10 be marked for<br />

naceseay carmctbns or a~rwal. Sw elso<br />

color composite; color proof; color proof<br />

process; composite; tlnal compoalta;<br />

gaflay proof;” hand proofi OK shaat;<br />

press proof: progreaahro proo?a:<br />

proofing.<br />

proper motion-That oompenant of the<br />

space mation of a celestial bedy parpendicul.sr<br />

to the line of sight. rasuffing in the change of a<br />

star’s apparent pcraitien relative to a soordinata<br />

system such as right aewrrakr. and declination.<br />

This change is axprasaed as a vefoolfy, suoh as<br />

seconds of arc par century.<br />

propo~y map—See cadastral map.<br />

proparty ●urvay—See land survey.<br />

proportlonato maasuramant—A<br />

maasurament that appfias an aven d=tributiin<br />

of a dstarmined excess or defiiierq of<br />

measurement, ascertained by retracement of an<br />

established fine, to provide concordant reletiwrs<br />

between all parts. See alae doublo<br />

proportionate moaaurament; shrglo<br />

proportionate measurement.<br />

prototypa—See ●xperlmentel map; pilot<br />

sheet.


protrlslonal ediflort-A map or chart printad<br />

and dsvbutad for krpomry use with the<br />

fxwiao Ihrd it Wil letw be Superseded h<br />

died prollmina~ adftlon.<br />

proviolond map-Any nonoffiiisl map,<br />

pheto, or other material which is used as a map.<br />

H mey vary from a hlghfy accurate captured<br />

enemy map, which has not bean sanctioned for<br />

uaa, to a hsatify made dmwfng or sketch. n is<br />

uaudfy a hsstify made lie map bsaed on eerial<br />

phofogmphs, used as a map aubstifule.<br />

pmxlmlty wtelyaia-Analytical !echnqu.s<br />

used to dalemrina the reletiontip bahvaan a<br />

qxrcified point and its naigFbcva.<br />

pmxlmlfy aaerch-h analytical procedure 10<br />

identify occurrences of pradefined data<br />

efemants in the neighborhecd of a Aected<br />

fmint.<br />

proxlmlty-A measure of closeness to a<br />

specified point es dafined by a user.<br />

paaudoscoplc stereo-A three-dimensional<br />

impfe~~n, d, m~~f Wftkh k the reverse of that<br />

actuslly ex=tmg hen Ihe posiliins of a stereo<br />

pair of photographs are interchanged. Also<br />

called inverted stereo: reverse stereo.<br />

See also false stereo.<br />

publication acele-See raproductlon<br />

scale.<br />

Pulkovo 1942 datum-The geodetic datum<br />

defined et Pulkovo Observatory, U.S.S.R. using<br />

the Kraaevsky ellipseid.<br />

pull up-sac selectlon overlay.<br />

pulso Oopplar mep matching (POMM)—<br />

An image rrdching sonc+ employing a pulse<br />

Ooppfar mapping tachnque to locate three<br />

preselected unique edges within the terrain<br />

scerra viewed prior to reanlry of the vehicle.<br />

Edges are defined by differeffiw in mder<br />

reflectance. Range and mnge rate data are<br />

ob4einad from a small elemental area of the<br />

ten’sin lllumitWed by the antenna beam apet<br />

durfrrg a fbt action. A rangdmnge rate map of<br />

the spot area is then oc.rrehxted agsins! a<br />

reference map of the particular edge to provide<br />

e range end vefocii update to the onbesrd<br />

vahcle Inertisl measurement unit (IMU). Three<br />

such aucceasive fm corretat’kms are exacufed 10<br />

enable a trilatem!ion eolution of the vehcla’s<br />

MI L-HDBK-850<br />

205<br />

peeifiin relative to the farga+ scans by the<br />

aanaor’a cxunpufer. Tharafore, the IMU can<br />

cakxfete a cxwracftie manawar prior to }@Cf.<br />

PYfJmY meter—A small cup ~ currant mater<br />

tor usa in totv vabchy maaxwwnarrte m afmflow<br />

StM8MS. ~b M8t= & llsad in ~jUtlCtiOfl with<br />

wsding rode onfy.<br />

Pythagorean right-englo lnvarsor— A<br />

a@fe dfrvic8 whiih provides a nrachankal<br />

selutien for tinner end angular alemenfs of<br />

mcfifiition, thus parrnifthg any enfargar to be<br />

msda autofocusing provided nagetkva, lane, and<br />

aaaal pfenaa era psmtld.<br />

PZS trlangla-see ●etronomlc triangle.<br />

,. ..., ... . . . ..: ... . .


quad corner IIraao-A user-defined<br />

measure relsling to the pertwn of a<br />

quadrangle mapping sheet where it @ins<br />

two or more other sheets.<br />

quadmnglo map-See quadrangle.<br />

MIL-HDBK-850<br />

quadrangle report-A brief history of the<br />

vine of a apecifc qusdmngle. It<br />

accompanies the mapping materisl through<br />

ash phase of production, and la filed with<br />

the map materiel. The nemslive summary<br />

for each opemhnsl phase stressas<br />

conditions that may affect Ister phases.<br />

quadmngle-A rectangular, w nearly ee,<br />

ares covered by e msp or plsl, usualty<br />

bounded by given meridians cd longitude<br />

and parallels of Iatitwde. Also cslled quad;<br />

qundrmrgla mep. See alse standard<br />

quadrangle.<br />

quadmnt—1.. (rrssthernst.ks) .4_6a~lm @YinE,<br />

an arc of 90”. 2. (surveying) A surveying or<br />

astronomic instrument compased of e<br />

gradusted arc sboul 90” in length (1 80° in<br />

rang a), equipped with a sighting device.<br />

The quadrant msy be considered a form of<br />

sector. Some survey quadrante combine<br />

both surveying and aefronom’k tuncfions.<br />

quadretura-i. The Posi)on in the phase<br />

cycle when the two principal tide producing<br />

Htes (Moon ard Sun) ara neeriy at a righl<br />

angle to the Earlh: the Maon is then in<br />

quadrature in its first qusrler ar tesl quarter.<br />

2. The sifuetion ef two periodic quantities<br />

differing by a querier of a cycle.<br />

quad—Abbrevieled form of quadrangle or<br />

quedrileterel.<br />

quality control—The process of taking<br />

steps to ensure the qualii ot dsta w<br />

ooemtic+rs in keeoirm with standards seI for<br />

the system. -<br />

quarter eectlon corner—A comer et an<br />

axfremhy of e boundary ef a qusrler<br />

section, Writfen as 114 section comer, not<br />

as one-fourth section mrner.<br />

quarter ●stlon-One-foutih of a section,<br />

containing 160 acras mora or less.<br />

Q<br />

quarf-rquarter soctlon corner—A comer<br />

at an esfremity of a boumfsry of a qusrferquarfer<br />

tiion; m~nl between or 20<br />

chains from the ccrrrtmlting cc+nara on the<br />

section or township boundaries. Written as<br />

1/16 eec+km comer. Akso celled sixteenth<br />

section corner.<br />

quartz pendulurrr-A pendulum of fused<br />

qusrfz ueed for determining the<br />

eccelerat”m of greviiy. QUS* ie errployed<br />

in the cohsfrwtkrn because ifs thermal<br />

~Penebn tiient is OntY one-fourth that<br />

ef Invar.<br />

quary langrsage-A set of commends used<br />

for deta rnen~uietion in data beae<br />

management systems.<br />

quick-look plot—A “draft’ plot done very<br />

fast, which may not adhere to the positional<br />

accumcy or syrnbolizetien of tha final plot.<br />

“- qblritarii-A s%rrtant having a range of 144°,<br />

or an arc ot 72”.<br />

206


MIL-HDBK-850<br />

1. R4D-(Raady for L%tributii) A term referring to<br />

printed MC&G products rmdy to be distributed<br />

to the customer.<br />

R4R-(Ra.ady for Reproduction) A term rafsrring<br />

to raprmductii rmkial reedy to be printed.<br />

radar ●ftlmetw-An instmmant used for<br />

determining aircraft ffying height above terrain<br />

by meaaurarnant of time Inta+vala between<br />

emiaakxr and relum Of elacfromagnatic pulses.<br />

radar hltltu~llre alt~ude cd en aircraft or<br />

s+acacrafl as determined by a radar alfima!ec<br />

thus, the actual distance from rhe nearest<br />

terrain feature.<br />

radar chrwf-A chart intended primarily for use<br />

with radar, or one suitable for this purpose.<br />

molar clutter-(JCS) Unwanted signals,<br />

echoes, or images on the face of the display<br />

ttbe which interfere with cbaarvetion of desired<br />

signals. ‘ ““”<br />

rsder correlation-The process of<br />

electronically relating raattime radar images with<br />

amrad digital data on the radar refladance and<br />

pasifiorr of terrain and features on the Earth’s<br />

surface. It is used to pmv’k3a positioning<br />

information to cerracf or check air navigation<br />

and guidance systems.<br />

radar coverag~JCS) The fimits within<br />

ti!ch objects can be detected by one or more<br />

mder stations.<br />

radar fix oolnt (RFP)-The most significant<br />

-..:. .raoarscopa<br />

grourro raarura tor a gnfen<br />

geographic area. The faattaw rrmy be radar<br />

reflective or ccwrrpleiely void of raflactivii to<br />

show cc+ttraaf with the surrounding area: e.g.,<br />

ferrdwater w ahcrwlrro show. Posit”kmirrg data<br />

estabfiehad for RFPs are used in offeat aiming<br />

procedures or for anmuta and final update of<br />

navigation systama.<br />

radar horizon-(JCS) The lams of pints at<br />

which the rays fmm a radar antarrna become<br />

tangential 10 the aarth’s surface. On the open<br />

sea this Iccua Lehorizontal but on land ii varias<br />

according to the topographical features of the<br />

tarrain.<br />

R<br />

207<br />

radar Intelligence ftom-A feature which is<br />

radar aignifiint but wlkh cannot be identified<br />

ezectly at the moment of its appearance ea<br />

homogarraous.<br />

radar Intalllgmco map (RIM)-A n<br />

intermediate ekrmarrf in lha pmcaaa of lightopticd<br />

radar airrru!atian and in fha pmducfion d<br />

anafyiiil predictions.<br />

radar map-A map pmducad through th6<br />

a@iition of radar techniques.<br />

radar photography-A cornbkretion of the<br />

pfrotagraphic pmcaaa and radar techniques.<br />

Electrical impulaas are sent out in<br />

predetermined diracfiins and the reflected or<br />

returned rays are ufilizad to present images on<br />

cathode-ray tubaa. Phalographs are then taken<br />

of tha information d=played on the tkae.<br />

radar prediction cntogorlas—in fhe<br />

bmadesl sense, radar prediction is saparmad<br />

into-two major categories, ‘axperierme pradiiion<br />

and analytical prediction.<br />

radar pradictlon tormats—Radar<br />

pradiiliorm appear in a wde variaty of formats,<br />

ganerally indicative of irrtarrdad appliit”krn. The<br />

four most common formats are spot<br />

predictions: strip Dredict”kxrs; radar intelligence<br />

maps (RIM); and Series 200 Atr Target Charts.<br />

radar pradlctlon typas-Eech mapr radar<br />

prediction categay is dwided into three types of<br />

pradkf”mna: single heading ~ediiiorrs:<br />

omnidkectional pradictionq and omnigain<br />

pradiitiorrs.<br />

rsdsr r@connalaaanca-(JCS) Reconnaissanoa<br />

by means o# radar to obtain<br />

infomratkm, on enemy acftilfy and to determine<br />

tha nature of tarrain.<br />

radar raflactivfty plata-A scaled, threadimenslonal<br />

madel of e large! area cxxrafructad<br />

of radar reflective materials on a transparent<br />

plastic pfate, used in a radar trainer to simulate<br />

Iha radar returns of that araa. Alaa dad radar<br />

simulation plate; radar trainer pleta.<br />

radar reflector-A device capable of or<br />

intended for reflecting radar signals.


adar raturn ●islysla-Those items of the<br />

rsdsr eignifiince ardysia mde (RSAC), fhe<br />

~ial arm (SA) krforrnsfien, and the radar<br />

eigntfiint powarliie (RSPL) informstien which<br />

his been devebpad from en mstyeia d<br />

sartographc, phomgraphic, and intelligence<br />

mums.<br />

radar r-turn cod. (RRC)-An<br />

omnidirtrctionsl radar prediiicm based on the<br />

decibel radar prediiicm system and depicted in<br />

a mbr mde on cartein air target cfwta.<br />

redar ●fredow-A cxmdiiion in ~ih radar<br />

signals do not reach a region bemuse of an<br />

intervening obs4ructi0n.<br />

radar signlfkanco ●nnlysh code<br />

(RSAC)-The unique radsr intensity ategories<br />

of buiff-uo areas end other rsdsr reflacflve<br />

objects ~ structures bead on surface<br />

msteriaffheighf factors, and depicted by a<br />

system of cder axlkrg.<br />

rsder significant power Ilrm (RSPL)-A<br />

power transmisaien fine wlich, because of its<br />

unique .physicsl. charactericks sn#Or vottsge<br />

capsciiy. is known to possess rsdar reflective<br />

quafitias, and is therefore dktirrctively diapfayad<br />

on e target graphic.<br />

radar ●lmulatlon plate-See radar<br />

reflectivity plate.<br />

radar te raet—An obiect whch reflects s<br />

suffiiienf t%mmt et a“radsr eignel to produce<br />

an echo signal on the radar screen.<br />

radar tralnor plata-Se e radsr ref Iactlvlty<br />

plate.<br />

Radar, Synthetic Aportura (SAR~A<br />

radar in which a synthatiilly krng apparent or<br />

effectiie aperiure is mnatrustad by integrating<br />

muftiple ratuma fmrr the same ground call,<br />

taking edvanfege of the Dop@er effd to<br />

prcduce ❑ phase history film er taps that may<br />

be opticefhy or digifalfy procaaasd to reproduce<br />

an image.<br />

radar gram matry—That branch of<br />

photogrsmrrwtry whiih tdifiias radar images.<br />

radarscope overlay a-(JCS) Transparent<br />

overleys for pfacing on the radersmpe for<br />

mm’rparieon and identifiitiorr of radar returns.<br />

MIL-HDBK-850<br />

208<br />

redarscopc photography—(JCS) A film<br />

remrd of the returns shown by e radar screen.<br />

radar-(JCS) Radm detectiin and ranging<br />

equipment thst determines the distance and<br />

usueffy the diractiin of ebjacts by trsnsmiseien<br />

and return of e)ec+romegnefii energy.<br />

radial aeeumption-in an aerial photograph<br />

mntaining both fiil diapfecement and relief<br />

diipfacement. neither the nsdir poinf nor the<br />

imcanfar is the thaoraficalty corrad rsdd canter.<br />

llw phdogrsphic rmdir point sheufd be used ae<br />

the rediaf center if relief is the rruipr<br />

conektaration and the iaocantar ahoufd k IJA<br />

if tin is the mspr consideration.<br />

radial cantar-Tha aaieclad point on a<br />

photograph from which radials (directions) to<br />

varioua imoge peinta are drawn or maasure~<br />

that “s, the origin ef radials. The radial centar is<br />

either the princiil faint, the nedir point, the<br />

iaocanter, or a substitute cantar, Alee callsd<br />

center of redletlon; center point.<br />

radlel dlstorflon-Linear displacement of<br />

irnsge ~inta rsdmlty to or frern the center of the<br />

image fieH, csused by the fat! thet objects at<br />

different angular d~tancrrs fmm the lsna axis<br />

undergo different msgnifiitionc.<br />

rsdlal Ilrm lntereectlon-Thai point at whch<br />

Iwo or more rsdisl lines crass or inlerascf.<br />

redial Ilne plotter—Se e radial plotter.<br />

radial Ilne.-(suweying) A radius fine of a<br />

circufar curve to a designated point in the curve;<br />

if the fine is extended beyond the mrwex side of<br />

the curve, it is a prolongation of the radisl fine.<br />

radial plottor-A device wheraby two<br />

overlapping phetographa are viewed<br />

etereoacupicslfy, and the pfanimatrk details in<br />

their cwmmon ares can then ba transferred to a<br />

MSP or baas sheet through s mechanical<br />

linkage utifiiing the r.diil fine principle, ALSO<br />

called radial Ilrm plotter.<br />

radial plot—See radial triangulation.<br />

radial secsttor-See tomplet cutter.<br />

radial triangulation-The aerofriangulation<br />

procedure, efther grsphlcal or amrfytical, in which<br />

directions from the radial center, or approximate


I<br />

I<br />

, ‘,, \ ‘. ... .<br />

rad~l ctmaer, of each werbpping photograph<br />

! are used for horizontal corttroi extension by the<br />

I sucmsdve irrteraatian and maecfion of therm<br />

I<br />

I<br />

I mdlarrt<br />

direction fines. A radisl wirmgufetion sfsa is<br />

oorrectty sailed a mdfxl ptot or a minor<br />

controi<br />

is rolled<br />

plot. If made<br />

an ●mlytlcal<br />

by”ana~d methods,<br />

radial triangulation.<br />

it<br />

A radial trfanoufation is assumed to be anmhiml<br />

MIL-HDBK-850<br />

unlasa prsfis&lby the word snalytlcal; l!”is<br />

dse rmsumed to be based on the ~’*1 point<br />

unless prefoted @ defmilive t- such as<br />

Iwaoontsr or nadir point.<br />

mdlat-(phetogmrnmatry) A line er dwecticm<br />

frem the radal mrster to any peint on a<br />

phcxograph. The radial center is assumed to be<br />

tha principal point, unle= otherwise designated<br />

(e.g., nadir radml). See alsa lsomdlal: nadir<br />

radial; prlnclpal-point radial.<br />

●nergy-The energy of any type of<br />

electromagnetic radmlian. See also radlatlon,<br />

definition 2.<br />

radlatlorr-1. (surveying) The prccees of<br />

fowling pints by a knowledge of their diracfkm<br />

ard dlaiarsm from a known point. The directbm<br />

may be SZlmutha W. bearings read hom,a. , .<br />

theodolite or graphical directions determined by<br />

afidade and pfanalable. The dkdences may be<br />

tapad or maasunsd by stadia. 2. The proca%<br />

by which electromagnetic energy is propagated<br />

thrwgh free space by virlue of joint undulatory<br />

varfatiorrs in the electric and magnetii fialda in<br />

space.<br />

radio acouatlc ranging—A means of<br />

determining dstance by a omnbinatierr af radm<br />

and sound; Ihe radio being used to datennine<br />

tha instant of transmiaakm or reception of the<br />

sound, and the distanca being determined by<br />

ths time of transit of sound, uaualfy in waler.<br />

radio batrcon-(JCS) A radio transmitter<br />

ehiih emils a disthctive, or cheracteriatk, signal<br />

used for the determination ef bsaringa, cwreea,<br />

or lccatien.<br />

radio dlrectlon flndlng+JCS) Radio<br />

fmafiin in wh~h only the directbrr of a statian is<br />

determined by means ef ita emiasirma.<br />

radio faclllty charf-See onroute chart.<br />

mdlo ffx-(JCS) The location of a ship or<br />

aircraft by determining Ihe dkacfiorr of radii<br />

signals comin~ to the ship or aircraft from two or<br />

more sending stations, the focations of wisiih<br />

209<br />

are known.<br />

radio lntorferornatm-An intarfemmetar<br />

operating at radio tr~wsncies; used in radio<br />

astronomy end in satellite traoWsg.<br />

mdlo navigation-(JCS) Radm bcatiin<br />

intended for the determination af position or<br />

direction ar far abatruct”mrr warning in navigation.<br />

mdlo mnga flndlngs-(JCS) Radio Lmetion<br />

in which fha diafam of an ab@ct is de4emrined<br />

by maana of ita radii omissions, whether<br />

independent, reffacfed or retransmitted on the<br />

same or other wev@ength.<br />

radio rango statfon-(JCS) A radio<br />

navigation land station in the aeronautical radii<br />

navigatbn service prevkfing redia aquisiffnal<br />

zones. In certain instances a radio ranga station<br />

WY be placed cm board a shii.<br />

radlomotrlc camera caflbralion—The<br />

cdibratiin of a camera for spectral recording<br />

characteristics.<br />

mdlomotrlc finearlty-The gray levels are in<br />

fineer Prop3n”krfl to the Iigh! intensities within rI<br />

celor band.<br />

radiometrlc nonlinearity-The analog to<br />

digital oanveraion system that provides signaf to<br />

nOiSe (~) ratios of the sensors, where the S/N<br />

is calculated by the differenm of the eeneds<br />

❑veraga dark signal value dwfdad by the mat<br />

mean square dark noise value. Intermediate<br />

intensities will be finasr representations fmrrr<br />

average whita refamnce to the sverags darfr<br />

reference. Irrlermadate inlenaitics will be<br />

represented using a tinear tonal transfer curve<br />

fer each cmbr ctsannef. Error inlredumd during<br />

the dhgitiitkrn pmcasa whibh causes ma gray<br />

scale valu- for a cder carrponerrf (RGB) to not<br />

ba in tinaar proportii to the aourca intenaitiia<br />

for that component.<br />

radius vactor-Ths fine (distance) and<br />

direction mnnectirrg the origin with the ~“nt<br />

whose positian is baing defined. See also polar<br />

coordinates.<br />

random ●rror-Random errors are these not<br />

classified es bfundera, syatermtic errors, or<br />

periodii errors. They are nurrsamus, indwidualty<br />

arrmll, and each is as Iikefy to be poail”we as<br />

negativa. Aleo celled accidental ●rror;<br />

casuaf srror.


,<br />

. .. .<br />

MIL-HDBK-850<br />

mndorn lhw-A trial line, directed aS cbaety<br />

es Possible toward a fbred terminal point whiih is<br />

invisW3 trom the initbl ooinl. The arm of<br />

closure permits the tiutalkm of a cormctien<br />

10 the initial azimuth c4 ihe random fine; if atso<br />

permfts the conprrstien of offsets from the<br />

random Iiie to astabkh points on the true tine.<br />

rendom mlcrolonticular screen (RML)-A<br />

high denahy hetftone screen with no specific<br />

screen angle or pattern used to pmdwa high<br />

resolution printing from continuous tene images.<br />

mndom traverakA survey traverse run from<br />

one survey stelien to enother station whch<br />

annef be seen fmrn the first station in order to<br />

de!ermine their relative positicns.<br />

Range Only Correlation System<br />

(R OCS)—An all-weather terminal guidance<br />

system that uses ranging information to<br />

determine its pesition by comparfng two radar<br />

images. The images are taken 90° apart end<br />

m-r~ Wirh a reference (or prediction) of<br />

Cc@resl edge informet”mn (bright @s) in the<br />

mnge return ~g~l. The checkpoint is e<br />

geographic refereme I-tkan, s.dded prier to<br />

the mission, by which the vehicle can determine<br />

course corredon.<br />

range f lnder-An instrument, using the<br />

parallax principle, for finding the distance from a<br />

ptsce of ckreewatic.n to pc.infa et whiih no<br />

instmments are placed.<br />

range lhsa-A boundary of a township<br />

surveyed in a north-south diredon, See alse<br />

townahlp Ilnas.<br />

rengo markam+JCS) A single calibration bfip<br />

fed on to the tima k= of a radial dis+lay. Tha<br />

rotafii af the time base shows the cingte btipa<br />

se a circle on the plan p=asitiin irshcetor esqm.<br />

It may be used to measure range.<br />

range plla-Any pile sewing as a guide for<br />

marine surveying.<br />

range pole-See range rod.<br />

range mto date-information gethered by an<br />

instrument thei measures the mte of change in<br />

the distance (range) to e moving cbject.<br />

rang. maolutlors-(JCS) The ebiiify of the<br />

molar equipment to separate two reflacfing<br />

210<br />

objects cm e simibr bearing, but et dflar.sot<br />

ranges from the antenna. The abiii ia<br />

determined primerity by the pulse length in use.<br />

rang. rod-A etender wod w metal rod, 6 to<br />

8 feet krng, tih a pirrted metal shoe, usuelfy<br />

painted in cmfraatirrg mbra (red and whiie),<br />

alfemetety, at 1-fed intervals. ff is fraquenlty<br />

used es a sighting sigrbsl at the ends of traverse<br />

courses. Also called line rod; Ilnkrg polo;<br />

rango polo; mnglng polo; ●lght rod.<br />

mnge signal-A buoy, rod, flag, or other<br />

similar object used to MS* and identify range<br />

points when taking coundhsgs dwfng a<br />

hydrogmphic survey.<br />

mng-1. (JCS) The distance between eny<br />

given peint and an object or target. 2. The<br />

difference batween the maximum and minimum<br />

of e given aet of quantities. Ses also distance.<br />

3. Two or more objects in line, Swh sbjacfs are<br />

said to be in renge. 4. Any series of contiguous<br />

fownships situated nerfh and eeulh of each<br />

othec also sections similarty ahuated within a<br />

townchip. S. The well-definsd Iinm or courses<br />

wlmee pc@iens are known and are used in<br />

determining eeurrdings in a hydrographic survey.<br />

ranghrg data—lnformet ien gathersd by an<br />

instrument that measures tha diatem (range)<br />

to the object in question.<br />

ranging pola-Sea range rod.<br />

ranging-in—See wiggling-in.<br />

Rester Product Standard(a) (RPS)-A<br />

suite of ueer ayetem eriented sten&rrls<br />

ancompaseing rester deta structure digitizing<br />

amventione, slerage formats and tiling<br />

echemea.<br />

raster data atructurs-A method of<br />

representing MC&G data characterized by n<br />

matrix ot evenly spaced rows and columns of<br />

data peints. These data pointe (celled “pixels’ in<br />

image and scanned map date) fypicelly<br />

represent some value at that peint, while the<br />

peeifion within Ihe columns and rows dalerminee<br />

the geographic position. Raster data structures<br />

are fypicelty used 10 record scanned maps and<br />

charts (MC&G grephw data), image data, or<br />

grktded data.<br />

raster tormat—See raater dats ●truot um.<br />

rastar llnea-The lines of scan of the CRT


I<br />

beam a- the CRT face. See also raster.<br />

raster map product (RMP)-A generic tamr<br />

for mater scanriad tmp knagaa not fourd 10 be<br />

in accodarma with the DMA ADFfG Spaciiiicvr<br />

W =mn Pro9rw t%XCkIdt3S~~.s ADRG.S<br />

(rasler aeperates).<br />

mstor to veotor-The precaaa of converting<br />

an image msda up of calls info ona described<br />

by fiiae end pofygona.<br />

taster-l. Pattern of horizontal, parallel lines<br />

of varying inlensily forming an image (uauafly)<br />

on a calhoda ray I* screen. 2. A regufar grid<br />

cd calls covering an area.<br />

rate ststlon-See drift station.<br />

I mtlo print-A print h wh~h the scale has<br />

bean changad from lhat et the negative by<br />

photographic enlargement or reduction.<br />

. . . .<br />

ratlograph —See ratlomatar.<br />

ratlomoter-An instrument used to help salve<br />

the mathemal”cal relationship of a photograph<br />

to a mosaic.’4t.detmminas Scala -ratirx’ from,,.<br />

which, thrwugh methemctical Ierrnulas, a<br />

rectified print csn ba meda on e pmperfy<br />

caiibratsd rectifying printer.<br />

rational horlzo*See calastlal horizon.<br />

rstlonalizatlon mathod~ technique of<br />

rekrtive orientation wfich lakes into<br />

oonsideratirm the Iimiling faders & the<br />

equipment tiIng used, ths nature rmd<br />

variations of tiff and crab fmgtas at susmsaive<br />

camera sla!ions, and providhg approximate<br />

pmj~tor adjustments based on thesa data.<br />

my of llght-The geometrical corcept of a<br />

single element of Iiihi propagated in a straight<br />

tine and d irrfhitesimvd cress aactii~ used in<br />

arMfyiicaffy tracing tha path of light through an<br />

optical system. See also besm of light.<br />

ray tmclng--(optics) A trigonometric<br />

cafculafion of the path of a tight ray through an<br />

optical system.<br />

Rsydlst—The tmde narna of an alectmnlc<br />

distance measuring system. A nonline-of-sight<br />

syatam capable ef aimutfaneous multiperfy,<br />

ranga-range operatioty if gives cmfinuous<br />

mwa information from fwe basa sfetions<br />

.<br />

MIL-HDBK-850<br />

211<br />

opamtirtg e.huhanacaaJy wffh ona or more<br />

aircraft and surfecs veasek.<br />

mat lmag*An inmge actually produced and<br />

capable dbaingahotwr onaaudaca, as ina<br />

camera,<br />

raaltima meth rnodai-A set of equalione<br />

that definse hags Oootitnetes as funcfkrns d<br />

thma-dimerwbml object coordinate for a<br />

region ot fmgery.<br />

rsar ●lamont—See lane elemsrrt.<br />

rsar nodal point—See nodal point.<br />

racsll-(digitel) A p-urn which raatoms the<br />

previeus entry.<br />

resaat-lo changa a map fmm one horizontal<br />

da!um to another by cppmprialely changing tha<br />

gsographc values of the rnsp grclicule.<br />

rasolver-1. (pendulum) A heavy -oest metal<br />

box within which the pendulum is suspended<br />

end seine auxiliary equipment plscad whan<br />

rrmking observations for the intansfly of gravity.<br />

2 (setetfiie surveying) The aqulpmcnt<br />

nacaasery 10 rexive signals brosdcasl fmm the<br />

Navy Navigat”mn Sstellhe System, including an<br />

antenna, preamplifier, processor, oscillator,<br />

OUIPUI device, and power systam.<br />

raclprocal bearing—See back bearing,<br />

defiiifion 1.<br />

mclprocal levetlng—Trigonomefrk leveling<br />

wherein vetl’kxd angles have %n observed at<br />

both ends of the line to efimirmta errors.<br />

rsclptocal obsarvatlons-Obsemations<br />

teken backwati and forward such es vertical<br />

angles at both termini of a Iina for trigemxrretric<br />

Ievaling.<br />

racipmcal vartlcaf angle-A vertical angla<br />

measured owar a line at both ends in<br />

trigonometric leve~mg to efiminate (at Ieasf<br />

paflly) the effects of curvature and refmcfiorr.<br />

Raciprscal observations mud be made as<br />

simuffaneousfy as predicable to obviate error<br />

caused by changing refmcfiva condiiicms.<br />

mclaaelfy—(digifaf) A prosarfura 10 change fhe<br />

classification of existing data.<br />

recognition—in photointerpretation, the act of


I dmvering<br />

the true identity of en olject.<br />

recompilation-llze proce= of producing e<br />

map or theft thst is essantislly a new item and<br />

which r@ecas e previously pubfiihed item.<br />

NormslFy, rtxmmpilatkm of a nwp a chart<br />

irwofvas e@ifkant cfvsrrge to the horizorwsl<br />

Posffiin of features, revisiin of vertical values,<br />

irrpmvenrarrt in pbnimatric or nsvigetbrref dete,<br />

or eny combiraetion of these faders.<br />

MIL-HDBK-850<br />

reconnalssanco map-The plottad results of<br />

e reamnaisasme survey and date obtsirssd<br />

fmm other source.<br />

reconnalssanco photography—(JCS)<br />

Photography taken to obtain Infermstbn on the<br />

resuffs of bombing, or on enemy rnxamants,<br />

rnncentrstiins, activities ad forces. The<br />

primsry purposes do not include msking msps,<br />

chmts, or rnossics.<br />

reconnaissance sketch—A drawing which<br />

msambfes a reconnaissan.xr msp but is Iscking<br />

in acme rnep element.<br />

reconnaissance survey-A preliminary<br />

. .. . . Sulvsy, usually asecuted repidly and at relativdy<br />

low cast. The information obtained is mc.mded,<br />

10 some estent, in the form of a recennsiseence<br />

msp or sketch.<br />

reconnelesance-(JCS) A mission<br />

undertaken to obtain, by visual drsarvatbn or<br />

other detactien methods, information aboui the<br />

acfiviiiss end r~urces of an enemy or pofantial<br />

enemy or to secure dsta corrceming the<br />

meteerologicd, hydrogmphic, or gaagrsphic<br />

charsctaristica of a particular ares. SW also<br />

eerlal raconnalasancsi; hydrographlc<br />

reconnal~aanca: rader reconrs.slsaance:<br />

triangulation raconnalsaanca.<br />

reconstructed Imagery -lmsgary on film<br />

derived from processed digital imege dste by<br />

means of film printer.<br />

racording ●tatoacope-A atatoacope<br />

equipped tih a recording camare hose<br />

shuiter is synchrenizwj wilh that of the aerial<br />

camsrs and the imsge of the statoscope is<br />

recorded on each indwiduel frame.<br />

racovswad control—See recover.<br />

recovery of station—See resover.<br />

212<br />

racovar-(suweying) To visit a survey station,<br />

identify ifs mark as euthentic and in its orighal<br />

bcetion, and vady w revise its dasc@cm. Ths<br />

Wrrn is usustty modiiiad to indiite the type or<br />

nature of the rscaery, such as mccrvsrd bendI<br />

rnmk, w a racevsred Wisnguletion stat”mn.<br />

rectagrav@r-A acribhg instrument wl’kh raete<br />

on the scribing sudsce during the operation and<br />

only the culfer erm moves to scribe each<br />

symbol.<br />

rectangular chart-A chart on tha<br />

rsdsngular prqeotkm.<br />

rectangular coordirmta plottor~ e e<br />

coordlnatogreph.<br />

rectangular cnordInatas-Coordinsles on<br />

any system in which the rues of reference<br />

intarsecf al right angles, See alao Cartaaian<br />

coordinates.<br />

rectangular map projection—A cylindrical<br />

-P Pmi*ion with uniform spacing of the<br />

parailels.<br />

roctsmg ular polyconlc map projection-A<br />

rnedifkl polyconic msp projaclhn having a line<br />

reprsasnting a slandsti psrsllel divided to mwacf<br />

scale, through whose division points pass the<br />

Iinas representing the gaogrsph~ meridians,<br />

intersecting the lines which repra~nt the<br />

geographic parallels in right angles.<br />

rectangular spaca coordinates—The<br />

perpendicular distarwes of a point from places<br />

dafinad by eech pair d a sat of three rurea<br />

wlsich are mutually perpendicular to esch other<br />

at a cemmon point of erig”m. In<br />

pfwlogrsmmatryr specs cocmtinstes are also<br />

called survey coordlnatea, and ere the .scoerdinstes<br />

and yamdinstes whidr ddins the<br />

horizontal positii d e point on a grcund<br />

system, and the zummdinste, which is Ihs<br />

elavatiin of the Pc4nt with reference to the<br />

ground system. Alss csllad elr coordinates.<br />

rectangular survey s-A system of surveys in<br />

~ih en ares is diiidad by a bssa tine<br />

mtersecfed at right angl~ by a princiial<br />

meridian, tha intersection termed tha inilal point<br />

from which the partitions ere subdivided into<br />

equal size townshps containing 3S ssctimw of<br />

lend each.<br />

rectlflcatlorr-(JCS) In photogramrnstfy, the<br />

.,. .


MIL.HDBK-850<br />

process of p+cfing a tiffed or obfii<br />

photograph onto a horizontal reference plane.<br />

lAlf~h the process kr applied -My to<br />

aerial photographs, il may also ba applii 10 the<br />

correction of map daformalion.] Sea also<br />

●talytlcal ortont.stlon; ●mplrlcal<br />

orlontatlon; graphical ractlflcatlon;<br />

multlplo-sksgo rectlficatlon: optical<br />

rectification; p=per-sttlp method; polntmalchlng<br />

method; transformation.<br />

roctlfled ●ltItuda-Saa eppmsnt ●ltitude.<br />

rectified prhrt-A phetogra@r in whiih tilt<br />

dspkrcemant has been removed from the<br />

original negative, and witiih has bean brwghf<br />

to 8 daaiiad scale.<br />

rcdifiar-A apacially daaignad proj-ion<br />

printar wtrosa gaomatry is variable in order to<br />

aiimlna!a till from an aerial nagativa. There are<br />

fwe basii IYPSY those in whch tfra optical axis<br />

of the racfifiir lens is the mmrnon ralerance or<br />

base diredbn of the instrument, and those in<br />

whiih the line batwean the Princ@le point of the<br />

negative and the rectifier lane is the common<br />

reference. Also called cutomatic rectiflw<br />

ponoutom~t Ice .wtif!er; nontiltlng- lens<br />

4“ “ ‘“”‘-iectlfler; nontlltlng-nogatlve- plane<br />

mctlfler; rectifying camera; tilting-lens<br />

rectlfler. See alae autofocus rectifier:<br />

transforming printer.<br />

mctlfylng camOra-See rectifier.<br />

rectifying latituda-The tatifude on e sphere<br />

such that a great circle on if has the same<br />

length sc a meridiin on tha spheroid and such<br />

that all lengths along e maridkm frem the<br />

Equator are exactly equal to the cerraspending<br />

Iangfhs on tfra Wheroid. Rectifying Mtude is an<br />

atmihy latitude used in prcislerns of geodesy<br />

and Canography.<br />

mctlfylng printer—See rectifier.<br />

rectilinear coordlnatoa—Sea rectangular<br />

coordlrrataa.<br />

mctobllqum plotter-See ●ngulator.<br />

rectoplanlgraph-An instrument utilizing e<br />

vertical photograph mounted in a verlical<br />

pcdth, and used in the preparation of<br />

planimatric maps.<br />

red Ilght madabls ma~A map printed with<br />

epeciel inks vhiih can be read under condiIiona<br />

Z13<br />

requiring E@CXASI fighting e.g., in a tank or<br />

aircnsfl during rtightfkntr oparatbna.<br />

red magnetlarn-The megnetiarn of the<br />

north-seeking and of a freely auapwwW<br />

magna. This is the magnetism of ths Earth’a<br />

south megnafic pole. see also blue<br />

ntegnetlsm.<br />

reduced gmvlfy~rvsrd gravity that has<br />

trwn reduced to the gaoid or to some other<br />

rafarence surface by one c4 the gravily<br />

reductions.<br />

reduced latltuda-Se e parametric<br />

latitude.<br />

reduction factor—Sea scale of<br />

reproduction.<br />

reduction printer—See diaposltlvo<br />

printer.<br />

raductlon to ●lllpsold-l%e correction<br />

aubtrackl fmm or addad to the maaaurad<br />

horizontal length d a Iina at avaraga<br />

topographic elavatien to mduca & to the<br />

ccmrastmndhg length on the pertinent etfii.<br />

Tha haighI used in Ihlc raducthn vAtl dtier by<br />

the amount of the gaoid heighf from the hdght<br />

mad in reduction to saa Iavel.<br />

reduction to sea level—A reduction applied<br />

to a measured horizontal ferrgfh on ltra Earth’s<br />

surface to radma it to the surface of the focal<br />

aaa level datum.<br />

reduction to the merldlan—l%e procaee of<br />

aPPfYm9 a ~r-tbn to an aftftude O&XSCWVad<br />

tien a body IS near the celeet”kd maridiin of Ihe<br />

Mraarvar, to find the al!ifuda at maridiin tranah.<br />

The allilude at the time c4 such en cbaarvation<br />

is called an ●xmerldlan altltudo.<br />

reduction-to-contor-l. The emeunt which<br />

must be appiiad to e dwacticur ebaervad al an<br />

-ntric statien or to an =Cantrb signet, to<br />

raduce such dtractien to what it would be if there<br />

were no such sccentricii. 2. (aafronemy) One of<br />

the values used in finding Ihe equation of time.<br />

reference datunr-A general term applhd to<br />

any datum, plane, er surface usad as m<br />

reference or base frrrm wtriih other quantiiiaa<br />

can be measured.<br />

reference dlrectlon—A direction uaad as a


I<br />

,<br />

!<br />

I<br />

1<br />

’<br />

;<br />

besis for compsrkn of other duact”ms.<br />

rekwsnco ●lllpsold—See reference<br />

sphorold.<br />

rofermtcrn frama-See coordlnrstoe.<br />

rm?mrwsco grid-See grid.<br />

rsrforanco lovol—See datum Iovol.<br />

MIL-HDBK-850<br />

mfomnco Ilne-Any line whiih csn serve as s<br />

mfemnce or base fer the masauremant of other<br />

qusntitiea. Alae celled datum line.<br />

reference mark—A permanent<br />

suppfamantary msrk cbas to a survey atetiin to<br />

which it is relstsd by an accumtety measured<br />

dktence end direction, andfor a difference in<br />

elevetion.<br />

rofarsmco maridlmr—See local meridian.<br />

reference monument+% iron post or rock<br />

csp eczxssory used where the peint for a comer<br />

rncmumsrrt is such that, for prectiial purposes, a<br />

permsnent comer rrmnumant cannot be<br />

eclab%hed, or If mooumentad, a full<br />

=m@emsnt of bearing trees or bsering ti)acts<br />

are not obtainable.<br />

mfarenca plane-See datum level.<br />

mforonce point—See detum point.<br />

reference clgnaf-in telemetry, the signel<br />

against whiih data carrying signsls are<br />

mmperd to measure dtierenceg in timrj,<br />

phsae, frequency, or other veluas or quantities.<br />

reforenco spheroid—A Iheore!ical figure<br />

whoaa d!msnsione cfosafy approach the<br />

dimensions of fhe E@@ the exact dimensions<br />

are delenninad by various consideretiona of the<br />

section of the Eenh’e surfeca concerned. Also<br />

cdlad reference .Ilipsold: sphorold of<br />

roferonco. See al- World Geodetic<br />

Syetem.<br />

referonco statlo*A place where tide or tidsl<br />

current ocmstants have bean determined from<br />

observations, end whloh are used as a standard<br />

for the comparison of simuftrmseus<br />

observations at a subordinate station. Ako, a<br />

piece fer whkh Independent daily predictions<br />

are obtahad for other locations by means of<br />

dfierencas or fectors. Also cslled stenderd<br />

214<br />

po~, standard ●tstlon.<br />

rafarenclng—?he process of measuring the<br />

Iwizontsl diaiemee and dradioms from a<br />

survey station to nearby Iandmsrka, refarame<br />

rnsrka, and other ob@cfe whfi can be uafxf in .<br />

the ~ary of the station.<br />

mttactad ray-A my extending outward from<br />

e point of mfktii.<br />

ratlactlng prlsrrt+i prism thst devietee a fiiht<br />

besm by interrsd reflection, Practkslty all prisms<br />

used in photogremntatric” instruments ❑re of fhia<br />

type.<br />

reflecting pro]ector-An instrument whmh is<br />

used to projsct the imege of photographs,<br />

~1% ~ et~r gmphik= enio e copying tsble.<br />

Ths scsle of the projected irrmge can be varied<br />

by raising or bwering the pro@bar or, In some<br />

models, the copy bosrd, Thsae fatter models<br />

sko ellow the tilling of the copy besrd in x- and<br />

ydiractions in order to compensate For tip and<br />

tilf dktortbn in aerial phetogrephs.<br />

refloctlon—The return or change in the<br />

direction of travel of psrtidae or mdmnt energy ~---~ ~ -- ,<br />

vhkh irrpinges on a surfaca bui does not enter<br />

the substance providing the reflecting aurfaca.<br />

See also dlffractlon; dlffuso rafloctlon;<br />

refraction; specular reflection.<br />

reflector constant—The emourd thsl a<br />

distance measurement must be reduced *en<br />

using glass reflectors bcause the velocity of<br />

light is sbwer in glass thsn it is in air. The<br />

constant wili also include the distence difference<br />

between the reflector housing plumbing pOim<br />

and the effective reflecthg plane of the prism.<br />

refiight-lmother flight over the same crmree<br />

to xure photographs to fill in for those missing<br />

or dsf ective.<br />

refrected ray—A ray extending onward fmm<br />

the pint of refrect’bn.<br />

refracting prlsrn-A prism lhst deviates a<br />

beem of fight by refrsctiom The angular<br />

deviation is e functien of the wavelength of light;<br />

therefore, if the baem is composed ef while<br />

light, the prism will aprasd the beam into a<br />

spectrum. Refracting prisms can be used in<br />

opticel instruments onty for small Cieviitkrna.<br />

See also wadgo.<br />

mfractlon ●@a-That poti~on of an


.. . .<br />

dzaarved zerkifh distance, wlich is due to the<br />

affect of almaapharic rahzdon.<br />

refraction dlsplacomwrt-fhplaosment ot<br />

Images mdiaky oulward from the PMogmph<br />

nadir bacauae C4 afrnoz@erk rdmdica It ia<br />

assumed fhmt the r8fmction is symrnatficcd<br />

about the nadii direction.<br />

mfractlon Ilne+l line of eight to a survey<br />

signal wtrii becomes visible onfy by the effect<br />

of atmospheric refraction.<br />

rofracflon-lha change In dmactkm d moficm<br />

d a my of rad=rd energy as t passes cbliqualy<br />

from one rnadkim into another in whiih the<br />

speed of propagation is dflarant. Sss also<br />

angle of Incldonce; arrgla of rotractlon;<br />

astronomic rafmction; atmosphorlc<br />

mfrsctlon; coastal rdractton; eoofficlamt<br />

of rafmctlon: .Jectronlc rofmction;<br />

horizontal refraction; lateral rafrsctlon;<br />

mean red mction; mfmcted ray;<br />

refraction ●ngle; refraction Hno; Snell’s<br />

law of mfracllon; torreatrial refraction.<br />

regional grodlont—See regional gravity.<br />

. . . . . . . . . .<br />

reglond gmvky—in grsvity prospecting,<br />

contri~lons to the obsewed rmomslies due to<br />

dendy irregufariti= et much grader d+hs<br />

than those of the pxsible structures, the<br />

kcalion of wh~h was ths purfmsa of the survey.<br />

Also cellad ragional gradient.<br />

reglatar hole punch—See prapunch<br />

raglster system.<br />

reglater marke+JCS) Designmad rrmrks,<br />

such es smell crmsas, circles, or other patterns<br />

applkl to original copy prior to reproduction to<br />

facilitate registratii d plstaa ad to indicate ths<br />

refattie positions of successive in=prtiorrs.<br />

Also called corner marks; corner ticks;<br />

roglstor ticks; reglatration ticks; ticks.<br />

ragfstsr ●tude-Sea pmpunch regist~r<br />

●yatam.<br />

mgfster tfcks—See mglster marks.<br />

mglator trtals-The, test runs necessary to<br />

obtain the proper mmbinetion of the degree of<br />

partial vacuum and the length of the heeling<br />

cycle required for irxfiiiduel models in forming n<br />

pktic mliaf msp.<br />

MI L-HDBK-850<br />

215<br />

r-g lstor-(JCS) The correct poaifii of one<br />

~mnf of a cmnpodte IIMP *ge in<br />

mlatiin to the other components, at each stage<br />

of production.<br />

raglstratlon Uoks-see register marks.<br />

regmaslon of tha nodaa-Processional<br />

motion in a direcfii cppcde to the dmaction of<br />

revolution d a sat d rmrh. sea also<br />

procaaslon.<br />

regular ●rror-saa syatsmatlc ●rror.<br />

ralatfonal data baaa+l data base that<br />

mm&sc#af bxtorze@bb, which, rntum, is<br />

made up of rows and columns. Tat4es in the<br />

data base am rebted to one another through<br />

the value in at least one cotumn tit is common<br />

to two or more tables.<br />

rdativa ●CcurOcy— 1. (genaral) An<br />

evaluation of the random errors in determining<br />

the pocltiinsl onenfatkzn (e.g., distance,<br />

azimuth) of one pint or feat um with respect to<br />

another. 2. (chart, faatura 10 graticule) An<br />

evaluation of the random errors in chsn faaturas<br />

with reaped to ths grsticule axckiing any emcv<br />

in the grst”cub or the datum dafinad by Iha<br />

graticufa. 3. (chart, feature to feature) An<br />

accuracy evaluation based on random errors in<br />

determining the positional accuracy of one point<br />

featurs wiih raapacf to another feature.<br />

ralatfve apertum-(JCS) Tha ratio of the<br />

equivalent focal length to tha dmrneler d the<br />

entrance pupil of photograph~ tens, expreaaad<br />

as f4.5, etc. Also called aperture ratio;<br />

aportura stop; diaphragm stop; fnumbefi<br />

Iana ●pead; spead of lens:<br />

stop; stop numbara.<br />

relative coordinate ayatom—Any<br />

motdht e eystem whkh m moving w~h respect<br />

to an martial coordinate systam.<br />

rofatlvs deflection--See ●atrogoodatlc<br />

deflactlon.<br />

relatlve dlrectlon-Horizontal diraction<br />

expressed as angular dktance from a heading.<br />

relatlva dlatance-Distenc-e ralative to a<br />

spdfmct reference point, usueliy one in motion.<br />

mlatlve ●rror of closure-The value


obtsinad by dikling ths total error of cbsure by<br />

the tdal length of the traverse, ~v<br />

‘V- W a tii kti~ a rxlmarstOr<br />

equal to unity, e.g., 1/1,640. H is uaad fer<br />

ddermining the dagraa d eccumcy ef a survey.<br />

rafatlvo gravtty-Qrav”w determined trom<br />

gravity dflerence rneesurements (e.g.,<br />

gravirnefar, “mfatlve pandufum) batwaen tha<br />

okaver and a reference atshn. Ths vsfue<br />

obtskred is refstiie with rasped to tfw refarertoa<br />

station.<br />

relstlvo mOtlon-See ●pparent motion.<br />

rolatlvo mOWment-MOtion of one object or<br />

bdy relative to andher, The expression is<br />

ususlly used when d~r’ibhg rafstiie<br />

rnovenrsnta ofhar than fhet ef a calesdsl body.<br />

See else tpparent motion; direction of<br />

relative movemont.<br />

relatlvo orlontatiort-The reconstruction<br />

(arvdyticeliy or in a photegrammetric inatrumsnl)<br />

of lhe same gac.metric oondtiions b.stwaan a<br />

pair d photographs thst existed when the<br />

phmognxphs were taken. In the instrument, this<br />

is atilevsd by a syatemstb pnxedure -of<br />

retaticmd snd trsmslationaf movements of the<br />

projectors, Ako csllsd clearing y-parallax.<br />

See elso absolute orlontation; vertical<br />

deformation.<br />

relatlvo pendulum-A device for measuring<br />

relslive gravity through the difference in the<br />

period of a pendulum at two slct’kwrs.<br />

relative posftlowThe Iecstion of e point or<br />

feature with respect to othsr peints or festures,<br />

either fmsd or reeving.<br />

relativo rallef-The refaticm of the aftitudes of<br />

ths highsst and lowest points of fsnd in any<br />

aree. The differanca batwesn the highasf and<br />

lowest peints is fhe ampfiiude of rafative rsfief,<br />

Variws typas of maps hsve bean devised to<br />

show ths, usualty depenrthg on griddkrg the<br />

eres on a mcp, finding e value for the ampfitude<br />

in eech grti wuara, and producing en iaepfdh<br />

or dot map to depict the disftibution of these<br />

velues.<br />

MIL-HDBK-850<br />

rel.stlv. eettlng-in tiff ansfysis of ebfique<br />

pfmtogmphy, the dihedral angle between the<br />

twe pfenes passing through the principal @nt of<br />

the oppeshe obfiiues, the princ”pal point of the<br />

veriical photograph, and the cornmcm axpoeura<br />

statiin. Thii angle ie msasurod on the vert”ul<br />

216<br />

phetogrsph se the angle befwaerr the two<br />

ieofines, or ss the deffeciiort angle befwaan the<br />

~ulam from ths principal point of the<br />

veriic.el phdograph to the fwo isohnea.<br />

ralatlvo awing-fn ths titt rmafyeia d &tiiue<br />

phologrsphs, tha single cd rotation of ths<br />

obliius CSmara aboul ifS H axis with r’6.s@d<br />

to W plans of tha V6t’fiOd ptrdqrraph,<br />

mssaurad on fha obfiqua phofogrsph by ths<br />

eng!a bstween ths iaotina and a tine phing tha<br />

fore and aft fducial mark<br />

refattvo tift-The engukw relationship batwaan<br />

two ovadappiig vattical photogmpha with m<br />

reference fo an astabtiahsd dstum.<br />

releasability code lsdter-A coda letter<br />

pretii to the ctuwi identifiition number which<br />

tim”m the releasabifii et e psrlkular chsrt to<br />

specifii uaem.<br />

rellablllty diagram-A diagram’ incfuded on<br />

some MC6G products depicting horizontal and<br />

vartical accuracies and date(s) of inferrnctien<br />

relief displacement—Displacement radisl<br />

from the nadir peint of a phomgrsph caused by<br />

dtierancas in etevation ef the ccmespxding<br />

ground ebjects. Also callsd height<br />

dlsplacomxmt; relief distortion.<br />

relief distortion-See relief dlsplricemant.<br />

relief modof-A genersl category ~kh<br />

demtes any threedimensional representation<br />

of an ebject or geogrsphc area, rrwdelad in any<br />

size or madium. See eleo plestic relief map;<br />

terrehr model.<br />

rollef strotchlng+ee hypxirstoroo-<br />

Scopy.<br />

rellef-(JCS) Inaqualfties of alevatlon and tha<br />

configuration of Isnd festures err the sudaca of<br />

the Eerlh whmh msy be rapreaented on msps or<br />

chsris by contours, hypsometric tints, shnding,<br />

spd eleval’mns, or hcchures.<br />

Relocatable Terget Assessment Data<br />

(RTAD)-DM4 digitel date sets of attributed<br />

and rrc.naymbofiiad feature information<br />

segregated irrto thematic files perir’eying rued%<br />

railrctrds, vegetation, surface dreinsge, and<br />

fimited eurfece materisf.s which can be mdnd<br />

into three sapmste tevels of dsta. All three<br />

lads use etarrdard DTED Level 1 to dalennine


I<br />

I ,.,..<br />

I<br />

i;<br />

1<br />

I<br />

I<br />

-- ._ .- __..<br />

raprcsontatlvo tratilon (FJF)-(JCS) The<br />

sde et E map or chsti wqmxaad as a traction<br />

or ratio. [Relates unk d-rice en the map to<br />

dstanoa moaaurad In the same unl! m the<br />

ground.] Also called tmcttorrd scale;<br />

netural seele.<br />

reproeentetlve pattern+csrtc.graphy) 1.<br />

An accurate portrayal of the surface of the Earth<br />

in the eras being cor@ad. 2. The sabcfkrrr<br />

ard portrayal of the moat prumfnant of a danse<br />

group of similar features.<br />

reprint—lho process of ualng dating<br />

reproducible wfthoul change to print srddiiion.el<br />

MIL-HDBK-850<br />

eiavatbn, slope, and irrterviarblfii and am<br />

imendcrd 10 be usut with muttiirel er eksctmoptical<br />

image pmducfa. RTAD is used to assess<br />

potent”bl ter@ bcatii.<br />

remote ●onslng-The maaaurarrrarttor<br />

acquisitbrr of intormatien c4 wrrra ~ of am<br />

$~%t~~=or%~~%”~tha<br />

object or phsnomanon urder study. &rmofimas<br />

rasfricfed to the practice d data co%ofion in the<br />

wsvelangfhs fmm uUrsvbJaf to rartb regbna.<br />

remet. ststion-See ●lava stMort.<br />

repostablJJfy-A measure of the variation in<br />

Iha eccuracy of an “mstrurnarrf when taats era<br />

made ovar the same line(s) at dflerenf times of<br />

the year, with dfiamr# eperatore, and with<br />

dtierenf bul equivalent inafrumantb’, ail using<br />

Ora same pmcsdures. See slso ●sternal<br />

●rror.<br />

ropmstlrsg lnstrumOnt—Soa ropeetlng<br />

theodollto.<br />

repaetlng theodolfta-A theodolife so<br />

designed that successive measures of an angle<br />

WY k SCCWIWbItEd en the graduated circle,<br />

and a final reading of the circia made whiih<br />

raprasenta !ha sum of the repetitions. Also<br />

called double-canter thoodollte;<br />

repeating inatrumant.<br />

rapetltlon of ●nglea-The accumulation of a<br />

series of measures of the rarne angle on the<br />

irorizontel circle of a repeating theodofite er<br />

Surveyofs transit.<br />

raplac~A pmcadura to replace all axlsting<br />

occurrarwes 04 e spacfiad data eiamant with a<br />

new data element.<br />

217<br />

qwmtitiaa d a pmcfucd.<br />

raproducibio-Arry capy ca@ia d being<br />

used es a maatar+o-be. May be aiihar a<br />

nwt~a of positiwa tr6n6pr3fan0y.<br />

roproductlon materlsf-(JCS) Materfal,<br />

generally in the form of poaitiva or nagativa<br />

~~fimor~foreh~@e, from<br />

whiianrap orcharf rrraybempmduod<br />

without redraffhtg. Aiao cdiad repromat.<br />

reproduction positive moid-The poaitiie<br />

rrmld wh~h Ima been drilled thtigh vdth<br />

vecuum fsehs, and over which the plaslic raWf<br />

map is formed.<br />

reproduction ratie-See scale of<br />

roprodtrctlorr.<br />

reproduction ●cala-l%e scale et which a<br />

map w chart is pktiied or is to be phlished.<br />

Also csllad publication scale.<br />

reproduction-l. The summation of all the<br />

pmcaesea irwolvad in printing copies from an<br />

original drawing. 2. A printed copy of an origlnd<br />

dmwing made by any of the prweasas d . . . ‘... ‘“=repmduotion.<br />

repromat—See rsproductlon meterlal.<br />

Ropeold besa-llrm maaauring<br />

apparatus—~ optical bese-fins maasuring<br />

aFW~~, comPO* of a steel bar<br />

~mximately 4 matara brig, whose amct<br />

Iarrgih at any Ierrparatura is known, and whose<br />

temperature ia detannined by rnesna d a<br />

metallic thermometer conposad d the steel<br />

measuring bar and a similar bar of zinc, the two<br />

being fastened together at thek middle points.<br />

roaampling+digitsl mapping) Techniqua for<br />

transforming a raster image to a psrkulsr scale<br />

arid projection, Common ressmpiing<br />

tecfiquea inciuda zem-oder (nearest.<br />

neighbor), first order (bilinaer itierpoiatien) and<br />

Cubb Corwolurkrn.<br />

rascala-An edjuafmenf of values or<br />

parameters representing magnitudes or intensity<br />

so that the data reflects an aapeci more suited<br />

10 the user.<br />

reoemr-1. A glass plate on which ia etched<br />

an accurately ruled grid. Sometimaa wed aa o<br />

focsl-plsna plate to provide a msrana of


calibrat”m film dkifort”m used atso for<br />

sehkrratrng pbfting inetrunrertts. Also celled grfd<br />

ptate. 2. Intersecting oRhogonaf lines<br />

euperi~d oww photo irmsgery.<br />

maactlon station-A station kcated by<br />

msadion methods.<br />

rwactlon-1. The graphical or enetyik-al<br />

dsterminatim of a positii, as the irdarsactien<br />

of at fee@ three fines of known direction to<br />

cxxreaponding poirrta of krc.wn pcrsiticm. 2.<br />

[wrvaying) The detarminefim of the horizontal<br />

poeifii d a eurvay station by sbaarved<br />

directiia hurt the etetim to points of known<br />

poaitkms. Atso, the line drawn through the<br />

plettad location of a atetion to the oscupied<br />

station. 3. (photogrammetry) The determination<br />

of the position arrdhr attitude of a camera, or<br />

the photograph taken with that cemere, with<br />

meP@ tO the @de* caordhate system. Also<br />

called thraa-point method. See also<br />

Intersection, definition 2.<br />

residual devl.etion-Devietion of e magnetic<br />

UXrrPSSS aher adjustment or compensation.<br />

rasldrml error-The dfierence batwaen any<br />

value of a quantity in a series of observations,<br />

oorrected for known systematic errors, ❑nd the<br />

value of the quantity obteined from the<br />

combkratkm or adjustment of that series.<br />

Frequently used as the difference between en<br />

obsarved velue end the mean of all observed<br />

values of a etatistisally valid act. See alao error<br />

residual. The latter term is generally used in<br />

referring 10 actuel values in a apesific<br />

computation.<br />

MIL-HDBK-850<br />

raddud gravity-in gravity prospecting, the<br />

portion of e grevify etkd remairrirrg after<br />

removal of some type of ragkmsl gravity, usually<br />

the reletivafy small or local anomaly components<br />

of the total or observed gravity field.<br />

msldual porallax—Srnall amounls of yparallas<br />

whii rney remain in a model after<br />

refative orientation is emm@ishad.<br />

residual+ general term darroting a quantity<br />

remaining after some other quantity has been<br />

subtraded. ft ooxra in a variety of particular<br />

sontexts. For exemple, if the true value of a<br />

varfabla is su~recfed from an observed value<br />

then tha dtierense may be called a maldual; it<br />

ia also frequenlty oelled an ●rror. Similarfy, if a<br />

methemetioal model Is fitted to data, the valuee<br />

by which the observations differ from the model<br />

218<br />

veluee ara satietf raslduala.<br />

resolution In baartng-lhe minimum<br />

detectable separation of crb@ta at the same<br />

range and the same elevation, expressed in<br />

terms of the horizontal angular dielarrce<br />

LWlween Sush Objesta.<br />

maolutlon In ●levatlorr-The minimum<br />

detestable ~ralierr ef objjs et the same<br />

range d aanm bearfng, espreaaad m terms of<br />

the vertical angular drntanm.<br />

maolutlon in renge-The minimum<br />

detwtabfe separation of objests in the same<br />

line of alght, axpressed in terms d the dietarrsa<br />

between them.<br />

resolutlmr Ihrrlt-fn grevily end meanetic<br />

pro~ing, the aeparetion of two distorting<br />

bodias at hich coma obvious indiiticm, in a<br />

measured quantity. of the preserme of two<br />

se~mte bdeS ceasas to bs visible.<br />

resolutiobl. For raster epplicetimrs,<br />

reaolulion is the number or pisels per unit<br />

distance. 2 (JCS) A maasr.rremant of the<br />

amsllast-detail .whiih c=n.ba diaiirguished by e<br />

sensor syatam under spat’k corrdii”mns. 3.<br />

The minimum dieterrce batween two adjacent<br />

f.3alurss, or the minimum size of a feature,<br />

which San be detested by a remote aarrsory<br />

system. 4. In gravity or megnetis praspding,<br />

the ir’viication in some measured quantity, such<br />

as the vertical somponeni of gravity, of the<br />

presence of two or more cloaa but separate<br />

disturbing bdies.<br />

resolving power target—A teat chart usad<br />

for the evaluation of photograph, oplicel, and<br />

alestroc@cel aystama. The deeign ueuelly<br />

consists of rulad fines, aqueres, or circles varying<br />

in siza according to a spasified gamnetric<br />

pregreeeion.<br />

msolvlng power-A mathematical expression<br />

of dafinitbn in an imaging ayatam, ueuefly<br />

stated as the ,-imum number of finsa per<br />

millimeter that can be seen as separate lines in<br />

the image.<br />

recponder-hr general, an irratrumenf that<br />

irrckates reception d an electric or<br />

elactromagrretic signel. See also tr.snspondor.<br />

I’.8P0nS0r-A radio receiver which receives the<br />

reply from e transponder and produss an<br />

outpul suitable for feeding to e display system.


mstftutlorr-(.fCS) The process of determining<br />

the true @anirr@ric pdtiin of ebjeds whose<br />

imegea appear orr pholographa. [Rastfhrlbn<br />

comacta for distortion reaufting from both tilt and<br />

ralief d~facamant.]<br />

matoratlorr-Tha remvery d one er more<br />

lines or corner poaifbna, or Mh, d a prior<br />

aurve~ the raplacemenf d one or more loaf<br />

caners or clzliiemtad monuments by SFPmved<br />

methods, irrcfuding the substantial ranawal d<br />

one or more menuments, as required for the<br />

pUlpOSO d a auwey.<br />

raauttant ●rror-llre error in any<br />

rnaasumment that is the dfierenoa between the<br />

measured velue arrd rtre true value fors<br />

quenlify. Also called true swror.<br />

MI L-HDBK-850<br />

mtrcrdlractive prlsrn-A prbm correiafing of a<br />

did gfaas damerrf having tlwaa mutually<br />

PW@tiC* rafkhg surfaces and a fourih<br />

surface eMiie to he three r@Wcting surfaces.<br />

A Iiihf beam entering through the obhque<br />

surface is rrrfbofad on each d the three dhar<br />

aurfasea and turned 1W to be retumad abng<br />

the aarne etrpalh whbh it traveled to the<br />

retmdkaathe prism.<br />

retrograde rnotlorr-1. Motbn in an orbii<br />

opposite to the USUSI orblfal direction d celestial<br />

bodks witfdn a @varr aydem. Spacificdly, d a<br />

aateflife, moth in a dhrction -e to the<br />

direction d rotation d the primary. 2. The<br />

afprerrf mot”mn of a pbrrat westward amot’rg<br />

the stare. Alao callad mtrogrermlon. Opposite<br />

of progressive motion.<br />

resurvey-A retrecing on tha ground of the<br />

lines d an earlier survey, in whiah afl points of<br />

the aewfier survey tfW are rsrsoverad are held<br />

fixed and ussd es a control. If Ieo few points of<br />

the earfier survey are rasovered to satisfy the<br />

retrograde vernler~ vernier scale which<br />

has spaces or divbions alightfy brrgar than<br />

t~ of the primary scale. The nurnka on the<br />

vamier scale mn in the ~aite dbection from<br />

lfroaa en ha primary scale.<br />

control raqukements of the resurvey, a new<br />

survey may be made. A resurvey is related rotrogrossion—See mtrogmdo motion.<br />

dkectty to an original aurvay, though several .. -,..


MIL-HDBK-850<br />

rovolutlon-1. The turning cd a body akruf an<br />

exterior pdnf or Sxis. l-ha ~ dmindii<br />

betwaen mvdutkm mxi m4atii is given m the<br />

stetsrmanf Wra Eatih revolves around the Sun,<br />

and rotstes on its ssis.” 2. (mmwying) A turning<br />

of an indrumant or part Of an klStNMSld.<br />

rhomboidal prfam-A prism thet displecee<br />

the esis of the beam of Iiihf only Iefarelly.<br />

rhumb b.arfng-1%.s direction of a rhumb fiie<br />

through fwu terrestrial points, axpessad es<br />

angdsr distance from a reference diracticm If is<br />

ususlly massurad fmm 0° et the referents<br />

dkacf”mn cbckwiaa to 3S0”. Also celled<br />

Mercator boerlng.<br />

rhumb dlr.otiort-sea Meraator diraation.<br />

rhumb Ilno dlstanca-Dtskance alerm a<br />

rhumb line, ususlly exprassad in nsutical miles.<br />

rhurnb llrre-A line on the surface of the Earth<br />

cutting all meridians at Ihe same angle. [A<br />

Ioxcdrome or Ioxcdmmic curve spiraling toward<br />

the poles in e mrrsten! true dkct”mn. Pmelbls<br />

ard maridisns, whiih elm msintairrcxrrrstsm L,<br />

true dhctiona, msy be considered spac”ml 0ssss<br />

of Ihe rhunrb line, A rhumb line is a straight line<br />

on e Mercator projection.] Also csllad<br />

equim’rgular eplral: Ioxodromo:<br />

Ioxodromlc curva; Marcator track.<br />

ridge llno-A grephk representation cd mejer<br />

*I36 u* to gtie more definition to the<br />

Iepographw character of an ares for the<br />

determination of low rdtiiurle rsdar prsdktions.<br />

They are shown onty in areas of rise grediant to<br />

depict those plscae in vhich the elevated terrein<br />

femrs a sufficient background to pwlislly screen<br />

visien at low altitude.<br />

right ascmmion systmn-An equatorial<br />

system d curvilinear celaetLel ceordineles wtrkh<br />

hss the Equator es the prknery ra4ererce ptsna<br />

and the pxypmdwlar hour circle through the<br />

vend aqumox as the samndary refereme<br />

plane. The direction to a bedy is given by ifs<br />

right ascension and declination,<br />

rfght asconslor+l%e angulsr distance<br />

meesurad esafward on the Equator from the<br />

vemrd equines to the hour circle through the<br />

celestial bcdy, frem O to 24 Imura.<br />

right bank—Thet benk of a stream or river on<br />

ths right of he oLrserver when ha ia facing in the<br />

220<br />

duadion of fbw, or dewnstraam.<br />

rlgM ●WO-Ttr@ cdeatisl sphere es &<br />

~,m tO ~ observer at the E@or, tire<br />

celestial balms rqpeer to rise verticality nbove<br />

the herizon.<br />

rfght-mrglo primn-A @ thel turns a baem<br />

d Iiihf through a right engla. It irwarts (turrvs<br />

@e down) or reverts (tuma rigid for left)<br />

mxading to the csier$stii of the piism.<br />

right-roadlng-A descriptive term for cm<br />

imege which, when viawxl through the bese,<br />

reeds the esme es the original, Other terms<br />

sometimes used to identify image dimcfien,<br />

such aa normel madlrrg, natural<br />

readings, etc., are not recommended<br />

bacauca of possible cod- k-l nagalivepcdive<br />

ralationehip.<br />

rlgld tripod ●ngrsver-A scribing instrument<br />

with three @nls of mrrtscl surface, to ~rb<br />

the normal irrbelance of the qeretofs Imrrd<br />

pressure.<br />

ring—(digitel mepp4ng) An edge which is a<br />

memtmr d.e-dtierant closed hep of edges,<br />

risa gradient—A color-ceded omnidirsdional<br />

grsphic representation of those terrain sbpes<br />

which are predicted to be low altitude redsr<br />

significant.<br />

rlae tkna-The timo at wh~h a seteltifa’s<br />

brmdcesf cen be picked up by e auifebfy<br />

equipped cbssrver, as fokan from an elert. Set<br />

lime and time of cfoaosf approach are elso<br />

given. Sss also ●lerts; rlao.<br />

rlsa-1. To cross the visibla horixon while<br />

ascending. 2. (sstelliie suweying) To cmsa the<br />

obaowets herfzon while ascending; demcteble<br />

by bmadcest dela mcahmd.<br />

rltrlng tide-See flood tide.<br />

rlvar cmsslng-(laveling) Carrying a Iirrs of<br />

levels across e atresm or other body of water,<br />

when ne sultsble bridge k aveilsbla and the<br />

width of the Lmdy of weter is gmster than the<br />

maximum ellowsble length of sight for the<br />

leveling, requires a special serias of<br />

cbssrvetions tibh taken mllecridy is known<br />

es a river cmaeing.<br />

rhrerlne nrea—(JCS) An inland or coastal area


I<br />

conwiaing both fsnd and water, characterized<br />

by Iirnifad fsnd tii of Cwnnrun&tion, with<br />

estsmsive wstar surface ars+’or krisrd wsterways<br />

lhsl provide nsh.rrsl mules for surface<br />

trsnsporfsliorr and canrnunicdicms.<br />

road ma~A rnadiurn-or small-scale specisl-<br />

pw q. 9enemlfy *win9 Onfy<br />

planirnatnc detsil, with enqhasis upon the reed<br />

network and retstad data. Its main purposs is to<br />

furnish ptinsnl road information for tacf”al and<br />

administrative troop mevemsnl.<br />

rosd net-(JCS) The system of resds svailsbfe<br />

wilhin 8 psrticu!fsr lcdify or ares.<br />

rorsmer-(JCS) Grids arnstrucfad to rmrnmon<br />

msp aceles used for determination of map<br />

coordinates.<br />

rod correctiorr-(levefing) That correction<br />

which is applied to an cbsewrxl dflerence of<br />

elevation to cor’rsct for the error introduced when<br />

tha Ievaling mds sre nol ectuatty of the length<br />

indiitsd by the graduations.<br />

rod fiord-A smsll cvfindricsl tube of anv<br />

rrwterial,. ckysd at tie berrom and wsigh’wd<br />

with slmt until it flosts in an upright pasitiin with<br />

atxwl 2 to 6 inchss projecting above the wsler<br />

surface. Current velocities era datenninad by<br />

dksct observations,<br />

rod levet-An accassery for use with a leveling<br />

md or a afadia rod to assure a vartical position<br />

of the nsd prior to instrument rssding.<br />

rod surn+eveling) The algebraic total of plus<br />

and minus sights in a given Iavel Iina.<br />

rod—See leveling rod.<br />

rolf-(JCS) 1. The rotation of an aircraft or ship<br />

ekul its longitudinal sxis. 2. In air photography,<br />

the camera rotation sboui the longitudinal<br />

amess ef the aircrsh. Also called tilt. Sea also<br />

tilt snglo.<br />

rommnlzntlon—1. The procsss of r=ording in<br />

mmsn script either the sounds of a language or<br />

the grsphic symbols of s nonrornsn writing<br />

system. 2. An item of a language w+kh has<br />

undergcme this process. See also<br />

tranecrlptlon; tranalltaratlon.<br />

roof prlam-A type of prism in which the<br />

irnsge is reverted by a roof, that is, two swfacas<br />

MI L-HDBK-.95O<br />

221<br />

inclined al 91Y to each other.<br />

root moms aqusm wror-!%s standard<br />

●rror.<br />

roots of rnountaln theory-See Airy<br />

thaory Of lSOtSSy.<br />

rotathrg prism camara-A class of<br />

panoramic camera in whiih a double dove prism<br />

ia rotstad wlite the Isne system remains fusd.<br />

Ttda conf~umtion csn achieve a scan of 180” or<br />

more.<br />

rotating prlsrn-Saa dove prism.<br />

rotational movomen!+photogrammatry)<br />

The systamalic rotation of prejectora or projector<br />

assarnbfiss. Whan spplkd to ths pro@ctor body<br />

within Iha gimbal inner ring, the nsevernant is<br />

about tha z-axis awl is called ewing. Rotation<br />

of the innar ring is sbouf an xaia (s.smndery<br />

sxia) and is csllad x-tilt. Rotalion of the outer<br />

ring is about a y-axis (primrsry sxis) snd is called<br />

y-tilt.<br />

rotation-l. (aslrenomy) A turning of a body<br />

.sboui a- ss&onlainsd, sxis. es-the daily retaticm<br />

of ths Earth. See alsa<br />

route chsrt-1. A chart showing routes<br />

belwaen var”mus places, ususlly with distances<br />

indtcatsd. 2. An aeronautical chati covering the<br />

mute bstween spscitii terrninsla, snd ususlly of<br />

such scale as to include the antire route on a<br />

single chsrl. Also csllad flight chafi.<br />

route map-A msp showing ros& to be<br />

Iollowd and nssby peinfs of military<br />

aignifmnce.<br />

route smrvay-suweys for Iinasr construction<br />

such as rsilrosds, highways, and trsnsmisaion<br />

lines whch include the layout of lines and<br />

grsdss for thsse projects.<br />

row+digiiaf) An ordered collection c4 fwlds in a<br />

date bsse pertaining to an entity or rmrd.<br />

rubber blanket—See offset flthogrephy;<br />

of faat preua.<br />

rubber sheeting—A rsctificstion process wisich<br />

resamples data to trsnsform (stretch or<br />

~mwe=) ii frem one statistical model tO fti<br />

enother model.


ubborbrmd-The abWy to fa the encb of n<br />

he, or aalacted points along a tine, in a @tic<br />

pos~mn arvd then “atretc~ the line between the<br />

fised points 10 establish naw gaomatrb shapes.<br />

run of micrometer—See ●mr of run.<br />

MIL-HDBK-850<br />

run-length codo-A data ccmqxession<br />

method for large fwxnogennus ragiorra of me!er<br />

daia. Data Ls racorded aa tupfee which daaignata<br />

the quantify of a repeating vefue and the value<br />

itaaff. Also known as inn-length ancdng (RLE).<br />

running flx-(JCS) The intersession of two or<br />

rrmre poshii firms, n.d 0b4ainad<br />

aimulfanaousfy, adjusld to a common tima.<br />

running mOan-Ses consocutivo moan.<br />

running-(laveling) A continuous series of<br />

rrwmsurad different- of elevation, rnsds setup<br />

by a setup in one direction abng e aectien of a<br />

line of tsvab, which resufts in a measurement of<br />

the difference of elevation between the banch<br />

marks or other points, either Iernporwy or<br />

pe-ent, at the ends of the section.<br />

. ., . . . ... . .. ... . . ,,-..- W*..X ..—. . . .<br />

run-1. (lithography) The number of<br />

irnpre~ions msde on a press for a given sheet.<br />

2. (micrometer) See error of run. 3. (.ICS)<br />

(aerial photography) That parf of a flight of one<br />

plmtographc reconnaissance aircraft during<br />

which phonographs are taken.<br />

222


24-hour aaldllta-sea synchronous<br />

Slltolllta.<br />

MIL-HDBK-B50<br />

aag corractlon-(taping) The dfierenca<br />

between the effectke length of a tape, or part of<br />

.9 tape, when s~ad oontinuouafy<br />

thmugheuf ife length and when sqrpettad et a<br />

limited number of independent points. -<br />

tapes uauafly are used wfth three or tie points<br />

et ss.pfmt, and hang In curves (cateneriae)<br />

betwean edjjcenf aupperfa. COrr*ion for aeg is<br />

not required wften the method of .sqmrf in use<br />

is the same as was used in the afandediicdiort<br />

of the tape; only the etandercfizalion comedian<br />

ieaPPIiad. Abasstspa MuYIIkb used<br />

su~rted througheuf or with four Pc4nts of<br />

support, as on a reilwey rail. Also Mllsd<br />

catanrwy correction.<br />

aalllng chart-A snrell-acele chart used for<br />

offshore sailing between dktant coastal perk<br />

and for plotting the nevigator% position out of<br />

sight of tend and as he appmechas the meat<br />

. frem the eptm omen. mey sfmw eftshors-=.<br />

soundings and the rrrcxt importanl fights, outer<br />

buoys, end naturel landmarks which are visibte<br />

e! considerable dstancsa.<br />

selling dlrsctlone-A descriptive book for the<br />

use of msrinera, containing detailed informatkrn<br />

c4 maatet waters, hmbor fecifiiies, etc. Alao<br />

cslled coast PIIoU plloL<br />

samplo varlrmca-True varience can only be<br />

cOnWUtd from some aemple. The term<br />

sampfe variance is used when wishing to<br />

rnske reference to e cwrqmlad verience from e<br />

cpecifii aarr@e, as opposed 10 an assumed or<br />

prevbuety edirnetad variance of some parliiuter<br />

cleas et observations or pererneters. In general,<br />

If the aemple verbnce et some class of<br />

observations in a weighted beef square<br />

edjuetrnenf dfiers km gredy from the assumed<br />

varience used for wei~hinn the cbservet”ime. the<br />

edjuatrnenl aheuld be-re~ated with refined<br />

weights besed on the ssmple varienca. see<br />

vtwlancb.<br />

sampla-A set of ebaervations, used to<br />

determine the rrrest probable velue of e<br />

parficuter parameter, anrllor used to asfinrate<br />

the accuracies of the drearvations aruU or<br />

accuracy of the parameter.<br />

s<br />

223<br />

Smrson-Flamstoed map projectlo*S ee<br />

sinusoidal map projection.<br />

saros—llra eofii cycle of about 18 years,<br />

afmeal the same fangth as 223 eynodicd<br />

rnodw. Af the and of asdr same, the Sun,<br />

Mom, and fine of rmrka raturn to approxirrmtely<br />

the same raJetive pdtions and another aerisa<br />

04 Scfiiaea be “n% Cbaaly raaernbling the series<br />

jti cornpl~ J . Sss elao lunar cycle.<br />

Setolllt@ Goophydca Programa-DMA<br />

pmgrems thet provide fcw the operation and<br />

maintenance of fmad turd rrmbile =tefliie<br />

trecking systems and the prcceaeing of dete<br />

frem geedetic aeteltites. The date collected by<br />

ths- stalioms are used In gad profil=, pr=isa<br />

aetelfite ephemerides, geedetic point fmaifione<br />

and relsted products.<br />

satellite geodeey—l%e dkcipline whch<br />

ews ~=yalbm c1 an Eefth S8teIrie I.<br />

estract geodeltc mformetion.<br />

,. . . -,, -- . . . .. . . . . .<br />

satelllt@ survey lrrg-1, (Doppler) The<br />

prwcss of potitoning one or more peints cm the<br />

Esrfh’s surface by cdledng Dof@w shift deta<br />

frem peseas of Navy rravigetion aetelfites. See<br />

elao point posltlonlng; short arc;<br />

tranelocatlon. 2. (NAVSTAR) The position (by<br />

reaecfien) d a point receiving signals from four<br />

aetaliiies of the Gbbel Po*loning System.<br />

sateflito trail-A e!raak fike image of a<br />

eatelfiie receded on e afeller plate by a<br />

photographic time aspesura.<br />

●atalllto trlanguletlon ●tetlons—<br />

Trienguletien stat”bns whose anguler poaitkms<br />

relative to me another are determined by the<br />

aimultanaous obaarvet’bn of en Earth =tellifa<br />

from two or mere of them.<br />

●atellita trfmrgulatlon-The datemtination<br />

of the angular relationships bSttVSSn two or<br />

more atelions by the simultaneous observation<br />

of an Earth astelfiie from these statism.<br />

satelllta-An attendant body, natural or rnanmede,<br />

thet revolves about another bcdy, the<br />

primary. See also actlvs aatelllte;<br />

Communtcatlons satalllte; Earlh<br />

eatolllte; equatorial satellite; geodetic


“-<br />

satsrlllte; lunar satellite; NAVSTAR<br />

Global Podtlonlng Systsm; Navy<br />

Nav@tlon Sat*lllt. Syatam; passlva<br />

●atelllta; polar satelllto; synchronous<br />

8at*lllt9.<br />

ssturabl. rsactor—See flux-gat.<br />

magnatomat.r.<br />

scalar-Any phy~icsl quantity wksa fidd can<br />

k described by a single numerical value at<br />

each point in apace. A scalar quant”~ is<br />

distinguished from a veder quantify by the fact<br />

that a scalar quantity pe asasaas enly<br />

m%@fude, whereas a vactor.quantify<br />

PIXSSSSSS both magnitude and duaction.<br />

scale chacklng-1. The process of<br />

determining the scale of en aerial photograph,<br />

w more correctly, the altitude above sea level<br />

which best fiis the print, 2. (stereecompifation)<br />

The process of determining the scsfe of a<br />

vertical phologmph for points at a specific<br />

elevation and the subsequent measurement of<br />

dirwlien and distance therefrom.<br />

Scafo error-A systematic error in the lengths<br />

@ su~ey.finas *ual&.,prowrt”Dnal to lb<br />

“ ‘“”lengths of the “lines. See alse Instrument<br />

err-or.<br />

MIL-HDBK-850<br />

acafe factor—A muffipfier for reducing a<br />

d~tance obtained from a map by computation<br />

or scaling to the actual distance on the datum of<br />

the map. Afso, in the state coorcfhate systems,<br />

scale factors are sppfied to gaedetia lengths to<br />

obtain grid Lengths, or to grid lengths 10 obtain<br />

gacdelic lengths. Solh are lengths on e sea<br />

Ieval datum. but the mid Iarmths are aff=ted bv<br />

Ihe scale change of ~he me; prbjecfion. -<br />

scale lndlcator~ Iegarilhm’k scale devised<br />

as a rapid end convenient methed of<br />

defemnining the natural ~le of e map from the<br />

dwiskms marked on the grsphk scales, or fmm<br />

the intervals of Isfiiude en a map.<br />

scale of raproductlon-The enlargement or<br />

reduction r8tio of an original to the final copy.<br />

Thfs rstie is exprsssed as a dismetar, percent,<br />

times (X), or a frsctii. Afso called<br />

enlargommtt facto~ roductlon fector;<br />

reproduction ratio. See also contact 8120;<br />

diametar ●nlargement: mnka Ilno;<br />

porcant of ●rtlargamontfroductlon; tlmos<br />

(X) ●nlargamant.<br />

scale-ratio moaalc-lm assembly of<br />

224<br />

photogrspfvic prints bruught to a cemmon<br />

by prejsction printing 10 sde factors otrtaiii%$<br />

fmm map distancas to allow the best FQeeibfe fii<br />

of titigueus photo detail.<br />

acafe-1. (JCS) The ral”m or fradkn between<br />

the distance en a map, charl, or phdograph<br />

and the correng distance on the surface<br />

dthe Sarih.2. Aaeriaa ofrnsrk orgradusfkna<br />

at definite intervals en a measuring davica or<br />

instrument. 3. Meaeuramenf by manna d a<br />

scale, See also compifatfon aoale;<br />

convoralon ●calsi; ●quivalent scale;<br />

graphic aoala; Invar ●cala; model ●oalo;<br />

photographic ●cala; plottlrrg ●cala;<br />

prlnclpfe ●calo; reprecentatlve fraction;<br />

reproduction scale; scallng; x-scale; y.<br />

●cale; z-ecalo.<br />

scaling the model—See acallng, definition<br />

2.<br />

acallng-1. Alteration of the scale In<br />

phetogremmetrfc triangulation to bring the<br />

model into agreement wkh a plot cd herixontsf<br />

corm-al. 2. Fitting e stereoscopic model to a<br />

horizontal arntrel pbt. A step in ake.dute<br />

orientation. Also called scaling the model.<br />

3. Determining the scale of a ptmtogrsph w<br />

graphic, 4. (cariegraphy) Sas catiomotric<br />

ccsllng.<br />

scan Iinoe+uccsssive parallel strips of<br />

c@ursd data from B sensor, ‘such as a mw of a<br />

raster grid. 10 bs printsd on e sirrgls line d a<br />

rsstar display device; or recorded in a single<br />

sweep of lhe mirror of an optical scanner system,<br />

or radar scanning system: er a eingle addressing<br />

of the finsar army detector of a puehbroom<br />

scanner.<br />

scan poaltional diatortlon-in a psnoremic<br />

camera system, the dkplacement ef images of<br />

ground points fmm their expected cylindrical<br />

positions caused by the forwmd motion of the<br />

vahicle as the fans scans.<br />

acannar-1. A device for automatioalfy<br />

converting images from maps and photographs,<br />

or fmrn IMrI of the reel worfd into digital form. 2.<br />

Any device that aysternat”mlly decompoaaa a<br />

wnaad image or scene into pixels and then<br />

records some attribute of each pixel.<br />

ocatteromotry—A method of using radar to<br />

measure the variation of radar aceftarfng<br />

coefficients. These variatbna may be used by<br />

geoscientists to discriminate between surfaces


I<br />

~<br />

.-.<br />

with differeti roughness and ~t~fa. ‘II-W<br />

acafferomeler la distinguished fmrn other radars<br />

by its ebifhy to measure arr@fuda.<br />

MIL-HDBK4350<br />

●corto gensratlon-A two-dimanaionel<br />

dispfsy with undarfaying tenain data pwlreyad to<br />

appear ae if three-dimemsionaf. Normally, en<br />

image c.mafsts of an cbfiiua view wffh<br />

perapacfive.<br />

●cenei matching area cormlator<br />

(SMAC)-An elacfrooptical correlation ayslem<br />

whwh uses photogmphii rsrterence material<br />

mStChSd with OllbOSrd raaffirna scenes to<br />

echteve ccmelation. The reference scene is<br />

prepared from ramrmaiasance photegrapha and<br />

is stored In the form d a photogrsphc<br />

trans~rancy. The reference is ptscad eruund<br />

the inner circumference of a drum that retatas at<br />

e high engulsr vefcdy. The reference then<br />

forms e continuous strip which modulates or<br />

cheps the projactad image being fccused on if<br />

by the optical system. The reaffime energy from<br />

the ground within the fiafd-ef-view is spetisl~<br />

modulabd by the trsnsmksivify ef the reference<br />

transparency.<br />

. .Schaimpflug ,,sondition.-The requirement<br />

thet object, lens. and image p!arres intersecI in<br />

a common line for sharp fetus in eny dkecl<br />

projection system.<br />

@chema-The description of the logical<br />

afrucfure of en entire data base acwrdhg to a<br />

conceptual model.<br />

Schott baae-llne measuring epparetua—<br />

A contecf, compensating base-line measuring<br />

apparatus mrrrpmed of three psrsllal bars; the<br />

middle bar of zinc, the outer bars of steal. One<br />

and of each steel bar is free; the ohm end is<br />

fastened to en end of the zinc bar, a different<br />

end for each steel bar. The lengths of the bars<br />

are so p~rtionad wilfr respect to their<br />

coeffiiiarrts of thermal expansion that e<br />

cerrsterrf d!atance is maintained between the<br />

free ends of the sled bars.<br />

sclntlllatlon—See srhlmmer.<br />

sclasora lnveraOr—See PeaucelllOr<br />

Inveraor.<br />

acroan angle-(photogmphy) The angle<br />

which the rowa of halftone dots make with the<br />

verticel when right-reading. The engle is<br />

measured clockwise whh O“ a! 12 o’cfock.<br />

-.<br />

Z25<br />

●croon fng—See madrfng.<br />

. . . .<br />

scr*On-See4 ●raa pattern semen;<br />

blangle ●crean; dot ecmwr; halftone<br />

●craen; magenta contact screen.<br />

scribed pleta-see scribed sheet.<br />

ecrlbad sheet-A scribing aurfeca on whnh<br />

the raproddion scribing has bean cempfeted.<br />

Atae called scrlbad plate.<br />

acrlber—An instrument hefdirrg a acribhg<br />

point; used for scriling en coated plastics. Alse<br />

called ●ngraveq gravec scrlblng<br />

Instrument. See alas sngratmr<br />

rectagraver; rlgld tripod ●ngrava~<br />

ctrnight Ihre gmver; subdlvldor; ●wlvol<br />

graver; turret graver.<br />

sicriblng gulda-See guide.<br />

scrlblng krstrumorrt-See scriber.<br />

scribing points-Needles or btsdes in various<br />

dmmelem or cress-saction shapes ground ❑nd<br />

sharpened 10 prescribed dimensions. Used in<br />

scribers for scribing on add plastics.<br />

scribing—(JCS) A method of preparing a msp<br />

or charl by cutting the tines into e prepered<br />

mating. ~he pmcesa of preparing a negative<br />

Aich can be rs+woduced by contact expesure.<br />

Portions of e photographically opaque coating<br />

ere removed from a transparent base with<br />

spacielly designed tools.] Also called nsgatlve<br />

scrlblng.<br />

aee level contour-A contour fine delineating<br />

peirrts at sea ievel.<br />

ssa Ievsl datum of 192 S-See Nationel<br />

Goodatlc VerZlcal cfatum of 1929.<br />

sam Ievsf dstum—See msan sea Iaval.<br />

sea lmrsl variation-sea level variea from<br />

day to day, from month to month, end from yesr<br />

to year. This verieIicm is aftrfbulad 10<br />

meteorological renditions end ahoufd not be<br />

mnfuaad with the lunar fiiea.<br />

ses lsvsl—The height of the surface of the<br />

sea at any time. Sss also Ideaf sea Iaval;<br />

mean aaa hfbl.


soamloss data baaa-A data base<br />

afrtmned wifhotd tmgmarrtaticn or tiliig,<br />

thereby afiminatirtg the need to begin and<br />

tmntinafe chains ❑t boundaries and have<br />

topclogiil peintera mferanoa fiksa as well as<br />

cdhw entities.. The mad ia a data baas<br />

phyaicatty smsllw than a Wed one but one in<br />

whiih aaarch times can be quite brig.<br />

MIL-HDBK-850<br />

search ●rd raacuo chari-A chart designed<br />

primarffy for dirding and conducting search and<br />

rescue operations.<br />

ascent conic chart-See cordc chart with<br />

two standard parallels,<br />

aacant conic map projection—See conic<br />

maP PrO@tiOn with two standard<br />

I parailels.<br />

secant tndhod-A method of determining<br />

lhs psrsllel of fatttude for the survey of e bate<br />

fine or standard parallel by offsets from e graatcircie<br />

line which cuts the psrallal at the first and<br />

fifth mile corners of the township beundary. See<br />

also secant.<br />

. . . . . . . . .<br />

secant-t. A fiia that cuts a geometric cuwa<br />

or surfece at two or rrwre points. 2. A<br />

trigonometric function of an angie. See also<br />

secent mathod.<br />

sec@Or-See templet cutter.<br />

second-order bench mark—A bench mark<br />

camacfad to the datum (uaualiy mean sea<br />

Ieval) by continuous cacond-cwder Iavefing or by<br />

a cuntinuoue combhation of first-end eacondorder<br />

leveling.<br />

second-order leveling—Spirit Ievefing which<br />

does no! attain the quafily of fircf-ordar leveling<br />

but does conform to the current spacifiiation for<br />

second-order (cfass I or clssa 11)leveling per<br />

“Clasaifiition Standmds of Accuracy end<br />

General Specifications of Geodetic Control<br />

Surveys.” Recommended for denaifiition of<br />

the National Network end for Ioceliiad cruatal<br />

nmvemant and engineering pmjacfs.<br />

●aoond-order travers*A survey Imveraa<br />

which exfands between adjusted poatilona of<br />

fhs first.cmler or aamnd-odar control surveys<br />

and which conforms to the current spacifiiliona<br />

for aaoond-crrdar (class I or cfsss 11)traverse par<br />

“Classification Standards of Accuracy and<br />

General spacifi~fiis of Geodetic Control<br />

226<br />

Suwaya.” Racmnrnandad for darrs+fkatkrn of the<br />

Natienal Netwoti and metropolitan area wrvaya.<br />

sacond~rder triangulation-Sacond-order<br />

trkangulafiort was at one time known as<br />

●acondary triangulation; changed in 1921<br />

to prlnrary trfangulatlorr, and in 122510<br />

socond+rder trlmtgulatlon. Thaas surveys<br />

mnfomr to the currmt apac&atkons for aascnd-<br />

Older (C18aa I or Cfaaa 11)triang@aWl par<br />

“Cksikation Standards d Acwresy and<br />

General Spacif&licna ot Geodetic @ntml<br />

Surveys.” Racomrnerrdad for dansifiiion cd the<br />

National Network and mafrcpofifan area surveys.<br />

second-order work—lhe designation given<br />

any wrvey work of naxf-to-tha-highaat order ol<br />

accuracy and preciakm.<br />

secondery clrcla-See s-condery great<br />

circle.<br />

secondary compilation—A spacialiy<br />

pmpamd matte plastic rneterial used to dqicf<br />

umxmactad or diesrete coutitngs in balhyrrwtric<br />

compilation.<br />

sacondery control point (SCP)-A peint<br />

pldogmph~al)y identifiable, poaitiincd to a<br />

high degree of accuracy using an averege of<br />

6sveral shiran horiionlally mntrollad<br />

phonographs. Seven to thirteen mntrollad<br />

photographs, each remaining the point, ere<br />

taken ovar each of tour quadridirsdional paaaaa<br />

intersecting parperdiiularfy over fhe point.<br />

Photogrammetric measurements are used to<br />

determine the position of the point by relating if<br />

to the ahiran positional nadir point on each<br />

photogmph. Thaae posilions are mathernstisalfy<br />

averaged 10 obtain the most probatrfa<br />

cootdhatas for the point.<br />

seconde~ great clrcla-A great circle<br />

WfW@Cukr to a Pri~ry great cimle such as a<br />

meridian other than Ihe prima meridian. Also<br />

called secondery; secondary circle.<br />

aeconda~ grid-Any grid, other than the<br />

primary grid, required for combined opamtions<br />

application. Ttck marks along the neat fines are<br />

Iha preferred method of portrayal. Such grids<br />

sheuld remain on the maps or charts so long as<br />

ha aacondary grid remains in use.<br />

1~econdery<br />

ctatlon-An additional<br />

1:tiangulstion<br />

rdation, uwalty marked and<br />

identified,<br />

established to strengthen horizontal<br />

1nap<br />

conlrol, Secondary statiens are connected


I<br />

MIL-HDBK-850<br />

to the main schema stations but am not<br />

cxmsiderad au being part of the rrmin-sshama<br />

Mt.l-hay kradfan uwsffw piding rnaarm for<br />

cJlacbandtor ~ ~.<br />

auxxrdary tkk atatton-A tide station whii<br />

is opendad fa a short perkd of time 10 obdn<br />

data for a *i purpose.<br />

sasondary-1. See aecondmy grant<br />

Gird.. 2. A cakstiil body revokhg mound<br />

another body, its primary.<br />

SECORA phaaa~mqwiaon efacfronis fongrsnge<br />

dmanca-msaauring system used to<br />

determine podiirra end OlbitS & SIXtefkke or<br />

flight vehklea thnt contain the necasaa~<br />

transponders. This term is an esronym for<br />

“sequential collation of renge” (now obsofste).<br />

section eorner~ somer at ths exlrsmify of a<br />

section boundary,<br />

sectlonrd charf-A series of eeronaufissl<br />

chsris et e 1:5@3,000 scale severing W entire<br />

United Sletes, suitable for wntasf or visual<br />

flying.<br />

, . ... . . ... ....“. ---- . ... . -. ,,<br />

aaction-1. The unfr of aubdwision of a<br />

townshp wiih tmmderies sonferming to the<br />

mcfanoilar svetem of survevs. nominslM 1 mifs<br />

squsre~-coni~iiig 640 acr&’s.”See also’<br />

fractional ●octlon. 2. (leveling) That portion<br />

ofaline ofkvals vhiihisracwdad and<br />

abstraciad as a unit. Sae afae fractional<br />

sactlon; half cactlon; quarter section.<br />

mctorkl harmonke-l%e set of spherical<br />

hermenisa wttich change fmm poaitiie to<br />

negatiie es a furrdion of kngifuds only. Sas<br />

alae teassral harmonics; zcmal<br />

harmonics.<br />

secular abarratlon-The aberralbn due to<br />

the motien et the oentar of mesa of the solar<br />

svsfem in smace. Also celled aberration of<br />

ffxod strwa.<br />

secular perturbations-Perf urbatiorrs to the<br />

orbii of a pfanet W seleltiie that continue !0 act<br />

in one dkasfion wifheuf limit, in crmtrast to<br />

pariodc parturtmtimts whish cfwmgs diresfbn in<br />

e regular msnner.<br />

secular tarrrm-in tha mathematical<br />

expreaakm of an orbii, terms which ara<br />

pr’OPOIt”wal to lima, rssuffing in secular<br />

penurbaliens.<br />

227<br />

satactlon overf*y-A trasing of aalactad nmp<br />

Muca *II Oorr@ad on lmrrs+mnf rrmtariel;<br />

USW#Y d=- by the name d the Ieekuas or<br />

ddaie depicted, such ●s contour ovartsy,<br />

W#@#Wt SW9ffJXY.Alra cslbd tifi pUli Up;<br />

●elonocontrlc coordinator-Oussntitias<br />

Mich expmaa the posifbn ef a print with<br />

raepacttothacarrferoftha Meon.<br />

●elerrocantrlc-Rafating to tha canter d the<br />

~ referring to the Meon es a canter. A1.aO<br />

sallsd Iunlcentrk.<br />

●olenodoey-@CS) Thet bmnch of appfkd<br />

mathamatiss vhkh detarmhwe, by cbeervatien<br />

and maaeuremant, the exact padons ef points<br />

and the figurss and areas of large pertions of<br />

the Man’s surfece, or !he ehapa and size of<br />

the Moon,<br />

aelanodetlc-(JCS) Of or pmlsining to, or<br />

determined by, aelenodeey.<br />

selanographic—1. Relating to the physical<br />

geography ef tha Moon. 2. Spacifiilty,<br />

referring to pasitions on ths Mom measured in<br />

latitude horn the Mmn’s aquetor erxl in<br />

bngifude from a refareme meridkm.<br />

selano logy—That branch of astronomy that<br />

desk with the Moon, ifs megnifufe, rnofkm,<br />

consfifuficm, and the Iika.<br />

solenotrope-A devise used in geodetic<br />

surveying for reffscfing the Mcar’s mys to a<br />

d~ant point, 10 aid in bng-diefsnsa<br />

ebsarvations. Sea also heliotrope.<br />

salf-lavellng fevd-A Ieval ufifiiing the actiin<br />

of gravity in ifs operation. A prismatic cfrwiie,<br />

called a companaator, is an integral part of<br />

the instrument whd, ora tha imdmrrrd I’we<br />

been roughfy leveled, causes the optical eyefem<br />

to ewing into proper herizontel fine d sight and<br />

to msinfain that psifion during readings at a<br />

given statien.<br />

saff-raadlng Iavallng rod-A rod with<br />

greduefien marks designed fo be mad by the<br />

ebsarvar el the Iavaiing instrument. Also sailed<br />

speaking rod.<br />

●elf-mgktarlng gag*Any tide or stream<br />

gsge which providas a continuous record of the<br />

,,


1<br />

MIL-HDBK-850<br />

variatkm d ii or stream level with the passage<br />

of time and whii will cparate, w@WnrMd, for a<br />

nu~ of days. Abo sailed ●utomatic gag..<br />

somlarralytleal trlmgulatlo~The<br />

maaeurerrmrd of x-, y-, ad &modal coordirsatas<br />

on an ansbg inelrumant and the trensfomrat’bn<br />

from rrralal cwxdinstsa to grid coordinates by a<br />

cwrqmtat bnaf pIDCOdUm.<br />

cemlcontrollad moaalc+JCS) A mosaic<br />

cotrpxd of corrected or uncorrected prints laid<br />

so that major ground features match thair<br />

9~~h~l coor’dimtas. Sss al.ua controlled<br />

mosaic; moealc: uncontrolled moaalc.<br />

●omldlamoter eorractlorr-A mmsdien due<br />

to eemldiamater, psrticufarty that sextant affiiuda<br />

cerredim recutting from dmcwvatbn of the<br />

Wpr w bwer limb of a catastial body, rsthar<br />

than the center of that fmdy.<br />

semldlameter—1. The radius of a closed<br />

figure. 2. HsH the angle at the observer<br />

subtended by the visible diatr 01 a celestial bdy.<br />

semldlurnal constituent-A lidsl constituent<br />

that has Iwo rrraxirmmrs and Ivm. minimums<br />

each constituent day.<br />

eemldlurnaf-Having e psrbd of, eceuning in,<br />

or related to apprcrximatefy hsff e day.<br />

●emlmajor axl-1. Ona-haff the longest<br />

dwmetar of en allipse. Also cellsd moan<br />

dlstanca. 2. (geodesy) Equatorial axis of e<br />

ephareid w elfipeeid.<br />

semlmlnor axla-ona-hslf the shoneef<br />

d~melar of an effipsa.<br />

sormlblllty-(spirit level) Sss senaltlvlty.<br />

aarrelblo horlxorr-Thst circle of the caJeSial<br />

sphere formed by the intersectbn of the<br />

celsstiel sp+tere and a plane through any point,<br />

such es the eye of an observer: and<br />

Parpandiiuler to the zanith-nsdu tine.<br />

aensltlvo trltimoter-See baromatrlc<br />

●ltlmotsr.<br />

aarreitivlty-(sphif lavafJ The aocurtwy and<br />

precision which a spirit level is capable of<br />

producing. Ssneitfvii depends on Ihe radius of<br />

curvature of Its Iongltudlnel eactiin; the longer<br />

the mdius, the more eensillve the level.<br />

228<br />

.Saneitiwify is mtsd by qding the hear fan@h<br />

of a dwbion between gmduatkm MSrIW on the<br />

fswel tti and ifs arrgufar value at rho oanter of<br />

curvature of the t~. A&a died aanalblllty.<br />

●enaltomotrlc curve-sea charactoristlc<br />

curve.<br />

●ermltometry-llre rnaasurernant of the<br />

mePMSS of a Pfmt=mnaifiwe nratarial to Ihe<br />

acticn of fight.<br />

sensor Image Simulator (SIS)-A DMA<br />

system buiff by Goodyear (now Lord) 10 mimic<br />

sirndstors which use DFAD and DTED. S1S<br />

~g= DFAfJ end DTEO and assigns molar<br />

mffedivii. Aboueed byoMAaasnadii<br />

station.<br />

SenSO~ =lmUlatiOn SyfNe~A device, such<br />

as naVlgCitIOnsimulator or trainer, in ~h<br />

spscifii types of sensor simulator msterials are<br />

utiliisd for tmining purpesss. See also ssnaor<br />

simulator materials.<br />

aerruor simulator materlal~Those terrain<br />

models or maps, factored tmnsparencies or<br />

rsdsr reflectivii plates dcrvekrpsd or pmducsd --, . . ~<br />

from mapping, cherthg, geodetic, snrYor<br />

intelligence dala or compilstiorrs for use in<br />

waspn system or navigat ien simulators or<br />

trsinem,<br />

sa’mor—A technical rncwms 10 esterd man’s<br />

natural aen.ses. Also a sensing davica er<br />

equipment whiih dalacts and records in the<br />

form of imagery, lhe energy reflected or emitted<br />

by envirerrmsnfel areas, features, objects, end<br />

events, irduding natural and cultural features<br />

rind phys’kaf phanernans, as well as rran-mada<br />

features, ebjecfs and adivities. The energy may<br />

be nuciear, eledromsgnetic, including the visibls<br />

and invisible portions of the apadmm, chemical,<br />

bielegical, thermal, or mschanicel, including<br />

sourd, Meet, end Earth vibmtim.<br />

September equlrrox-See ●utumnal<br />

equinox.<br />

aequentlal data atructura-A vector date<br />

structure in wh~h each tsature in a vector data<br />

eat as a point, line, or pofygm, with ire<br />

coordinates and attributes all in fhe same<br />

raaord. No spatial ralationshipe are establiehad<br />

between features. Also cailsd apaghattl<br />

vector.<br />

series designation—A descriptive titla, a<br />

.-


I ., .,-.,.<br />

nudrer, w a codrination d a letter ard<br />

rrutir, used irrdMduefty m cdlesiiveiy to<br />

tirrt&y a g-or farrity d ~, dwts, or<br />

related pubhceticma.<br />

serlos speclflcatlorrs-S e e<br />

specifications.<br />

SOrl@a—Saa coordhrated ssrlea; map<br />

●orIs*.<br />

sot forward-see setup.<br />

setback—The horixontel dietense fmm the<br />

fducisl mark on the front end of a taps er psri<br />

of tape, Wrfch fa In use at the time, bsck to the<br />

point on the greund mark er monument to which<br />

the particular msasure is behg mede.<br />

satu~l. The instrument (trnnsif or level)<br />

pfeced in position and fevebd, ready for taking<br />

messuremsnt~ er a point tire an instrument<br />

ie 10 be or hes been pkrcad, Atso called<br />

Irmtrumont stetlon. 2. In base-line<br />

measunsmen!s, the horizontal dstance fmm the<br />

fiiucisl mark on !ha fmnf end of e t+ or psrt<br />

d tap which is in uee at the time, measured in<br />

,-. ,., R for-wad dk~ton to the pint on the ground<br />

nwlrk or rnonumeti 10 Whti the particular<br />

maasure is behg made, Alee celled set<br />

forward.<br />

eat—l. The diractkm toward which the current<br />

ffows. Usually )ndicated in degrees trua or points<br />

of lhe cornpees. 2. A finite or itimite numbar of<br />

objects of any kind, of entities, or of soncepts,<br />

that have s given properly er properties in<br />

somrnon. 3. (surveying) A apesifiad number of<br />

Obeervatiorm, es of eatmrromic azimuth,<br />

astmrromic longitude.<br />

sexagoalmaf ●yetorn-A ayslem et noletion<br />

~ increments of 60 as the dwision of Ihe circts<br />

mto S60 degrees, esch degree into 60 minutes,<br />

and each mimde into 60 seconds.<br />

BOXtDnt altltude-llre aflitude of a celeafiel<br />

body sa indiited by a sextsnt or e eimilsr<br />

instrument bafore cermstiena ere applied.<br />

saatant chart-A chart with curves enabling a<br />

graph~l solution of the three-pokrt problem<br />

rather then using a three-arm protractor.<br />

88xt8nt-A doubfe-reflesfing htatrument fer<br />

measuring angles, prfmsrify aMfudes of celestial<br />

Htes. Aa originally used, the term applied only<br />

to ir-dwments havrng an arc of 60” (m-d a<br />

MIL-HDBK-B50<br />

229<br />

~We of120”),fmfn which the i~trument<br />

derived its name. In modem prectica the term<br />

apfrks to eimilsr kwtmnante, mgan2m3a of<br />

mnge. ALSOSS[bsd hydmgrapftii 66mstn. s6s<br />

stao bubbfs sextant: marine sextant;<br />

octant; quadrant; qulntant; surv.ylng<br />

●sxtmtt.<br />

shade .rror-That error of an optical<br />

instrument dun to rs4rac4ion m the shade<br />

gfeeaes.<br />

●hadad mllaf-(JCS) A cartogrsphii<br />

technkqua that provides an apparent three.<br />

dm neienel oonfigumtion d the terrain on meps<br />

and cfmrta by the use of graded ahadowa that<br />

weuld be cast by high ground U fiiht were<br />

ahhing from the northwest. Shaded retiet ia<br />

uaudly used in somkdnatiorr wiih ccmtours. See<br />

also hill ahadlng.<br />

shaded-relief map-A mep err whish<br />

hypacgraphy is made 10 appear threedimansional<br />

by the use et graded ehsdow<br />

effects. Generally. the fasturss are shadad as<br />

though illuminated fmm the rrerthweet, A<br />

sheded-relisf rrwp may also contain senloura or<br />

hechures in cornbinatbn with the aharhg.<br />

ehsdow fnctor-(JCS) A muffipltilicm factor<br />

derived fmm the Sun’s declination, the Islitude<br />

of the target, and the time of photography, used<br />

in determining the heights of objects from<br />

shadow tength. Also called tan ●lt.<br />

ahedow projector-An optisel devica<br />

devaloped for checking dimensional ascuracy of<br />

the various casts ef refiif models.<br />

sheer—Trensformet ion of e rectangle in!o a<br />

parallelogram.<br />

sheet. Ilnee--see neatflnea.<br />

ehea4-A singfe map, either e comptete mep in<br />

one sheet, or bebnging 10 a series.<br />

ehlft— (.ICS) (redsr) The abihty to move the<br />

origin of e radal d~fay ewsy fmm the center of<br />

the cathode-ray tube.<br />

●hlmmer—An atrrmapherie effecf due to<br />

etrnospherk turbulences. If may be mere crilisel<br />

h photograph observations of celeatiel objesfe<br />

Ihen refraction. The cdimmar mskee the imege<br />

flusfuate rapidly. ff everagee out in the case d<br />

bng exposures but is serious in case d fleshes.<br />

Shimmer affesls both right e=enaion end


I<br />

ddinetti in a random manner m-d, unfike<br />

m9UbW tict”~, “B lmf ZIHO at ha zenith. Ako<br />

called aclntlllatlon.<br />

ship.towhor. triangulation—A method of<br />

triangulation invotving simuftanaous<br />

ebservatkma from three shore etafiirw on a<br />

target csrrid by a shii offshore d the middle<br />

station. The mktdla stsfii must be vkibfe from<br />

aach of the two ad Sfatons.<br />

Ships Inartlal Navigation System<br />

(SINS)-A precise dasd-reckoning system<br />

tvhiih rmirrfains ships’ position and heading<br />

thrcrugh maasursments” made with gyroscopes<br />

and eccalerornatem.<br />

shlran-An efactrenic dtstancs-messunng<br />

SyStSm for rrraasuri~ d@fmces with @OdatiC<br />

accuracy fmm an airborne station to each of<br />

tour ground stations. ~hia term is en acronym<br />

for “S-band high precision short-range elscfronti<br />

navigation. “]<br />

shoot—1. (trsfronomy: eurveying) To meke en<br />

observelbn wkh an instrument. 2.<br />

(photography) A slang term ussd to denota<br />

photographing copy, such as a map msnuscripl,<br />

with a copy camera.<br />

shop calibration—Adjustments 10 precision<br />

instruments made in an instrument<br />

msintensrrce shop having e limited amount of<br />

specialized testing equipment.<br />

ahoran range-The mazimum possible<br />

operating distance between shc.rsn eircreff and<br />

ground stations as limited by flying height,<br />

ground-station elevation, terrain, erd Earth<br />

curvat urn.<br />

shoran r.ductlon—The computation process<br />

of converting from a shorandiatance reading to<br />

an aquivalant geodetic dstarwe.<br />

●horan trltataratlorr-A mathod of extending<br />

hortzorttal control in whiih the sides of<br />

appropriate figures are measured by the shoran-<br />

Iine cmsaing methcd.<br />

●horwr-controlled photography—A<br />

methd by which the positions of aimraft are<br />

determined ~ distance measurements to two<br />

ahoran ground afatbns aimutteneously with<br />

photographic exposures.<br />

MIL-HDBK-850<br />

s..<br />

z do<br />

●horan-llno crosdng-A metfwd crt<br />

daterrnining distance Lmhvaen two pims by<br />

ftyiig across the adjjlng line.<br />

shoran-wavsr pattt-Tha path taken by tha<br />

ahcvan wave as it travata fmm the mobile<br />

(airborne m shi@ome) ststkrr to the ground<br />

station.<br />

shormr+JCS) A precise chart-rsnge efecfmnic<br />

rrsvigst’on system whkh uses the tima d lravsl<br />

of pulsdyps transmissions fmm fwe or rrmre<br />

fbred stslicm to measure rdent-rengs distance<br />

fmm the stations. Also, in conjunction with a<br />

suitable ccwrpufer, UA in precision ~@f.<br />

~ term is an aorwrym for the phrase %hortrange<br />

navigation.-]<br />

shoreline of focl—See coastal refraction.<br />

short ●rc geodetic adjustment (SAGA)-<br />

Ths Iassl squares adjustment for position,<br />

elevation, azimuth, and distance of a number of<br />

stations using Doppler sateltite obsarvelicns of<br />

the earns passes. The satellite posificms are<br />

permitted to vary. Only pcrlkms of sstefliie arcs<br />

me obsarwd. Paints afong thase short arcs are,<br />

mmpulad for the times of the cbaarvstions as<br />

an intermdtala step towards deriving the<br />

station posiiions. See also point positioning;<br />

short arc; short arc network.<br />

short am nofwork-A network of peeitions<br />

established by adjustment of simultaneous<br />

satellite chservatiorrs.<br />

short am reduction mathod-A<br />

computational procedure in which only shorl<br />

arcs of tha sstellife orbit are employad in order<br />

to minimize the Izffacts of secular and long<br />

period perfurbatirms.<br />

shorl ●e-A small pmfion (usually lass then<br />

hatf) of the orbiial em traversed by a salelliie in<br />

making 1 revolution aboul the Earih.<br />

ehm’t distance navigational aide-(JCS)<br />

An equipment or system which provides<br />

navigational assistance to a rsnge not<br />

exceacfhg 200 stalute milss/320 kilometers.<br />

$hort parlod parfurtsatlona-Periodic<br />

psrfurbsticms in the ofii of s ptsnet or sstellita<br />

which exacute one complete periodii varistian in<br />

Ihe time of one orbiiel period or leas.


I<br />

dtort rod-A Javel md, U6ussfiya Phkdelphii<br />

md, pemriffing rrndings of 7 feet or Jam. See<br />

also long rod.<br />

MIL-HDBK-a50<br />

dde can eoner-A system utifiiing sonar<br />

fmnedumm mounted rrearfy horJzOntaffy and<br />

pa-i to the line of travel, to pmtray<br />

Lmffom feetume fo the side c4 Ifsa survey vew4sl.<br />

dde oquatlon tests-skfe equst’km tests ere<br />

a mdfiition of fi”de eqrsat’kme which are<br />

helpful to gsodetis field parfias in ctsaakirrg the<br />

arxumcy d &ssrrvatkme snd h Jeseting the<br />

fminfs where horizontef-diredion ohservatioms<br />

may be in ernw.<br />

●ldo aquatlon-A cendiiion equafkm which<br />

expr~aas the lekilbnSKfp bahveen lhe various<br />

sides m e Itianguistion rigura as they can be<br />

derived by csxnpidation from ona another.<br />

●ldo llna-Apphed to a strip d land sr.roh ae a<br />

street or rigfrf-d.way, it defines the brndaries<br />

of that strip: ncl applied to the ends of s strip.<br />

rrldo overtsp-Also called side lap. See<br />

I-..<br />

. . overlap, dafinllion 1:<br />

. .<br />

I aide shot-A rsrsding or measurement from a<br />

survsy ststbn to locate a point whti is not<br />

I inlendad to be used es e bees for ths axtension<br />

of the survey. A side shot is usually made for<br />

the purpose of determining the fmsition of some<br />

o@acf wldcfr is to be ehown on the mep.<br />

●ldo test—in trienguistion of e quadrilateral or<br />

similar figure. where distances san be cmrrputad<br />

fvm dflfemnf ways, the ratio of the diffarensa<br />

between the two aom@ed results to the length<br />

of the Jine.<br />

aJd@-lookJng alrborno radar (SLAR)—<br />

(JCS) An airborne radar, viewing et ngM angks<br />

to the axis of tha vehlcla, which pmdffias a<br />

prsaentation of terrain or rmving targets.<br />

●lda-alght-A sight rnsde with the transit to a<br />

pdnf not on the line of traverse. It may be a<br />

dde shot or an obsarvetion 10 locate an in-andoul<br />

station. an sximulh msrk. or an intersected<br />

point.<br />

sldcmaf day—The interval of lime from a<br />

Uerreft & the (tnse) vamel equinox across the<br />

uppar March of a glvan meridiin to ifs next<br />

succeeshre transit across tha upper branch of<br />

231<br />

- ..-<br />

the cams merid!an. Afso asllsd ●qulnootJal<br />

day.<br />

aJdamaJ tocua-Tha posiliin of the pnnc”~l<br />

fad plane of a Iena eysfam. A crmtam or<br />

teleac+s is m aidersrsl fcsaa wtrerr incidem rays<br />

Jmmagmdd iebsncac ometoafocua intfm<br />

plane d tha phofogrrs@ plate or of the r@icle.<br />

Afeo cdad solar tooue.<br />

●Jdaraal hour ●ngla (SHA)-Angular<br />

distance west d the vensef equinox the arc d<br />

tha celeatii equelor. or tha engle al the<br />

aelaetisl pole. between the hour arda d the<br />

vernal equinox and the hour circle of a pdnt on<br />

the oalerrtisl sphere, measured weetwerd fmm<br />

the hour cfrde d tha vernal squimx through<br />

360”.<br />

aldema.1 month—The interval of time<br />

batwaan two succasstie peeasges of the Mmn<br />

past e Iuad star.<br />

ddeteal parlo+l. The time taken by a<br />

planet or sstellffe to aOrr@ete one revolution<br />

about its prirnery and as referrsd to e freed star.<br />

2. +cifkalfy, Ihe interval between rwo<br />

sumesswe returns c4 an Earth satellite in orbit to w . -+<br />

the ssme gemealric right escensk<br />

aldoreal time-llma based upon ths rolelkm<br />

of the Eerth relative to the vernal aquimx.<br />

ddereel year-llse perid of one apparent<br />

revolution of the Earth around the Sun, with<br />

rcspacf to the lied stare, wiih an accepted<br />

valua of =5 days. 6 hours, 9 minutes, 9.5<br />

semnds in 1900; and increasing al the rate of<br />

O.OCQ1 second annusliy.<br />

●idereel-Of w pertaining 10 the etars.<br />

Although sidereal genemlfy refers lo the. stars<br />

arxf tmpiml to the vernal equinox, sidereal time<br />

and the sidereal day are based upon the<br />

position of the vend equinox relatiie to the<br />

meridian.<br />

aJght lnmp-A sorrpaci, portable, bettary -<br />

epareted electric lamp rssradaa a target for<br />

observations on surveys of high prsaklon<br />

(ususlty on first- and semnd-ordsr geodetic<br />

triangulation). The parabdii reflector is mounted<br />

in a special was to fadifate poirrting and<br />

adjuating.<br />

dght flna-see Ilno of collirnatlon.<br />

sight mductlon tablee-Tablas for


MIL-HDBK-850<br />

performing sight reductions, psrticufsrfythoee for<br />

determining computed atfiiude for comparison<br />

with tha obsetved altitude of a cefastisl body to<br />

d~errrine the attiiude diierenca for estaMtimg<br />

e fine of poaitbn.<br />

sight reductlo~?’he pnxaaa of deriving<br />

tmm cbaervation d a caleslisi bdy the<br />

information naedad for aefsbkshing a fine d<br />

positiin.<br />

sight rod-See rang. rod.<br />

sight trae-See line tma.<br />

slght~ssrvatlon of the altitude, end<br />

semetimes efao the azimuth, d a celaefisl bedy<br />

fer a fine of position; or the data obtainad by<br />

such observati.m.<br />

slgnatura-lhe characferiefix or psfterns of<br />

phys”kal features that permit objects to be<br />

recognized on aerial imagery. A ceIegory is said<br />

to have a siansture onkv il the cherscferistic<br />

pattern is hi~hly repr~ntative of all units of that<br />

category.<br />

slgnlflcanl data-llw date that represents -<br />

the best eppmxirnattin of the date of the<br />

product’s informs!ion; e.g., the date of<br />

Cmnpifstii or the date of the source msterials<br />

used 10 revise the product.<br />

slmpla conle chart-A chsrf on a simple<br />

conic prqecfion.<br />

simple conic map projection-A conic map<br />

projection in which the surface o! a sphere or<br />

sphsmid, such as the Earth, Ls sorrceivsd as<br />

dwelaped on a tangent cone, whiih is then<br />

spread oul to form a plane.<br />

simple feature-See feature.<br />

slmplo harmonic motion—lhe projection of<br />

uniferm circular rmtion on a d~meter of the<br />

Cide of such motion.<br />

simple pendulum-A theoretical concept. A<br />

heavy particle suapandad from a freed point by<br />

a fins thread which is inexfensibla end withouf<br />

weight. A simple pendulum cannot ba realized<br />

in ecfual work. A simple pendulum is, however,<br />

Ihe basis of rsdtiions of obaarvations made<br />

with an astusl pendulum. Thoaa ebservatione<br />

have cormrctiona sppfied to them to obtain<br />

resufls wtich woufd have been prodmxd by an<br />

232<br />

equivalent simple pendulum.<br />

●lmplifkatlon-Smoc4 hing the characfar of<br />

feafums withotd destroying thrir vidbk skwpa.<br />

Sit’r@iiiticm incras.sas as map Scala decreases.<br />

Slmpaon’o 1/3 rule-A mathematical<br />

expmasion for d~enninkrg arass between en<br />

irmgufar boundary and a trsvarsa fiie tire<br />

aquslly spscad offset msssuramsnts have been<br />

Iakan.<br />

●imultarwous aftltudea-ltfliiudaa of two or<br />

rnera dsdial fxufies drserved at the same<br />

tima.<br />

simultaneous double line-sea<br />

slmultaneoua level line.<br />

aimultanecrua Ievef fine-A line of spiril<br />

Iwefing c9nqxxad of two singla tinaa run over<br />

the same mule, both in the same direction, but<br />

using dflerent turning points. Alse cslld<br />

elmultaneous double Ilne.<br />

simultaneous mode-A satellite method for<br />

delarmining the position of an unknown station<br />

by the simultaneous ‘ranging’ fmm thrse stations<br />

of known pmsiticm and the unknown siation, or<br />

5imuftane0u51y obseming direction fmm fwe<br />

stations of krrovm pesifion and the unknown<br />

stat”km, and matharnatioally reducing ths data to<br />

sohe for a fine or aurfaca of position of tha<br />

unknown. TMs technique permits Pc6ifien<br />

determination independent of a satellite’s orbital<br />

paramatars.<br />

aimultaneoua obaervetlono—(satallite)<br />

0b5arvations of a sstefliia that are made from<br />

two or mora distincl peints or tracking sfst”krns at<br />

assctfy tha -me tima.<br />

●htgla ●etronomlc station datum<br />

orlentatlorr-Tha orientation of a geodetic<br />

datum by accepting tha a6tmnomfcaIty<br />

determined aacidinstes of tha Ori@n and ths<br />

azimulh to one other sfatien without any<br />

curracfion.<br />

single proportionate measurement— A<br />

mathcd of properfioning rnassuramenls in the<br />

restorstkrn of e ksst comer whose position is<br />

determined with raferenca to alignmant in ona<br />

duacfion. Ezarr@es of sush comars are quarter<br />

secfien canera on the fins between two section<br />

comers, all oorrwm on standard paralbta, and all<br />

krtenrmdiata positions on any township<br />

boundary fine. Tha ordiiry fmkf problam


1<br />

MI L-HDBK-850<br />

COneisb of d~rbuting the excess of dakiancy<br />

bafwaam fwu existent comers in euch s way thet siphon baromater-A mercwy bemrneter<br />

the emount given to each krtarvat shall bear the rxmsisting of e column of metcury m e gtesa<br />

acme propc+tion to the whole d~ererrw as the 1* Whii is bard S0 8s to heve two vettical<br />

rawrd length of the interval bears to the whole brenches. ene abeut one-fourth the Iemgth cd<br />

record +s4ance. Attar heving applied the the other. The end cd the kmgar bmnch is<br />

PWrfW@e difference to the record length of cbaad, endtheair krffiedwbytha<br />

aech Irrtervat, the sum of the several parts will nvmury, but the shorter branch is feft open, and<br />

aquel the new rneesurarnerd of Ihe whale<br />

distance.<br />

----<br />

the memury is thereby subjected 10 atrnO@Wic<br />

Pra=ure. ha dtierenca of the height d the<br />

mercury in the hw branches is a measure et the<br />

slngl-besrr method-A technique of etrnwpheric pressure.<br />

barornalrk leveling utilizing two beromatera. One<br />

barumawr is dasignstd se a base and a nltustlon map-(JCS) A rnep showing the<br />

second,, or revirrg, barurrreter is uesd to tectical or edrminMrative sfiuetion et e patl”tifer<br />

detemrma pressures at specific pints. The and time. Sea afso map.<br />

pressure arc recorded S! each poeitic+r ooc@ad<br />

by the roving bemmeter and tires end pressure slxtoonth soctlon corner—A wmer et an<br />

ere recorded every 5 minutes by the besa<br />

esiremify of a boundary of a quarterquarfer<br />

baremeler. Data ere reduced to elevations<br />

OffiCe computations. See also barometric<br />

by section; midpeint between or 20 cheins from the<br />

mntmlling cornem on the section or townstilp<br />

leveling.<br />

boundaries. Written es 1/16 section caner. Also<br />

●lngle-hcadlng rader prediction-A reder<br />

called quarferquarter section corner.<br />

prediction made for a single aircraft poaitiin or size-l. To coat with eny of the various<br />

fmm one specfii peint in reletien to the targe!. II glutinaus msteriels used for filling the pores in<br />

mey be either an experience or an enalyiicsl the sufiace of pepar, fbr, er of a rnoseicking<br />

,. prediction.. bard. Z. To cakxlate tha msssuremants .. . ..required<br />

in photographing a mep to a desired<br />

single-mocfel instrument—A general class scale.<br />

of sterawxiic plotting instruments with a<br />

@W~ll”W for Pmie~in9 a s!n91e ~er~m~el<br />

setup. This cle= of pbtter IS dsaignad for<br />

Per SIZI ng tho lithe-An operetion performed<br />

order to determine the estual mmsuramenl<br />

in<br />

S$<br />

Wmpiktion only end is dependent upon<br />

the original tiihegrephic maps to be used es<br />

supplementary photogremmetric Techniques 10 aeurce for e mep revision in erder 10 determine<br />

accomplish nace!wery sterecrlriangulation. whet distortion and changes of dhnana”bns ere<br />

nacassary 10 fi the okf map inside the new<br />

single-point transfer Instrument—Any projection.<br />

irstrumerd used for the transfer of planimetric<br />

dateil frrrm a single photograph. These<br />

akatch map-A msp made from loose,<br />

instruments are of two general types, reflecting unconwollad suweys. The information thereon is<br />

projscfor and camera Iucide. generslly s+arse.<br />

single-projector method—See one-awfng<br />

method.<br />

●lrrgla-terget Ievellng rod-Any target rod<br />

having graduations on one fete onfy.<br />

slnuaoldel map projection-A particular<br />

type of ha Benne rnep projection, empleying<br />

Ihe Equetor as the slandsrd persllel, and<br />

showing all geographic parellets es trufy spaced<br />

psrellel atreight lines, along which asset scale is<br />

prasenfad. Thks is an equel.aras mep projection.<br />

Also called Msrrcetor aquel-aree mep<br />

projactlon. See also Saneon-Flamsteed<br />

map projection.<br />

233<br />

sketchmaster—A form of camara Iucida that<br />

permits superimposition of a rectified virtuel<br />

irrmge of a pfrotogreph over a map menuscrfp.<br />

See also oblique ●kotchmaetaq unlverael<br />

anafog photographic rectiflcetlon<br />

system; universal sketchmester; vertical<br />

●ketch master.<br />

skewed map projection-Any ctandard<br />

projedien used in map or chart coneirucfien<br />

whkh daas net cenform to a general nertfraoulh<br />

formal with reletion to the neallirras of the<br />

map or chart.<br />

slant ranga-(JCS) The line-of-sight distance


etween We points not et the earns fevel<br />

retstive to a spadfii datum.<br />

davo staflon-l%at *alien in a given system<br />

of stetiena that is cxmtrofbd trf the meater<br />

station. Also called remote station.<br />

divwa+digifaf) Pofyws formed when two<br />

diimftt ~fw.a do W *@ abng e single<br />

mrnrrmn ne and leave e smell SOSCa between<br />

the fargertwo.<br />

xdopa angle-The angle between a dope and<br />

the horizontal.<br />

slope chalnlng—See slop. taping.<br />

slope correction of tape-See grade<br />

correction.<br />

slope correction-l. (hydrography<br />

surveying) Tha correction applied to soundings<br />

ermneoudy fxieilionsd as a resuft of an echo<br />

smmdar rese”wing its initial return from a point<br />

upslopa frem its racerdad position. 2. (Isnd<br />

surveying) See grada correction.<br />

slope taping-Taping wherein ‘the ‘Iapa” (or 4<br />

chain) is hakd .s raquired by the sbpa of the<br />

ground, the slope of the tape measured, and<br />

the horizontal distance computed. Also cslled<br />

.Iope chalnlng.<br />

Elope—See gradient.<br />

slot cutter-See templet cutter.<br />

slotted templat—A Iempiet on wh}ch the<br />

radtals are represented as a slot cut in a sheet<br />

of cmdboard, metal, or othar material.<br />

slottod-templet plot—See @lotted.<br />

templet triangulation.<br />

slotfad-tamplet triangulation—A graphical<br />

radial triangulation made by the use of slotted<br />

templets. Also called slottad-tamplet plot.<br />

Small Wettad Area Twin Hull (SWATH)—<br />

A vessel designad for stability by having ils<br />

buoyant volume rrmstly underwater, presenlly<br />

being avaluatad for use in hydrographic<br />

surveying projests.<br />

small circle-A circle on the surfaca of the<br />

Earth, the plane of which does not peas through<br />

the Earth% center,<br />

234<br />

smell-ecale map-A map having a ecsle of<br />

1:Soo,olx or Smsfler.<br />

smooth ●haet-A final pbf o! fmfd corrlrd end<br />

hydrugraphc devebprnent such as courrdings,<br />

fathom curves, wire drag arass, etc., to b. used<br />

in chart mnetrucf ion.<br />

amoothlrrg-1. A sat ef pmceduraa for<br />

removing short-range, errzdic variat”mna from<br />

lines, aurfasm, or date series. 2. (itige<br />

prcca~ng) The avereging of dansitk in<br />

adjscanl ar~s to produce more gradual<br />

transitii.<br />

srrakosllp-see ●tch slip.<br />

snap markar—See point marker.<br />

Small’a law of refractloxThis law states<br />

that the sin. of the angle of incidence divided<br />

by the sine of the angle of refraction equefs a<br />

mnstant termed the index of rafrectiin when<br />

one ef tha media is air. The index C4 refraction<br />

can also be .xpIainad as the ratio of the vafocily<br />

of light in one medium to thst in anothar.<br />

. . . . .. .. .. . .<br />

aoftcopy —Products which are maintained in<br />

digital fomrst for use with automsted data<br />

processing equipment.<br />

solar rdtltude-Angular distanse of the Sun<br />

above the horizon.<br />

solar attachment-An auxiliary instrument<br />

which may h attachad to an engineer’s transii,<br />

parmitthg k u= as a solar oornpaes.<br />

solar day—1. The duration of one retation of<br />

the Earth on ifs axis, with respect to the Sun.<br />

This may be either a maan eefar dsy, or an<br />

apparent solar day, aa the referance is the<br />

mean or apparent sun, re6pectWety. See also<br />

.ePparent solar day; moan solar day. 2.<br />

The duration of one rotatkm 04 tha Sun.<br />

solar declination—Angular dktarwe of the<br />

Sun expreasad in degrees nerth or aoufh d the<br />

celestial aquatoc it is indicated as “+” wften<br />

north and .-. whan south of the Equator. Also<br />

called dcrclirretlon of the Sun.<br />

solar ●cflpse mathod—A means of<br />

determining the angular distanca betwean two<br />

observers along tha canter fine of fhe path of a<br />

aolsr .dipaa.


I<br />

I<br />

,1<br />

I<br />

aofer ●ctlpee-The dscuretion of the Iiiht of<br />

ths Sun by the Moon A eoler ecfipse is WH&rl if<br />

tha Sun is @fy obscured: total If t@ enlim<br />

wrface is ~ured or mrwfar ii o thin ring of<br />

the Sun’s aurfese ~rs around the obscuring<br />

w.<br />

solar ●phomorf~ deity fabuteticrr of<br />

estmruvnis poeilbtm & the Sun.<br />

solar fomm—.%e sldor.al focus.<br />

eolar occultation-An ooxltation of the Sun<br />

by the Mawr.<br />

eolsr pemllax-The angle subtended by the<br />

equatorial radius of the Eerfh at a d~tence of<br />

one astronomic unit (i. e., the equatorial<br />

horizontal parellex et tha Sun).<br />

solar mrflation prosaura-A perturbation of<br />

high fty@ erlifiiiel satellites of Isrge dmmater.<br />

Ths graster psrl is diractfy from the Sun, a minor<br />

psrf is from the Eetih, whiih is usually dwkhl<br />

info diract (reffesfd) and irrdksx Ierresrrial<br />

(redated) radiation pressures<br />

soler time-l. Ttme based upon the rotation<br />

of the Ewlh relslive to the Sun. 2. Tmvs en the<br />

Sun.<br />

eolar tmnaft-A regular transil to whkh has<br />

bean addad a solar attachment, which affects<br />

the imdsntanecus mechanical solution of the<br />

estmnomic triangle (Sun-zenith-pele) and<br />

permits tha establishment ard surveying of the<br />

astronomic mefidmn or estrbnomic parellel<br />

diractly by observation.<br />

solar year-see troplcd year.<br />

solid ●igle-The integrated engufer spread at<br />

the vertex<br />

figure.<br />

of a sons, rrvram!d, . or other aofkf<br />

solstice-one of h points of the acliptk<br />

fattheat from the celestial aquatoc one of fhe<br />

two points on fhe celest”nl sphere eccupied by<br />

the Sun at meximum declination. Also ssllsd<br />

aolstftial point. See elso summar solstlce;<br />

winter ●olotic*.<br />

solstltlel colure-The hour circle through the<br />

eolstiiae.<br />

solstltlal point—See soletlce.<br />

MIL-HDBK-850<br />

235<br />

eonar-1. (JCS) A sonic davioa used primsriby<br />

for the Macfbrr end location a4 undanvalar<br />

objects. 2. A system fer determining dkdew of<br />

an underwater ~jed by maaauring the interval<br />

of lime between transmission of an underwamr<br />

*or ~ ~wl md return d as eCIW.<br />

~ri tamr la dar&ad form fha wrds ‘sound<br />

navigat”~ and ranging.”]<br />

sonic depth firrdor-See echo eounder.<br />

sonic navigation—See acouatic<br />

nevlgetlon.<br />

eotio plot-(JCS) An overiay representing the<br />

ares on a mefr covered by imegaty taken during<br />

one serfie. Also called photo Index.<br />

aortle-(.fCS) In air oparstions, an eperatienel<br />

flight by one aircrsff.<br />

Sound Survalllance Syriteme Chsrte<br />

(SOS fJS)-Charts which portray generalized<br />

bslhyrnetry and othar prescribed system<br />

oriemed infornsstion supporting Anti Submerirw<br />

Warfare (ASW) survellkmce.<br />

. . . . . . . . ,. . .<br />

sounding datum-The plane to which<br />

soundings are referred.<br />

sounding pole-A round, wooden, 15-fool-<br />

Img pole, used for sfmal water soundings. It is<br />

graduated in feet and half-fast frcm the oanter<br />

toward both ends end numbered corrsecufivefy<br />

fmm Ihe ends towerd the center.<br />

aoundlng—1. The measured or chmtad depth<br />

of water. 2. A measurement of the depth of<br />

wster expressed in fe~ or fathoms and raduosd<br />

to the tidal datum shown in the chert title. Alse<br />

called hydrogrephlc aorsndlng. See atso<br />

depth; depth number. 3. In geophysics,<br />

eny penetrf+m of Iha rrelurel envirmmersf for<br />

●clentlflc obaarvation. See alao ●cho<br />

sounder; echo sounding; Iced lk+; off<br />

eoundings; on soundlnga; wlro drag.<br />

Soumo Acqulsltlon Segment (SA/S)-<br />

Segment of DMA’s DPS which provides the<br />

csPsbi@ to msnege image Ibrary holdings and<br />

to rrreintain the gsodstic confrol deta bsse. See<br />

elso Dlgltel ProductIon System.<br />

Source Pmperetlon Sagmont (SP/S)-<br />

Segrnant of DMA’s DPS which provides the<br />

m~bifify to accomplish source aeaesamant,


I<br />

I<br />

rnurce rafhemsnt, and gaopoaitiiing.<br />

Oparslors perform eeaasamnt of imagery end<br />

of tardual ard graph= rr%atarielto data4’mine<br />

their chemctwisiics md utility. This segment<br />

also provkka for mansurefiirt to support<br />

Iriengutatkm wiih the exis4ing Hardcopy<br />

Expfoiiefkrn Segment. See also Dlgltsl<br />

ProductIon Systam; MARK 90; Hardcopy<br />

Exploltstlon Sogmont.<br />

sourco map-The map used for the selection<br />

of map or chart detail.<br />

eeurse trraterhsf-t)ate of eny type required<br />

for the pmd~tion of MC&G products including,<br />

but not limited to, ground control, aerial and<br />

terrestrial photographs, sketches, maps, and<br />

cherfs; topegrsphk, hydrogrephk,<br />

hypsogrsphic, magnatic, geodetic,<br />

oceanographic, and meteorological information;<br />

intelligence documents end written reports<br />

pertaining to natural end msn-msde features of<br />

the ares to be mspqmcf or charted,<br />

south docllnatlon—See declination,<br />

dafinifii 3.<br />

mouth goographlctrl.. pol~The. -. - .<br />

gac.gmphicsl pole in the Smrlhem Hemisphere,<br />

at Miiude 90”S.<br />

south geomagnetic pola-T h e<br />

gaomsgnatic pole in the Southern Hemisphere.<br />

south magnetic” pola-llw magnetic pole in<br />

the southern Hemisphere.<br />

south point—See celeatlal marldlan,<br />

couth polar clrcla-See Antarctic Clrcla.<br />

southbound nods-See deaoandlng<br />

node.<br />

southlng—See Iatltude difference.<br />

Spaco Obllquo Mercetor—A mepping<br />

projection modeled on the dynamics of the<br />

IANDSAT apececmff motion. It incorporates<br />

tirnadepsndent veluas of satellile pfaffonn<br />

motion and the Earths motion in e continuous<br />

pro@fion of the area viewad in the LANDSAT<br />

ecene.<br />

specs coordinator—(photogrammetry) Any<br />

geneml three-dimensional coordinate system<br />

used to define the position of a point in tha<br />

MIL-HDBK-B50<br />

236<br />

ob@cf space, es distinguished from the image<br />

of tfw pofnl ort a phofogmph.<br />

spsce motion-MOtion of a caketial body<br />

through space. see elao prmper rrtotlon.<br />

space-polar coordlnatbs—A system of<br />

ccmrdinrdes by which e point on the eurf~ of e<br />

sphere is located inapra2aby (1) ftsdistamce<br />

fmm a fbd point et the canter, caffad the polo:<br />

(2) the odstifude or angle between the polar<br />

axis (a reference Line through the pofa) and the<br />

radius vector (a sfmighf Iiie connecting the pole<br />

and the point); and (3) the longitude or angle<br />

between a refarence pfane through the polar<br />

axis and e plerra through the mchus vector and<br />

polar axLs.<br />

sp.scecrsft-Davices, manned ard<br />

unmanned, wtdch are designed to be plecad<br />

into an orbh abwl the Esrfh or into a trajectory<br />

to another celesfiel bcdy.<br />

spedirtg-Removing scribe costing from tha<br />

base material by usc of a wide fiat blade.<br />

apaghettl vector—A d!gifal storage format in<br />

which all lines end pints are unrelated 10 asch<br />

othsr.<br />

Spetial Data Transfer Sp.sclficatlon<br />

(SDTS)—A ~ecificstion under the Spetisl Data<br />

Tmnsfer Standard (SDTS) designed to rnaet the<br />

rac@zad requirement for easy transfer of<br />

spatd data from ona qatial data herding<br />

system to anether, with both systems possibly<br />

residing on computer hardware end cpersting<br />

system software of dNferent makes. Under<br />

SDTS, the contents (specification of fields eml<br />

r.ubfields) are clasrfy sepsrsbd from the<br />

impfementalion (the encoding of fiefda and<br />

subfields on tha madii).See Spetlal Data<br />

Transfer Standard.<br />

Spatial Data Trensfar Standard<br />

(SDTS)-A standerd consisting of definitions<br />

and references, the Spatial Data Trsnaf er<br />

Specifiition, a qusfii report on digital<br />

cerfogmphic data, a conceptual rnsdal for<br />

describing cartogmphk featuras. and a sfandsrd<br />

ml of defined entities and affribufas derived<br />

from topography maps and general nauficd<br />

charfs. See Spatlel Data Trsnafar<br />

Spaclflcatlon.<br />

spatial anslyala—Analyf icel techniques<br />

Baaocietad with the study of tha location c4<br />

geogrsph=l entitias togelher with their spatial


dmnaions. Afso referred to as quanf”tittie<br />

ensfysis.<br />

cpatlal data baao~llediens of similar<br />

end mfstad spstial data racerds that ere<br />

ramrdad for use by a computer. Ssa afm<br />

Geographic Informntlon System,<br />

MIL-HDBK-850<br />

spatial data astsr-Collactions of similar end<br />

mletad apstial date raamts Shst ere recorded fm<br />

use by a wrrqrufer.<br />

spatial data-Dats perfeining 10 the focatian<br />

of gaogmphii entities Iogelher with lhem<br />

spslial Cfhrw-@ens. S@al dsts are cfessifii m<br />

pdrrt, fins, er~ or surface.<br />

.<br />

spatlel “model-See stereoscopic model.<br />

speaking rod—See self-reeding Ievallng<br />

rod.<br />

special-purpoea map-Any map designed<br />

primarily to meet specific requirements.<br />

●peclal area (SA) annotation—A structure<br />

or group of structures fmssaasing urdque<br />

physical chsracterislics, bui whoss arss or fitiar<br />

dimensions do nof qualify for appiiostion of one<br />

of the radar significance anslysis codes.<br />

spsclaf job-cover m.sp-(JCS) A small-scale<br />

MSp US+ to ramrd progrw on pbtogrspfsic<br />

raconnatssarce tasks covering very fsrge arees.<br />

As asch porfien of the tssk is mmpletad the<br />

ems covered is oulfinsd on the map,<br />

epeclal meander comer—A corner<br />

eeSeblishsd at the intersection of s survayad<br />

SubdiiiSIon*f-sacf ion fine end a maender line or<br />

the intersection of a mrnpulsd center Ifne of a<br />

sacfion and a meander fine. In the fatter case,<br />

the centerline of tha sact”mn is celculatsd and<br />

suwey~ on a thaomticsl bearing to an<br />

infersachon with the meander fins of a lake (over<br />

50 acres in ares) wfich is heated entirety wfthin<br />

a section.<br />

spoclal-swbjmt map—See topfcal map.<br />

specific forca-The difference between the<br />

inartbl .mcalerstion and gravitation acting on a<br />

WY. The physical gravity eanead by<br />

accalerometera. All spirit Iavels are normsl to the<br />

spacifii force vector.<br />

apoelficatlone—The rulas, regulations,<br />

237<br />

..... .<br />

Syrrtrofegy, end e ccxnprehansive eel of<br />

St.snderds *i heve bean astabfiihad for a<br />

~tticulsr nmp or chart series w SIe gmtp.<br />

Spa@fiibnS vary wilh the ae and tb<br />

purfxma of tha graphii.<br />

spectral band-A set of adjacent<br />

wevalengths in the elactromsgnbtic spectrum<br />

with a mnw’non characteristic, such as tb ViSJMS<br />

band.<br />

●pactrophotomatar-A devics for the<br />

maasuremant cd spectral transmittenoe, spectral<br />

rafbcfanca, or rafstive apaofml erniitanoa.<br />

cpactroradlomot~ r—A device for the<br />

mseaurernant of spectral diiribufion of radiinf<br />

enargy.<br />

specular reflectlo n—(oplics or microwava<br />

thaery) The type of reflection charscferMlc of a<br />

highfy pelishad pfane surface from whwh efl rays<br />

are raflactad at an angfa equal 10 the angle of<br />

incidenca. See also dfffuee raffactlon.<br />

●pead of fens—S ee rafatfva aperture.<br />

upeed—(phetogmph~) The response or<br />

sensitivity of the material to fight, otlen<br />

expressed numerically acawdng to one of<br />

saversl systems (e.g., H and D, DIN, Schekrar,<br />

ard ASA exposure index). Sas al= relative<br />

eperturo.<br />

sphera-A body or the space bounded by a<br />

sphericsl surface. See also celeetlaf sphere;<br />

obflqua aphare; paraI1.sl sphera; right<br />

sphers; tarrastrlal sphere.<br />

spherical aberration—An aberration sausad<br />

by rsys fmm various zones of a lens coming to<br />

focus al dflerent places abrrg the sxis. This<br />

results in an object point being irnsgad as a<br />

blurred circle.<br />

apherlcaf angla-The angle between Iwo<br />

intersecting great circles.<br />

spherical coordlnatea-A system of pofsr<br />

merdinatas in which the origin is the center of e<br />

sphere and the poinls all iii on the surfece d<br />

the sphere. Ths paler axis d such e system cuts<br />

the sphere at its two poles. In photegmmmatry,<br />

sphericsl coadinstas are useful in defining the<br />

refstive orientation of perspective mya of exas<br />

and rneke if possiMe to state end mfve, in<br />

simple forms, ninny related problems.


i<br />

MIL-HDBK-850<br />

sphorfcal ●xcosa-l%e amount by which the<br />

sum of the three arrgfes of a triangle on a<br />

sphere axoeade 180”. In gaodatk work, in the<br />

co~yfafbn of trisngbs, the difference between<br />

s@r3rrd angfas and sphamidal angles is<br />

generally nagfecfsd: Sph- angles are used,<br />

and Lagarrdm’s thsorem ki applii to the<br />

dsribution of the spherical excess. That is,<br />

a~roximatefy ona-thd of the @mrical axcaaa<br />

of a given spherical triangle is subtracted from<br />

each angle of the triangle.<br />

spharlcal hsrrnonks-Trigonometric terms<br />

of an infhife .saries used to approximate a W*<br />

or thraedkrransiortd furrcfbrr of ~t~ns w or<br />

abeve the Earlh.<br />

spherkal Ion- lens in whmh .s11euriacas<br />

are segments of spheres.<br />

spherical trlangk-The cbsed figure formed<br />

when any three points on the surfece of e<br />

s+rhare am ~kred by ems of great circles.<br />

ctpherold junctlorr-An eccentuatsd line on e<br />

VP or chart, separating Wo or more major<br />

,.- grids which ere. based on d~eran! spheroids,<br />

spheroid of referonc~See refarence<br />

spheroid.<br />

spheroidal angle-An angle between two<br />

curves on e spheroid; meesured by the angle<br />

between their tangents at the point of<br />

intereeXiin.<br />

spheroidal axcess—Tha amount by which<br />

the sun of the three engbs of a O’iangle on a<br />

spherokf exceeds 180”. see also spherical<br />

excess.<br />

spheroldsf trlangl*A triangle on tha<br />

surlece of e sphamid.<br />

rtphorold-1. (genetal) Any figure differing<br />

slightly from a sphere. 2, (geodesy) A<br />

mathematical figure cbsaly approaching the<br />

geoid in form and size end used as a surface of<br />

reference for geodetic surveys. In geodesy<br />

spheroid and elf!!sokf are synonymous terms.<br />

See ebu Afry ●pherold (afllpaold);<br />

Australian Nstlonal apherold; Eaasel<br />

sphorold (slllpsofd); Clarko spheroid<br />

(olllpsold) of 1868; Cfarko cphorold<br />

(olllpsold) of 16S0; ●flipsofd of rotetlon:<br />

equilibrium ●pherofd; Everest spheroid<br />

(ellipsoid); Hayford sphorold (ellipsoid);<br />

za8<br />

Intorrmtlorml ●phoroid (alllpsold);<br />

Kraaovaky sphtsrold (alllpaold); oblato<br />

●pherold: prolsto ●pharold; roferanco<br />

●pharold.<br />

●phoropotm!tlal surtaca-See apharop.<br />

●pharop-An aqu”~tential surface in the<br />

normal gravily field of lhe Earlh. Also celled<br />

●phoropotmtlal ●urtaca.<br />

spldor tempfet—A mechanical templet which<br />

is fwmed by afteching skoftad steal arms,<br />

representing radiifs, to a central sore. The<br />

spider tenqdet san be d~ernblad ard the<br />

parts used agein. Also called mechanical arm<br />

templet.<br />

spider-tomplmt p}ot-See spldcr-tomplot<br />

triangulation.<br />

spldar-tamplet trienguletlon—A grephicsl<br />

rad!al triangulation made by the uss of spider<br />

Iempbts. Also called spider-tempfet plot.<br />

spiral curve-(mufe surveying) A cutve of<br />

uniformly vsrying radius mnnacfing a circuler<br />

curve and e tangent, or two circular curves<br />

whose rsdii sm. rqtiivaty, bngar and ahorler<br />

than its own extreme radii. Afso called<br />

easamont curve; tranaltlon curve,<br />

spiral to spiral (SS)-A common point<br />

between two spirals.<br />

splrlt Iavel axis—The fine tangent to the<br />

surfece of a spiril Ieval tube (vial) egainsf which<br />

the bubble forms, at the center of the gmduetad<br />

scale of the level, and in the plane of the<br />

bngiwdinsl axis of the tube (vie!) and its center<br />

of curvature. Also called axis of lava~ axle<br />

of Iho level bubble; bubble ●xk.<br />

splrft Ieval wind-Lack of parallelism<br />

between the axis of a spirit Iavel vial and the fine<br />

joining the centets of its suppals. When wind<br />

(pronounced to rhyme with find) is prasant, the<br />

bubble will respoti with a bngitudinal<br />

movemenl Wren the spirit level is rocked on ifs<br />

Suppotis.<br />

nplrlt bvallng—The determination of<br />

Islevetions<br />

of points wfih respect to each otfwr or<br />

\ with respect to e cumrnorr datum, by use of a<br />

Ileveling<br />

rod end en instrument using a spiril<br />

level to esteblish e horizontal fine et sight.


MIL-HDBK-850<br />

splrft favof-A dosed gfeaa Uire (vlel) of<br />

circubr oroeasacfkm, hscarrrerline ataeforning<br />

a arcubr arc, tts interior aa-fete being grcurrd to<br />

PrecksafonT ffiafiJJed wJffrelhs$ erlquidoflow<br />

~ e~ugh free apace being left for ti<br />

fcrrneticn of n btie of air and @S. Ahe celled<br />

bubbla lsvol. See sfao chsmbarad splrlt<br />

Iovel; circular level; hmtglng Iswol;<br />

Idtudo level; loval trlcG plato loval;<br />

reverslblo level; rod level; strldlng level;<br />

telslscopo Iovel.<br />

spiff cwnama-(.JCS) An aeeembfy of two<br />

cameras d~aed et a tied overbspping engle<br />

retettie to each c4her. [Meinty used for<br />

remnmiasenm purpoeee.] AJao cefled srplltvertlcel<br />

cam.ra.<br />

split photography-See split-verflcal<br />

photography.<br />

spilt-varflcel camOre-See spilt cameraa.<br />

split-vorflcal photography—(JCS)<br />

Photegrephs Ieken simuttanaousfy by two<br />

cameras nmunted at an angle from the verlird.<br />

one lined to the Ml and one to the right, to .,<br />

obtain a s-II side overfep. Abe called splJf<br />

photogrepl?y.<br />

●pok@?+JCS) (radar) Pwiodii flashes of the<br />

rotating time base on a radml display.<br />

Sornetimaa caused by mutual interference.<br />

spot ●levatlo~JCS) A point on a map er<br />

chart whoee elevetii ia neted, (Elevations are<br />

shown, wherever pmcfiible, for mad forks amf<br />

interaacfiorss, grade meesin~, mxnrrrits ef hiJJs,<br />

mountains, and mountain pames, water<br />

surfeces of fakes and ponds, afreem forks,<br />

boffem elevations in depraaaima, and Jarge flat<br />

areas.]<br />

. .<br />

AJSO<br />

.<br />

calJed<br />

. .<br />

spot<br />

. .—.<br />

height. See<br />

. .<br />

also<br />

crroctcoa ●per ●mvation: ●mvauon;<br />

uncheckad spot .l@vatlon.<br />

spot helght+ea spot ●fevstlon.<br />

spot pradlctlon-A single heeding radar<br />

prediitbn intended to fmrfnry, as nearfy as<br />

posaibla, a cwnprehensive anatyaJa of the<br />

radaraoope at a precise geegraphn fcc.aliorr.<br />

spot dsa+JCS) The sJze of Iha electren SPYI<br />

on the face of the oethodsrey tube.<br />

●prhtg balanca-An accessory of taping and<br />

239<br />

. . . . .<br />

base measuringapparatus which is used m<br />

aPPb’%7 p-r tension to a fsipe.<br />

spur Iina of bavola-A line 64 Ievals nm es a<br />

branch from fhe main lie d Iwals, either fer the<br />

PWPWI ef detarminiig the tshvatiom of merke<br />

net corrvsmierrtfy mxhad by the main he of<br />

Ievefs of to cormact with lidsl bench mark or<br />

other previously aefebfished bench rrrerke in<br />

obfainiig checks on eld IeveJing either aI the<br />

beginning or end of a fine of Jevels or et<br />

intarrnadale jurrctiens ebng the new bna of<br />

IsrveJs.<br />

spur travorae-Any short traverse that<br />

branches cd the tiihed traverae to reach<br />

some vantage @nt or poaificm. AJSOcefled<br />

stub trmrarao.<br />

stabilized mount-A mount controlled by e<br />

gyroscope vertical reference unit designed to<br />

maintain a rna@ng or itional camera or<br />

other devices euch aa r PR enlenna in a near<br />

vertical orientation<br />

and roll,<br />

independent of aircraft pitch<br />

stsble bnse-A general term apgdied to<br />

reaming materials poeseesing .9 high degree of<br />

dimensional stebilii,<br />

stablo grevimeter-A gravimeter having a<br />

single weight or spring such that the aensitivify is<br />

pvrtbnd IO the ~uere of its period.<br />

stablo-basa fflP(JCS) A perficuter type of<br />

film having high atabilii in regard to ahrinkege<br />

and stretching. [Suitable for aerial rne#ng<br />

phetogrephy and map production. Uauelly<br />

referred to by its commercial narrw.]<br />

Btsbla-fypa gravlmet*r—A gravimeter whwh<br />

was a high erder of ep:iccd ardor mechanical<br />

megnifiition ac that a charrga in Poaifiin of a<br />

weight or associated properfy is measured<br />

directly.<br />

stadia circle-See Baaman arc.<br />

atadla corrstant-(leveJing) The retie which is<br />

rnuftiplied by tha stedii interval to cbtain Iha<br />

Iangth et a sight in mafera. A!so, the ratio by<br />

which the sum cd the aiadia inbrvals of all aight6<br />

of a run ia mrwerled to the length of the rrm in<br />

kilometers,<br />

stedla dlagra m-A chml or drawing whwh<br />

provides a means for rapid fieJd reduction of<br />

etadia reedin~. Ueuslly it is prepared on croaa-


aadicm paper and drawn to tha acsle d the<br />

survey being performed.<br />

stadia Intorcopt-see ●adla Interval.<br />

stadla Intsrvd-(lawefing) The length of rod<br />

subterdad between the tcfs and bottom cross<br />

hake (crms wires) in the Ievefii instrument as<br />

saan pmjectad against the face of Iha Iavefing<br />

rod. Atao called stmdla Interc+t.<br />

stadla rod-See stadfa.<br />

MIL-HDBK-850<br />

atadla s[ldo mle-lhs most rapid melhed of<br />

radusing atadm rasrfhge k by the USE d e slide<br />

rule which has, in .eddifiin to tha csdinsry scale<br />

of numbers (bgsrithme d the distances), two<br />

scales espacislly constructed for @ad= work,<br />

ona consisting of values of tog WS2 a and the<br />

other of bg 1/2 ah 28 for dMer~ values of a.<br />

On some rotas, the values of a range from 0°34’<br />

to 45”; on others, from O“@ to 45”. In -<br />

forms the horizontal distance is mad diructty; in<br />

others the horizontal correction (1— COS2) or<br />

sin2 k given. A 1o-inch slii rule giv- resufts<br />

sufricientty accurete for all ordkumy purposes,<br />

‘ ‘‘” ‘ 8~di-’” trav=m~ traverse in ~ih”<br />

distances are measursd by the stadia msthod.<br />

stadla trigonometric l@vellng—A technique<br />

of extending supplemental vertical control in<br />

arass of moderate or bw relief. Oistwrcas are<br />

measured by stadia methads and can be done<br />

with plantable, transit, or theodolile. Field work<br />

is rsducad to ussble form by trigonometric<br />

computat’mns.<br />

stadla—A grsduatad rod uaad in the<br />

determination of distance by observing the<br />

intersep on the rod subtending a smell known<br />

engkt at the pint of observation. In prectice,<br />

the engb is usually defined by two fixed lines in<br />

the reticle d e telasrmpa (trend or telescopic<br />

cdiisds). The term stadla is also used in<br />

ccmnscfion wilh suweys where distances are<br />

determined with a atmfia, as a;acfii survey.<br />

stadm method, stadia distence, etc.; also used<br />

to dasigmste psrts of the instmment used, as<br />

atadia wiraa. Also called Media rod. See also<br />

horizontal stadla.<br />

●tadlmotar—An Instrurhen! for determining \ha<br />

dwance to an object of known height by<br />

measuring the angle subtended at the obsawer<br />

by the object. The instrument is gradusted<br />

directly in dietance. See also rsngo finder.<br />

240<br />

staff gag.-The sin@asf form of tide or<br />

strasm gage consisting of a @uufad staff<br />

=csr* f+enad to a pda or other SU*<br />

SUP. ff ta so designed thst a segment of the<br />

SISfftink-Mbwnter~<br />

mmmfad mud the rsrmidar till be strove wafer<br />

and positiinad for dired obearvaticwra from<br />

shore or =#ne other vantage point.<br />

Stampfsr fevof-A type of Ievaling instrument<br />

hsving the telescope tkss so mourned that it<br />

could be movsd in a vartical plane about a<br />

furizomtel axis, rnvshhg the uaa of a @idi@f<br />

level ●nd ● micrometer screw.<br />

Standard Llnaar Format (SLF)-A<br />

atandsrd formst used and modifisd try DfAA for<br />

digtial osrtogrsphii dsts. SLF uaas a chainncde<br />

spatial structure to avoid duplicatii of<br />

common tmundarias,<br />

standard automatic tide gage— A<br />

chrcmogrsph uaad where extended time<br />

raadings of tidsl changes are required. Ths rise<br />

and fall of the tida is communicated by a wire<br />

(sttsched to a float) 10 a wnn screw on ths<br />

gage, which moves a psn transferring the dsta<br />

to a permenent psper record.<br />

standard cornmr-rl senior comer on a<br />

standard parallel er bsse line.<br />

standard deviation-See ●tandnrd ●rror.<br />

standard arror (r?)-The aqusre root of the<br />

varisnce. It irrrphes a 6&27% probability that<br />

tha parsmater of cbaarvation hss an error the<br />

abselute value et whrch deaa net exceed o.<br />

Also csliad standard devlatlon.<br />

standard error of the mean-The standard<br />

error(s) of e mest prcbsbkr value establiisd sa<br />

ths masn of n observations. It is rigemudy<br />

derived as the standard error (c)of then<br />

observations divided by ths aqusre reef of n. It<br />

atso hss en implisd pmbabiii of 68.27%.<br />

standsrd grids-The Universal Trensverss<br />

Mercater (UTM) grid and the Universal Polsr<br />

Ster-graphic (UPS) grid.<br />

standard lrrdoxhtg ●yatom (SIS)-A<br />

eystam develcfmrt for use within the Department<br />

d Defense fer the indexing of sfl aerial<br />

phetcgrsphy held et netionsl level. Aerial<br />

phetogrsphic missions are plottd on acatate<br />

shssts covering 10 squsres ef tha world at a


I<br />

I<br />

Scale of 1:250,000.<br />

standard ttm~ ltq wttch Wr@iBS with<br />

apaclk ktep Acan’acy Standards end<br />

gukfelhes.<br />

standerd merldlo~l. The meridian used<br />

for determining stendard time. 2. A merfdian of<br />

o MSP PWW, afong whiih the scale ia aa<br />

Sfetad.<br />

stendard of iength-A physisal<br />

representation of a linear unil that is apyovad<br />

by oorrqrafent eurhority.<br />

standerd paraflef-(JCS) A parallel on s map<br />

or chart abng whiih the asda is as stated for<br />

that map or chmt. 2. A parallel of Iatksfe used<br />

In the computation of a map pmjecficm.<br />

standard port-Sac roteronco station.<br />

standard quadrangle-A quadrangle of e<br />

apedfm series, conforming wtih the systematic<br />

pertem of the aeriee.<br />

standard station—See reference station.<br />

., !.,’.., ,. .,.<br />

at.endard ●urvoy-A survey wlich, in scale,<br />

aocuracy, and conlenl. aati#les cxfteria<br />

prescrifmd for such a suwey by competent<br />

authority.<br />

standard trmsbn-(teping) That tension or<br />

pull at which a tape was standardized.<br />

standard tlma-kleen solar time for a<br />

selected meridian adopted for use Ihrougheut a<br />

belt or zone.<br />

standardization—The comperi~n of an<br />

insfmrnent or devise with a atanderd to<br />

determine the value of fhe instrument or device<br />

in tarms of an adopted unit.<br />

etendard-(JCS) An axact value, a physical<br />

ent’w, or en abatrecl consept, aefablishwl and<br />

defined by authority, cuatem, er common<br />

consent to serve as a reference, model, or rule<br />

in measuring quantities or qualitim: establishing<br />

preoticee or procedures, er avaluatmg results. A<br />

fried quantily or quality.<br />

star chati-A chart or map of the caleafial<br />

ephara showing principal stars which are useful<br />

for ebeervationa for navigation or field<br />

aatronomy.<br />

MI L-H DBK-850<br />

241<br />

star fhxfar-A devbe to facilitate the<br />

~~~ ~ -, partisdarfy fer IXIrpcmaa of<br />

nevrgef”bn and geodet”k aetmrremy.<br />

afer trail-A streak-like image of a star<br />

mcordad on a stellar pfale by a phofogmphic<br />

time exposure causad by the mtalbn of the<br />

Earth.<br />

start node-(digifal mapping) The firaf rd. of<br />

an edga (m edga is Iravaraad fmm atetl neds<br />

to end rrede).<br />

etrrfilng controf-Control aveilable for the<br />

absolute orientation et the first plate pair abng a<br />

Iii. 54 fliiht fer which control is to be azlended.<br />

stats baae map-A base map of the area of<br />

a state as lhe unit used as a base upon which<br />

data of a spacielized nature ate compiled or<br />

overprinted.<br />

atete coordlnato systems-lhe plane<br />

racUrn@ar mwdinate eysterns aetebliihad by<br />

the National Gec+etic Survey, orw for each<br />

stale in the Unitad Statas, for use in defining<br />

POSif;OrrSOf 9*etiC stations in terms of plane<br />

rac+angular (x end y) coerdinetae, Ako called<br />

atat6 ayatem of plana coordinates,<br />

state system of plane coordlrratoa-See<br />

attrte coordlnato aystteme.<br />

state vector-A set of parameters that define<br />

the position acd vefecity of an c@ct et a<br />

spacifii time with respeci to a reterensa system.<br />

static gravity meter—A type of gravity<br />

instrument in which a linear or angular<br />

dispfacamant k observed or nuffed by an<br />

nppsing fome.<br />

static marklnge-(photogremmetry) Marka on<br />

photcgraphk negatives w other eamor imagery<br />

caused by unwanted discharges of static<br />

elect-.<br />

station adj uatmsmt—The adjuat menf of<br />

angle measurements at a triangulation or<br />

traversa station 10 satisfy Iced requirements<br />

(such a. horizon cbsure) without regard to<br />

ebeewatiena or umditiem at other points. Also<br />

celled local ●djuatmenf.<br />

station error—See daflectlon of ths<br />

vertlcel.


MIL-HDBK-850<br />

station msrk-A mark on ha ground, either a<br />

monument at apacmf anetmcfion, or a natural<br />

or arfiii ebjc@ witii pirpinfs the location of<br />

a auwey station. Sea also mark definition 2.<br />

station polnt6r-See three-arm<br />

protractor.<br />

stetfrmaq field-Any natural field d forse, as<br />

e 9mvimatric w tmgnetic f~fd.<br />

stationery orbit-An orbii in whii the<br />

salelfiie ravefvas about the primary et the<br />

anguler rate at which the primary mtstaa on Ifs<br />

axis. From the prirnsry, h daffile appaara to<br />

baafaficmary ovsrapoinf mthaprimary. sea<br />

also synchronous satellite.<br />

station-l. (surveying) A definite point on the<br />

Earth whoaa LxAion has bean dalarminad by<br />

surveying methods. If may or rmy not be<br />

rnarfmd m the ground. A station usualfy is<br />

defined by the addition of a term which<br />

de-”ks ifa origin er purpDcs. Usually marked<br />

on the grew-d by a mcnumem 01 spackd<br />

rnnctnwlim, or by e natural or etiifiiial structure,<br />

2. (mute surveying) Any peinf w+wsa pocition is<br />

given by ifs total distance from the starling hub;<br />

aLso, aach steka sat al 100-1001 intervals along<br />

a route survey. See also A-station; air<br />

station: astronomic atatlon; auxiliary<br />

●tatlon; B-statIon; harm ct=tion; control<br />

station; date ncqulsltlon station; drift<br />

station; ●ccentrlc station; gravity<br />

referermo stations; ~ravlty atatlon:<br />

around -.. . ..— station: horl;onta[ control<br />

atatlon;<br />

station;<br />

station;<br />

station;<br />

stetlon;<br />

atatlon;<br />

ststlon;<br />

In-and>ut station; IntersectIon<br />

Laplace station; magnatlc<br />

mrdn schame ststion; mastar<br />

oceanographic station: plus<br />

primary tide station; projector<br />

radio range station; refarence<br />

resection station; satellite<br />

triangulation ●tations; secondary<br />

ststlon; seconda~ tide station; setup;<br />

●lavo ●tatlon; stream geglrrg ●tetlon:<br />

subordlneta ●tatIon; subaldiary ●tatlon;<br />

supplamentn~ ●tatlon; taping stetiorr;<br />

tide ●tatlon; tracking station; traverse<br />

station; triangulation atatlon.<br />

●tatoscopa-A aarrsif Fve form of barometer<br />

used in aerial photography for measuring arnall<br />

diffqrencaa in aflifuda betwean sumassive air<br />

sfafons. Uaualfy ramrdad automatically on tha<br />

fiim at the instant of exposure. See recording<br />

atatoacopa.<br />

242<br />

otollsr aberratlorr-The diapfacamanf c.f tha<br />

cbcerved pcraitii from the poahkln wf-lars the<br />

body was geometrically Iosatad at fha inaranf of<br />

obewvation dua to tha motion of tha obaarviig<br />

platform,<br />

stellar tamer-A cemara for photographing<br />

tha stare,<br />

●tellar magnitude—sae magnltudo,<br />

dafinifii 1.<br />

stellar map matching+ pmcesa during the<br />

ffight d a vehwle by which a cl’wt cd the stars<br />

sat info the guidance aysfam is aufotrmticalfy<br />

matched with tha @ion of the stare obaarvad<br />

through telaas~ SD as 10 give gu”danca to<br />

Ihe vehicle. See aiaa map matching<br />

guidance.<br />

stellar parallax—See annual parsilax.<br />

stellar plat~A pracisafy ground glass plate<br />

coated with a photographic emulsion uaad for<br />

raoording satellite imegss against a stellar<br />

background.<br />

staD cast—The neaativa or c.ositiva<br />

rep~cduction of the”~tapped te~~n baas of ❑<br />

relief model.<br />

step tablet—See step wedge,<br />

stap wedgct-A strip of film or a gfaaa plate<br />

whoaa transparency dimin”~hes in graduated<br />

stepe from one end to the other; often used to<br />

detannine the density of a pho:ogmph. Al=<br />

called gray scale; step tablat. Sea also<br />

contlnuoua tone gray acala.<br />

Stopheneon fevallng rcrd-A speaking rod<br />

having graduations forming a diagonal acafa,<br />

with horizontal finae through the tanth-d-foot<br />

rnarlcs. This md is read to hundredths et a foot.<br />

steradian—The unit of measure d a aDfkf<br />

angle.<br />

atoreo oblique pfotter-A device which<br />

pern’k cominwus pfotting of planirnavic detail<br />

from oblique phofegrapha. Essentially, the<br />

devica consists of IWU photoangulafora linkad<br />

under a aferaoacopa atwd is provided with<br />

pfoffing erms.<br />

stereo pair-See stereoscopic pelr.<br />

. . ..e. ..r


stwwo triplet-A etemogrsm cwposed of<br />

three photogrspfts, the center phefo heviwg a<br />

oc.mrncn fkkl of view with the twm adjscenl<br />

phetos, arranged in such a rmrmsr as to permit<br />

omp~te SJWSOSC+S viewing of the center<br />

photograph.<br />

MIL-HDBK-850<br />

●taraocomperagraph+ reletivefy dr@e<br />

and tills sfereoscapk instrument used for the<br />

preparstbn d @mgmphii mspa from<br />

phetegraphy. Dfiarences in elsvsticm ere<br />

detewniwed by meesuring psrallar dflererxe on<br />

a sfereescopic peir.<br />

●toraocomparator—A stereoscopic<br />

instrument for -Suriwg peral@ ususlty<br />

irdudes e meens of rrwasuring phdogreph<br />

ccudimates 04 imege points.<br />

storeOcompllatlOn—See compllatlon,<br />

definifii Z.<br />

●teroogram-(JCS) A sterecmmpic set (pair)<br />

of photographs or drewings curredy erbnted<br />

end mcsmted (or projected) for stereosc+c<br />

viewing. Sse also stares. triplet.<br />

,., ,,.. . .,


MIL-HDBK-850<br />

stwwoacopic modof-(JCS) The mental<br />

ipd Of,an ame or objacf seen rM bafng in<br />

thraa dim ansscms when viawed aferaoampimlfy<br />

on phofegrapha. AISCI oellad spsttal model;<br />

stwaomodol; storooscoplc Imsgo.<br />

atoreoaooplc pair-(JCS) Two photographa<br />

with auffiiiant overlap of detail to make poaakde<br />

attmnscspic examination of en objacl or en<br />

area common to both. Afao called aferao pair.<br />

slorooscoplc parallex-See ●bsoluto<br />

starsoaooplc psrallsx.<br />

starooscoplc plottlng lnstrumsnt—A n<br />

inafrumenl for cxxrpiling a map or obtakring<br />

spatial solutions by observation of stereoscopic<br />

models formed by areraoampk pairs of<br />

pholegrephs. see also double-projection<br />

direct-viowlng stereoplotter; radial<br />

plottec slnglo-model Instrument; stereo<br />

crbllquo plotter; etoroooomperagraph;<br />

stereo planigraph.<br />

stereoscopic prlnclple-The formation of .9<br />

single, threedimensional image by birrccular<br />

vision of two photographic images of the same<br />

termin taken from differenf axpawe afations.<br />

stereoscopic vlslon—The particular<br />

e@ication ef binocular vision which erurbfes the<br />

ebsarver to oblain the impression of depth,<br />

USUSUYby maarra of two different pamqmstives<br />

of an ‘&@ct (as two photographs iakei from<br />

dflerent camera stations).<br />

starOOscOplc-Of or pstiaining to<br />

stereoampy.<br />

stereoscope—The science which deals with<br />

Ihreedlmensional effects and the methods by<br />

wlrich they era preduced.<br />

storeotamplet triangulation- Aerotriangulatien<br />

by means of ateraoiernplats. The<br />

~thod permits SCSle aolulions by area and is<br />

not reatnstad to aelutiem eking flight atrips.<br />

storeotomplet—A cmmposite slotlad templet<br />

edjusmble in acafa end repraaantat”we of Ihe<br />

trerizontal pkd of e aieraoacopis model. An<br />

asa8rridy ef afereetempiets pmvidas a means<br />

of eerofriangulelion for horizontal positions with<br />

a stereoscopic pfeffirrg instrument not designed<br />

for bridging.<br />

244<br />

stsrootopographlc<br />

grmmmatrlc map.<br />

msp-See photo-<br />

stor80trlangufntlon-A triangulation<br />

procedure thal ueas a cferacwc@c pbfting<br />

Insfnmrant to ebtain Ihe ~e orfatit’brra<br />

of tha efaraoscepk pairs of photographs into a<br />

mntinuoua ettfp. The spatial salution fer the<br />

aflanaien d herixonfal andor vetticaf mnfrd<br />

using these strips (or ffiiht) soardinatea may be<br />

made by aitfrer graphiil or mnptational<br />

prosedurea. Al= called brldgfng; Instrument<br />

photolrlangufstlon; multlplax<br />

trhmgufatlon. See afao vatlcal<br />

ater.otrlangulatlon.<br />

stereo-l. Contracted or short form d<br />

aleraoampic. 2. The cwierrfatien of pholographa<br />

when pmparfy pesitionad for afareoampic<br />

viewing. Photographs so oriented are aafd to be<br />

.in starae.”<br />

aticku~dhesive-backed or wax-backed film<br />

or paper tich map names, symbols,<br />

dascriptiva tarma, ate., have been printed, for<br />

application in maP and chart production.<br />

. . 4 .’ ‘-=. . . - ‘,<br />

atilllng devlcs4My devise or structure<br />

placed in the vtilnity of a gage to reduce wave<br />

action and afford mere accurate reading of the<br />

gage.<br />

etippla-A rendom do! pefrem used to depict<br />

certain topographic features such as sand.<br />

Stokes’ formuls-A fermufa Ior computing<br />

gaeid heights from grevify data.<br />

atone bound—A substantial stone poaf sef<br />

into the ground with ffs top approximatafy flush<br />

with the ground surface 10 mark amuratafy end<br />

permanently tha imporfent oemera of a land<br />

survey.<br />

●top numbara-see ralatlve ●perture,<br />

stop—Sac aperture atop.<br />

atorege tuba dlspfay—A CRT dkpley on<br />

which an image @n be storad on Ihe acrcan fer<br />

award minutes or longer with a singfa peas of<br />

the ekrctmn beam.<br />

●trelght Ilne grsver-A variatiin of the rigid<br />

tripod graver so designed that the scribing point,<br />

the vertical vane, and ena aupperting leg are aU


,..<br />

diradj in tine; used with a straightedge fer<br />

Sclibng brig, straight IiiUs.<br />

etretegk map+JCS) A map of medium<br />

-b, Ot wdw, - for pfrltlti~ d<br />

eparsfiis, including the mwaman!,<br />

carrcenfration, arrf at@y c4 trocfxs. Sea also<br />

map.<br />

strataglc plannlng modal-Small-ecale<br />

terrain models dapictiig only ths general<br />

chsr~er d tha kmairr and features of<br />

cmmidarable pmrnfnenca. They ganarafly<br />

etiraoa continental areas, countries, eztenaive<br />

fsnd mass arasa, er prindpsl tind mssaas and<br />

are most fraquantly uaad in high echelon<br />

plsnning acfiviiiea.<br />

stratoaphor~.f(X) The layer of the<br />

almosphore abwa the Wrposphera in whiih the<br />

change of temperature with height is relatively<br />

small. Sae also atmosphere.<br />

stream gaging ●t.stlon-A point along e<br />

strasm at which periodic msasurenrents of<br />

vekcii or discharge are rnsde, and at which<br />

daity er continuous raoxcfs of the stege of<br />

heiaht of Ihe water surface above a rsiven<br />

dstum is obtained.<br />

stra ngth of figure+ triangulation) The<br />

~mparaltie Pr=ision of computed lengths in a<br />

Inangulation net ES determined by the size of<br />

the englas, the numtwrr d cmrdiikms 10 be<br />

sslidisd, and the distribufien of bssa lines and<br />

points of had posiiion. Strength of f~ure in<br />

hiangulation is not based on an absolute scale<br />

but rather is an espr-n of relstiie strength.<br />

Also sppikable 10 ths indvidusl gaemetnc<br />

f~uras within a given net.<br />

stretching apparatus—See tape<br />

stretcher.<br />

●trldlng lwef-A spirit level so mounted that it<br />

can be pieced aluve and parallel wiih ha<br />

horizontal axis of a surveying or satmnomic<br />

instrument, and se supporkl thst il csn be<br />

used 10 measure the inclination of the horizontal<br />

szis to the pfsne of the horizon.<br />

strip ad]uatm@nt—Stmiiar to e bbck<br />

adjustment, bti Iimksf to e single strip ef<br />

photographs.<br />

strip coordlnatea-The crrordhales of any<br />

point in a atrip. whether on lha ground or<br />

sctuslly on air ststion, rafarrad to the origin arrd<br />

MI L-HDBK-850<br />

245<br />

cures of he txrcvdinale system of the first<br />

wedsp.<br />

●frfp fikn-A Phofogrsphb fdm in #ih tha<br />

emtdsion rnadmma can be rarrrwad from its<br />

tenrperery bara after exposure and pmceasirrg<br />

the marrbrrme is lhsrr fransfarrad to a rraw<br />

base. Pr’klc@slty used in corraclion work Afso<br />

called stripping fflm.<br />

strip mosraic-A ntoadc wnaisfing ol one strip<br />

of aerisl photographs taken on e single fligM.<br />

strip plot-(JCS) A port”orr of a map or werfay<br />

on which a nurrbar of photogra@a teken ebng<br />

a flight line is ddinested without defining the<br />

outlines cJ irdividusl prints.<br />

atrlp pradktlon-A single hesdmg pradiition<br />

intanded to convey the genard nsture and<br />

pettem of rsdar returns conlinuouafy along a<br />

spacifii flight path.<br />

strip redlal plot—See strip radkl<br />

triangulation.<br />

strip rodlel trianguletlorr-A direct rad!el<br />

triangulation in whch the photogmphs are ,.<br />

plotted in flight strips withoui reference 10<br />

ground control and the strips are later adjusted<br />

together end 10 Ilw ground cosrtrd. Aise ,called<br />

strip radial plot.<br />

strip width-The everage dimension,<br />

measured normel 10 the flight line, et a series ef<br />

neet medels in a flight strip. St@ width is<br />

generslly mnsidered es equal to width between<br />

flights.<br />

strlpplng fllnt-See strip film.<br />

strlppkrg—The cutting, attachment. and other<br />

operations for assembling cut film sections to<br />

preduce a flat.<br />

strip—See flight atrlp.<br />

Structured Quary Language (SOL)-A<br />

user-friendly, non-procedural dsta fsnguage<br />

which is a slendard for dsla msnipulstien in<br />

relational database rnsnagement systems.<br />

etub trevorao-Sae opur trwerae.<br />

style. sheet-A graphic gu”@e for the format<br />

and portrayal of grid and marginsl information.<br />

Alse called mock-up.


subaqueous rocontmlssanco sunmy—A<br />

hydrugrapfris survey which is a rapklly executed<br />

prelknirmry euvq of a rag’km to pruvti<br />

edvenca information 10- immsdiite military<br />

needs. Nerrnetfy made at arna~ ac@e, kf is<br />

usually rmf confrdled by Iriangulelkxr, and may<br />

be little more than a sketch with onty a few<br />

crifii soundings shown<br />

subaqueous running survey— A<br />

hydrography survey of an nxpbmlcsy nature<br />

afortg an unknown or hostile coast made from<br />

shiird to deharrnins the general form of the<br />

coast and the nsture of the ares.<br />

subrwtral point—Sea subatallsr point.<br />

●ubdlvhkm ●urvay-A type d bnd euway in<br />

Whkh ths bOSl boundsrias of an area are<br />

bcatd arxf i-to area is dwided into parcels ef<br />

bfs, sfrasfs, right-ef-way, and other eccassorias<br />

All necaSaely comem or dividhg lines are<br />

merksd or rnonumented,<br />

siubgravffy-A ccmdifion in whch the resuftant<br />

ambient acceleration is between zero end one<br />

9.<br />

sublunar point—The geographical position of<br />

the Moon. That point of the Eeflh at which the<br />

Moon is in the zenith al a 6wcified time. Sea<br />

also Subaatelllta point.<br />

submarine rsflaf-Vrmiations in elevalion of<br />

the ocasn fbor, or their mpresentatkm by da@h<br />

curves, tints, or soundings.<br />

subordlnata station— 1. One of the places<br />

for wlich tide or tidal currant predictions are<br />

defarminad by a@ying a correction to the<br />

predktions of a reference station. 2. A tide er<br />

tidal currant station at which a shorf ~ria~ of<br />

observations has bean med., whkh are<br />

raducd by cemparfeon with simuttanaous<br />

obaarvatiorrc at a reference station.<br />

subsatellfte point-The point al which a line<br />

from the sstelliia perpandkular to the elfiieoid<br />

intersects the surfeca of the Earih. Sea else<br />

sublunar point.<br />

subaidfery station-A station esfabfiahed to<br />

overcome some bcsl obstacle to the pregrass<br />

of a survey, and ncd to determine position data<br />

for the sfat?on point. The term subsidiary etetion<br />

is usualfy a#ied to A-stations of a traverse<br />

suway. Subeidisry statiena usually are<br />

MIL-HDBK-850<br />

246<br />

ter’rporary in cfwader and nor parmanenfty<br />

msrfwxi ff serving the ackfiiioml purpose of<br />

SU~IS9 COntrd for a Iocaf survey, such station<br />

NY b. Pemsananity marked and ii is hers ●<br />

.s~plementary statbn.<br />

subsolar point-The geogrephid poehbn of<br />

the Sun, Tlwt point on the Earth at which the<br />

Sun is in tha zaniih at a apecifii time. See afao<br />

subatallar point.<br />

●ubatalfar point—llwr geographal fmsition<br />

cd a star. TM point on the Earth at which the<br />

s7sr is In the zsnilh at a specfkt lime. Also<br />

rolled ●ubastrsl point. See also ●ubaolar<br />

point.<br />

subatltuta cantar+l poinl whiih, because of<br />

its ease of idanlifiition on ovarb@ng<br />

photographs, is used insraad of the principal<br />

point as a radial center.<br />

subourfaca float+ hdbw cylindar, with ita<br />

axis held verlicfd, at a constant depth by the<br />

buoyant effect of an indicating surface float:<br />

usad to determine current velodtiss in streams<br />

or chcnnels having a relatively uniform depth.<br />

-. ,..<br />

rtubtenco bsr travorce-A traverse method<br />

in which course Iengrhs ere measured by usc of<br />

a subtenae bar.<br />

aubtanse bar—A horizontally hefd bar of<br />

pracise~ datemrinad length, used to measure<br />

distance-s by observing the angla it subtends at<br />

the distance to be measured.<br />

aubtanao baa. trevare*A trsvame<br />

mathed in which distancea are dat amsined by<br />

precisely measuring, at one end of the course,<br />

the angle subfandad by a precisely measured<br />

baa. at tha other and of the wursa end<br />

approximately normal to if.<br />

subtonse method-A procedure by tiksh<br />

distance rnsasuremsnts are obteinsd by USe of<br />

a subferuw bsr.<br />

aubtractlng tape-A calibrated survayots<br />

tape with ths first foc4 (or meter) at each end<br />

graduated in tenths w hundredths Also called<br />

cut taps. See also adding tape.<br />

Summary of Corrsctlone-A aummsry of<br />

outstanding notices affecting all nautical charts<br />

and publications. This information is also<br />

accessible on the Navigation Information<br />

Network (NAVINFON~,


,,’<br />

,’:<br />

,., ..,,+;,.,<br />

●ummor soletlce-1. That point on the<br />

acl@ii OcCu@ad by the sun al mimunr<br />

northerty declination. Also cafled first point of<br />

Carwmr, 2. Thai instrmf at wtiiih the Sun<br />

reaches the point of maximum ndwty<br />

dadiition, abut June 21.<br />

sun synchronous-An Esrffr ~telljfe OWd jn<br />

which the otbhal pksne is near polar and the<br />

eftitude euch that fha sateffiue pasaae over all<br />

places on Earth heving the same Ietifts% twice<br />

dAfy at the earns local time.<br />

Sun-zenith distance-The angle between<br />

the zerrtih and the sun’8 disk<br />

Sun—The luminous celesfiel body at the center<br />

of lhe solar aysfam, around which the planets,<br />

planetoids. and cemefs revofve. It is an average<br />

star. See also apparent sun; dynamlcat<br />

maen sun; fletltlous sun.<br />

supOrfeatura--Several feature components<br />

having the same, or similar, attribution that are<br />

jeined together to create cme feature. An<br />

example of a supsrfeature muld be e raiiread<br />

cyatem consistkig of all the railroad backs,<br />

spurn, sidings, temninats, bridges, and culvatie<br />

withh that system.<br />

superior conjunction—The conjunction of a<br />

planet and the Sun when Ihe Sun is betwean<br />

the Earth and the other plsnet.<br />

superior planate-The planets wiih orbiis<br />

larger then thst of the Earth; Mare, Jupiter,<br />

Saturn, Uranus, Neptune, and Pluto.<br />

superior transit---see upper trarrslt.<br />

superwlde-angle lone-A lens having an<br />

angle of coverage gresler than 100”. A lams<br />

wtmee focal Isntjh is epproximatefy lees then<br />

one-half the dwgersal of the forrrmt. Abe callsd<br />

ultrewide-angl.s Ions.<br />

●upplomsrtrtal control point-A<br />

pfremimege @rt for whiih an elevation or a<br />

horizontal position, or both, is to be, or hes been<br />

determined. See elsa control point.<br />

supplemental control-Points estabtisfrad<br />

b Wbdhete suiveys, to relate aerial<br />

pL tographs used in mepping with the system<br />

of gecdetic mntrol. The points must be<br />

positively phetoidentified, that is, the peints on<br />

MIL-HDBK-850<br />

247<br />

th ground must be poaitivefy rmmlefad wlh<br />

their imeges w the photographs.<br />

supplemental ●levatlorr~ point whose<br />

vertical pocifiin hes bean determined by<br />

photograntmetric metfreds and is intended for<br />

use in the c4antafion of other photographs. Alae<br />

callad vertical pass point.<br />

supplem~ntal photography- Noncarmgrriphk<br />

aerial and ferreatriel photography that<br />

isused to erhanca qmcifii charscteristii of<br />

~P~9 and cfrerfing photegraphii pmducfs.<br />

Primarity, supplemental photography is *ainsd<br />

with a r=ormakaance camera using a relatively<br />

long fecal length 10 pmvkie graater imsge detail<br />

then is evailatrie in photographs ebfainad with<br />

mapping cameras.<br />

supplemsmtsl plat—A ptal prepared entirely<br />

frem effica rmords designed to shew a ravked<br />

subdivision of one or more aectkrns without<br />

change in the section boundaries and wkhout<br />

other rrmdfiitiorr of the subsisting raoord.<br />

supplemmrtal posltloti point whose<br />

horizontal position has been determined by<br />

ptmtogrsmmetrk mafhcds and is inlended for . ... - . ~..:<br />

use h the cwismlalion of other photographs. Also<br />

called horizontal pass point.<br />

aupplemerrtaf poets for survey<br />

monuments—See Identlficatlon posts.<br />

Bupplomental station—Those ststiona<br />

asteblished only for eupplememal varfical<br />

cmtrol. They nmrnally are not permanenl~<br />

marked (some are merely phelo”klerrfifiad) and<br />

accuracy doea net lmva to be of the same order<br />

as the horizontal control to which it is tisd. Also<br />

called vertical-angla station.<br />

aupplemantsry bench mark—See<br />

temporary bench mark.<br />

supplementary contour—A contour line<br />

between intermediate contour lines to increase<br />

the topographic expraaaien of an area, usually<br />

in araas of extremefy low relief. Alse callsd<br />

euzlllary contour.<br />

supplementary lnstrrsctlons-New<br />

information, mr.srrdments, or changes to<br />

specifications or compilation inafmctiens<br />

affecting the production d a specific map or<br />

chart, or a swies of maps or chstts.<br />

cuppleman!ary station—An auxiliary survey


I<br />

*tbn, Oarabliahsd to increasethe rrurrtrerof<br />

oontrol stations in a givan area, or to placa a<br />

~afbn in a desired boofbn Mare If k<br />

U1’PMCtMe u un~ to @abtiah a<br />

princ@l StaIbn. s~kmentsry Stsibna are<br />

perrnenerSiy marked, and are earabliihad with<br />

an accumwy and Pm&ion somewhat bwer than<br />

is required for a principal statii, sirwa they do<br />

not serve as bases from whiih rmtensive<br />

surveys are nm. Also called secondary<br />

station.<br />

●urfaco ●nomalloa—lrregularhias at the<br />

Earttr’e surface, in the weathering zone, er in<br />

near surface beds wfrbh interfere with<br />

geophyaicsl maasuremants.<br />

surfaco chart-See weather map.<br />

surface corractlOns-Corrections of<br />

geophysical measurements for surface<br />

enomefies ard ground elevations.<br />

surface float—A device, spacialfy designed or<br />

improved, used in hydrogrephic surveys to<br />

determins surfece movement of e sfmsm.<br />

surface-A level of spstiel massumment Y . .<br />

referring to a thrsa~lmenzionsl defirmd space,<br />

e.g. contours, izolirras, bsthymatry, etc.<br />

aurprlnt—See overprint, defin~lon 1.<br />

eurvey coordirretes-See recteng ul.rrr<br />

space coordlrmtea.<br />

survey nat—1. (horizontal control) Arcs of<br />

triangufat”bn, sowrefimes with lines of traverse,<br />

connected 10 form a system of beps or circuits<br />

exietilng over an area. Also callsd horizontal<br />

control survey net: travereo ne~<br />

triangulation net. See alse trlmngul=tlon<br />

system: trilnteretlon not. 2. (vertical<br />

cmnlro~ Lines of spirit Iavefing ccmnacfad to form<br />

a system of *s or circuits extending over an<br />

area. Also called control not; framework of<br />

control; level ne~ nat. See 6[s0 ●r.a<br />

trlengrrlation; U.S. control aurvoy nets.<br />

●urvoy photography—See mepping<br />

photography.<br />

survey ●lgnal-A natural or arfifmiaf object or<br />

sfrrm!ure whose hori.zontef and aomafimes<br />

verf’kal position is cbtairred by surveying<br />

methods. Signals ara given special designations<br />

accerding to the kind of survey in wfrich Ihay em<br />

determined, or which they -y tater aawa.<br />

MIL-HDBK-B50<br />

248<br />

●urmy t,oww-A ekuctura dwaii tor rapid<br />

mmdmdon and removal to raise the survey<br />

instrumerS and observer ekova tiruct”m<br />

such as trees end buildings to permit a lme-ofsight<br />

as required in higher order triangulation,<br />

triletsration, or treversa. See also Bllby steel<br />

towor.<br />

survaylng eccaeeorlae-Thoee suweying<br />

devices wtich assist in making measurements<br />

with e aurveyirrg instrument.<br />

●unreylng dtlmater~n aneroid bammater<br />

with a dief gmduated to read feat or matars of<br />

affiiude, used to determine approximate<br />

diiarancas in alevat”kmrbafwean points.<br />

surveying cemer~ee mapping<br />

camera.<br />

aurvoylng lnatrumanta—Those surveying<br />

devices with vhich masaurements are made.<br />

See also electronic dlatancrr-maasuring<br />

equipment: Iavellng Instrument:<br />

tachometer: theodollte; tranalt.<br />

aunreykrg aeztnnt-A sextant intended<br />

primerity for use in hydmgrsphii surveying. Also<br />

called hyrfrographlc eestent. See alse<br />

marina sextent.<br />

Surveyor”a errow—Ses pin.<br />

$uWOYOr’a chalrr-See Gunter’a cheln.<br />

survey-l. The act or oparetien d making<br />

measurement for determining the relative<br />

positions of points on, above. or beneath the<br />

Eanh’s surtaca. 2, The re.sulta of such<br />

opomtions. 3. An organ.uation for making<br />

eurveya. Sea also eerlal ●urvoy; Airborne<br />

Control system; alrborno .Iectronlc<br />

survey control; ●rea survey; metronomic<br />

surveying; boundary ●urvey; ced-etral<br />

eurvey; city eurvey; compeee ●unrey;<br />

control ●urvey; controt ●urvey<br />

clenalflcatlon; dependent reeunroy;<br />

electronic survey; ●nglnmerlng survey;<br />

exploreto~ survey; field InspectIon;<br />

flrat-order work; gaodatlc survay;<br />

gaoalactric survey; gaographlc ●urvoy;<br />

geologic aurvay; gravimetrlc ●urvay;<br />

ground aurvay; hydrographlc ●uwey;<br />

lndependant roeurvey; Inventory ●urvoy;<br />

land survey: location survey: magnatlo<br />

●urvey: magnetometer survey: meteeand-bounds<br />

survay; mlna aurvay;


i<br />

mlnoml survey: ocomtographlc survey;<br />

photogrsmmotric survey; photogmphlc<br />

●wvay; plane survey; prsillmlrmry<br />

survmy: reconnaissance ●srrv.y; rectangular<br />

●srvoys; raxurvey; routm survey;<br />

eslelllto ●mveylng; second-order work;<br />

standard survey; subaqueous reconnalssanco<br />

survey; subaqueous running<br />

survey; subdlvlslon survey; third-order<br />

work topo-graphic survey: town-sltc<br />

survey; transit-and-stadia survey;<br />

trilinsar surveying.<br />

SWATH survey-see multlbeam survey.<br />

See also Small Wetted Area Twin Hull.<br />

sweep bsr-A heavy section of skmf rail<br />

SUsfMndad et e pradeteminsd depth by two<br />

vefikal cables and lowed by a vsss.sl for precise<br />

determination of navigation obstructions during<br />

a hydrographic survey.<br />

srwlng offset-The perpendicular dblanca<br />

frem a point to a transit fine found by holding<br />

the zero point of e tape at the givan point and<br />

awinging the tape in en erc until the minimum<br />

(horizenlal) distance is obtained,<br />

swing-swing method—A technique for<br />

clearing y-parallax during relative orientation by<br />

SPpfying identid swing (or ~motion) to both<br />

projectors of a pair at the =me time, Thff<br />

methcd has the advantage of affecting ypsrsllax<br />

cmmcfion withoul the use of<br />

Irensla!ional motions.<br />

ewlng-1. The rotalion of a photograph in its<br />

OVM plane abeuf ifa camera esis. 2. On<br />

trimslrogren obfiques, the angle between the<br />

principal fine and the y-srris, or ths angle<br />

bshvaen the isomstric parallel and the x-sxia.<br />

Sea al= rolatlve swing. 3. Tha angfa et the<br />

principal point of a photo measured clockwise<br />

horn ths posifiva ~axis to the principal Iina at<br />

the nadir poinl. 4. (triangutalion) See<br />

sccentrlc roductlon.<br />

SWIVSI graver—A scribing instmment with a<br />

swkal macfw+am that psrmits chsngss in<br />

dirsction of scribing.<br />

●ymbollzatlon-The method of portraying<br />

topographic faatures onto a rnsnuscrip!. The<br />

oymbols used on the msnuacript are either a<br />

ooint (dot). a time. or an area (a defimifina fine<br />

cbsing @n ifseif).<br />

●ymbollzed graphic data (SGD)—A data<br />

MIL-HDBK-850<br />

249<br />

eat wlriih contains affrfbufkrn for gmphfc output.<br />

Dale rrrsy Include eyrrbohiion @ions such<br />

as point, ha, sma, psffarn, orienlsf”b+s, oofor<br />

(hue, value, lone, and rntenshy), siza, stwpa,<br />

and texture.<br />

symbof-A dsgram, design, fetter, chsrsder,<br />

or abbreviation placed on maps, charts, and<br />

other graph= Wl&h by mrwanfiorr, usage, or<br />

mferenca to a @and is undersfcuf to Sand for<br />

or raprasati a epadfii chsrsderisfic or feature.<br />

synchronous satelllts-An Earth satellite<br />

moving aadwsrd in an equatorial, ckculsr orbii<br />

%’&R’3’#EEiR%f2PLE$&’%21<br />

to (synchronous with) ths mfaliorml parbd d the<br />

Esrlh. Such a sateffiie will remain fixed over .s<br />

point on the Eerfhs Equator. Ab called fixad<br />

sstalllte; 24-hour sstelllte. Sea also<br />

atationaW orbit.<br />

synodic period-The intarval of time bstwaan<br />

any planatafy configuration of a celestial body,<br />

with raepacf 10 the Sun, and the next successive<br />

same configuration of that body, as from infarior<br />

injunction to inferior conjunctkm.<br />

,. ,..<br />

oynodlcal month—The eversge period of<br />

revolution of the Moon ebouf the Earth with<br />

respsct to the Sum approximately 29 1/2 days.<br />

Also csflad lunar month; funstion.<br />

synoptic charf-See weather map.<br />

aynthatic aparture radar (SAR)-See<br />

Radar, Synthetic Aparfure (SAR).<br />

Syatam 9-A geographic information system<br />

with a feature orianlad data base and<br />

mntinuous mapping. Devebped by<br />

Compufervision.<br />

ayatem modsf-A representation of the<br />

information types, dkect’bns of flow, production<br />

sfegas, and user imetiaces for a system.<br />

syatam of aatronomfc constants—A n<br />

interrelafad group et vafuae constituting a modal<br />

of the Eatlh and the motions which togather<br />

with the theory of ce!estisf mechanics serves for<br />

the calculation of apharnarides.<br />

sysstamatlc error—An error thsf occurs with<br />

the same sign, end often with s eimifsr<br />

mfsgnffude, in a number of consecutive or<br />

otharwise related obsorvatiorts. For axarr@a,<br />

hen a base is meaeurad with e WTOngty


’<br />

1<br />

I<br />

calibrated tspa, there till be systematicemors.<br />

In addiiion, mndom e8rora will occw. flepetitiin<br />

Cbeafirrle ornothmp toreducsthaioaff=t d<br />

eydeimt~ errors, wiriih ere a rnosi wxtar?ireble<br />

feeture d any aet of 0&ww4iona. Much c4 the<br />

are in rmekhg obaervstiina ia diredsd toward<br />

eliminating or correcting systenwdic errors. Also<br />

called regular error. Ses alao ●ccumuletlvo<br />

●rror.<br />

www-A r=inl of f.hs otifl of a pknti w<br />

aateliiie M which it is in injunction or<br />

I c$mxitiin. The term ie used chieftv in<br />

tinrraction with the Moon, when it-refers to tha<br />

points occupied by the Mum at new and full<br />

phaaa. Sea alao equlnoctlal colura;<br />

●olailtlal co)ure.<br />

MIL-HDBK-850<br />

., .,., .,.- , , ,,


Tsbb of mmldlonal part*A table listing<br />

lengths c1 the maridbn fmm the Eqimtor to ihe<br />

Varbus panefa d Iatauda b=aaaad in ths<br />

p~~”~ wird to show ksngthe abng the<br />

perallels equal to the corresponding length<br />

along the Equetor.<br />

Tabufar data-Date in row rsrd oolumn format.<br />

See also ralatlorml data bass.<br />

Tachymotar (tachoometor or<br />

tachomatc@-A surveying Instrument<br />

designed for use in the mpid determination of<br />

dstanca, direction, and dfiersnce of alsvatkrn<br />

from a atngfa obaawaffon. There era aaverel<br />

forms of Iheae instruments that may be classed<br />

as hchymatars: (1) An instrument in whiih the<br />

baas line fer distance determimtiorr ie an<br />

integral patt of the imtrumsnt, The term<br />

tachymotor is ususlty epplied to this group. (2)<br />

An inafrument equipped with stedia wires or<br />

gredienfer, the bsw for dstence determination<br />

being a graduated rod held at the distan! point.<br />

See EIlsa autoroduclng techymeter.<br />

Tachometry (techomotW)-A surveying<br />

mstfd uaad to quicldy determine dstance,<br />

direction, end reletive ekrvetim of e point with<br />

respect to the “matrutimrtt staiien by a single<br />

observation. An exemple of techymatry in the<br />

United States (where the term is less familiir) is<br />

the stadia method.<br />

Tactical Pllotage Chart (TPC)-A<br />

1:500,000 scale, coerdmted eerfes of<br />

muttiilomd charts ulii ara produced in<br />

selected areas of irrtersst. Dasiranad to sat”kfy<br />

visuel and radar rwigatbn of Hgh speed<br />

tectical aircraft operating at low ettttude. Also<br />

used for detailed preflight planning and mission<br />

ansfysls.<br />

Tactical Termln Anatysla Data Bsss<br />

(lTADBkA set of transparent ovarlays keyed<br />

to 1:50,000 Tacticel Line Maps TLMs)<br />

portraying netursl end culturel feeturee of<br />

miliiery dgnifk=snce. Ths date trsse consists of<br />

overlsys and wppertlng dete for surfece<br />

configuration (s*), surtece meterists (sole),<br />

vegetation, surfece drsinege, trenaporfetion,<br />

ard obstedea. TTAOBs prwvida larmin and<br />

men-made lnformafien to a~pert the<br />

gsnemtion of e variety of field user produced<br />

synthesized produck to include Linsa of<br />

MIL-HDBK-B50<br />

T<br />

251<br />

Communication, Cross-Cwntry Movement, and<br />

tier & Concaaknent.<br />

Tactical Tumln Data (lTD~The basic<br />

d~itaf oparatbnel termin deta set -ing<br />

ftiura lend conbet. lTD All be a value addad<br />

daWbaaa aifkowfrrgfor the erMii and @efe<br />

of dete by the user. Featume and attributes are<br />

mdad usin~ calsgorias mnfained in the Feature<br />

Attribute Cod@ System. 1111 will anteirt<br />

contents & lTADB thematic ovarfaye, as WBll as<br />

tralsckd features fmrn TLMs and C@rrkret<br />

Charla. Sea -k Tmctlcal Tarraln Atmlyela<br />

Data Ease.<br />

tecticd map-(JCS) A large-seek rmp used<br />

for tact’kal end administrative purposes. Sss<br />

elw map.<br />

tactical planning model-fAediIm- or lergescale<br />

rrmdals provking conaJdarabls de!ailad<br />

lerrsin informsbn; generelly used for planning<br />

OPemUOnS of e fecticel neture.<br />

tsn al!—See chedow factor.<br />

tengont conical map projsctlon—See<br />

conic msp pro~nctlon.<br />

tangent dlatanca-The distance from the<br />

point of intersection (vertax) of e curve to its<br />

point of tengency or paint d curveture.<br />

tengent plane grid ●ystom-(engineer<br />

surveying) A grid eysfem in e tengenf plens with<br />

origin at the point of tangency. Ueuelfy Ihe origin<br />

is designated 10,000 N end 10,000 E, or some<br />

aimilsr amounts, to keep 811ooerdhstes poaitiie.<br />

This system never extends for eny greet<br />

dialanca, See also plane rectangular<br />

coordlnetos.<br />

tangent pleno-A plane that touches a<br />

curfed surface 01 double curvature at one end<br />

onty one point or that touches e curved surfsca<br />

of eingle curveture abng one or more parsltcd<br />

straight tines which are elements of the surface,<br />

wtihouf intersding the surface. In geodetic<br />

work, a plane tangent to the spheroid et any<br />

point is paqwndiiulm to the normel et thet<br />

point.<br />

tangent to aplml (TS)--The paint et the end<br />

of a tangant end the treghning et e spiral.


tengsntld distortion-Linear displacement<br />

of irmga points in a draction nwrnsl b radial<br />

Ii fiorrr the car-tar of rlra f-ii.<br />

tangent—(surveying) 1. That part of a traverse<br />

or alignment incfudad between the point of<br />

tangency cd one curve and the point of<br />

curvature d the nest curfe. 2. A great circle line<br />

tangent to e peraflel et Iafiiude at a tonmsh~<br />

mmer. 3. Sxnafirnaa qibd to e bng straight<br />

Iii of n wavame, as@aUy on a mute survey,<br />

whether or nd the Ierrrini e! the Line are points<br />

of curve.<br />

tape corractlOna-Quantifies appfied to a<br />

fapsd distance fo efimkte or reduce ermra due<br />

to the physical rmndiiion of the Iape and to the<br />

my in wfrich if is used. Sea also sligrtmartt<br />

correction; grade correction; Iangth<br />

carroctlon; sag correction; temperature<br />

correction, definition 3; tendon correction.<br />

tape gaga-A dav”ka consisting of e tagged or<br />

indes~ ehein, t-, or other line used for<br />

maasuremsnt or testing. Gege heighf or<br />

measurement is read on a graduated staff or<br />

index. Also called ctmln gaga.<br />

tape rod-A rod consisting of e freme with<br />

rollers al both arsis over which an endless,<br />

graduated metal tape rnovas. It is designed to<br />

pemt direct readings by the instrurnant man,<br />

efiminsting all addiiion and subtraction functions<br />

required by o!har fypaa of rod readings. Atao<br />

called ●utomsitlc rod.<br />

tape stretcher-A mechanical device titch<br />

fadfiiama holdlng a tape at a prescribed tension<br />

and in e prescribed poakion. Alae called<br />

●tretchlng ■pparatus.<br />

tapa therrtsomatar-A precision thermometer<br />

fflad in a ~ially designed case to clip cm and<br />

against e metal tape in order to daterrnina<br />

temperature corracfiens for prackkm bee or<br />

Iraveme tape measurements.<br />

tapa-(surveyirrg) A ribbon of steal, Inver,<br />

specially made cloth, or other suitable material<br />

on which graduations are placed for the<br />

maaauremenf of lengths or dkrfmroas. Sea also<br />

●dding tape; bass tapa; Inatantanooua<br />

raadlng tapa; hrvar tape; Lovar tape;<br />

piano-wiro tap.; ●ubtractlng tape.<br />

teping ●rrow—See pin.<br />

MIL-HDBK-850<br />

d52<br />

taping buck—Sac taping stool.<br />

taping pin-sea pin.<br />

teplng stMon-The daka marking each<br />

interval (one tape length) ebng a tmversa from<br />

fhe initial pdnf abng mad centerlines end<br />

similar survey operations. Sae also plus<br />

station.<br />

taping atoot—A mataf dcol ua6d fcv precka<br />

taping epamhns. Steob are portable and<br />

provide a stable elevated tebte on which the<br />

pc6ifii et the survay tape ends can be<br />

acarala~ marked, Abo called taping buck.<br />

taphrg—Tfra epereticm of measuring distances<br />

on the ground with a laps or Mm. Formerly fhe<br />

words ehalnlng and taping were used<br />

synonymously, but ha ward taping is now<br />

praferrrd for all surveys escapt tln.aa of the<br />

pllbfii brd 8y6teM. For the hftar, because d<br />

historical and legal reaaom, fhe term chaining<br />

is pref arrest.<br />

tara-An abrupt offset in the grevimater nermal<br />

rearfkig level.<br />

Target Matarlala Program (TMP)-1.A<br />

DeD program aatabhahed for tha production of<br />

all dosurnenm apacifiilty supporting irrstaltalion<br />

target anafysis and cfxsrationel planning<br />

emploment. The DoD overall TMP rrwnagar ia<br />

DIA. 2. Tha producbn programs reapending to<br />

the JCS chsrfer for DMA 10 preduca unique,<br />

oritiil gao-locational inforrnatien su~irrg the<br />

long-range wotidwide requirements of the<br />

unifii and spackd commanda, miihary<br />

departrnants, and allied participants. Vha<br />

program ccmsists of precision poinl tccation<br />

prcducfs -h as the Inataltatkm Referance<br />

Point Qraphic (IRPG), Aim Pc4nf Graphic (APG),<br />

and grid ptxr!~ deployabJa Point Poattioning<br />

Data Saaa (PPDB) in either fdm, video, or diiital<br />

form; carfogmphii Air Target Matariats like tha<br />

AIr Target Ctunt and Jog-Radar and a variety of<br />

olher epacial materiala and services.]<br />

target acqulaltlon-1. (JCS) The delactkrrr,<br />

identif=tien, and Imatiin of a target in<br />

suffiiianf detail to perrnif the effache<br />

arrvioymanl of weapons. See aleo tergot<br />

rmalyele. 2. The prccess of opliceliy,<br />

n-amuslly, machenioatly, or electronically<br />

orienting a tracking system in diraclion at-d<br />

range to bck on a target.


target ●talycla-(JCS) An exeminstian of<br />

potential targets to determine m“fitfay<br />

imPJffarroe, ~ of affask, and waapa~<br />

raquird to cbfein a dsaimd level of dernege w<br />

casualties. See efso target Scqulsftlurr.<br />

target araa survey bsae-(JCS) A base firm<br />

used for the beating et targats or other points<br />

by the interserlion of obsarvdon.s fmrn two<br />

stations Iecaled at qffe .sds of the fine.<br />

tsrgat complex-(JCS) A geographically<br />

integrated sarfea d tsrget concerddons. See<br />

elao target.<br />

target concwrtratlorr-(JCS) A grouping of<br />

gaogrsphisaffy proximete tergets. See also<br />

targe~ targst eOmpl*x.<br />

target dosslera-(JCS) Fi)es of sssembled<br />

terget intelligence about a epecific gaographb<br />

erea.<br />

target folders-(JCS) The folders containing<br />

tsrgtrt intelligence and relatsd materials<br />

prepsred for planning and<br />

egainsl a specific Ierget.<br />

executing<br />

~ -<br />

ect”bn<br />

. . .<br />

target lntelllgoncc-(JCS) Intelligence Wlch<br />

porlrsys and locates the components of a target<br />

or terget cornfiex end irrdksles its vulrrerelility<br />

and relative importance.<br />

tergat Iavollng rOd-A type of Ievaling rod,<br />

~WW a ~~t, which is movsd into positiin<br />

eccordmg to ergrrels gwan by the instrument<br />

men; when the terga! Is bisected by the fiie of<br />

CdiMCtiOtI of the instrument, If is reed end<br />

recorded by the rodmen. See also doubletarget<br />

leveling rod; single-target<br />

levollng rod.<br />

------ --. -.,-, ---- .,-- “.- ------<br />

..r~-a nm. a.nn., ~r-pmm=.--m .mr~w<br />

materials.<br />

target mststfals-(JCS) Grephc, textual,<br />

labuter, or other presentations of target<br />

infeffigerrce, primarily designed to supporl<br />

operations against designated targets by one or<br />

more waapen ayetems, Target materials are<br />

suitable for tmining, pfenrdng, exasuting, and<br />

evaluating such opemtiorre, Also sailed target<br />

material graphlca. See afao Air Terget<br />

Chert.<br />

tsrget posltlonlng datt+The accurate<br />

MI L-HDBK-850<br />

253<br />

hodzontal end vertkal values which dsfine the<br />

bcstion of a tergd or point. Sea also praslaa<br />

Installation position; praclee rsdar<br />

slgniflcsnt Iocstlon.<br />

target eyatem compen*nt+JCS) A set of<br />

targets bbnging to one or mom grotqm of<br />

induafri= end tmsis utilities nsquired fo prcduse<br />

‘P”f pm M Ml and product atx$h se<br />

gezd’~-+damd COMMOditkM, such i6S SViS!iOr)<br />

gasoline.<br />

target sys.twrr+JCS) Afl the targets sSWatad<br />

In a particular geographm ares ard funofionelty<br />

related. See also torgat complox.<br />

target—1. (JCS) A geogmph-1 area,<br />

cOr@ex, or instakedon pfmned for capture or<br />

destrffilion by m“lkm’y forces. 2. An object which<br />

rafbcts a stilcient amount of a radiated signal<br />

to produce an echo sigrml on defection<br />

equipment. 2. The d~tincfive merking or<br />

inatrumentatbn of a ground pdnf to eid in ita<br />

idenlifiiatkm on e photograph. In<br />

photogmmmetry, tergat designees e materiel<br />

msrking so arranged and pfscad on the ground<br />

as 10 iorm e distinctive Ptterrr over a gsadet”c<br />

or other qntrol lmint msrker, on a pmpwty<br />

comer or Ins, or at the pcsifien of an identifying<br />

pokrt above an underground facility or feature. A<br />

target is elso the imega pattern on aarisl<br />

photogmphs of the asruel mark placed on the<br />

ground prior to photogmphy. See also sraa<br />

target; phtpolnt targ*t.<br />

but-wire apparatua-A 100-meter stranded<br />

sounding wire, gmdueted at 25-meter intervala,<br />

used to measure the diafancas balween<br />

oftshora control buoys during a hydrogmphb<br />

survey.<br />

tebmeter--(aurveying) An inetmment for<br />

de!armlning the dMance from ona pofm to<br />

another. some such Inatrurnenta employ a<br />

telaes+e and measure the angle subtended by<br />

a shotl base of known Iangth. See also<br />

●lactronlc tolemetor; t.lomotry.<br />

telemetry-Tha science ot measuring a<br />

quwr!ity or quantities, transmitdng the measured<br />

value to s distant etation, and there Interpreting,<br />

Indbetfng, or recordng the spmntftles measured.<br />

tolescopo levef-A spirff level attached to a<br />

tafesmpa, with ifs uis parallal to the teleesapa<br />

axis.


toleacope-An optiil instrument used se an<br />

akf in viewing or phcrfogmphii d*nt ob@cfs,<br />

parfkwlerfy calaatisl cbjscta. Sea also<br />

●chromatic telescope; ●mctlng<br />

teloeoopo; invorfirrg toieacopa; morldiwt<br />

teloscopo; zmlth toloscopa.<br />

teloacopic ●lldedo-A tsaual deaignstbn for<br />

an instrument ammosad d a telemeunled<br />

err a str~ghtedge ruler, d’rraadwith<br />

a pfenetsble in tepegmphk surveying.<br />

teloscoplng—see transr~ definffion 3.<br />

tellurold-A surface near the temsin being the<br />

bcus of points In whiih the apharupotentisl is<br />

the same es the gaopetenfial of corra~hg<br />

~ints an lhs terrsirt 116distance from the<br />

aphemid is the normal height.<br />

Tollurometor-A trade name for a microwave<br />

d-nce-messuring system in td’kh the velcdy<br />

of a radio wave is used to determine the<br />

d~tense betwen tvm instnrmants operating<br />

affemslety as rrmater stetti (intermgstor) and<br />

rernete station (responder).<br />

tornperature correction-1. (leveling) Thst<br />

correction whti is a@ed to en observed<br />

differe~e Of eiavatbn to ~m~ f~ the e~w<br />

irrtrcducad tin the ternpareture e! whch the<br />

leveling reds ere usad in the field is diierwrt<br />

tmm the te~a~ure et wl’riih they were<br />

standardized. 2. fpandulum) The quantify that<br />

is applied to the peried of vibrstion of e<br />

pendulum to allow for the dfierence in the<br />

Iangfh of the pendulum a! the temperature of<br />

obssmation and fts length at some other<br />

temperature whkh hsa been edopfad for<br />

purposes of standardization or for combining or<br />

cempsring corresponding values. 3. (taping)<br />

Ths quantify spphad to the neminal length of a<br />

tape to ellow for a chsnge in its effective iengfh<br />

due to kts being uaad at a temperature other<br />

Own Ihst for which its standard length is given.<br />

Wmpbst (template)— 1. A pattern or guide,<br />

ususlfy scmatrucfed of psper, plssfic, or metal,<br />

usd 10 ehape, deiimit, w fcxxte an area. 2. A<br />

devh used in radml triangular’krrr to represent<br />

the aerisl photograph; the tempiaf provides a<br />

record of he dimcfkrmi of radiila tsken fmm the<br />

photograph. See also calibration tampiet;<br />

double-nsodol ●temotempl.t; hand<br />

templet; Hayford deflocthr tomplots;<br />

Hayford gravity tompleta; mechanical<br />

tomplet; slotted tempfet: apldor<br />

MIL-HDBK-850<br />

254<br />

templet; steroots+mplsrt.<br />

tempkst crsttar-A machanicel devfce for<br />

punchiig canter holes and slots in Wr@ets.<br />

The abts rue centered on points tmnaferrad<br />

fmm aerial phetegmphs end are rdiil to tfm<br />

center heb. Al= calied aecatoc dot cuttefi<br />

radial sacator.<br />

tempbt laydown-Ths proceaa of<br />

asaarrbling individual sbtfed terrgrfats into a<br />

rsdal control net.<br />

templet method-Any of the various<br />

methods utilized in gmphbal mdial hfangufatien.<br />

templet mtlogmph-(photogrammetty) A<br />

device for dalennining the ml’b in decimafs<br />

betwssn two distances. Ons d~ la that<br />

between the principal pint ❑nd another<br />

designstsd point on the aerisl photograph. The<br />

other is the corresponding distsnce between the<br />

principsl fxrint on a tamplat end the msrked<br />

center of the stud for ths designated point upm<br />

C0@8tiOn of the tenrplet Iaycknsn. The<br />

rshograph ‘Lsdesigned fer a specfic Iemplet<br />

cutter. See also ratlometar.<br />

temporary bench mark (TBM)-A bench<br />

rnsrk al s junction of ~iens of s line ef krvels,<br />

at which no permanent bench rmsrk is<br />

eslabfished. Also called nonmonumented<br />

bench mark: supplementary bench<br />

mark.<br />

tension correction-(taping) The cerraction<br />

sppfied to the nominal iength of e tape to allow<br />

for a chsnge in effestive length due to ils behg<br />

usd at a tarraion othar than that for whwh its<br />

afandmd Iangth is known.<br />

tarabyfe (TB)-A unit of memory representing<br />

214 (1,099,51 1,627,776) bytes. hmmonfy. one<br />

Ierabyte repraaerds one billion byles.<br />

Terrain Analyele Producte (TAP)-<br />

(NATO) A standsrdiiad or norr-stendardued<br />

pnxkt from the Terrain Ansiyais Systam<br />

normalfy presantsd in graphic form for use in<br />

military dackion making,<br />

Toweln Anerlyels System (lAS)- (NATO)<br />

A system to meal military requirements for quick<br />

and comprehensive information on the terrain in<br />

anafog ancVOr digital form. II is a system in<br />

which saiacfed data about lhe tsmsin are<br />

collected and stored in a atwtumd way to


.<br />

I<br />

permit Ihaii flexible expfoiibrr in the provisiin<br />

of Tarrain Anafyeia Products.<br />

Tormlrr Edft StntlordElevation Matrix<br />

Procosslng System (TES/EMPS)--A n<br />

Inlsrgraph wrrktatb! used by DktA to adif<br />

terrain products. Gwea tmfh pten end<br />

perspective views.<br />

Tormln Profllo Racordor (TPR)-A n<br />

elacttmnic instrument that emits a pubad-fypa<br />

radar signal from an aircraff to the EarUt’s<br />

Surface, measuring vertiil distances In odar to<br />

obtain a profile beneath the track of the aimaft.<br />

Alse called Airborne Proffl. R-order. See<br />

aleo Ieur terreln profile recorder.<br />

terrahr enalysle (TA)- (NATO) The precess<br />

of cdlacliig, analyzing and evaluating<br />

W’39mphfc information on Ihe netural and manmade<br />

features of the temein and ifs<br />

inferpretdion in combination with other factors<br />

to provide pradbfive information and etilce<br />

abouf the effecl of the terrain cm mifibwy<br />

operations.<br />

terrnin contour matching (TERCOM)-<br />

The procese which u#ates navigational<br />

guidance systems through correlation with<br />

griddad terrain elevatien data derived from<br />

photogrammetric or large scale certographu<br />

sources. See also tarreln corralatlon.<br />

tcwraln corractioti positive correction used<br />

in conjunction with olher rmrrections in making<br />

gravity redutilons. M fakes into acsunl actual<br />

deviations from level terrain in the wee<br />

eurroundhg e statkm by removing rnaaaas<br />

above ha horixon and fifliig in mesa<br />

dafiiiencles bebw. Alas called topographic<br />

correction.<br />

tormfn correlation-A pmca= used by a<br />

vehicle’s guidance system in evaluating the<br />

elevations of the terrain if is ffyfng ovar and<br />

co~fig it with pmstorsd dqital terrain<br />

elevation dala. See also terrain contour<br />

metchlng.<br />

terreln embose—A model-making technique<br />

for portraying relief on a chart. A photographic<br />

P~ ia used 10 produce the shaded relief<br />

effect from an embossed model.<br />

terrain following-Tha flight rrmde by whch a<br />

vehicfe maintains a apacifii affifude above the<br />

Earth’e eutiace.<br />

MIL-HDBK-850<br />

255<br />

terrain lntelflgence-(JCS) Procaaaed<br />

information on the mifiiary signifiince of natural<br />

and nmn-rnade cfusrecteriaiic-s ot an area.<br />

tarmln modaf-A three-dimensional graphic<br />

mpreaanfation of en eras, showing the<br />

conforrrmtion of the ground, modeled to scale<br />

and uauatly handpainled to depict mefisdcalfy<br />

man-made and natural phyaiGsl fea!uraa. The<br />

vertical ecefa is usuefly eoraggereted, witheuf<br />

severe d@orfion, to _nfuafe the aspacf d<br />

rafief.<br />

terrain protlle photography- Cartographic<br />

photography obtained simuftaneowfy with<br />

posflionai carnam pfrotogmphy and recording of<br />

data ralaiing to profile elevat”mn inf-tion of<br />

the Iarrah abng or near the fpurd track of the<br />

aircraft. The terrain profile recorder k norrnalfy<br />

used as the measuring device.<br />

termln profillng-obtaining en elevation<br />

prdlle of the Earth% terrain alsng or nmr the<br />

ground track of the aircraff by use of a Tarrain<br />

Profile Recorder.<br />

terrain study-(JCS) An analysis and<br />

interpretation d natural and rnenmade, their<br />

effects on military operetiina, and the affect 64<br />

weather and climata on these faatuma.<br />

terrain—An area of ground conaidarad es to<br />

its astent and topography.<br />

terrastrlal camare-A camera designed for<br />

use on the ground. Also called ground<br />

cam. rm.<br />

terrestrial coordlnatas—See geographic<br />

coordlnat-a.<br />

terreetrlal ●quator—See aetronomlc<br />

equator; geodetic aquator.<br />

termatrlrd globeA sphere, en the outer<br />

surface of which by means of<br />

reference fines, ihe faatures of~*~~tic#<br />

the Earth are shown in relative pctaifiens.<br />

terrestrial Ietftude-fatifude on the Earth;<br />

angular distance from the Equator.<br />

terrestrial lon@rda-Longitude on the<br />

Earth; the arc of a pamllel, or the angle al the<br />

pcle, between the prime meti]an and the<br />

meridian of a ~int on the Earth.


torrestrld<br />

natlmm.<br />

tmr.strlal<br />

morldlan.<br />

mqfnotimn-Sea gaornag-<br />

morldlan—See ●stronomic<br />

torrostrhl perturbatlorrs-The largest<br />

grsvitsfiorrsl parfurbslions of artifkial eslatliias<br />

which are caused by the fscf fhst the gravily<br />

fiild ef the Earth is nat s#rarically symmetrical.<br />

terrestrial photogrgmmotry— Photogrsmmatry<br />

utiiiiirrg terrestrial phc40grsphs. Also<br />

called ground photogrammotry.<br />

terrostrlal photognrph-A photograph taken<br />

by a csmers Iomtsd on the ground. Also called<br />

ground photograph.<br />

terrestrial planet—A planet that<br />

a~roximstss ihe Earth in size (Mercury, Venus,<br />

Msrs, and Pluto) end phyaicael makeup.<br />

terrestrial pole-See gsiographlml polo.<br />

terrostrlal refraction—The refraction by the<br />

Earth’s atmmphere of light from a terrestrial<br />

source. The path of fight from a terrestrial eeurca<br />

is usually net far from trorizontat ii pssses<br />

through only the lower strata of the atrnnsphere<br />

and suffers refraction thmugheut its entire<br />

length. See also atmosphrdc refraction;<br />

horizontal refraction; lateral refraction.<br />

tarrostrlal ●pher.-The Earth.<br />

terrestrial triangl-A triangle on the swlsce<br />

of the Earth, aspscislly the navigatkmsl triangle.<br />

tesla-(gaomagnetism) The electromagnetic<br />

unit of rnagnet”c inrtucfkm. 1 tesla = 10-9<br />

nanotaskr. See also geuaa.<br />

Tesselatsid $pharold Modal-lV (1$)-A<br />

mordinsta sysrem whiih dwidas the wrld info 5<br />

Iatilude zones to obtain aqusl spscing.<br />

teeaeral harmonics—The sat of all a#herfcal<br />

harrswn”w thsf are functions of bolh Islituda<br />

❑nd brrgiiude. Secforial harmonics ma a special<br />

subsat of tessersl harmonics.<br />

test charf-Saa raeolving powar targat.<br />

teat rsngm suppoti-DfAA provided gaodatic<br />

surveys for the DoD test and trsining rsnges to<br />

MI L-HDBK-B50<br />

256<br />

SwPOrf weapons aysfarns and weapons<br />

eyatems usars raseamh, dsvaloprnmt, lasting<br />

and avalustbn.<br />

taztura-in a photo image, the frequency of<br />

changa ard smangamenf of tone.<br />

thematic mapper (TM)-A severr~hannel,<br />

prademinsntfy 30 meter instantaneous fiefd of<br />

view (IFOV) multiifnd scanner, deei~ad for<br />

rrmnifciing earth resoumsa. TM is uaad on<br />

board LANDSAT =Iellites.<br />

thamatlc map-Sea topical map.<br />

thematically ssparate-The segregation of<br />

a feature w a fimitad nunbw of features within<br />

a data bsse to highlight ths spatial<br />

chsmcfetistics d a aubrsaf er ha snviromnent,<br />

See also layer.<br />

thoodollte magnetometer—An instrument<br />

usad in rnsgnetic suweys consisting of a<br />

Ihaodeliia and a mgnarometor modified to fti<br />

into a oemmen base, wh(ch parmim tha<br />

determination of tha true rnaridisn and the<br />

magnetic meridian in a single observation,<br />

thaodollte-A precision surveying instrument<br />

consisting ef an alidsde with a Ielascopa. It is<br />

mounted on an accumtefy graduated circla and<br />

is equipped wkh nscassary Iavals and rsading<br />

devices. Somelimes! the alidsde carries a<br />

graduatsd vetiical cm4a. See alsa dne<br />

theodolitsi; dlroctlon Instrumwst<br />

theodollte; gyrotheodollta;<br />

phototheodollte; repaatlrrg theodoflte.<br />

theoretical corner-A term adopfad by the<br />

U.S. Gaelegical Survey to designate fhe turners<br />

on the map for which ne msrks era idantifiad on<br />

the ground. The Imstiens ara determined by<br />

adjustment and are indicated on the map only<br />

by the intersection of ths subdiviskm fines.<br />

theoretical ●rror-A systematic error .arfaing<br />

fmm nstural physical candiikms, beyond the<br />

control of the observer. Sss afse external<br />

●rror.<br />

theoroilcal gravity-The value of gravity<br />

dculetsd for a particular tstifuda according to<br />

an accepted formula. See also formula for<br />

theoratlcaf grevlty.<br />

theory of ●nharmonlc ratio-A theory<br />

principally mrrcemsd with the process-es cd<br />

trensfornmtbn and radifiilion wtmrstry<br />

. ... r.


’<br />

.,. -e . . .<br />

;! 4<br />

,.,<br />

,. .,.<br />

prqectivety refeled figures poaaeas ce~in<br />

metric chsractetistics whii are Invariant under<br />

projection. Also called thaory of cross ratio.<br />

thaory of cross ratl~e theory of<br />

nrrharmonlc retlo.<br />

thormel imagery-(JCS) Imagery produced<br />

by sensing arwt mcotding the thermel energy<br />

emitted or reflected from the objects whmh are<br />

imaged.<br />

thormomatrlc levellrrg-The determination<br />

of elwalbne above sea level from observed<br />

values C4 the boiling point of wafer. A type of<br />

indirect favefing.<br />

thick lens-A term usad in geometrical optics<br />

10 indicata Ihsl the thtinesa of a tans Ls<br />

considered and that afl distances are being<br />

massurad fmm the nodal points instead of tha<br />

lens canter.<br />

thin lana-A term used in geometrical optics to<br />

indicate thet the th~knass ef a lens is ignored<br />

and thet all dstances ere measured from the<br />

Iems centec usad for eppmximate<br />

computations...<br />

thlnnhrg-The process whereby a Ikrasr<br />

feetura is ganeralizsd through ths use of e<br />

series of rules thst reduces the number of data<br />

points while maintaining the bssic shspe of the<br />

feeture.<br />

third-ordar Iavellng-spirit leveling which<br />

does not attain Ihe quality of ~-order<br />

leveling, but doas conform to the current<br />

epacifiitkms fcx third-order Iavefirrg per<br />

“Clsesitiaition Stenderds of Accuracy and<br />

General Spacifiitiorw of Geodetic Cairn]<br />

Surveys.” Recommerdad for most general<br />

vertical control purposes within a fimited eree.<br />

third-order traveree-A survey treverse<br />

which extends between adjusfed positions of<br />

other control sunmys wfkh conform 10 the<br />

current .mecifiifiins for third-order [class I or<br />

class 11)iriangulafii per “Ctseeikeiiin<br />

Sbmdaida of Accurscy and Ganarrzl<br />

Spaciiitiene of Gaodefii Control Surveys.”<br />

ffaoommendad for meat generel horizontal<br />

control purposea within a fimifed area.<br />

Ihlrd-ordsr trlangulatlorr-Formerly known<br />

as terliery thrtgulalin, these survays conform<br />

10 current specifiitiona for Ihird-erder (cfesa I or<br />

class 11)triangulation per “Ckrssifiition<br />

MIL-HDBK-850<br />

257<br />

Stmdatds of Accuracy and General<br />

Spaciiit”m d Geodatii Control Surveys.’<br />

Ractrrnmerdedfor rrmaf ganeral horizurtal<br />

control purposes withn a limited ersa.<br />

third-ordar work—This is Ihe bwesf order d<br />

control surveys fer which monumentafiort b<br />

authorized.<br />

threa ●lgma(30)-The 99.73 percant<br />

wrrfiderrce interval C4 a dkfribution. See afse<br />

standard wror.<br />

thraa-amr proWastor+ full-circle protractor,<br />

equ@ad with three arms, the fiiucfal edgaa<br />

(astarrdad) d whbh peas through the carder of<br />

the circle. Ths middle arm is freed end raatfs 0°<br />

on the graduetsd circle. The other arms ere<br />

rnevsble, and thair pesitions on the circle ere<br />

read with the aid of verniers. The two movsble<br />

arms are equipped with clamps and msy be se!<br />

at any angle with raspd to the fiisd arm, withjn<br />

the limits of the inetmman!. It is used for firrdtrg<br />

a (ship’s) posiiion graphiity when the angles<br />

between three known fried points are available.<br />

Alse celled station pointer.<br />

three-body problem—That problem in<br />

classical Celestiil mechenics whiih Wets the<br />

motion et a small body, usually of negligible<br />

ins=, relative to and under the gravitational<br />

influence of two other finite point messes.<br />

thrsa-dlmanslonel (3-D) date—Volumetric<br />

data representing maesuremerrls in three<br />

dimensions, as angular or linear measures such<br />

as phHembda-kspps or latitude-longitudaalevation.<br />

thrae-point mathod—See raasctlon.<br />

thraa-point problem-Tha determination of<br />

the horizontal poeitiin of e point of observation<br />

fmm data compriakrg two cbsawed horfzorrtel<br />

angles betwean three objects of known position.<br />

The problem k. solved graphtcalfy by fhe use of<br />

a Ihre-ann protector, and anefytikdy by<br />

Irigormmetricel computation. Sea also<br />

resection; trlanglo-of-error method.<br />

lhree-wlra lovellng-A method of Ievefing<br />

applied when the reticle of the level hss three<br />

Iirras. The rod la reed al each of the Ihree fine=s<br />

and the avenzge is used for the final reeuft with<br />

an accuracy as great as it three lines of Iavefs<br />

had been run and the results avereged.<br />

llcks—Sae raglster marks.


tfdal bench mark-A bench mark S* to<br />

reference e tide staff HI a tidal .5tafien and tha<br />

elevation of which is determined with relation to<br />

the local tidal datum.<br />

tidal constltuont—See constituent.<br />

tktal corractlo~A mrrecfion aoolied to<br />

grsvifdioml observations to retie the effect<br />

of Earth t“~s on grsvimetric absarvat”ms.<br />

tidal current chait-A chart showing, by<br />

arrows and numbers, the average direden and<br />

speed of Mel currents at e pwlicular pen of the<br />

currem cycle. A numbsr of such charts, one fer<br />

each hour of the current WCle, usualfy are<br />

published together.<br />

tldel current-The efterneting horizontal<br />

movement of water eaaecialad wilh the rise and<br />

tell of the tide causad by the astronomic tidepmducing<br />

forcas.<br />

tidal datum plana-See tldel datum.<br />

tidal datu~Specific tide levels which era<br />

used as aurtaces ef reference for depth<br />

measuremems in the sea end es a base for the<br />

determination of elevalion on fend. Many<br />

different datums have baen used, perkularly for<br />

leveling operetiens. Also called tidal detum<br />

plane.<br />

tidal day—See lunar day.<br />

tidal varlatlon of gravity-Periodic<br />

deviations fmm normal of the gravity on Earih<br />

and the dkactbn of the plumb fine caused by<br />

the eftractkm of the Mean and the Sun’s mess,<br />

tlda gage-A devke for measuring the height<br />

of tide, It may be simpfy a graduated staff in a<br />

sheffered fecelion wtrare visual ebservetiena can<br />

be made at any desired time; or if may consist<br />

of an elaborate reading instrument mskfng e<br />

centinueus graphic record of tide haight egeinst<br />

time, Such an “instrument is usualfy actuated by<br />

a fled in a pipa communicating wth the see<br />

threugh a small hefe WMch filters out shorter<br />

waves. See elso float gage; nonrecordirtg<br />

gage; portable ●utometlc tide gage:<br />

prossuro gage; self-registering gage;<br />

staff gaga; atettdard automatic tide<br />

gag..<br />

tldo loval—See mean tide Iavel.<br />

MIL-HDBK-850<br />

258<br />

tide ovyr run-A reprintof a c5erl or rruip<br />

nacaasfatd by unusual condiiiens before<br />

extensive revisions can be accompiiied. Also<br />

celled ●morgency run.<br />

tlda station-A pface al whti tide<br />

cbaervetiens ara made. See also prlmaty tide<br />

station; secondary tido ●tatlon.<br />

tlda-producing force(s)-lhe slight kcef<br />

dflerence between the gravitational aftrhcfion of<br />

fww astronem’k bcdies and the centrifugal force<br />

that hofda fhem aIMrf. These forces are wrecffy<br />

equal end eppcdfe at the cerrfer of gravity of<br />

eifhar of the tcdiis, but, since gravtiationel<br />

attredkm is invereetj proportional to the square<br />

of the distance, if varies frcm point 10 peint on<br />

the surtam et the bedies. Therafore,<br />

gravifationsl aftracficrn predominates at the<br />

surface paint nearest to the other body, while<br />

centrifugal repulsion predominates et the<br />

surface point farrhest from the other bedy.<br />

HerWe, Ihere are Iwo regmns wlrere IiOepmducing<br />

forcaa are at a maximum, and<br />

normslfy there are two tides each lunar day end<br />

seler day.<br />

., .,. .= ... 4,.<br />

tldnmark—1. A high wcter mark left by tidal<br />

water. 2. The highest point reached by a h}gh<br />

tide. 3. A mark placed 10 indicate the htghest<br />

point retched by a high tide, or eccseicdfy,<br />

any specified state of tida.<br />

tide-The periodic rise and fall et the surface of<br />

the ecean resufting fmm the grevifational<br />

anraction of tha Moon and Sun acting upon the<br />

rotating Earth. See alse age of diurnal<br />

Inequality; age of parallax Inequality;<br />

age of phase lnaquallty; ●mphldromic<br />

point; amphldramic roglon; ●nnual<br />

Inequality; anomallatic tide cycla;<br />

apogaan tldaa: constituent; constltuant<br />

day; corrected establlehment: cotldal<br />

hour; degenerate ●mphldromlc ●yetem;<br />

diurnal constftuant; diurnaf Inequality;<br />

abb tlda: ●stablishment of tha port;<br />

flood tlda; harmonic constants; height<br />

of the tida; high watar; high water Iino;<br />

higher high wete~ higher high watar<br />

Interval; higher low water; higher low<br />

water Intarval; Indian spring low wate~,<br />

Indian tldo plana; International low<br />

wate~ low water; low water full and<br />

change; low water Ilna; Iowar high<br />

water; lower high water Intarval; Iowar<br />

low wetafi Iowar low watar intarval;<br />

lowest low watar; Iowaet low water


I<br />

1<br />

,. ...>,- .. . . .<br />

sprlng~ lunar day; lunar tldo: Iunltldftl<br />

Interval: mean dhmral hlsh water<br />

Inoquallty; mean diurnal low wwtor<br />

inequality; mean high water; mean high<br />

water springs; moan hlghor high watw<br />

mean higher high water ●prlngw mean<br />

low wstar; msan low watar sprlnga;<br />

M.=n Iowar low water; mean lower low<br />

wstor 8prings; memr range; mean rivar<br />

level; mean awn Iovel; maan tlda Iavel;<br />

nodal Ilns; parallax Inequality; phase<br />

Inequality; sot; somldiurtral constituent;<br />

tidal correction; tidal cutrsnt; tldwnark.<br />

tlo flight-see control ●trfp.<br />

tls point-l. Image points ktentiied on<br />

oblique photographs in the overfep area<br />

batwaen two or more c+csrd drips at<br />

photegrephy. They serve 10 tie the indwiduel<br />

sets of photographs into e single flight uni and<br />

10 tie edjscenl ffiihts into a common network.<br />

2. Paint of cbsure of a survey either on ifseff or<br />

on another sunfey.<br />

tie stripl. (cerfography) An overlay<br />

mnlaining all pfsnimefric and relief festures in<br />

he .srae akmg the edge of a msp or chsrt. It is<br />

used to insure the matching of these feetures<br />

on adjoining sheets. AIs cded metch strip. 2.<br />

(aerisl photography) See control strip.<br />

tlc-in—See tla.<br />

thrr-Any seriss of oontigmus townshps<br />

S.huatSd frS6f and west of each otha~ also<br />

sacfians simifarfy situated wiihm a township.<br />

tie-A survey connection from a paint of known<br />

psifion to a paint whose postion is desired. A<br />

lie is made to determine the positbn of a<br />

aucmlernsntsw ooint wheae Posilion is desird<br />

fo; tipping 6r iefarance puI@ss, or to cbee a<br />

survey on a pmviousfy detarmirred point. To TISin’<br />

is to rmske awh a wnnection. Sea afso tla<br />

point, definition 2.<br />

tiled covaragstA coveraga that hss baen<br />

physimdfy patffioned into smsller covereges.<br />

One or rrwre of these smelfer mveragee, where<br />

all shsre the asme eat of festure cfasses with<br />

the same daffnifbns. Each tile definm an<br />

independent topology.<br />

tlllng echame-The scheme used to define<br />

tile ahapa and size, and unkfua tifa identifibetbn<br />

number.<br />

MIL-HDBK-850<br />

259<br />

ttlt ●@-@CS) The rmgla between the<br />

qticaf asis of an air ssmwa and the vwtical @<br />

the tti of aaposure. Sea also ●ngle of<br />

dopreaalon; tilt.<br />

tltt drcf.-fn a tilted aerial photograph, a arcfe<br />

pesing through the kcrcsnter and having a<br />

diamefar Iyhtg efong the @nc@l fine. WsarI thffi<br />

dantater is drawn to a convenient fiir scale,<br />

then any chord through the lsooarrfer given the<br />

componanf of tiff for that particular direction,<br />

tiftdlapfacement-Oiicernartt rwdml from<br />

the iaocertter of the photograph caused @ the<br />

tilt 04 Ihe photograph.<br />

tiff sfide ryfe-A device wiriih facififates the<br />

determmaMert for aetfings on a frned-bns reclfier<br />

tian carfain tiff factors of an aerial photograph<br />

are known.<br />

tlltlrrg levef-A Ievefing instrument in whbh<br />

Ihe talsscope with its attached bubble !ube can<br />

be Ievefed by e fine screw a! ha eyepiece snd<br />

of the lelesmps indapendanlfy of the verticel<br />

e.sis, lhus avoiding the need for cerefuf Ievahg<br />

of the ir@rument as e whole. Tnis type d Ienrel<br />

was first dasi~ed for precise work, bul the<br />

principle has mms inlo pafrular use for ordinsry<br />

ievels.<br />

Nltlng-lone rectlfler-A CISSS of reclifiem in<br />

which the principsl paint is fried on its esie of<br />

swing, and cennet be diepJsced.<br />

tlft—(JCS) See roll. Also celled ●ngle of tlk.<br />

See also cross tilt; direction of til~ pffch;<br />

relative tilt; x-tilt.<br />

time rfiegram+A diagram in wheh the<br />

cefmfial equstof sppeers as e circle, and<br />

cefeslial meridians end hour aides as rediil<br />

lines; used 10 facifiiele sofutbn of time problems<br />

and others invohfhg ercs of the arfesfiel aqusbr<br />

or angfes at Ihe pots, by indiiing refelians<br />

b@ween varbus quenfities invofved.<br />

Conventiarraffy, the relationships are gfven as<br />

viewed frern a point over the south Pole.<br />

wasfwsrd direction being oourrterobofrwise. Afeo<br />

called diagram on the pfane of the<br />

●quinoctlai. See also diagram on tfra<br />

plana of tha cafastlal meridian.<br />

time dlatsnce-Time required for any object<br />

to h-evef betwaen two given paints 61 a given<br />

rate of speed.


,<br />

,<br />

tlmo gamma curvs-$ae characteristic<br />

curve.<br />

time morldlan-lmy maridiin ued as a<br />

reference for rdeming time, ptikularfy a zone<br />

or afandad maridii.<br />

tlms son. chart-A amalf-acala chart of the<br />

wmrtd designed to show the legal time kept on<br />

land.<br />

tima zona-An araa in e.11parts of wliih the<br />

same tirrw IS kapt. In general, aach zone is 15”<br />

of longitude in w“dh, cantered on a meridian<br />

wtrosa longitude is genaralfy dwisibfe by 15”.<br />

times (X) enfargament-The multiplication<br />

factor bywhich anorigimdie robe&r& in<br />

repmductiin. A two-tit-nag (2X) linear<br />

enfarcremenf of a 4. bv 5-incfr orioinal wmuld be<br />

8 @ ~ O inches. See &lao dlame~or<br />

anlargemont; scale of reproduction.<br />

time-The measurable aspect of duration. See<br />

elso Al time; appnront ●ldaraal time:<br />

aPParOnt aOIW tlma: astrograph moan<br />

tima: .estronomlc tlma; atomic tlma; clvll<br />

the; day; ephemeris time; equation of<br />

tima; Groenwlch apparent time:<br />

Graenwlch lunar. time: Greonwlch mean<br />

tlma; Greonwlch sidereal time;<br />

Greenwich time; local apparent tlma;<br />

Iocel ●atrfmomlc tlmo; local lunar time;<br />

local mean time: focal sidereal tfmo;<br />

10Cal tlma: lunar tlmaa: mean ●lderaal<br />

tlmo; maak solar tfme~ month; “rise Ume;<br />

aldereal time; solar tfme: standard time;<br />

Universal limo; UTO time; UT1 time;<br />

UT2 time; WWV tima; yea~ zone time.<br />

tlmlng corrsctlon-A correcficm a@ied to<br />

the length of a trilaleration measurement to<br />

~-e fm the deby of the radar signal as<br />

if passes through ths ground transponder unit of<br />

an electronic dislanca—maa Wing davilx.<br />

tlnte-Cobr gradat”w uwd on rnapa to<br />

designate depth or height. Sea afso<br />

hypsomatrlc tlntlng.<br />

tipped panoramic dktortion-fn a<br />

panorarmc camera rystem, Ihe displacement of<br />

images of ground points from their expected<br />

vett”kal panoramic positions caused by the<br />

Iip@ng of the scan ask dfhin the vertical plana<br />

of the flight peth. This diaforficm is additive and<br />

modif- again NW image positions of points<br />

MIL-HDBK-850<br />

260<br />

afraedy influanoadby panoram”m dktortkm, aan<br />

Pc6ilional dmtorfibn, and imaga mcliin<br />

compensation dMorrion.<br />

tfp-Saa pftch.<br />

tftla bJock-A space on a nonafandard<br />

graphc, SW51 es e nmsaic, photograph, w plan<br />

dmded to idenfiiition, reference, and scale<br />

information.<br />

tftllng (tftlo lnformatlon+That information<br />

lettered on aerial phrAOgraphc negativas for<br />

identikation purposes. Also, the placing of awh<br />

information on tha nagativas. Afeo called fffm<br />

tltlhrg; negatlvs tltflng.<br />

Tokyo datum-Tkds datum, with its origin in<br />

Tokyo, k dekad in temm of tha Belliisoid.<br />

It also covers Korea and Okinawa.<br />

Note: In the absence of information to confirm<br />

that this datum is identical 10 fha Old Tokyo<br />

Obaarvatoty Datum of 1918, the two datums are<br />

to be considered aaparately.<br />

toleranca-The mazimum allowabla variation<br />

fmm e standad or from qmcffiad conditions.<br />

.-. ,,<br />

tone copy—Thai rnalerisl in whwh tones or<br />

shedas of sohd cobr ap~ar.<br />

tone-(JCS) Each distinguishable shade<br />

variation fmm black 10 whiie on imagery.<br />

topical map-A map designed to porlray a<br />

specLal Swbjwi: e.g., administrative euMivkione,<br />

railroads, teleoommun”bslions, pewer fines,<br />

navigable waterways. Also called speolalaub]ect<br />

map; thematic map.<br />

topoengulator—An instrument usad to<br />

measure vertical angles in the principal plane of<br />

an oblique photograph.<br />

topocantrlc coordfnatea-Coordinates<br />

wlmee origin is on the Earth’e surface as<br />

distinguished from geocentric coordhetes<br />

whose origin is at the canter of the Emth.<br />

topocentrfc equatorial coordlnatea— A<br />

coordinate syslem centered at the obaewets<br />

position on the surface of the Earth whh one<br />

coordinate plane parallel to the Equator and<br />

one axis parallal 10 the north pofsr azis of fhe<br />

Earth.<br />

topocantrlc horizon—See ●pparent


.<br />

horizon.<br />

tOpecwrtrlc-Of meaeuremenfs or<br />

Wordirwfes, raf-d fe the poaMi of W<br />

cbeerver on fhe Earth as the ~m.<br />

Topogrephk Engineerlrtg Contor<br />

(TEC)-A~ Corps of Enginaem fCkrRdOdSS<br />

which wpport the Army% modem waapona and<br />

mrnmend arxfc4mfmf aymemeffnou#r meeamh<br />

and davefcpmarM kI mepphg, charting, Wrreln<br />

aq+j -r mfnofe =Mm. -t<br />

poaifiiirrg, surveying end fend navigation. TEC<br />

atac conducts ~ on arrvironmenfel effects<br />

on milii equipment, davekfae tcp@yz#ii<br />

~ syaenrs, and produces terrain andyeis<br />

prod@e. Forrnady kmwwr es EnghwM<br />

Topogmphk Lebomtorlea.<br />

Topogmphk Map of tho Unfted Stetea-<br />

The r~rrmmnded deafgneflon for the<br />

lopograpbii map of the United States being<br />

WWamd d quadrangle areas in atlas dread<br />

form, chiefly by Ihs U.S. Geokgiil Survey. Thii<br />

map portrays a@ basic inf-ticm about<br />

IW@M, a18+Vafkn, and extant et physical end<br />

cutiural features that are required fer prelimirvary<br />

—mic and er@neering atudks., and fer<br />

i~tin h a ~= fm - ~~~ fOr<br />

- Wm.<br />

topogrephk base film-An aerial<br />

photographic film with e dirnansknaliy stable<br />

bese used prirnar!Jy for rmppirrg.<br />

topographic correction—See terrain<br />

correction.<br />

topographic doflectiorr-lhet @ of tha<br />

defkdkn of the pfuti fine which in caused by<br />

the gmvhefffl pull exerted ~ topography<br />

maasarr. Tepogmphic deflection ~ not the came<br />

as dsffedii c# the pfurrb fine or slefkn emor,<br />

but la the ~atical affd prcduced by the<br />

rasuftanf grevirafiimd pull d the unevenly<br />

I ddrhded<br />

. . ..<br />

Sramn, m<br />

l~~h~<br />

alrow-<br />

.-seas around the<br />

—..—..—, -— A..,<br />

erring rnaae Iar reommc<br />

~Wen=thn. Akc<br />

tho defloctlona.<br />

called Indirect ●ffoct on<br />

topographic ●xprazalowl%e effect<br />

achieved by ehep”mg and spadng contour #nes<br />

sc that f~raphc feefuras can be interpreted<br />

with rreee and fhlii. Gmd aspreesion in<br />

achieved by delincmting the contours in<br />

aFPMfWi.ste relationship to each c4her, wilh due<br />

cmsideretion ghren to the male and mntour<br />

interval of the map. Also called configuration<br />

MIL-HDBK-850<br />

261<br />

of termln. See else topography.<br />

topogmphk feature-See topography,<br />

defiiitikn 1.<br />

topegmphk rnep-(JCS) A nmp which<br />

PmaarM the Vertkat poadikn d ferduree m<br />

mrresumbbforrn aswdtas rheirherfzorwef<br />

posffbns. See eke mep.<br />

topographic plot-Represenlatien, by means<br />

of confcu “mea, of the grooleg~~ ems,<br />

ahowrrlneste r’===@<br />

complletlon, dafinitiin 2.<br />

topography mrnre~ survey whikh has for<br />

/fs major purposes the dalarmbatii of the refiaf<br />

of the surface d the Earth and the focafii of<br />

nmurd and man-rrwfe faduras themen.<br />

topographkel latltude-See goodotlc<br />

Ietltudo.<br />

topogmphy—1. The mnf~uraticrr d the<br />

surfece of the Earth, including its relief, the<br />

positbn of its #reams, roads, dfies, etc. The<br />

Earih’s mtural and physical faatums cxkctivety.<br />

A aingk feature such as a mewksin er valley ia , ..termed<br />

e topographic kature. Tepogmphy<br />

is su~ded imo @7=w=@Y (~ r~i<br />

features , Fr@mgraphy (the water and dreinaga<br />

features 1.<br />

cuffure (mm-made features). end<br />

vegetation. 2. l%a science et daihmation d<br />

natural end men-made features of a place or<br />

regkn mpmiafty in a way to show tfrelr peaitkns<br />

and elevatiena. The term inotudee the scientiic<br />

and tdwtii fiekts of surveying, geedesy,<br />

9mPhYs4=. mifiiry 9e091=Phy.<br />

phebgranrmafry, cartography, graphk arts, and<br />

rakrtsd actfviiies to the axfenf that they are<br />

aasant.d to the amem@ehrmmt of the remet-y<br />

mfw@n9. 9~eq, erd mi~tiary geogmphm<br />

‘n’en’gems -n” ‘-‘n --%!?..ti<br />

term IS eppGed to e surface such aa t<br />

bottom or a surface c4 given cheractertstii<br />

wifhln the water mass.<br />

topologk ●rror dreckhrg-Tha pmce= of<br />

enaurirrg that the Iegkd mnsicfency of the data<br />

is inted, that is, ell pofygons am cloead, all arcs<br />

are rmmecfad to ncdaa, etc.<br />

topological cOncepta-PrOperfiea of<br />

gaometrk figures that do nof change under<br />

mntirruous (arrrcdh) transformation; such as, is<br />

mnnacted to, is inside of, is d~nacfed, has<br />

three connected pwta (none mnnacfed to eny<br />

other), is a peint on the beundary of, is on the


I<br />

I<br />

left of, is a nade where five segments meet, etc.<br />

topological data brxw-A date bsss lhst<br />

e~sthe ~ms@ d topebgy to irrdiite<br />

the mfalmnahgra of mrtogrepfdi features,<br />

gsometricsfty axprsrsasd as fmints, firms, and<br />

WrfWxw. Comrnonfy ernpfeyad as the bsaie fur<br />

data bssas to bs ussd in gecgrephii<br />

Informstien systems.<br />

Iopologlcal data atructur*A vector dste<br />

strudure whii *6 ths same cfrsredsristii ss<br />

the oheirr-node dete structure, but afeo<br />

esmbfii the lopofagkel refatimcfripe<br />

(connectivity, sdjjcency, and inctusion) between<br />

faetume in a vector dste set.<br />

topological ontltlee-A collsd”mn of ob@s<br />

(i.e., nedes, edg= ad f-) urrad !0 ddii<br />

ths spstisl rekrtioncfripe errrorrg ths features of<br />

the Earth% surface.<br />

topological relrdlonshipe-How dste<br />

ele~nfs relete to esch ather withtn the date<br />

base. In particular, how e change to one<br />

element affects other elements.<br />

Topologlcslly Int*gretod Geegraphlc<br />

and Roeourco Information Syatom<br />

(TfGRIS)-An abject oriented geographm<br />

informetkrn system with a conmlidatad data<br />

st@ure. Developrxt ~ Irrfergmph Caprxrrtlon.<br />

topologlcaf-f%npertiaa of geometti figures<br />

es adjecanq thet are nd etfared by distortion<br />

es Ieng se the surface “S not tom.<br />

topology-Tha wey in which geographml<br />

elements are linked torfether, inducting Ihe<br />

qwstiel retationslipe ~=iting among g-xrgrsphlc<br />

festures and the methods used wtthin the<br />

Wmfmfw efwironment to geomelricalfy depict,<br />

etore, and esemins the data wilhin this retstkrnal<br />

mntest. Topolcgy irwludes adjjerwy,<br />

irrchsion, and connactivii. See also<br />

ed]acency; connactlvlty; Inclusion.<br />

toponymy—1. The study ad treetment of<br />

!oponyms. 2. A trady of toponyms.<br />

MIL-HDBK-850<br />

topon m-A name eppfiad to a natural or<br />

cuifua<br />

~hti~<br />

7 feature. For U.S. Gtwernmerd<br />

governing P&e<br />

usegs,<br />

rswrres<br />

on Es* em estebliahed try the Un~ed Stetea<br />

Boerd on Geographic Namee. AJao celied<br />

geogmphlc name end plaoo Mine. S.afso<br />

daacrlptlva name.<br />

toPPf. Wt*ThCt horimntel a+<br />

v** to the (frorizmtd) qxn sob d a<br />

gyroscope, amumf whiih topple amure.<br />

tOpple-Tfre vertical cmnponsnt of pracss+m<br />

or wender, or the algebs”k sum cd the two.<br />

torsion bafenca-A devke for measuring<br />

mrnbiitiona of the eemnd der+vativee of tha<br />

gravity poteniisl, which are .cloaety ratsted to the<br />

horizart!al components of the ddection of the<br />

vertical. It mrrakzs of a bar susperrdd<br />

horizontally by an ekretic fifement, ona end of<br />

the bar being subjsded to the inffuence of the<br />

ettmcting force to a grseter degree then the<br />

other end. The attracting forca is balenaed end<br />

its cornp.erstive afrsngth meeaumd by the<br />

torsionsl readian of the filament.<br />

tonoloolcal structurincr-The maces of -.. . .. . . .3- ,<br />

or&u&g data Icptagiilly ec Uiat the<br />

total departuree-See ebsclsaa.<br />

relationch~s and reference finkages are<br />

speci%sd.<br />

totel drltt-The algebrsic sum of drift due 10<br />

preoesc”mn and thet due to wander. Alrm callsd<br />

topological vorlficatlon-The promes of drltt.<br />

vwifyfng the tofdogiil ralstkxrah~ betwwn<br />

deta elements.<br />

total latltudes—See ordlnatas.<br />

262<br />

totel magnaUc lntanslty—The vector<br />

resuftenf of tha rntensity of the horisontel and<br />

vertical oemponents d the Earth’s magrrstic<br />

tietd al e apecifii point.<br />

totel etetlon lnstrumerit~ aurwey<br />

instmmem capable d measuring ddta x, y, and<br />

z components without signiksnt afferetiins.<br />

touch plete-See klsrr plrNa.<br />

town pfen Inset—See Inset.<br />

town site sunrey-The rrddng of tines end<br />

comers within one or more regular units of the<br />

towmshii subdwision by w?rfch the fend Is divided<br />

into bfocks, etrsats, end alleys as a besis for the<br />

dispassl of tiile in parcels of land.<br />

township corner+ corner of a township.<br />

See also clorrlng township comer.


towrwhlp Ilnoe-l%e townsfdp boundsrk<br />

lhst run north md sotdh are trsmsrd rang.<br />

Ilrms; with few exoq#bns the rangs h are<br />

mnor’lesrrhefa dfiswbam inrandad loba<br />

oncarr9n81. Thsbolmdsrks Nwrdng Srwmd<br />

wad am tanned township ffnaw. Sy taw, fhay<br />

Mm Herded to ba on true pamRela of fatiiude.<br />

township-The Unit & survey 04 the pubIio<br />

fend-q nornmlty ● qudrangks appmrrfmatefy 6<br />

miles m n aide wfth boundsriaa tiomtlng to<br />

merkfiins ●d peraoala Wiftrkl aa&Mshd firnif80<br />

cmfairrhg thirfy-ais sadims, some d wtkl’t am<br />

designed to correct Im tha mnvsr@ca s4<br />

maridkms or range fines. Sss akm fractional<br />

township.<br />

trace-* selectlon overlay.<br />

tmck ●djustrnant-AdjuaimenI to a shp’s<br />

track resulting from set and drift d the vessel.<br />

track chmf—A cfrsrt showing racomrn ended,<br />

I required, or eatsbtiihed tracks, and usualty<br />

indicefing turning points, souraee. and<br />

I disla ncss.<br />

... . . . . .. . . . . . . . . . .<br />

tmcklng carnarm-Seo bellistlc cemorn.<br />

tmckfng station-A ground-baaed sornplex<br />

I set up to trsck an objsd moving through the<br />

atmosphere or qsce, by visual, photogmp~lc,<br />

! photoetectriq or efasfronic mathoda.<br />

tmsk-(JCS) The actual psth of en aimrsft<br />

above, or a shii on tha aurfece d ths Earth.<br />

Theccurae Lslhapeth whkhispfanti, the<br />

track is the path whii is actuslly taken.<br />

●-M- ----. -,1-- --L ----- m-.+ . . . . . . -.<br />

. . .,!.. *-p., -..”,, *“rrw,r,-—”( ,rGs,cs( “Jr<br />

nauficsl charts of sdrernes simad et radusinq<br />

the risk ~f cxrtlision in t%mgested andlor -<br />

converging areas by separating fraffii wing in<br />

cfpmsife, or nesrfy oppoafte, dml”mrrs.<br />

traffic-circulation map-(JCS) A map<br />

showing traffii rmdss ad the maaaums for<br />

trafftc regulation. ff indkafes fha rosds for uss of<br />

certain classes ef fref’k fhe location of frsffii<br />

sontml stsfbns, and the directions in whioh<br />

treffii rrray move. Also cslled clrsulatlon map.<br />

See also map.<br />

tra@tory-in generel, fhe curve that a body<br />

describes in apace. An arbii is a trajectory which<br />

dces not intersect the Earih,<br />

MIL-HDBK-850<br />

263<br />

trarmcrlbor—sae Point-tmnder dovlco.<br />

trsnssrkptkm-1 . The process of rtirrg<br />

the sounds ersks gmna’ne Iicat elements d e<br />

fanguagekr terms ofaepec&wriii W.em.<br />

ZAnttarrr dalarrgus@ vrhk4rtms~<br />

this procaaa.<br />

transduoar-Ary davice for converting w<br />

from ona form to mother (eJwctrkel, mdrewal<br />

wwooti) .lnsoner,i tususflycorkhas ths ‘<br />

fuy of a hydmphcme and n projector.<br />

transfar startdard-A oaf of formats and<br />

prc40c01s Usast to nmve ate frorrr - eyctern to<br />

another without baa. Mey be defkred at the<br />

bgbsl lava+ the physical level, or both.<br />

tranaformatton-1. (phofogrammatry) The<br />

procaaa of projecting a phofog-epfr<br />

(mathaJnst”kslty, graphic+, or phciogmphkelly)<br />

from its plane onto armfher pkane try tmmfafkn,<br />

rotstion. arrdkx scale cherrga. Tha pr+ctikrr is<br />

rnede onto a ptsne dalarrnined by tha angular<br />

relst”kms of the camera esaa and not nwo-ly<br />

onto a horizontal plnrw. See dao<br />

mctificdbon.. 2. (mmaying) The .+-.. .. . -<br />

==@at’-l prcawa of converting a pc@ibn<br />

from UTM or othsr grid ooordirmtes 10 @od@k,<br />

and V* v- fmm me datum end etiipetrid to<br />

another using dahrm 6hm oowtants and<br />

el@eo”kl paremefere. The survq poaitii d a<br />

point is fraquantfy given m several dfferanf gride<br />

or atliiid% local datum end Ooppfsr-darivad<br />

WGS w are mmrmon requirements.<br />

tranafomrad print-A photograpkrk print<br />

rnsde by pro@on in a tranaformlng printer.<br />

tmrrsformlng prirrter-A spacialfy dadgnad<br />

projection printar of freed geornatry used for<br />

hsnstorming the cbliiua corrqmnenfs of a<br />

=WM ~m installation, a multiple-lens<br />

=rwam, w a parmmmk samara onto a pfarm<br />

wwmkufm to the axis d the system. See<br />

ateo rutifloc unlvwaal tmnaformlng<br />

printer.<br />

tranalt Instrument-%e tranalt, definition<br />

4.<br />

trenstt Iine-hy line et a treveme whkh is<br />

projected, either with or withoul maasuramanf,<br />

by the use of a trsnsft or other detdre. ff k?not<br />

necessarily an actual line of final survey but msy<br />

be an accessory line. Also called traveree<br />

Itne.


I<br />

1<br />

tmrwtt micrometer contact corractton-A<br />

quantify appGadtO thechmnOgmphmcud ofa<br />

etartranek atwrvad eiththoaidof ● trarmd<br />

mkfomafar toasowfor tharhramquimd forrhe<br />

contacf ~tocroaa ona+affoftha widthofa<br />

contact atrlpin thahaad of them&wnatsw.<br />

tmrmft mlcromater-A form of ragiafering<br />

micmmaWwkh R.smovsble efiraptacad krffw<br />

faxdpkured anactmrrenkf rends vdafrigfrf<br />

arrglaatofhadradbn ofrrutbn oftkbnageof<br />

a afnr which b ebaarved at or near cufninatbn.<br />

Also called Impamonal mlcromatar,<br />

bacauaa & afrrrd carrpbldy dirninrdea the<br />

effect of the personal aqmfion on time<br />

Obaarvat”m made wkh it<br />

tranaif ~ rnathed of balancing a survey.<br />

Gxradbns cnrraapording to the dosing errors<br />

in Iatiiuda and dqmrfure are dmributad<br />

accordiig to Iha proportion: Iatiiude and<br />

mum of awh line of the traverae to the<br />

arhfrmatical sums of the tdfudas and<br />

d+arfurea ef the entire traverse. Tha hand rule<br />

isuaadvrhsm gieaacurnadfhat Iheckxing<br />

~ - dua I* to the errors in the ofzservad<br />

arrgtas than to armra in the ~~md distances.<br />

trarrslt trava~ survey traverse in which<br />

the angles am mcmsumd with an enginear%<br />

transit w thaodoliie and the Iangfhs with a matal<br />

tape. A transit<br />

.<br />

kaveraa is usual~<br />

Wremnlrofofhcaleuweysandm<br />

axecufed for<br />

Ofaacer@<br />

order m Ihlrd.ordar quafhy.<br />

transit-and-stadla survey-A survey in<br />

%ich horfzcmtal and vartical dirrrct”bns or angles<br />

are obearved @h a trard and did— are<br />

measured by tranaif and stad~.<br />

traneitlon ourv~ ●plral curve.<br />

trsrmft-1. The apparent pa9aage of ~ star or<br />

OfhW 00b8fbf bOdy aCrOS6 H dafktad tim Of h<br />

celeetlel @rem, aa s maridikm, prima vertical, or<br />

aknucenfar. The apparent paeeafJe of a 6tfU w<br />

ether cdadal body acrosa a Iiie in tha retisfe of<br />

e telctscq-s, or eerna line of sight. The apparent<br />

-ge of a mtrdkr celestial body acrmaa the<br />

disk of a larger celastial body. Tha tranait of a<br />

star ecroas fha nmridien oceura at the mOment<br />

of fls Wf@_MOrr, end the two terms are<br />

eomatmraa used se having identical meanings:<br />

aucfr usage is not comect, even whare the<br />

irrefrumant m M perfect adjuatrnant. At the polaa,<br />

e star rmy have no culminat’bn bul if will trend<br />

the meridians. Sea alao culmlnatloru lower<br />

MIL-HDBK-850<br />

264<br />

tmrmlt; nreddlan tranelt; upper tr*n8h.<br />

zAeurvaying inatNmant CcWroWdc4 a<br />

~-mmtdhati~<br />

andrmaiidada wkhaldeccupatida be<br />

ravaraad hkeqrports witfudbei~ Wad<br />

therefrom. see dao uroOdOuta. a. The Wf d<br />

~~tid~dat~ @MUm<br />

arourd ke horizontal esb. Also called plunge:<br />

Invwtlng; tohcophrg. 4. An astronomic<br />

irratnansd havhgatelaeqra wfrichcarr base<br />

adjusfed inpoaition theffhelinaof Slgmmeybsr<br />

madato&4ii 9Wrticdc4rc4a.Ab ocaued<br />

■atronomb tmnaff. sea afso broken<br />

telouopa tranal~ solar tmnstt.<br />

tmnsletiorral movwnant-Tha systematic<br />

rrmvernanf of pmjadcrr aa8enW& in tirle-dfliihf<br />

directions in a ateraopbfting irrafrunrarrf.<br />

tranelatlon-1. The procase of rendering oml<br />

or wiften texl of one bnguaga in terme d taxf<br />

of curreapondirrg meaning of mother fengusga.<br />

Sae alee romanizatlon tranacrlption;<br />

translttomtlon. 2. Movement in a straight<br />

fine withcrul retatien.<br />

trnnsllterntlon-1. The prcwasa of recording<br />

t~ ** gym Of one writkrg cystem in<br />

tmna d coneaporrdng graphii ayrrbols d a<br />

aacondwriting system. 2. An item of a<br />

Language whiih has undergone this pc.xaa.<br />

translocation-The determination of the<br />

rotafive pdticir batwean two points from<br />

eimulfarreous Doppler satelliie ebaanralions.<br />

tranalunsr ●paca-r% seen from the Earth at<br />

arry moment, space lying beyond fhe chit of<br />

the Moon.<br />

tranalunar tmjectory-A trajectory axterdng<br />

outside the Moon’s orbii aboul the Eorth.<br />

translunar+utskte the Moon’s orbit abouf<br />

the Earth. Sea else clslunar.<br />

transmlmsiorr-(aptics) The ratio of transrniffad<br />

Iiht to ttra indent light. ff ?00 units of liihf fall<br />

up e tmn~mnt material and I 0 of thgm<br />

succeed in paesing through, then if can be sakl<br />

thatthe material has 1/1 O or 10 percent<br />

tranemieewn.<br />

transparency-(JCS) An image freed on a<br />

clam base by means of a photographic, printing,<br />

chemical, or other process, aspecialty ada@e.ble<br />

for viewing by tranemhfad light. Sea also<br />

dlaposltive.


I<br />

trmtcpondor-@CS) A mcafvar.tmmsmtlter<br />

which will ganerafe n rqfy al@nal w pqer<br />

irrlarrogatiorr. Sea aleo rsspcmaor.<br />

transvorsa asla-l%a distanoe between the<br />

apeidas. If IS kfenfkal to the aemfmejor asta for<br />

aflipiiwl orbits.<br />

trmnavuce chart-A chart on a transverse<br />

pmjaction. Also cefkd Invoraa chain<br />

transverse cylindrical orthomorphk<br />

chart (lCOC)-See trarrswrso Mercator<br />

chart.<br />

transwraa cylindrical otihomorphlc map<br />

projoctlon —See trmrsverw Morcstor<br />

map projcctlorr.<br />

transvemo equntor—The plane which is<br />

parpadwbu to Ihe axis of a lraneverprojection.<br />

Aleo called Inverso equator.<br />

transversal graticula+l fiiitiius graticule<br />

baaed ~ a Ifarcwersa Pr+3cfion. See eka<br />

flctltlous gratlcuk.<br />

transveraa iatttudc-4u@ar dkttrmce from a<br />

tranaverae equator. Also called Inveree<br />

Iatltude. Sw Eke fictitious Iatltude.<br />

trmsveras Iongltuda-+ngutar distance<br />

Mvmarr a ptfme tranavarea meridian and any<br />

given transverse maridiin. Also ceiled Invaraa<br />

Iottgttudo. See also fictitious Iongltude.<br />

transvarso map projaotlon-A map<br />

projedkn in whiih the projection axis is rotated<br />

9tP in azimuth.<br />

tranawrse Mercator chart-A cherl on the<br />

transverse Mercator prajactiin. Afao called<br />

Inwrso cvlhrdrlcal orthomor~hk chart:<br />

Inveraa Mercator chart; transverse<br />

cyllndrlcsl orthomorphlc chart.<br />

trsnsvsrse Mercotor grid—An informal<br />

daeignetkn for a stale coordinate system baaed<br />

on a transverse Mercator map projection. Afeo<br />

celled Geusa-Kruger grid.<br />

tranaverso Msrcator map projection—A<br />

conformel cdindrical meD Dmiactiorr. being in<br />

principla aqiwalent to the ‘regular M“ercal~r map<br />

pmjedion Iumad (tranaveread) 90” in ezimulh.<br />

In ths projadon, Ihe central meridiin is<br />

MI L-H DBK-850<br />

. .<br />

265<br />

mpraaantod by a atrelgfd line, ccmwpmdi to<br />

thaline wtJchreprasenk fhe Equafaron the<br />

m@ar Mere.@or ~ pru@dii. NeiUws the<br />

o-c ~ne (Sxcapr the Cantrrd<br />

marsfiin) nor the geodetic pallek (faccept the<br />

Equator) are repmaamted by etm@ht lines. Ak<br />

CJSllad Inwrao cylktdrlcd orthomorphk<br />

msp projoctlon; Inverso Mercator msp<br />

projection; trutevoraa cyllndrlaal<br />

orthomorphlc map proJactlon.<br />

transwraa mwidla+ greet circle<br />

pWp3tiiUkf toe transverse equator. Tfrs<br />

reference tmneversa maridiin in cells! prima<br />

trsnavarca maridkn. Also calkd Invorssr<br />

meridian. Sea afao fictitious meridian.<br />

transverse model datum-See modol<br />

datum. definition 1.<br />

transverse parallel-A side or fine parellai to<br />

a transverse eque!or, connecting ell points al<br />

equal traneveree Iatfiude, Also called (nwrsc<br />

psrallal. See aleo flctltioua psrallal.<br />

tr.wswrsa pcrJAna of the !WO pints 90”<br />

from a transferee equator.<br />

. . .. ... . . . . . .. ,’..-..<br />

transnrerse polycordc map projection-A<br />

pofy=onic map pmjwfion * is turned<br />

(tranevaraad) 90° in azimuth by substffuting for<br />

the &sntral merkftan, e great circle parpandmular<br />

10 the gaographc rnaridiin to provide e control<br />

axis for the pmjectiin, akng whii axis will fIe<br />

the centara ci ths circular arcs ~rsser#ing ffnaa<br />

of tangency of cones with the surface of the<br />

sphere.<br />

transverse posltlon—A CPM camare<br />

instelktkn se poaitiinad that the pkne<br />

containing the arnare axis is pwpandicufar to<br />

the tine d fight.<br />

tranmrer- rhumb llnc-A line making the<br />

same cbliqua angle vkth all ftiis meridians<br />

of a transverse Mercetor projection. Tmnsveraa<br />

parallels and meridians may be Cu’laldamd<br />

special cases of the transverse rtru~ fine. Also<br />

called Inverse rhumb Ilne, See also<br />

fictitious rhumb line.<br />

trrmaveras-in cartography, panaining Io or<br />

maeeurad on a map prqection In wl’iih a<br />

meridien is ueed as e Iictit”kmisequator. Alw<br />

called In versa.<br />

traverae adjustment—See balsnclng ●<br />

survey.


!<br />

tmvwae ●ngl a4Aaawrwnerrt of tha<br />

frlxizwrtal Sngfe from e praoadlng Sdjjnt<br />

ststkm to the f~g ad- atetbn.<br />

tmvoraa ●rror of closure--see ●rrer of<br />

closure, detinitiorr 8.<br />

traverse Ilne-Sae trstnslt lln..<br />

tmvorss net—See survey ns~ detinitiin 1.<br />

trmram9 stetkrn-A point on a traverse over<br />

vMch an inabumant is pies+ (.s -up). Also, on<br />

atrevame, tstangthof 100 feat meeaured Ona<br />

given liM, ailhar straight, broken, or curved.<br />

travwsa tablas-Malhernetical tables listing<br />

the bngths of the *S oppeaife the obfiqus<br />

angles fer aadr of a series of right-angle pfane<br />

triangles as functions ef the length and ezimufh<br />

(or bearing) of the hypotenuse.<br />

traverse the Instrument-To rotate a survey<br />

instrurnwrt abeuf its vertical sxis: thst is, turning<br />

the instrument in szimuth.<br />

‘“-frs;a~~JCS) A rirathbd ‘of ‘6urVeying” in<br />

which lengths and directions of lines between<br />

pints on the Eralh are obtalnad by or from field<br />

-surbrnents, and used in determining<br />

@iOlls 0( ths p(lklts. [A SUfVOy tlEV01st3 MSy<br />

dekmni~ (ha raktttie positiis of the @nts<br />

Wf’1k41itoomecta insarias, smdif tiadtorsrntrd<br />

stations on an adc@ad dstum, the po.dtbns<br />

MY b’s MfeiTSd to that datum. Survey trsvaraae<br />

are c&salriad end ktantii)ed in a variety d ways:<br />

esccfding to methods used, as astronomic<br />

traverse; aaadfng to quallty 0( rasutte, as firslordar<br />

traverse; auording 10 putpa.s served, es<br />

9wmPhhl esptwmtiin traverse: and<br />

a~ng to term, as dosed treveraa, etc.] Sea<br />

al= mrgla-to-right tmv-rerr; azimuth<br />

traverao; cloead tmvarso: connecting<br />

tmvsme; doflectlon engle traverse; flrstordar<br />

traverse; fourth-order traversa;<br />

gsogmphlcal ●xploration treverse;<br />

lritertor ●nglc travoree: loop treverse;<br />

open trworsa; phototrlg traveree;<br />

planetsblo travaree; random traverse;<br />

second-rder traveree: epur tmvereo;<br />

st~dls trsvcrse: eubtense bar traverse;<br />

subtensc base travarae; third-order<br />

trsvorso; tranelt traverse.<br />

triengle closurs-See error of closure,<br />

definition 7.<br />

MIL-HDBK-850<br />

266<br />

trkmgla ●rror of clowre-%e ●rror ot<br />

closura, definkiin 7.<br />

trtangls of doubt~n a sinple two-peint<br />

probtem, the trbngle rasuhhg when the check<br />

ray faRs to peas ttsough the poird rX tiemacl”m<br />

of the two intaraading rays.<br />

triangle of ermr-lhs wianghs formed whan<br />

tluee fAottsd rays fail to intamed partadty. The<br />

santer ot the trfsngla may be oonaiderad to be<br />

the adIuslad positkrn. See also reaectlon.<br />

triangle-of+rror msthod-hr eurvaying, a<br />

technique for aoMrrg the trreqroint @lam<br />

grsphicaffy byatrfengle otam3r. Theaa matheda<br />

are ganamfly rafarrad to by name, such aa<br />

*6ser6 method, Co.sst-Suwey method, end<br />

Lehmsnn’s rnathed, eecfr of wfriih is based<br />

upen its own fadom. See ales triangie of<br />

error.<br />

triangle-See astronomic triangla;<br />

ceieatlal trlangla; navigational triengle;<br />

preliminary triengio; spherical triangle;<br />

apheroidai triangle; tarreetrlal trlerrglc.<br />

triangulated Irraguler network (TIN)- A<br />

terrain rrmdel created from continuouafy<br />

connected triangles derived frern the Oalsunay<br />

algorilhm. The vertkee of the trianglae form<br />

irraguierly spsced ekavatkm posts. Unlike a grid,<br />

the TIN elbws extra intorrnrdhn to be dispisyad<br />

in areee of smrples rekaf wthwt dbplayirrg<br />

dense or nsdunderrt deta galharad in amss of<br />

simpte relief.<br />

triangulation base Ilna-see bese llno.<br />

trlsngulatlon nst—See ●urvey neh<br />

dafiniticm 1.<br />

triangulation mconnalsssncs- A<br />

preliminary survey to select the Iocatbn of<br />

etsfiens to give the meat faasibte triangulst”m<br />

scheme.<br />

?<br />

triangulation signal-A rigid structure<br />

erected over or elms to e hiengulat”on slet”~<br />

snd used for suppmling an instrument and<br />

observer, or lerget, or instrument and observer<br />

and target, in a Mangulstion survey. Also, any<br />

object, naturel or artifciel, whcsa poeitbn is<br />

obtainsd in e Iriengulmion survey. The term mey<br />

be applied to a structure whose positbn is<br />

delernrined by triengula[ion, but whose primery<br />

purpose is to ‘sewe kr in s hydrogrsphx or


trlsngulatlon aystenr-lhe main schema, or<br />

nd,dprbrwya fafbnee ndfhaaudfbry<br />

Cfetions. nterrdna shrrmaf ethafmmawwkof<br />

Ifwayefem ardfaliadaf sav+maf* to<br />

prrwiauafy aatsbfiahad triangulation stations of<br />

equal or higher order. See also survey neL<br />

definition 1.<br />

trlangubtlon thoodolffe-$ee direction<br />

Inatrumont thoodollte.<br />

trbngufaflon tower-A afrudure ussd 10<br />

elevste the Iirm of sight atxxe intwvening<br />

obetecles. Usually wnsists of two independent<br />

efruduras, one within the ofhan the osnter<br />

sfwhtre s+portri the Umcdofiie end the outer<br />

.stndure s-s the observer and the slgnel.<br />

See also Bilby steel towor.<br />

MIL-HDBK-850<br />

bpogmpM ‘ survey,<br />

es a hydrographic<br />

wfmn it rmy baccxne )mown<br />

or topogmphlc ●lgnal.<br />

gmphy oM4ned by sirnuhanaous eXPSMe Of<br />

ttwee cameras Syetemefkany I&$ezad m the Sit<br />

vrrhisb cftimdo varb@nga r@aemtafivefo<br />

trbngulatlon ststlon+JCS) A pcint on the each other m csder to mvar a wide f~. See<br />

Eartfr* pasifii bdebrminad~.<br />

elso fan camera photography.<br />

trisngutefion. At60 cstfed bfg point.<br />

trig control-see field control.<br />

Mg doealor-A dafaUad reoud on the<br />

ftfangufatti of en ems, giving the coordkwtse<br />

d the triarrgldatbrr afationa.<br />

trfg llst+fCS) A list pdiehed by serfairr Army<br />

Urine Wtlidl itsludL9J e3eentbI HOrrrdii d<br />

accumfefy bmted rwvay poirda. [A pibfidion<br />

mntaining sII availebb puaibud data and<br />

etavatii wffh the raspedva daacr@bne of<br />

horizonfet andkv vettkad control points, uauatfy<br />

arranged asawding to lhe focatiin of the cantml<br />

points within the hits of map .shaefs of targsecele<br />

eark.]<br />

trig point-See trlnngulatlon atatlon.<br />

trigorromatrlc Iavding-lhe determination<br />

of dtfferencee c4 abvefiorw from observed<br />

triangulation-l+ method of surveying in whiih verficat englea wmbined wffh Iangfha of lines. A<br />

the sfeficns era @rrts on the. Ground whkh are. . ,fype of indiued bvekg.<br />

IOcsfad et the vertices of a chain or network cd<br />

triangtas. The angles 04 the trisngfes ere<br />

measured instmmarrtaily and the .eidEs are<br />

dwimd by canputetion from selected sides<br />

wtriih are termed bime Ilnas, the lengths O}<br />

whfc+r am obtafnad from direcd meeeurarnants<br />

on the gmurxf. See ebo ●ralytfcsl thma.<br />

point msectfon redlal triangulation; arc<br />

triangulation; ●raa trlangulatlon; besa<br />

neti dlmet radial Mangulatfon; firetordor<br />

trlwrgutatlon; flare trlangulatlon:<br />

graphical radial trlanguletlon; handtomplot<br />

trlangulatlon; Ieocentar<br />

trlangulatlon; mechanical-templet<br />

triwrgutmtion; rmdlr-point trlangulatlon;<br />

phototrlangulatlon; radial trlangulatlon:<br />

‘ satellite trlenguletlon; second-order<br />

trlwrgulatlon: aamlenalytlcal<br />

triangulation; ship-to-shore<br />

trtangtdatlon; stotted-templet<br />

trlengulation: ttplder-templat<br />

triangulation; third-ordor trlangulstlon;<br />

trllateratlon.<br />

trlaxtal ellipsoid-An eltipaold having three<br />

U~USl axes, the etwxfesf being ifs potar exia,<br />

while the two bnger onec lie in the pfsrre of ifs<br />

equator.<br />

trlcamora photography—(JCS) Photo-<br />

267<br />

trltetertrtion nat—A network of points W*<br />

positiis relsttie 10 one another aro determined<br />

by maeeuremenf end edjuafmanf of the length<br />

of the aides of the frierrgtes formed by these<br />

points.<br />

trllateretlon-A method of surveying wtrereln<br />

the Iengfhe of the trisngle aides are maeeumd,<br />

ueuefty by ebcfrotk methods, and the angles<br />

are rnmpufed from the measured lengths. SeS<br />

also trlmrgulatlon.<br />

triiinear ●urvayhrg-The determinatbn of the<br />

pesirii 64 e pohrf of observation by measuring<br />

the engles at that point betwean fines to three<br />

points cd known Poaiiion. See afso resection.<br />

trim marfm-Unae plasad on originel copy to<br />

serve as guidas in cutting or trimming the<br />

printd sheets to their prescribed size.<br />

trim dze--(JCS) The size of e mep or chml<br />

sheet tiarr the mmaas papar ouleide the<br />

me~in h= been trimmed off after printing.<br />

trlmetrogon camwe—A triple samere<br />

essembty with one vertical and two fried-angls<br />

obliques wfmse imegery overlapped the vertical


I<br />

I<br />

I<br />

I<br />

i<br />

,.<br />

andwith allthMS. S-S6Sk@lrnapbM<br />

Perpadwler to the fineofftiifrf.Most camera<br />

~dthiedadgn vmmmtmed ions<br />

trtmetrogon camera because of the<br />

widespread usage of the Metmgon fens in eerfy<br />

tricamwa photography.<br />

trlmotrogon photogmphy—Saa ta n<br />

camera photography.<br />

trlmmlng ●nd mounting dkgram-A<br />

Sketsh Showii how the prints of a tmndxrrlad<br />

mulfple-fens @rotogrs@ should be scwmcfed to<br />

obtain, h effect, a phofogmph ~ b ● *@<br />

kvra. Thehferrnetim k@mlnfkfom of<br />

d-rises derred to the fducial marks on the<br />

photq~, and is the reauR of the calibration<br />

test for he partkuter camera usxi.<br />

Tropk of Cancer—The nmfhem parallel of<br />

dectinslicm, approximsiefy 23”27 from the<br />

ceksliel equfdor, reached by the Sun at ifs<br />

msximum dedinetkn, or the oorrasPondiW<br />

pedal on the Earth.<br />

Tmpk of Caprlcor-l%e southern parallel<br />

af decfhation, approximately 23%?7 fmm the<br />

cekstiil,equstor, reached by the Sun m *S<br />

maximum dadimlien. or the corresoondnfl<br />

psrallel on the Earth. ”<br />

tropical month—The averege period of the<br />

revolutii of the Moon ebout the Earth with<br />

=Yo the V-l equinox, eppmximatety 27<br />

tropkal yser-The inlervel of time between<br />

k auccaaaive pasaugea of the vernal equinox<br />

by the Sun. The tropical year is the year of the<br />

aaeaone, ard the basis of the conventional<br />

sehdar year. Aiao celled mstronomlc yoer;<br />

●qulrmotlel yOaG natural year; solar<br />

y.mr.<br />

tropopeuse-(JCS) The trandtion zone<br />

bafwaen the atrefosphera and the tmp=phere.<br />

The tmpopauae normally ccwre et en aftiiude of<br />

about 25,000 to 45,tW0 feel in polar and<br />

temperate zones, end st 55,000 feet in the<br />

Impiss. See else atmoephem.<br />

tropotrphera-(JCS) The Imver layers of<br />

atmosphere, in wttich the change of<br />

temperature wilh height is relatively farge. It is<br />

the region where clouts form, oonvediin is<br />

acf”we, end mbrhrg is sonfhuous and more or<br />

lees mmplele. See al= etmosphare.<br />

MIL-HDBK-850<br />

268<br />

tmpospherk ecattor--(JCS) The<br />

LvwM@~ ~ radii vmvee @ edf~ ~ ~<br />

redl d uragikt’kii or diiimitiea in the<br />

pI@d propeti= d the ~.<br />

trough compac-See dtilinatolm.<br />

Troughton level-h Engfiah instrument<br />

hevingffte ePbiflevd Permar@b’af@=ffo<br />

thetopof fhstelessc$Mtube<br />

true ●ltitude-1. (.ES) The height of an<br />

airsrdf sa measured from mean sea level. 2.<br />

The actual eftiitde of a selaatii kc+ above the<br />

celasfhf horizon. Mao died observed<br />

●ltitude.<br />

true amplltude-A@dude retetive to true<br />

aasl or weat. See also emplltuda.<br />

trua enomaly—See anomaly, definition 3.<br />

true azimuth-The horizontal dkest”kn of any<br />

line measured cleckwiae fmm true north.<br />

true bfaering-The horizontal angle between<br />

the meridiin tine and a line on the Eerth. The<br />

term true baarlng is used in many cd the aerly<br />

descriptimrs of tand boundaries in the Uniied<br />

Stales. n Lseeeec4ated with true north, referring<br />

to the direction of the ninth psint ee determined<br />

by astrrmomlc observations. ff an estmnomkatty<br />

delemtined bearing ie used, howwer, the term<br />

mstronomlc boarlng is prefemed over true<br />

bearing.<br />

true dspresslon ●ngle-l%a setting of the<br />

obtlque oemama kr the phdographk a’kcraft w“kh<br />

retetion tothetrue herbomff~~ byarey<br />

fmm the exposure station through the prirdpal<br />

point et the abhque phdogmph and a my to the<br />

true horizon.<br />

true dlractlo~rizontal diresttin espraeaad<br />

as angular dist- fmm true north.<br />

true error—See resultant ●rror.<br />

true horizon—(JCS) 1. The baundery of a<br />

horizontal plane pesslng through e point of<br />

vision. 2. In pholograrnmetry, the boundary of a<br />

horizontal plane passing thrwgh the<br />

parap~~a center of e lens system. See also<br />

horizon trace.<br />

true llne-A line of con.stani bearing (rhumb


MIL-HDBK-850<br />

tepgmphk survey, bvtnm if may bemrns fmowr<br />

aa a hydrogmphlc or topographic slgnaf.<br />

trlangulstlon station-@CS) A point on the<br />

Earth whose positii is datedrred by<br />

triengutstion. AJm caflsd trtg point.<br />

triangulation Syste*The main schema, or<br />

M, d primaryststimam-d the awdii<br />

atatbne. Therrdn mherrrs lsthefmmewrk d<br />

he system and Is tii at aevemf pdrrts to<br />

previouaty aatabfished kiangulatlon stations of<br />

equal or higher order. sea afao survey *<br />

defiiitien 1.<br />

triangulation thoodolfta-Sae dlractlon<br />

Inatrumant theodollta.<br />

trlangatatbr tOwar—A sfrusture used 10<br />

ebvate the fins of sight above krtervening<br />

obstacles.. Usually consists of two independent<br />

atruduras, one within the othw, the aenter<br />

strtdure -S the Iheoddite and the outer<br />

structure s-s the cbsarver and the signsl.<br />

See alse Bllby steel towor.<br />

trlangulallon-A method of surveying in Mich<br />

the statiorra em points on the ground which are<br />

lesdsd at ths van”w cd a tin or netvmrk cd<br />

trisngfas. The anglea of the triangles are<br />

maaaured h16tNmSMS~ and ills aides are<br />

dw’tvsd by awnputstion from seJeded ddaa<br />

tiih are termed base Ilnec, ths lengths of<br />

wtr&h em cbfdned from direct maasuremsnts<br />

on the ground. See also ●nalythml thtaapolnt<br />

resection radial triangulation; arc<br />

trlmrgulation; arms trhrn~ulatlon: baso<br />

no~ dlraat radial tr’langulatlon; flratordsr<br />

trlangulatlon; flare trlanoulatlon;<br />

graphical rsdlal trlangulatlon; handtomplot<br />

triangulation; Ieoaenter<br />

trfangulatlon; mschartlcal-tamplet<br />

trimrgulatlon; rmdlr-point trlangulatlon;<br />

6hototrlsnaulatlon: radial trlangulatlon:<br />

katollite tfiangulatlon; second+-rder<br />

triangulation; aamlanalytlcal<br />

trlangulatlon; ship-to+hore<br />

trlangulatlon; slotted-templot<br />

trlangulatlon; spider-tamplet<br />

triangulation; third-ordor trlangulstlon;<br />

trltataratlon.<br />

trtaxtsl dUpaold-An ellipsoid hsvlng fhree<br />

U~USl eses, the ahorfsst being its pelsr exis,<br />

Mule the two bnger enes fie in the plsne of its<br />

equator.<br />

trlcamera photography-(JCS) Pholo-<br />

267<br />

gmphy obtained ky simultanaws exposure of<br />

ttras cameras aysfemsticdy @Oaed in the air<br />

vehicle et fixed twedappirrg angles mtstke to<br />

each other m order to -v- s wide f~. see<br />

abo fart camara photography.<br />

trig cantro~ ffold control.<br />

trfg douler-A detailed ramrd on the<br />

trhguwon d M a-, g“w-rgthe moldiim<br />

of the triarrgdsbrrStatbns.<br />

trfg llst+JC.S) A Eat pdiahed by mrtsin Army<br />

units which klctdea assentiel Mrrmsfii d<br />

accurately krmted SLS’Veypoints. [A @rtkatbn<br />

corrtainkrg all mmdabla poaitibnal dsta and<br />

efavatime with the reapedke daeer@ibns of<br />

t-mrizorrtel errdkr vertiml sontrol points. ususlty<br />

srrsngsd ssmrdirrg to the location of the control<br />

points within ths knits of msp Shasta of lsrgsscsle<br />

series. ]<br />

trig point-see triangulation atatlone<br />

trigonometric levding-The determinstien<br />

of diiersrrms et sIavstkms fmm observed<br />

vertical arr@aS mmhhsd Wth lengths of lines. A<br />

type of indirect bveJing.<br />

trilatemtlon not—A network Of peints wheaa<br />

p&tiens relative 10 one another are delarrninad<br />

by measurement and adjusrrnam et the length<br />

of the s.kfes d the trisngias formed by these<br />

pdrrta.<br />

trllateratiorr+l mathod of surveying wherein<br />

the lengths et the triangle sides sre measured,<br />

uauefty by elactronis methods, and the angles<br />

are computed from the maaaured lengths. See<br />

also triangulation.<br />

trlllno=r ●urvaylng-Tha determinstbn of tha<br />

podtii M a pdnt of cbm-vatbn by ~rfnu<br />

the angks al that peint between Ilnes to thrse<br />

pcints d knewn pesition. Ses afso rekmctlon.<br />

trim msrks4_inea placed on origird mpy to<br />

save as guides in cutting or trimming the<br />

printed sheets to their presaribd size.<br />

trim slza-(JCS) The size of a rnsp er chsrt<br />

shaet wiwsn the excess paper eufaids the<br />

margin has bsen trimmed oft after printing.<br />

trlmetrogon camara—A triple cemare<br />

assembfy with one vertical ard two freed-angle<br />

ob~ques wtrese,imege!y ovartsppad the vertical<br />

t


I<br />

I<br />

I<br />

I<br />

i,<br />

I<br />

I<br />

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and with dl tfVSS SXES tfii in a pk’t13<br />

perPczMkufar 10 the fins d ffiiht. Most SSM<br />

esssMea dthkdas@n wemmfan’ad tOSS<br />

trlmatrogorr camera because of the<br />

wideepreed uaega of the MatrogIxI lens in earfy<br />

trlcamara photography.<br />

Mmotrogon photo mphy-Saa fan<br />

1<br />

camsm photogmp y.<br />

trlmmlng and rnountlrrg dlagrmrt-A<br />

&eroh * how the prints of a tmnsfermad<br />

muft!!ldans @mtogmph should be corrected to<br />

oMaino h effect, a phdegm@r rrbsda bys airt@e<br />

Iana. lhekhrrn=fionieghfaintitirnr of<br />

d-m mfermd to tha fduckd rnadta on the<br />

photograph, end k the mauk of the salibretkn<br />

test fer ha particular samem used.<br />

Tropk of Cancer—The nerthem parallel of<br />

decfirrstion, approximately 23”27 from the<br />

celaetii equstor, raeched by the Sun at ils<br />

r-neximum dacikdkn, or the ocrreapondng<br />

parallel on the Earth.<br />

Tropk of Caprico~The aeuthem parallel<br />

of declination, Spproxirnatety 23%?7 from the<br />

--- ~W SUuator, reached @.lha Sun at ils<br />

mesimum .3eol@stim, or the corresponding<br />

parallel on the Earth.<br />

tropical month-The average period of the<br />

revolutii of the Meon Mrcmt the Earth with<br />

I mamd 10 the vernal tmuinox, eppmsirnetefy 27<br />

1/3” days.<br />

tropkal yeer-The intervel of time between<br />

k wcumaive peaaogea of the Varnel equinox<br />

by rha Sun. The tmpics+l year is the yaar of the<br />

aaaama. and the MS of ttm sorwetimnal<br />

sekndsr year. Ake celled ●stronomic year;<br />

squlrtootkl yaec natural yaec solar<br />

year.<br />

tropopttuae-(JCS) The trenailbn zone<br />

between the atratosphare and the tmpoe@era.<br />

The tmpcpauaa normally cxxwrs et en aftiiude of<br />

atmut 25,000 to 45,CKN feet in pokr afd<br />

temperate zones, end at 55,0M feet in the<br />

lrepka. See also atmoriphera.<br />

troponphars+JCS) The kwer Iayara of<br />

atmcaphem, in wtich the ctwnge of<br />

temperature with halght is relatively large. It is<br />

the region where ckwds form, oonvastiin “m<br />

ediva, and mtzing ia cordnuoue and more or<br />

leas somplete. See ak.o atmosphara.<br />

MI L-HDBK-850<br />

260<br />

tropoapherk ecMter+JCS) The<br />

Propegm’m d radii waves by scattering as a<br />

* d iIIEWtikW or d~inuibs in the<br />

physical properties c4 the tmpOs@m.<br />

trough compasa-See daalinatoim.<br />

Troughton level-An Engfkh inatmrnant<br />

having thaq)iritteval PamW8ntty atteched to<br />

the top of the klhcopa tuba<br />

truo ●ltttuda-1. (JCS) The height of an<br />

aimmft as maaaured fm.tn mean see level. 2<br />

The add afIiiwte of a oskslii body above the<br />

Sakstial horizon. Akc czdkrt observed<br />

●ltltuda.<br />

truo empllWla-Ampktude relative to true<br />

nest or weet. See also amplltude.<br />

true anomsly—Sefr anomaly, definition 3.<br />

true azlmuttr-The horizontal dkestion of any<br />

line measured clc-drwisa from true rsx’th.<br />

true bearln~The horizontal angle between<br />

the meddkn line ard a tine en the Earth. Tne<br />

term true bsartng ia used in many cd the earty<br />

dessripticms of knd boumianes in the United<br />

states. h is associated with tma north. derring<br />

to the direction ef the north @nt aS detanmined<br />

by astmrrornk cbserwliens. If an eatrcrrcsmicaliy<br />

determined bauring is used, howemr, the term<br />

astrsrnomk boarlng ie preferred over truo<br />

besrlrtg.<br />

true dsprasslon ●rglxl%a setting of the<br />

tique cameras In the pfmt~ abcratf W*<br />

rebdion to the trus frarizon. It k defined by a my<br />

from the exposure statism ttwm@h the principal<br />

point d the obhque phc&gmph and a ray to the<br />

tme hol-kon.<br />

true dlmctlon-herkotial direstkm sspreeeed<br />

as angular dktance fmm true nrnth.<br />

true arror—See resultant error.<br />

true horizon—(JCS) 1. The boundary of a<br />

horizontal plane passing through a point d<br />

vision. 2. In pho!ogrammetry, the boundary of a<br />

horizontal plane pesdng Ihreugh the<br />

pemp-~e center of a lens eyetem. See al~<br />

horizon trsce.<br />

true llrm-A line of constant b-ring (rhumb


I<br />

I<br />

I<br />

I<br />

fii) between fwem- ofa aurwy.<br />

tnm nwridlan-A kvm used !0 distinguish the<br />

gmst circle through fhs gsogmphbaf @se trom<br />

MsPtk Metiin, oompsss nreridii, or grid<br />

meridian.<br />

tN@ nori.h-(JCS) The direcibn fnwn sn<br />

observer’s @fiin to the geognrphii North<br />

Pole. Ths north dimdon d any @oun@c<br />

meridiin. ~ term was origiity ep@ied to<br />

aatronomlc narth to daingubfr it frmm<br />

magnetic north.]<br />

true placa-S ee two position.<br />

~No poaftfon-lhe poaifian of a eels.stiaf bdy<br />

sfrer all krmwn mrrect”mns including precoasion<br />

and ntrtefien have bsan rneda. Atso @Jed true<br />

place.<br />

~NO prfmo vertbakl%e vertical circhr<br />

through ths true asat and w- points at the<br />

horizon, es disfinguiahad from magnetic or gfi<br />

prime verficsl through the magnetic or grid esst<br />

end west points, respedhty.<br />

truo sidereal tlms-See ●pparent<br />

●Idoroal tima.<br />

true solar time-See ●pparent solar<br />

tlms.<br />

true sun-See apparent sun.<br />

true vahIe-Thst value of quantii whwh is<br />

=K@Et* f- ftOM arrera. Since lhe errors to<br />

whiih physical measurements are sbjwf<br />

cennof be knewn exscffy, it fotlows thst the true<br />

vafue of a qusntity mvmaf be known with<br />

mactness. In survey ti, ths most probable<br />

vafue ts used es best representing the true<br />

velue of the quantity.<br />

true-to. scale-A cendtiien where map<br />

tW.9sUr~~ts em in exad agreemenf wilh the<br />

afaled msp scale. Stnm atl map projadii<br />

invoke ecxns scale chsnge, the scale b rmt true<br />

at ell @aces on a’ msp.<br />

true-l. Ffefsted to true north as opposed to<br />

ms9~t~ north. 2. Actual, as contrsstad ~h<br />

Wiimua, as true Sun. 3. Related to a freed<br />

point, eitfww on the Emth or in spaca. ss trua<br />

wind; in cOntmSl wilh relat’we, Wlch & retsl~ to<br />

a moving point. 4. Corrected, as true effitude,<br />

S. One of two alternsta velues (TrueJFalse)<br />

MIL-HDBK-850<br />

269<br />

used in 6odeen bgii.<br />

turning point (TP~ poiti on vhii beth a<br />

minus sighl (icmsighf) ad a pfus Sigfd<br />

~) are taken on a &ne 0( dwOd bveta.<br />

Abe, in tcfqmphii Surveys, any point m Whldl<br />

fhelodie heldwhiletfre” ImtNmmtb movedto<br />

emthar 6idon. Thaee turing pohfe are often<br />

msrkedfor futlxaues aetieorcfreok points.<br />

turning point pin-A deal pin about one foot<br />

brig. In Ievefing Operstbrs, the tumhg polnf Is<br />

driwen info the ground where it is neceaaery to<br />

eababfkhapointthetw iUb asiaMe in elevation<br />

fsrasfrod perfodoftlme. Whenkfusaervedtfs<br />

Usefulness at one pokd. if is nanoved and<br />

canied by the rcdrrrm for subaequad reuse.<br />

turret grmrer-A acriing instrument wlrfch<br />

permits the use of points of several weights<br />

intsrchsngeebfy without the inoonvenlence of<br />

intenupfing the acriing 10 rt@ece pdnts. The<br />

turret head ia revolved to position tb cfeafmd<br />

poht, and a.cribhg is resumed.<br />

tumhe-An ink for dmftirrg printing amss on<br />

Iithagraphiipfates.<br />

tuschhrg-llw operst”wn of adding wefk to the<br />

image on o prsas plate, mrrecting Iinaa and<br />

Ietfetfng, and addii aotids by means 01 tuschs.<br />

Also cslled lithographic dmttlng.<br />

two-base mathod-A t=hnlque of<br />

bsmmetrb fevating ufifiing ffrrw berornefera.<br />

TW bsromatera, one high ssfabtii over a<br />

known elavatbn, and me bw estebJbhsd wet<br />

a known elevation, and a roving bemmetw<br />

operating betwaen the two fmown poslficms.<br />

High end low barometers are reed and<br />

recorded, hith tempemture, evety fwe minutes.<br />

The roving barometer and terrperafum ere reed<br />

and recorded at each ststion omupbed. Osta are<br />

reduced to position end elevstion by offlx<br />

~mP@f~n. The only bsmrnatrb leveling<br />

methad sble to consistently pmdum emxs fees<br />

Ihsn *1 meter. See afso fly-by-method;<br />

Ioapfrog method.<br />

twebody orbit-llre nrotien of e point msas<br />

in the prssence of the gravitational attraction, of<br />

another point ~, and in lhe absence of any<br />

other forces. Thii wbii is usualfy an eftipse, but<br />

msy be a psrsbola or hyperbola,<br />

two-body problenr-That problem in celastial<br />

mechanics which tr,sats of the relative motion or<br />

of two-peint msssss under their mutusl


1’<br />

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grevifbnal attraction.<br />

two-dlrnan8knal (2-D) data-Aresl dsla in<br />

w diinskm. such es nolihi~ing m<br />

lslifw&lonQiiude.<br />

twdlmonslonal pantograph-in relief<br />

modd Imtdng, a rnachim pamdffii tfra cutting,<br />

et .9 predetermined scsle. of tfm tfUaad-naional<br />

temsin base fmm the ffet msp<br />

contour dre~<br />

two-point problem+ problem in<br />

det~ the positii d a point with (he<br />

known fsctor hsing the length of one lime thst<br />

deaa nd include the point to be loc3t0d.<br />

two-stop ●nlargementiroduction-A<br />

tachnlqua of fxojecting and @i 8 SMSll<br />

imsge: then oopying and prqecling it egein to<br />

the raqulrad *a. This is often necesswy *n<br />

wpy sizekwpy cemem Iimitatiens do nol permit<br />

enlefgemard or reducticm in a single operstion.<br />

two-transit method-A methed of ship-toshore<br />

Mengulstion wtwsby the position of the<br />

eour@ng best w pole is determined by angle<br />

- ‘ ‘ 6bs61Vat0nS fmm Ww tmnsits on shore sst up<br />

over ~ints PrOvieusly positioned.<br />

W-n w~ting (typogmPhy) a mstel blcck<br />

hsvirw s mised fetter w figure whiih, when<br />

inked, is uesd to meke an irqwesaion on peper<br />

orothar mstsdel. Typecen aleo bainthefmm<br />

of negetiue or poaltiie stripping film. Cetagcdes<br />

of type include frond-set sold type: her type,<br />

such as Limfype; Monotype (punched rspe to<br />

metaf~ photetype (film negsdtie or posiliie); end<br />

Pfrdonryps (reps to film). Type is identifkct by<br />

its afyia and size.<br />

typography-The art of type eemposition end<br />

printhg from misad type surfaces.<br />

MI L-H DBK-850


U.S. control ourvoy nata-’l’he two corrtml<br />

survey nafe bdng extended over the United<br />

stabs by fhe National f3eodefk survey fer the<br />

tird of rrautkaf cAarfe and fcfmgrapfric mapa,<br />

z=d(k~=z”sv<br />

=-d’”””+”” fJ=Wma, afawofwhioflhava<br />

bean Llxullfd by the Unflad stems Geological<br />

Survay. The Corps& Englnaara, arxl other<br />

-~ m date Cfarivd h lfrls survey<br />

are being c&@Lefad and CcrTafatad on the<br />

North A~ datum d 1927. lb Natfcrral<br />

Gacdafk Survey la currently rawrrrpufirrg the<br />

hortsonfaf corrfmf network to the North American<br />

dalwn of 19ss. (2) The Variical amfml cAlrvey<br />

net consisting of tires & firsf-crdar and aacmld.<br />

order spirit bavahg wtrkdr datarrnirre the<br />

ebvatbns of tfrouaarrdsd bansh rmwka nbove<br />

a aernmorr datum, mean aee level. Thb nd<br />

includas times of levels run by the United States<br />

Geobgkal Survey, ha Cape of Enginaem, and<br />

other organizafii.<br />

U.S. Engineer praolso taveling rod- A<br />

~king rat of T-ahepad cmes aasfiotr, 12 bet<br />

*, 9tid In .arrtirnfrters.<br />

U.S. Gaologkal Survey lavet-A level of<br />

~ d- ~, -wed at atah+as ateet. ft<br />

has en infernal fccusing la!aasopw the level<br />

b-e is omfemd by the end-ccrirrckienca<br />

method, affeofad -h t~ aid of s ptfwll dSVi04<br />

and Sfellife mirmr wirkh can be ad@tad by the<br />

observer.<br />

U.S.<br />

rod-1.<br />

Gaologkal<br />

A -tdrm .C––.<br />

SurvoY prods.<br />

d rkduetad<br />

Iermllfrg<br />

in mrde md<br />

hactima deyard. %”rn-&forea&~th&<br />

oruaatvima tothenaaraat thcuaarxifh of ayard.<br />

llw eum of tha three readings is than the mean<br />

raetimg in feet to fha naamst thouacndfh. 2. A<br />

target md of ptus-algn (+) cross aaclkn, a Me<br />

over 12 feat in Iwrgfh. Rrare are two krrrns cd<br />

this rod fhe aingla-fargat rod and the doubkrtergat<br />

rod.<br />

U.S. National Map Accuracy<br />

Sfsndarda-1. Horizontal accuracy: (I) for<br />

~P8 al Publkat”mn scales Iargar than I :20,000,<br />

90 percent of al wall-dafhed faaIurss, with the<br />

exsaptbn of those unavoidably displaced by<br />

exaggerated aynrbcfizatbn, will h foctded Within<br />

1/20 inch (0.8S mm) of their geographic<br />

MIL-HDBK-8S0<br />

u<br />

paffbna as rderrad<br />

fwrraqr at p&fbUon<br />

te the map pmiadkw<br />

scales d l:~,000or<br />

(2)<br />

smaller, I/W) irwh (0.54 mm). 2. Vertmsl<br />

OOparced daffsonfwasnd<br />

elavafti infaplafad from ocmtcum till ba<br />

ascwafe within ena-fmf cffhafmakcorrtour<br />

Ir$ervef. Dkcmpamw “ in ffwcccumcytrf<br />

ccmfcnus and S&vafiona bayond fflk tcl’sransa<br />

-Y ~ -~ by assuming a horizordal<br />

d~m wfthin 1/50 imfr (0.S0 rrun). Alac<br />

called map accuracy standards; national<br />

map ●ccuracy standards.<br />

ultrawlde-angk kna-%a suparwldo-<br />

●ngfo kna.<br />

uncheoked ●pot ekvatlon-Ekvalion<br />

detemrhad by undmakad Wd ew’vay maffrata,<br />

such as eida tis on rladia lima. undmkad<br />

verticai angles, and bammafria iavdkrg. Also an<br />

elevation datarminad by rapealad<br />

photogrammatric raadtrrg.<br />

uncontrolled meaak-(JCS) A masaic<br />

-- ~ uxerraded prints, the derails of<br />

whii have baarr r-na$chad from print to print<br />

withcut grmrnd control or other orientation.<br />

Accurate maasummenf and dimcfkrn cm?rrd ba<br />

asomn@ibhad. see ako controlled moaalc.<br />

undwgmund marfr-A survayinu mark eat<br />

●-d plurrbad below tha Oantar d a eurfase<br />

mark and eapamtad Iharefrorn so as to praserva<br />

t:~~ticm in 0ss0 of acsidari to the aurfaca<br />

undershoot-A data omisabn which coours<br />

during the dats CSpfUm p~m, prdc.shrfy<br />

during rnarrtsrd d@tiirng. In an undershoot<br />

situatbn, baar rkta falls ahwr d rrnsting an<br />

interaaafbn. An undarahool may be oormotad<br />

by a snap dtwam function.<br />

undevsrlopable-A surface, such as a<br />

6phera, that cannef be flattened to forma plane<br />

without compressing er stretchkrg aema part of<br />

it.<br />

u ndo-(dqifal) The ability to cwcel a previous<br />

command to the mmputar.<br />

undulation of the gaold—See geold<br />

halght.<br />

L71


I MIL-HDBK-850<br />

I<br />

unldlmortcrlonal rnagnlflcstion— Translorrnclion<br />

ef One redangle into tihar of different<br />

PfoPoff*.<br />

Urrlversal Pokr Storeographk (UPS)<br />

grid-A rdler’y grid system baaed on the paler<br />

sferecgraphk pmjecfii, a@ii tornefMof the<br />

Eettlfs pokr regions north cd 8.t”f4 end south d<br />

Sons fsthdaa.<br />

Unlveraal Rectlfler (UR)-Pmc=sor used to<br />

rectify knsgery In wpporf of DMA production.<br />

W prirmrry furrdbn et the UR is te generate<br />

recfifii point poeifiin dets beses. Sea sleo<br />

Unlv*r8el Rectlfl.r Segment.<br />

Unlversat Rectlflor Segment (UfUS)-<br />

Sagmerrr cd CMA’s DPswhichpmoSS9m<br />

imfrif=yh df copyformate pmdUCXPOiIII<br />

Peaifiorring Dsfs Seees. See alee Urrlvoraal<br />

RsctiflOq Dlgitd ProductIon System.<br />

Unlvorsel Spece Rectenguler (USR)<br />

Coordlnete System—A right-handed<br />

orthoganel cmerdkmte system with its erigin et<br />

the mar of the Esrth, poaifiie x~is in the<br />

equetorkal plcne and pesslng through the W<br />

meridisn, poskiie y.a’k ~ the equsterial plane<br />

end passing ihreugh 90° east meridian, and<br />

positiie z-exia ebng the retetierral sxis et the<br />

Earth and psdng through the North Pole.<br />

Unlverul The (UT)-(JCS) 1. The besis fer<br />

aacfinettd disaarnirration of time signets,<br />

co-ed tmm 00W et mktnluht. Also called<br />

Coordinated Unlvaraal Time (CUT);<br />

unlvaraal time coordinated. 2. In celesfiel<br />

@elti Sppketlcma, the time whiih gives the<br />

errecf rofafbrral orientatkrr of the Eerth cbfeined<br />

fmm CUT byq#yiiincmmem s determined by<br />

the US Nevd Ctt%ervatery. S. The otfii *II<br />

time of the United Kingdom. Fermarfy celled<br />

(?rewwloh Moon Time.<br />

Universal Tr.sneverso kfercetor (UTM)<br />

coordlnatss-Quantities vvlich designete the<br />

Iecatien of a peint err ths Universal Trarwweree<br />

Memtti grkf.<br />

Unlvareat Trmrsveree Mercstor (UTM)<br />

grfd-(JCS) A dfifary grid system besed on the<br />

trensveme Mmcstor Projectii, applied to mePs<br />

of the Earth’s surface exierxfhg to 8.tON end<br />

80”S Iatifudaa.<br />

univarsal analog photographic<br />

rectlflcetlon syste-An electronic<br />

I 272<br />

I<br />

radifiitionayefsm pemiffingtb rapd trsnder<br />

ofrketeil from trimetmgen w eny othw type of<br />

awisl phefogm@y, tO ~~ ~~<br />

cvversge. The system =msists d low bssic<br />

oompenerdK input Szanner, cnrrpular, console,<br />

ard x-y pfoffer. Ateo cekrd ●lectrorrlc<br />

sketctrmaster.<br />

unlveraat lnatrument-See *ttaztmuttt<br />

Instrument.<br />

universal Iovot-see circular favol.<br />

unlveraal plottfng sheat-A plottkrg sheet<br />

on whti eiiher the fefiluda m bngitude hres am<br />

om”med, end are to be drevm in by the user,<br />

making if pcssibte to quktdy cam’ratrucfa pktfing<br />

sheet Ior any part of the Estth’e surface. see<br />

alsa plotirrg chart; posltlon plottlng<br />

sheet.<br />

unlvsrsel sketchmaster—A type of<br />

skekhmaater in wtkh vertkal or c4~que<br />

photographs mey be utilized.<br />

universal time coordkretod (UTC)-AISO<br />

cal)ed Coordinated Universal Thne. See<br />

Univemel Tima. . ---\<br />

universal transforming printer—A apecielly<br />

designed printer for rrrekirrg gless d-as in<br />

whiih e known cemera distofiion is aiiinstad or<br />

wnw==id for,. or in some cesee infrcducad,<br />

The @as -wee my be rapmrtuced at<br />

ade, entarged, or raduoed.<br />

unperturbed orbit—See normal orbit.<br />

unsteblo-type grmdmeter-A gravity meter<br />

which utifiies a moving system Wrkh<br />

epp-thee e poiti of instabiki such thsf emsll<br />

ctuwrges in grevity produce relatively large<br />

nmtims et the system. Sss elso astatized<br />

gravlmeter.<br />

updetlng-lhe sepabilii to rneke chsnges or<br />

add new inforrmetien to exietirrg deta.<br />

uPPO~ bmnckmt half d e rne~~n or<br />

celestal merkliin from pele to pole whiih<br />

passes through e place or its zenith.<br />

upper culmlnatlO*See culmination.<br />

uPPer llmb-lhat helf of the outer edge of a<br />

celestlal body heving the greatest effimde, in<br />

mntrasl wiih the lower limb, thet hrdf hsving the


I<br />

I<br />

least altitude.<br />

.— ..— .—. .——_ _<br />

IJPPr MOtb~6WVeYbg) Rotation of the<br />

upper *M 0/ a repasting ~.<br />

war tinah-Tranti d a cdtdd ~ ~w<br />

the ippar brench of ths celrdal meridiin. Also<br />

celled cmtpartor transit. See also<br />

culmination,<br />

uaar httaflaca-Ths method by wlich the<br />

human qaamtcx mmmunidns with the vWiOuS<br />

dste base and appliibrra modules.<br />

user raqulramant ●mlysls (URA)-The<br />

study of the needs C4 ths polerrtisl system<br />

Uaara.<br />

UTO tfme-Tfre mesn universal time ~<br />

frem otmewetii ol Iims ot eisr transils. Sinca<br />

tha directions CAthe maridismr chsnge with tima<br />

b-usa of the motion c4 the pole, the IJTO time<br />

will, thus, be affected and N, thamfora, ba<br />

Irrsgutsr. See also UT1 tlma; UT2 tlma.<br />

UT1 tlms-l%e true angulsr rotation of the<br />

Emth about its instantaneous spin sscis in the<br />

mean ~untorisl 6y61em of dstas. UTl is<br />

cbtsirrsd fmm Lrro by 00r1adii UTo f’w the<br />

dfierence between the instsrrtsrreous and<br />

maen kmgttude e! the obsawing station, Sines<br />

LITI is keyed ~ to the instmda-s<br />

mtden ef the Esrth, wlii is not sttitly uniform,<br />

UTI does not ~- urdicimly. Saa also UTO<br />

time; UT2 tlms.<br />

UT2 tlma-llre mean angulsr motion ot the<br />

Esrth, treed of pmdHtb& periodic vtui.don bul<br />

still affected by bregular vatiatii and aeculsr<br />

varMerra. UT2 la cbtgin.art b UTI ~<br />

cOrmdng u—rlfor Maaaral vartstions in rcddii<br />

rote. Sae elso UTO tlma; UTl tlma;<br />

unlvoraal tlmo coordlrmted.<br />

MIL-HDBK-850<br />

273


vacuum box-The frame, wrrfeinirrg ils own<br />

Vssuum unit, Whfch encfmes the rrmkf fer the<br />

fermktg d pfeafii refid maps.<br />

Vaia81a Comp*retor-A precise dbtarrce<br />

measuring Inatrumsrrt thel uses c@icel<br />

imarferometry for making masauremsnfs. h can<br />

reassure distensas ss grast as MM meters with<br />

Ofr===Ydl Wfmlo7.<br />

value-Sas abaoluto VShlO; ●d]usted<br />

valrm; most probablo value: obaanmd<br />

valrm; tru. value.<br />

vanlshlrrg llna-The straight fine on a<br />

photograph t@n which lie 811the vanishing<br />

points of all aystema ot psrellel lines psrallsl to<br />

one plane.<br />

vanlshlng paint-l%e knege, in the pfane of<br />

a ~~~h. of the peint towmd whish a<br />

system of parallel firrEs in ths .3@ect spsce<br />

mnvergas.<br />

varlablo contour interval-A nonuniform<br />

mrrtour intsrvsf. ft msy rssuft tmm the U6S of<br />

cartogrsphk source me!erkrls which do not<br />

so~in a constant sentour interval er from<br />

ade@ng the oortteur interval to specifii types of<br />

Wrmfn for the optimum perfrsyal of diet<br />

fsstures.<br />

varfabfa Iongth field-A field WIWSS length is<br />

determined by the amount ef sforege needed 10<br />

atom ifs contents. Useful for chsresfer strings and<br />

ceotdhs:e atrfnga, both of wh~h are huhty<br />

vsriabfa in length.<br />

variable fanrnh recorde—These remrds may<br />

heve a variabl-e number of fiefds (dele elemantsj<br />

or the fields msy be of varying fsngfh, or both.<br />

Verieble-fmgth mmrde typiilly hsve defimifsd<br />

fiekls atior &yie murrts to fediiate pmcsseing.<br />

Sss also fixed-length records.<br />

varlabfe perspective camera system— A<br />

system whti, in its simpfsst fwrn, mnsisfs of a<br />

rAemJard+pa view camsrs, a Isrge eparture<br />

front-surface mirror of spherical mnfigumfiin.<br />

end en eesal used in tfrs recfifiiticm of highfy<br />

tifted bng focal-length phetegrephs, and the<br />

trsnaformstion of maps and charts fmm one ,<br />

projecflmr to another. When the csmera<br />

MIL-HDBK-850<br />

v<br />

2 74<br />

mnponeM krqkced wifhapm@fOr, if<br />

~ possibk 10 expedite the recfifkationof<br />

Iuner pt@Ogmpfy tekan by terrsetriel<br />

observatori8a.<br />

variable ratio pantograp&S e e<br />

pantograph.<br />

verWrco(u2~Tha most SornmOnly used<br />

measure of d- or error In atstiatkef<br />

ansfyeia. ffieefao oelfsdthe mesnaquered<br />

davietii. Vaderroe is cdctdsrd by ri tddng<br />

fhaeumof thaaqusM davWonshomtha<br />

mean fof each of n cbaervetiens. Then the sum<br />

is dii”tied by n-l.<br />

varlatlorr of coerdlnato rrmthod- A<br />

malhcd et e@a~mg massursrrrants in wtriih the<br />

mordinetas of geodstk points ere varied so as<br />

fo bsst fit the obaarvstiorm snd retain<br />

msthemstlcel Ivwmrgeneity. Sea obaawatlon<br />

equationa; varlatlon of perametera.<br />

variation of latftude-A 6MsII dwmge in the<br />

astronomic isthude of points on the Eerfh, due<br />

to V.srfet)orl d fhe @es.<br />

varletlon of pamrneter-1. An interactive<br />

msthcd to edvii mm@ex equations by<br />

successively cJeam epproxirn=dkms of tha<br />

variables, usuelfy arnpl@ng the more rrignifiint<br />

terms of the rust dsrivatiwes c4 msthemstioelty<br />

prsciss funcfiens thst must equal zero cdy<br />

when the correct vefuas 64 the variables sre<br />

uti to compute the funcliorw. 2. The<br />

okmrvsfksr eqlaMona method of beef squares<br />

adjustment is eemafhnss referred to as the<br />

varfation of parameter mctiod of Iosat<br />

●quaras sdjuatment bmausa the<br />

peremetam of ebservat”km equetlmrs era<br />

determined by varietion of perametem.<br />

varletlon of tha poles-A small variation of<br />

the Imetkrn et the irr.stantanseus exis of rotation<br />

of the Eerth with rseuecf to the ohvsicsl surface<br />

thereof. Also called “polar motion. see elso<br />

conventional Intarnatlonaf origin.<br />

varlstlonal lnaquallty-An Inequality in the<br />

Mean’s rnetien, due msinly to the tangential<br />

m~nent of fhe Sun’s attraction.<br />

varlstIon—See magnatlc varlatlon.


I<br />

1<br />

vartomster+trr instrument for ccr~ring<br />

~-~ fo-! aspecialty of tha Earfh’s<br />

megnatic bakt.<br />

vactograpM stwaowopk photogmph<br />

~- of two Stpadnpaad imagaa that<br />

pdarfxe fight inpfanae 9Wapart. W?rarrfJwwa<br />

imagcm are viewed through Pdardd apsrdades<br />

wifhfha @adxatii mmaaftightnn@a, an<br />

impraasbrr d dapth fa dfdneri.<br />

Vector Product Format (VPF)-A 9aorafatii<br />

data structure daaigmd fm the<br />

Ixeviekrn C4vader pmduda en CD-ROM madii<br />

and manff?ufalad fn G~f Irdormetbn<br />

Syafema envfmnmants.<br />

Vaotor Pmduat Standard (VPSM aulte<br />

of uaaJ aysranl Oriardad atmldards<br />

erwornpaseing VPF d~itiiing conventkms, Wing,<br />

facdum atfdtrdng and ooding. see ab Vector<br />

Product Format (VPF).<br />

vaotor data-CIata which represents aach<br />

cartographic feature by an enti7y description<br />

(feature sode) and a spatial axtent (gaogmphii<br />

pesitii). Gtrograph= poairien mey ba m<br />

~. nmarwmd (horizontal poaitiin onty) or ihreadtinabnaf<br />

(incfudhg alevaticm). Featurea are<br />

Catagm’izad se point, tine, or area faalurea. The<br />

poaitii of a peint faattme is d~ bye<br />

tingle cowdkude @r (or triplaf for fhms<br />

dimanskrad date). The e+fii mxfant of ● Iina<br />

feature Is daawbed ty a string of cOOrcfiitea of<br />

polnta lying along the finabvhihip~ ~nt C4 en<br />

area feature k ~<br />

boundary aa e fine featura, Vader data may be<br />

sterad in a ~uential, 4 chain node, or a<br />

tefmlogical data atruckxe.<br />

vector map product (VtAP)-A ganaric term<br />

uaad to dasmiba an ataUrOnk map d~fay<br />

product, m vador form. The VMP coufd be tiie<br />

~m (--). pof~s or arrm fmfygon<br />

dafiiad araaa, diapfayad aa such or<br />

avrrbofizad. The f6atmaa mav be attrftarfad aa<br />

ki aurtece I-natarid. Structuraf”cmpasirion, or<br />

radar aignifkanoe. For visual displays color fill<br />

aefhvam may be required.<br />

vaotor quantlzatlon—A Ioaay compression<br />

krchniie in tiih bbcka of data ara matched<br />

to a limited sat of defmad Lrfoc& calfad<br />

ccdewords.<br />

vector refresh dleplay-A cethede ray tuba<br />

on which the image ia dkpfayad aa e vaster and<br />

MIL-HDBK-850<br />

. ..-<br />

L 75<br />

whiih mu.s4ba mtrashad by a new pass of the<br />

eladmr baam about SO timaa a sacond.<br />

vactorlnl ●ngla-l%a angle betwean the<br />

fbrad Ii b which the diractien ia referred and<br />

the mdiua vactcv. sea ake polar<br />

coordlrratea.<br />

vector-1. A quartity ~ing both<br />

magniluda araf dkacfbn. 2 (data StnJcfura)<br />

A data strudua which ssqhalzaa peatfii.<br />

Hmmgwmam write ●m pehla, lines, and<br />

@YI@S. 3. A ~=fd ins segment, wffh<br />

magn~da comrnmrfy mpraaantad by lha<br />

ooerdmetaa for the pak of and points. 4.<br />

(-W pr%rtin@atbrnaff+ Vector<br />

dararafamto titnrntha tonn dan array wkh<br />

Olla dimanabn.<br />

velecfty cOrraatfon-A aorractbn appfbd 10<br />

the aped of fight to obtain the true apead in<br />

cxm.sidaratbn of humidii, temperature, and<br />

altitude for use in ahoran operations.<br />

Venlng Mdnoez forrrrulna-Formulas for<br />

coming deflectbns d the vatt”kxd fmm gmv”~<br />

data.<br />

verbal acala-Sea equivalent ●cala.<br />

verffy-1. To datarmfna @rather a<br />

tram=r@tii of data er cxhar ~bn has been<br />

acc4m’@shad acauratety. 2. To senfirm the<br />

accuracy, poiirayaf, and con@atenaaa d digitaf<br />

data with reaped to es4abliahad standarda or<br />

qmdfkations.<br />

vernal aqulnox-That pdnt of intamectiorr of<br />

the adii.k and the Salaatial aquater, occupied<br />

bythe S.naait changaa fromaeuihtonorfh<br />

dadirmtion, on or ekouf 21 March. Also cafled<br />

tfrat of Arfea; firer point of Arfes; March<br />

●qulnox. Sea afae mean equinox.<br />

vemhr cloaum-l%e dfieranoe between tha<br />

initiil ard W vernier raadinga duting the<br />

survey qmrafien d akaing the herizen.<br />

vernier—A short, auxiliiry scale affuatad<br />

abngaide the graduated asale of an instrument,<br />

by maens of which fredonaf pmls of tha<br />

amalleef dwision of the fxknaty acafe can be<br />

rnarmurad aocuratefy. sea also contact<br />

verrder; direct verrrler; folding vomlen<br />

optical vernier; retrograde vernier.<br />

vertex (vafilcea)-The higheat point, The<br />

vert”ces of a great cimle are fhe points neareat


I<br />

I<br />

I<br />

I<br />

I<br />

Ihe p0b6. AfsC ded ●pOX.<br />

Vorfox of curve-sea point of<br />

Int.rsoctlon.<br />

Vettkal Obetructlon Data (VOfl)-Oata<br />

fib containing dmte poaitim and hei@t<br />

irderrrmt”bn d menrneda smf nstursl objads<br />

exfartdii ebove the esrth’s a.urfeca et haiihte<br />

thst Coufd mnstmin eipkanean dcnliwmisaife<br />

ffiiht6 at levels Sslsbliihed by tin planners.<br />

Vetlkd obcfr@kta Include msmnsde<br />

ObStfUCf”~S such es radm towers, emekastaoka,<br />

b~es, powwfinas, and other ebjada above<br />

apeciried minimum efsvatbna. vOD is<br />

~ by the Prcb6fMiiic Varfksd<br />

obstruction Dsfe (Pvoo). see akm<br />

Probabillstb Vottlcd ObstructIon Data.<br />

vartkd sngk-t. An angfe In a vatticsl<br />

plsne. 2. (surveying) One of the direstbns<br />

whii form a vemid engle & uauaffy either the<br />

dirsctbn of the verticsl (zenith), snd the angle in<br />

termed the zorrfth dlatanccu or the fine of<br />

intersection of the vertkal pfane in wtkh the<br />

errgfm free with the pfsne of the trorizen, and Ihe<br />

angle is termed the angfa of clevctlon or<br />

●rgb of dopresslon, or simply the altltudo<br />

(plus or minus, as the csse msy be). Ths vartiil<br />

~W~ ~~ We di=ims, rrsilhsr of ti~h<br />

has in the ptma of the horizon er caincicbs with<br />

the vertii, is uauelfy dtsined from the<br />

canbinatim of tvm verticsl sngfas se defined<br />

above.<br />

vartical ●gulatiOn-The pmcesa of<br />

OMaining difhe.nces of efevation by means of<br />

obearvaf vertical engfae, cotinad with Iangfha<br />

ef fines. In geodatb wdc, trigermrnatric fevefing<br />

is used wilh the same rneening.<br />

v.rtlcd ●xla+lheodefiie: trsnsif) Tha fine<br />

through the center d the msfrumsnf abouf<br />

#ii the akdede rotates. FW an instrument in<br />

cxm@sfe adjustment, this axia occupies a<br />

verfioel pesifkm, passes through the oemer of<br />

the fmrizorrtal tilde, and is perpendicufer to its<br />

plane.<br />

vortlcd bridging-see brldglng.<br />

v.rtlcal ckcla-1. A great circle af the<br />

celestial sphere, through tfrs zenflh and nadir.<br />

Veti’ksl clmfss are perpendhhr to the hodzc.n.<br />

2. A gradueted disk mounted on en instrument<br />

in such a manner thst the plane of its gredusted<br />

surfsce can be pfsced in e vetticsl plane. It is<br />

primarily used for rn9ewring vertical angles in<br />

MIL-HDBK-850<br />

-.<br />

z’76<br />

warenomic and gacdetic wark.<br />

vanicsl colllmafor-A tekcoopa so mounted<br />

fJ’WtiCdtiti@-k~ tocmirckle<br />

wifftffre vettisa d(wdktitidti~k).<br />

The Vanicef COllinmaor Satv- as en @u<br />

Plun-hhxl tmaybadaaimadf or-hpf=+tw<br />

amsrkctt thOgrOUrKf dwOCfiY~r an<br />

h’@Nti en n h~h tower w * cantering an<br />

iluSN_ Oil 0 h@l klWSr di=t& OVOr a I_tUt’k<br />

on ths gmurrd. Abe r4ed optfcd plummet.<br />

verflcd cornparator+pendulum) A stand<br />

das@tedforfhasqurtcfapnduJm, aixr<br />

of known length, and fvm mismrnefar<br />

~, so placed with rdaretv=a to one<br />

another that the fengfh d the pandulun can be<br />

measured.<br />

vertkal control datum-Any feval surface<br />

(as, far exan’pfa, mesn see Isvef) teken aa a<br />

wrtssa d refere- fmm which to reckon<br />

elevations. Alee called vwtlcaf datum;<br />

vertical gnodetlc datum. Sea also d ●t urn<br />

Ieval; refarence level; reference plane.<br />

vorflcal control net-+ee eurvey net.<br />

doflnltlon 2. ,<br />

verflcal control pOlnt—See controf point;<br />

control mtmtlon.<br />

vertical eontrof-The rnessurements taken<br />

by aurveymg methods for the detemrimsfbn of<br />

ebvetbn onty with respect to an imsgfnery favef<br />

wrfac9, uauaffy rnsm aee leveL Sea afse<br />

survey nat dafinitiin 2.<br />

vertical coordlnetea-llm vartical dwtanca<br />

of a point above or babw a rsfarenoe datum.<br />

Points mey bs piua or minus ~mg to<br />

whether the point is ebeve or bebw the datum.<br />

vertkal cutva-A psrabofii curve d to<br />

connect gradea d dtierurd afepe, and used at<br />

the vertex d e grade to avdd the sudden<br />

chsngs M directim in peaa4ng from ma grsde to<br />

the other. Tfis rnathed of grsda change fa<br />

ususliy used when there is an afgebmis<br />

dflerence of more thsn 0.2 percent in the two<br />

opposing gredes.<br />

verflcal datum—See vertical control<br />

datum.<br />

vertical deformation—in refetive orientetien,<br />

the cumulst”we medel warpage affecting Ihe<br />

vettksl detum from x-fill error and ~tift error.


vcrlical ●xaggoratlon-1. The change in a<br />

rrrcdel aurfeca Crelted by pqerthafly raising<br />

lhe~rarrr heighrof alfpoitissbeve the b9sa<br />

~.<br />

level tie mkdning<br />

Urcmea90ftha<br />

the same base scale.<br />

vartksl scafernferthe<br />

2.<br />

herizontd<br />

retiaf map.<br />

scale ef ● Iermrn model or plssfii<br />

vortlcal ●xtenslo~ ●xtenslon,<br />

defsitii 2.<br />

vortlcal geodotlc drrtu~ee vwtkd<br />

control datum.<br />

VWUCSI lntonslty-The magnatk intens”~ of<br />

the vertical ~rrent of the Earth’s msgnetic<br />

field. rtrckened positive if dewnwsrd, negative it<br />

upward,<br />

vertical parallax—see y-parallax.<br />

vertical pass point-ses supplemental<br />

olevatlon.<br />

vertical photogmph—An eerisl photograph<br />

takerr with the axis of the earners being<br />

tintsined as okxdy as possible 10 a truly<br />

vertical posbion with the rssuftsnt photograph<br />

laying a~roxirrralefy in a horizerrtal plane.<br />

vertical ptana-1. Any plane psssing<br />

Ihmugh a point on the Earth end containing the<br />

zerdth and mdir of thst pdnt; else a plsne<br />

containing a plumb line. 2 (surveying) A plsne<br />

at right angles to a horizontal pfsne and within<br />

whkh angtes and dMmcee are observed.<br />

vertical sketchmeatar-A type of<br />

sketchrnaater in tilch verfiosl phoregmphs are<br />

Ufifiied.<br />

vortlcal etoreotriangulatlO*That perlien<br />

I OfStWSOtriSr@Morl &ncemed with lb<br />

eatabfiimanf of vedikot data. Varkal<br />

stersotriangulation is etten Iirnfted er prscluded<br />

aa an cparatkrn due to the more rigid scarmcy<br />

starxtards established for vertical pesitiens thsn<br />

for fwfzorrtal pcMorrs.<br />

vertical-anglo bench mark (VABM)—A<br />

bench mark with ef.evalion estsbliihed by<br />

vertksl angle me!hak. See alse bench mark.<br />

varllcel-anglfr station—See<br />

aupplamantal etation.<br />

MIL-HDBK-850<br />

Z77<br />

vOrtlc~f-The fine perparxliidsr to the gsoid at<br />

~Y~*.tktid~rn~ UWfCSCeaf<br />

grawry sch. sea UJsobed Vartkal; mass<br />

●ttmctfon vortkal: normal, rlefinltion 3.<br />

vfbmtiOrr-4 eingfa rnovemanf of a pendulum<br />

irrahher dbctbn,toorfro.sea Stso<br />

osclllstlon.<br />

Wdeo Point Posltionlng Data Baa.<br />

(VPPDB)-A DMA analofj VkfeO dac prodrrd<br />

rhii pmvkiaa ● mmmrxpk precise positiiing<br />

ca@@yniriihi amoreversattia rrdeaeLarfe<br />

uaa fhn the Anstyiiil Photogramotrk<br />

Peaitiing System (APPS). VPPOB was a<br />

WmOMl COIWJfw to Mow reel time aordinate<br />

rasdouK designed for ease of use arxl m“nirnsl<br />

Imining time.<br />

video disc [MCGTJ-A 30.5 cm (12”)<br />

Cmstont Angrisr VaJcdy (CAV) ansbg video<br />

discca#rle ofstorir# video imeges ones~<br />

aide (equkwlerd 10 spproxirdely 200 everag-<br />

Si2ed map chests at m dflemrrr kids of view).<br />

See also CD-ROM.<br />

vldao rrrop-hy one of a - of<br />

cartogrsphk preduds thst are *umd, stored,<br />

m-d d~yed using anslog video signals.<br />

vlewfltrder-(aerial camera) An atmiliiry devica<br />

which show the fiikt d view of a camera. tt is<br />

used in the takingd VOrticsl.9arkIpfrotqephy<br />

to con-act cmb angle and rrmintnin fonvmd Isp<br />

(end Iep).<br />

vlgnatthrg-t. (photogmphy) A gradual<br />

reductiorr hdenaity ofpafla ofephetegmphii<br />

image due to the stopping of some of the mys<br />

errtering the lens. Thus, a kms nmurrting rrmy<br />

Inlerfam with the sxtrems oblii mys. An<br />

ant”~netting fitter is one thst gmdrmlty<br />

decmsses in density frerrr the cs’ttw teward the<br />

adge$ it la used with msny wide-angle lenses to<br />

procfuce a photograph of uniform den.shy by<br />

cuiting down the overexposure d the center of<br />

the photograph. 2. (fiihography) A photographic<br />

IXOCeSS wfriih portrays a soiii cmlor in a soreen<br />

vdkh shsdes oft gredudiy inlo Ihe unprinted<br />

paper. @xr water is often ahown by this<br />

methed.<br />

vlrtuel gravity-The forca of gravity on an<br />

etmmspheric parcel, reduced by cerrtrrfugat hrce<br />

due to rhe rrmtk.n of the parcel ralalive to the<br />

Earth.


virtual Image-An image that cannot be<br />

shewnen aeudeceb ufisvkbk,as ina minor.<br />

virtual PPI reflactoacopa (VPR) chart— A<br />

type d mder cherf.<br />

vlslblllty chart-A epacisl-purpoee MSP or<br />

other grephii shmvirrg wtrii amae sen be seen<br />

ard these whiih sennet be seen fmm a ghmn<br />

observation pint.<br />

visible horizo~See apparent horizon.<br />

visual esuify-rl meeaum of the abiiii of the<br />

human eye to aapraie dafails in viewing an<br />

+ect. The reo@cel of tha minimum ●ngufer<br />

eepsmtbn, in minutes of em, of hvu lines of<br />

defeil whiih am be seen separafefy.<br />

MIL-HDBK-850<br />

vlsuel renge-The fimifing range of a light<br />

determined efier teking info eocount both Ihe<br />

geogrephk range and the luminous range. The<br />

g~me mnge is the msximum disfence at<br />

which the curvature cf the Eerfh pmrniis e fight<br />

to be seen fmm e paniculer heighl et eye<br />

willmuf regard to the luminous intensity of the<br />

I@!, The luminous range is delafrninei tmm .<br />

the Iomwn nominal luminous mnga, calied the<br />

nominal mnge. and the existing visibifii<br />

wnditions. –<br />

voting (TERCOM)-The technique et having<br />

e vehkte ffy ever the tarmln cs4emd by three<br />

unique but canqiernentary mspe wilhin a fmife<br />

d~fencxr, cmn’pering the calculated positional<br />

accuracy within each d the maps arsd<br />

determining whether or not to @ata the<br />

vehkie navigetien eyefem bemad on hew obeely<br />

the three poeitbnsl accuracies ceqxwe wffh<br />

each other,<br />

vulgar ●stebllshment—See establishment<br />

of the port.<br />

278


MIL-HDBK-850<br />

wading rod-A rod, gmduafad in bat snd<br />

larihs c4 feat, used for @ream gaging in ahaflew<br />

wster.<br />

wall map-A spscisf-purpow map of a targa<br />

ama daaignad IO be dkpfayad on a waff.<br />

w8ndor—Sas zpparant preooaalon.<br />

want of eorreapondcmee-%e y-psraflax.<br />

warpad mocpl-hy spatial rrrodal wtkh, due<br />

to PWOW@UO dielfnthma or wiantdon errors.<br />

haeamodef datunrwhich iadsfermedor<br />

otherwise inaopabls of behg leveled. see also<br />

flat model.<br />

water leveling-A mallwd of obtaining<br />

rale~e abvationa by obaating heights with<br />

rs%=f to the aurtace d a tmdy of stilf wstar.<br />

water atape recordor-An autornstk<br />

r- kwtrumant wirkh rwwrds the ~e *M<br />

tall d the wstar surfacs at s atrasm gaging<br />

station.<br />

wavelength--9 usntilafive apeeifketion of<br />

kinds of radsrd energy. %s ak dominant<br />

Wavolongth.<br />

waving the rod-in leveling, a techn’que<br />

whweby the rodrnan slowty pivots the ksvafhg<br />

rod toward and away fmm Ihs instrument<br />

poaitim The least reading obtainable is the<br />

propar orw to be rwxrrded.<br />

waathar rnap+JCS) A map showing tha<br />

I weather aonditii prsvrding, or predicted 10<br />

I<br />

I<br />

I<br />

Pfma, ovswa sonddersbla araa. Usually, the<br />

rnep is baaed upon westher observations taken<br />

atthaaama Wnestanumberc4 atatkma.AlaO<br />

called ●urfaaa charta; ●ynoptlc chert.<br />

see also map.<br />

waber—(gsomsgneiism) Unit of magnali flux.<br />

In the mks Wstem, 1 weber = 1 pulalamp = 1<br />

kgm2/arrrp .s&.<br />

wedg+optics) A rt#mcting prism of very smsfl<br />

deviation, swh as those used in the eyepieces<br />

of some stemoacopaa. Ataa called 0ptlc8/<br />

wedge.<br />

w<br />

279<br />

weight fasturaa-l%e process of<br />

syatwnslicdly hcmasing the value d IS<br />

padiwlsrdats akwnsr$ ordamantaaoaato<br />

give that akwnanf more aigniticara in the<br />

Snsly.da m .kwtatkme.<br />

walghted mami-A value obtained by<br />

mWW~*da-*d VdUSSbykS<br />

assigned weight and dividing the awn of those<br />

pruducfs by the sum d the waighte.<br />

weight—The ralatiie wIua of an observation,<br />

aourc.a, or qusntity vhwr oorqmmd tih @her<br />

ebservaliona, sources, or qusntdiaa of the aams<br />

or ralatad quanfkii. l-ha Vafua ~fJY<br />

ths most reliable rnsthod is &Qti the<br />

grsatesf weight.<br />

Werner map projectlo~A particufsr caae<br />

of the Bonne map prujectii. in which the<br />

standard psrsllaf is al the pole, end the tangent<br />

cone bamrnaa a tangent pisrw. Any one<br />

geographk rneridiin is cheaen w the centml<br />

meridian and reprasenlad L7ye atrsight &rm,<br />

dwided to axsct scsie. The gsogmphia psrallefs<br />

are raprssamOd bf circular ems, also diviisd 10<br />

exact scale, and the olhsr meridiins are UJrvad<br />

lines.<br />

wast point-see prfma vertiaal plane.<br />

woatlng—See daparture, definitkrn 1.<br />

wide-angla lwt~ lane hsving an angle of<br />

covaraga between 76” end 100”. A bna whose<br />

focsl length is equal to a~roximstaly or#raff<br />

the dmgonal of the format.<br />

wlggflng-fn on firm-..see doubfo<br />

centering.<br />

wlgglJnp-in—A survey proaadura ussd whsn it<br />

is ~ry to astabtish a point, exsdfy am line<br />

befwean two confrvf poinfe nafthar of titi san<br />

be oocupied. If is sssanfialty a tr%d-and-armr<br />

fecfrrriqua where repeated lore end beck<br />

raadinga are taken and the instrument shifted<br />

after each pair of readtrrge until exadfy in tine<br />

with the etaliene. Also called ranging-lrr.<br />

wind rosa-l. A diagram showing the relat”kfe<br />

frsquancy of winds blowing from differsnt<br />

directions. It may also ahow avarsge apssd or


I frequarrsy of Occwranos of varieua speeds hem<br />

diffaranl directions. 2. A diagram showing the<br />

I average relafienstrip between winds horn<br />

ddfamti diraotioms srd lhs mrm~ d c4har<br />

I mereordog-kxd phenomena.<br />

I<br />

Windew-1 , An fnferfaca Wqmnant far<br />

I<br />

carrpders ftwwgh which ~eds and @ions<br />

am preasntad 10 users. 2. A radangufar frsms<br />

I Wifha SpSoUISd &etititbnonti<br />

of an interecfhfe gmphbs system,<br />

suean<br />

and within<br />

which a raUangdar pd’brr, or vvlndow, C4 the<br />

data b d@syad.<br />

1,<br />

wlrrg photograph-A photograph taken by<br />

oneefttra afdaorwing~d arnuftipfe-fsma<br />

m-.<br />

I<br />

wfrrg<br />

along<br />

pofnt-lfmae aseify idantiimd pointc<br />

esc+r side of an aerial phOtogn@, one<br />

near cash oorner snd one near the rniddfe.<br />

Used in tfw extension of radml oontral in making<br />

I<br />

Ccmtmlkd rnossics.<br />

I<br />

wlntor solstice-l. That point on the acfiptis<br />

mpbd by the Sun et maximum southerly<br />

cfacfhml’mn. Afso aefled ffrst pokrt of<br />

Caprlcomus; December coktico. 2. That<br />

indrmt at whii ha Sun meshes the point of<br />

maximum southerly dacfineticm, on w shout 22<br />

Dacafier.<br />

wl~-on printing plates—A printing plata<br />

~=~ a fighf-aenaitiieseatingappfiad by<br />

I WIN dmff-+ sounding devise sorrdsting of<br />

WSJ9hfsd Wiraa WhfOh are maintained at a g“wen<br />

-h bv fkwfs, and then dmggad over anY<br />

dad -eoursa.<br />

wltnesa comor—1. A marker set on a<br />

fxwarfy fins Mn9toa@mcu@*m iris<br />

irrpmdbsl to maintain a monument et the<br />

wrrrar Itself. 2. A monumental survay point<br />

usually on the fine of survey near a comer<br />

debfiti as a raferance wiren the armer is sa<br />

eiiisstad se to render He monumanfallon or<br />

ready use iqxectbsble.<br />

w ffnesa mark-A mark placed at a known<br />

distance and diractikm from a property comer or<br />

auwrrj etafiin to aid in ha raarvary and<br />

idantifiition. Also called wftrress posG<br />

wltnaas stake.<br />

witness pofnt—A monumenlsd station on a<br />

tine of the suwey, empbyad to perpetuate an<br />

MIL-HDBK-850<br />

280<br />

imnf ~t”~ wittmut spacisf ralatbrr to any<br />

remrbr ~r, essapt that the bearing or<br />

diiance may be known.<br />

wftnosa post-saa witness mark.<br />

witrtoss stake-Sea wftrmss mark.<br />

Woodward bass-flno meaaurlng<br />

●pparatus—see Iced-bsr ●ppsratua.<br />

World Gaographlc Raforerrco Systam<br />

(GEOREF)-A workfwkle poaifkm mferanse<br />

Syatwn that maybe applied to Sny nalp or Chell<br />

graduated in fatftude and bngitude (with<br />

Gmanwish aa prima mwidiin) ragardfaaa of<br />

prO@@on. If prevktes a matlmd d mqwedng<br />

~rorw In a fomr suitable for rnporfing and<br />

*W. The primmy use is for tntersarviaa and<br />

intareffied repmting d aircraft and air target<br />

poaitiins.<br />

worklrrg pendulum-A pendulum whiih is<br />

used (swung) in a detemrirration oi tha intensity<br />

or gravity.<br />

working-in on o line-See doublo<br />

conterlng.<br />

World Oata Bank II (WOEII)-A CIAproduced<br />

digiial rafxeeentnticm of tha world<br />

dwidad Into fwe g~gmphk areas. Eaotr area<br />

mntains vector data on coaatfinea (iuding<br />

iafends and fakes), rivem, and intematbnsf<br />

boundaries. WOSII was digifiuad aI acelaa<br />

m~ing fmm 1:1 milliin to 1:4 mflfibn.<br />

World Gsodotlc Systam (WGS)-A<br />

coneiataml sat d paramafera daaadbing the size<br />

snd shape of the Earth, the poaifiins ds<br />

natwmk et points with raspacf to the center of<br />

mass of the Earth, tmnsfomations from mspr<br />

geodetic datuma, and the petsntief d the Earth<br />

(uauaffy in tetm of harmonic soeffiiierrts).<br />

World Mean Elavstfon Deta (WMEO)-A<br />

OMA data baas of minimum, maximum, ad<br />

mean terrain efevaliana. Provides seams<br />

resolution elevation data wfth sentinuous<br />

wmfdwiie covemga, which may be used to<br />

support militaty planning and cmmmand and<br />

control systems.<br />

World Vector Sfrorellne (WVS)--A digital<br />

data file devebped to aupporf map display<br />

systems, GIS, and weapon aysfeme at<br />

1:250,000 scale vdrich conlsins shorelines,<br />

intametional boundaries, and country nsmes of


i<br />

,1<br />

ffwworki<br />

worfd @Yoonlc grid-A grkJ eystem in tii<br />

a grid narWxfl is Ms!fren’dcahy derived frem<br />

ekwnarda d a polysonis pjedion.<br />

writo 8nco, raad many (WORM)-1. A<br />

k disc Syafsm for Cusfern data bsae<br />

oreafion. Thediss ssnbeencoded entyenca<br />

by tha user but may be reed an unfhmifad<br />

nin’dmr d tirrws. WORM * are not<br />

OXIW@bb tih a CO-ROM disc ptsyer. 2. A<br />

werm is a software pregram that oopies itaeff<br />

from one systwn to another, uauaffy without the<br />

syatams uaem Imewkdge, if may also cause<br />

harm to a system, e.g., by desrmying fiha.<br />

wrong-roadlng—A descriptive term for an<br />

irnagewtidr isemwfad ermkrwknsgsdthe<br />

eriginal. Other teana. cwch as reverse reading,<br />

etc., ere aematimes us6d to idenfii image<br />

duecfion bbl are not rewmnded because ef<br />

peaable confusion m film negativ-p@ttie<br />

rsiatienahp.<br />

WWV tlm.-Ascurstely controlled tires signala<br />

transmitted frem stations (radii) WWV in<br />

Cderada and WWVH in Hswaii. Tfwse stat”ons<br />

bm4caE4 UTC (universal time coerdiifed)<br />

tii ia offset trem Al by e variatie amount<br />

dslermined ennushy before the atarf d the year.<br />

Ths epcch is shifted in “bwrements c4 100<br />

miltii if if departs km far from UT2.<br />

WY. (Y) lavel-A leveling instrument having<br />

the teles@pe, with attached epkif level,<br />

SUPPOftSd in Y-shaped bearings. The teleawpe<br />

osn be rotatsd about its Ierrgiiudiil asia<br />

(a.llimstion axis) and il can be Iiied and<br />

reversed, end for end, for testing and<br />

ad]ustrrwnt. Alse sailed Y level.<br />

MI L-HDBK-850<br />

281


1,<br />

I<br />

I<br />

I<br />

1<br />

MIL-HDBK-8S0<br />

x+xle-i .(JCS) A f’mrkmntal axis in a<br />

x fligtt NW saw llStsyslem<br />

of reckmg.lsr cxmrdiiaa; that Iii<br />

onwf+sh dstarrr=btb6rlfJiu kdt(easl x-y ssalor-An instmmant that provides W<br />

or west) of the rderarwa line are marked, and ycoonfiiaa h d~iial form horn<br />

=P=w~aw,ti.w9@’L2.<br />

anakrg dsta.<br />

llw line ~ining the qmaife fxluoial marks<br />

kithed_ which kstnoSfn6dyf Mdbl<br />

to the fins d fligfd.<br />

x~-rdlnate—~ abscissa.<br />

x+orractlort-llra correction to en XdmcfJorL<br />

x+llrectlotin efxetvsd diradirm in a<br />

VimgulAion figure for which an<br />

approximate value b obtained and treated<br />

like an obaarved diraction in the adjustment<br />

et the f~ure. The vmrtr of a Ieasl squares<br />

adjtimant of e trianguleticm figure<br />

aomaiimas requires the use of an xdiraclbn,<br />

for which an approximate value is<br />

obtainad by an inverea poshion<br />

~Wfi, by Ihe solution of the lhraepoiti<br />

pcbkrm, or by other means, and than<br />

using the .xdirecticm in the adjustmard and<br />

c&4.ainiig a cormctien (x-correction) for it,<br />

whioh makes fl consistent wkh the ad@ted<br />

values of the observed diredons.<br />

x~leplaeemen!+ somponam of hnsge<br />

dslaoament. When a @rt knaga is 10 be<br />

Iesated ~ ooordkstae with respect to<br />

rsctanguier axes. xdiaplasament<br />

rep-ts the dskmce rrmvad in the xdiracfion.<br />

x+notlon-in a atereopletting instrument,<br />

tit Ikraar adjuxtmant appmx’bnatefy<br />

parallel to a line conrwsting fwo projastor<br />

stations; the path of this adjustment is, in<br />

#fed, coin&dan! wiIh the flight line<br />

between the twu relevant exposure<br />

stations.<br />

x-pearra\la+See absolute stareoscoplc<br />

x+cele--(.lCS) On an ob~que photograph,<br />

the scale akmg e line parallel to tha tme<br />

horizon.<br />

x-tilt-llre corqxrnen! of lift aboul the x-exis,<br />

which is most nearfy in the direction of<br />

282


I<br />

!<br />

..<br />

MIL-HDBK-850<br />

Y<br />

yacls-f. (.fCS) A vertkd e.siaina eyafem yeDr—Tha period of abou! 365 1/4 adar days<br />

d mdar@ar cedimtes; fhet Iii m<br />

~~ dktsnm= ~a or babw (nerth w<br />

aoufh d) a mfemrax Em am rmrfrad.<br />

requkod fer one<br />

emmd the Sm.<br />

yoarq edondar<br />

revdtiian d the Earth<br />

Sea also ●remallstlc<br />

yoaq wIlpse yesr:<br />

XwYm.#frP,<br />

ard paaa6a<br />

M. or WaPh. 2.<br />

~~~x-~<br />

through the origin.<br />

fictitious year;<br />

yaar; tmplcal<br />

great<br />

year.<br />

YO*C dderaal<br />

y-coordlnatsis-See ordlnatos.<br />

y411splacoment-A wmponent of imege<br />

displacement. When a peinf irnsge is !0 be<br />

bcatad by cmordiias with respect to<br />

rectangular asea, ydiaplacement<br />

represents he distsnca moved in the Y<br />

direclion.<br />

)+!VS4-S9!3 Wyo Ievd.<br />

y-parallax-lhe dtierence bstween the<br />

~~wlar dktarrces of the two irnsges<br />

of a pornl on a pair of photographs from<br />

the vantil plsne containing the air base.<br />

The sxislsnca of Ypsrakx ia an indiiion<br />

of till in either or tm!h plmlogmphs, or a<br />

diffaenca in flying heights, and in!erferss<br />

with eleramcop”~ ceasminrdbn 04 the pair.<br />

Also .-lied vertical partrlla~ want of<br />

corroapondance.<br />

y-cala-(JCS) On an ob/iiue phetogmph,<br />

the scfria abng the line ef the principal<br />

vartii or any other line, inherent or<br />

plotted, vdrich. on the ground, is parsllel to<br />

the principal vert”bal.<br />

y411t-See pitch.<br />

yaw—l. (sir navigation) The rotstimr ef an<br />

alrcmff abour its wrtica! exia so se to cauaa<br />

the aircraft’s Iengitudkd sxis to dev”mte<br />

from the fl@ht line. Also celled crab. 2.<br />

(phatogrammetry) The rotation of a csmem<br />

or a pfwtogmph coordinate system aboul<br />

either the photograph z-axia or the exrerler<br />

z-ssis. 3. In some photogrammetric<br />

instruments and in anahjliil appliilions,<br />

the symbol rc may be used.<br />

yaw angle--See engle of yaw.<br />

283


I<br />

i<br />

MIL-HDBK-E150<br />

z+xis—in a threa4me rvzional rectangular<br />

mxdhste system. the axE3 & rdemnca xerm tltna-Tha kxaf meen time of a<br />

ttd is pwpendkwlar to tmfh the x- and y- preference zene. See afse thne zone.<br />

arms af their @m 0! Wwsec4ii.<br />

zoom systOrn-Saa pmrcretlc systam.<br />

z-rnotlon-Movement of e atereepfotting<br />

prmjecfor in a verl~l dfmcfien. ZUIU tlma--see Untveresl TIma.<br />

z-ecale-(JCS) On an oblique photogmph,<br />

fheecale ueedincalcufaIing tha height of<br />

~ e@cL Afao, the rmrne given to th~<br />

method of height delemrinstion.<br />

z41me—See Unlveraal Time.<br />

z-value data pelnta-Oata points providing<br />

a value perpandiiuIer er norms] 10 a<br />

specified surface (elevaticm).<br />

zenitfr-Thet point of the celestisl sphere<br />

vefi”keliy overhead. See alse geecentrlc<br />

zenith; geodotlc zamlth.<br />

zcnlth engie-see zenl!h dls:ance.<br />

zswrlth camor8-A epecief camera se<br />

designed thst its opticaf exie m9y be<br />

pointed ac=xreteiy toward the zentih. 11is<br />

used tor the determinstlen of astronomic<br />

fmeificma by phetographmg the positii of<br />

the z&m, See also photographic zenith<br />

tube.<br />

zenith diatanca-The venicd engle<br />

between the zenith end the object whii is<br />

etmerved or defwd. Zeniih d-rice is the<br />

COI#WMW of the akttude. Afee caffad<br />

zenith sngle. See elso coaltltudm<br />

zenith taleecope-A portable instrument<br />

adapted for the measurement of smsfl<br />

differences of zenfth distsnce, and used in<br />

the detarminstiorr of astronomic latiiude.<br />

Zenhh81 cf’rert-see azlmtrthal chart.<br />

zenlthal map projection-See<br />

azimuthal” map” projoctlon.<br />

zonal hermonlce-The aet of aphericel<br />

hsrmonti that are functions of latitude only<br />

and therefore do nef effect the rotatierml<br />

symmetry of the surface about !@ pofer<br />

exis.<br />

z<br />

284


I<br />

I<br />

Afr<br />

AAflF<br />

ASC<br />

ADAS<br />

ADh4<br />

ACNIG<br />

AFS<br />

AWFM<br />

AMSD<br />

ANMS<br />

ANSI<br />

APPS<br />

APR<br />

ARAPS<br />

ARC<br />

ASCII<br />

ASW<br />

ATC<br />

ATM<br />

ATMP<br />

ATRAN<br />

AITG<br />

AVHRR<br />

AWAR<br />

AWSDE<br />

BAD<br />

BC<br />

BGN<br />

6M<br />

BMD<br />

BNC<br />

BNPC<br />

BRAC<br />

C31<br />

CAC<br />

CAD<br />

CADICAM<br />

CADD<br />

CALS<br />

CAM<br />

CCM<br />

z<br />

CD-ROM<br />

CDB<br />

CE<br />

CEDD<br />

CEP<br />

CERL<br />

CG<br />

CGS<br />

MIL-HDBK-850<br />

4. LIST OF ABBREVIATIONS, ACRONYMS, AND INITIALS<br />

Akrng T-<br />

Autornated Air Faciliiias Information I%e<br />

A~ Cultrol<br />

Aulwnetad Digital Annotation System<br />

Aerunaukal Data Msinbmance<br />

ARC Digitiiad Rsater Graphics<br />

Aatial Film Speed<br />

Aukwnetsd MeppingF-citiii Wenagemenl<br />

Ad@led Ma@ng SUJpOrtmtn<br />

Automated Nc4ic0 tOkfiMwss)%kll<br />

A rnarican National Standarde Instihh<br />

_A@ti~~e raa;ric Pea#iening System<br />

3<br />

~ea Raquhnenta and Produot Status<br />

Equal &c Second Eastar @mtlMsP<br />

A-n Natiod Standard Cede fer Intornwtien Interchange<br />

Ard.kubrnatina Wariare<br />

Ad Targa! Chari<br />

Au Tnrgd Materials<br />

Au TErgat Maleriets Program<br />

Aulormetic Terrain Rmognition and Navigation<br />

Automated Tect.kal Target Graphk<br />

Advanced Very Nigh Reselutkn Radiiler<br />

Araa Weighted Average Re.sotuiion<br />

Advar’ced Waapeffi and Syaiems Data Base<br />

Bathymatti Archwe Data<br />

Bettwn OontOur Chart<br />

Board on Geogm+ii Name=s<br />

Benchmark<br />

Balhymahic MOdd Dam<br />

Bathymattic Navigation Chert<br />

Bathymetric Navigation Planning Chart<br />

Bathymetric ReccweqI Arae Chart<br />

Cenrrnand, Contrel, C9mmunicaticms and Intelligerwe<br />

-~er -sAed cartegrePhM ~r==~ ACWOOCI@~l ChSI’I<br />

@mputef ~ DA@ Drafting Carrputer &aiiad Deaigr@ratIing<br />

CcmpRer A.ded Draftm#Deaigm Computer Aided Manufacturing<br />

~rtqxAer Adad DesJgrJDrafthg Computer Aaeisted Daaigwlhfthrg<br />

Computer Ad LO@”ti Suppt Procaaaing System<br />

Computer Aided Mapping; CsrtographC Automatic Mapping; Computer Aaaisted<br />

Creea-C0ur4ry Mevement Map<br />

Conthwrntal Control Netwxk<br />

CO~uier COrrqAible Tape<br />

Cot?pact Disc-lnlerectiwe<br />

~rrpad Dkc-RSSd Only Memory<br />

Cartographic Deta Baaa<br />

Critiad Design Review<br />

Ckulsr Error<br />

Cammittea on the Exchanga of Digitel Data<br />

Circular Error Probable<br />

GmW’ta3ion Engineering Resaarch Laberalery<br />

city Grephc<br />

Cantimatar-Gram-Second<br />

285


I<br />

gwi<br />

Clct<br />

CLD<br />

CM<br />

CMAS<br />

co<br />

COMIREX<br />

CONOPS<br />

COTAT<br />

COTS<br />

CPE<br />

CRG<br />

DAFIF<br />

DAPPS<br />

DBDB<br />

Dcfs<br />

DcAc<br />

bow<br />

DDM<br />

D EIS<br />

CJEM<br />

DFAD<br />

DGI<br />

DGIWG<br />

DH\<br />

DHO<br />

DVS<br />

DIGEST<br />

DLG<br />

DLG-E<br />

;:3:<br />

DLO<br />

DMA<br />

DMAAC<br />

CWAcse<br />

DMAHTC<br />

DMAFIC<br />

DMASC<br />

DMATSC<br />

DME<br />

DMS<br />

Doo<br />

OoD MC&G<br />

Pragrams<br />

DaD WGS<br />

DOS<br />

DPpDB<br />

DPS<br />

DRLMS<br />

DSIS<br />

DTAD<br />

MIL-HDBK-850<br />

ClassMad Hydmgmphio Iniorrmtbn P mceasing system<br />

Chart Up&de Manual<br />

COnvanfienal Inmmafional Origin<br />

Gtiar Lii Data<br />

COnf~uraIiOn Managamenl<br />

Ctmufar Map Aocuracy standard<br />

COesaal chart<br />

C@mniffee on Imagery Rsquiremenfs and Grpfoifatien<br />

Conca@ d Operetbna<br />

Correfatien Tracking and Triangulskm<br />

G3mdel Dff4he-Sheff<br />

CWfar P*8 Error<br />

CW Route Gra@ii<br />

Coerdineted Universal Tkna<br />

Digifef Aermeufical Ffiiht Infonnafiorr Fife<br />

OMA Automated Pdiithn Production System<br />

CMgifal Bathymetric Defa Baae<br />

Digifel COnpraIor Segment<br />

Dwfial Ccmcapfs Ansfysis Center<br />

Digifef Cnies Data Ssss<br />

Da5ign Concept Review<br />

Digital Charf of fhe Worid<br />

Distnbufad Data Management<br />

Data Exiracficm Segment<br />

Digital Elevation Matrix; Dwifal Eleva!ierr Mcdel<br />

Digital Feature Armfysis Data<br />

Digital G@gre@k Information<br />

Digital Geogmphk lnforms!”~n Working Greup<br />

Defense Hydrographii Initiative<br />

Maen Diurnal High Water Inaquatii<br />

Data Integration segment<br />

Digilal Gaographc Information Exchange Standard<br />

Diiifal Line Graph<br />

Digital Line Greph-Enf=mced<br />

Digital Landmes5 Btanking System<br />

Digital Landmass System<br />

Mean Dkmml Low Waler Inequafii<br />

Defarw.e Mapping Agency<br />

Dafense Mapping Agency Aerospace Canter<br />

Defense Mapping Agency Combat Suppml Center<br />

Defense Mapping Agency Hydrographtiopogmphc Center<br />

Defense Mapping Agancy Restcm Center<br />

Defense Ma~ing Agency Sysiems Canter<br />

Oefenaa Ma~ing Agency Technicaf Services Centei<br />

Distance Meeauring Equipmant<br />

Defenas Mapping school<br />

Dfgifaf Nauficaf Chart<br />

Department of Defenaa<br />

Oepatiment of Defense Mapping, Charting, & Geodesy Requirements and<br />

Department of Defense Worfd Gaodatic System<br />

Disk Operating System<br />

DigitizecUDigital Point Positioning Dela Base<br />

Dlgffal Producfien System<br />

Digital Radar Lsmknass Simulator<br />

Data Services Segmani<br />

Digifel Terrain Anatysis Data<br />

286


DTC<br />

DTD<br />

DTED<br />

~V~F<br />

ECDIS<br />

EDME<br />

EFL<br />

EGA<br />

EMD<br />

EOD<br />

EPI<br />

ERDAS<br />

EROS<br />

ESNA<br />

FAC<br />

FACC<br />

FACS<br />

FADT<br />

FAF<br />

FAT<br />

FWS<br />

FGDC<br />

Ffccoc<br />

;;s<br />

FIPS Puss<br />

FODB<br />

G&G<br />

GAT<br />

GB<br />

GBFAIIME<br />

GCT<br />

GEOREF<br />

GGF<br />

GGS<br />

GM . Ii<br />

G:1s<br />

G... KS<br />

GLtORIA<br />

~;T<br />

GNC<br />

GNPS<br />

GOSIP<br />

%s<br />

GRASS<br />

GRS 80<br />

GSD<br />

GST<br />

GUI<br />

MIL-HOBK-850<br />

Data Trarster Cettridge<br />

DeaJrned Type Dahiiion<br />

D@il Tamsrn EbaIkrrI Data<br />

Digital Terrain ModeL Qigii:Jerrarn Matrk Daw Trader Medulea<br />

Digital varticafDbShKkn<br />

Eledmnic Chart DI@ay and Information system<br />

EROS Data Canla<br />

Efactmnic fMs@Iw= “ M~ E@PIMU<br />

Effective Fecal Length<br />

Enhensed Graph= Adapter<br />

Eladronk h4sp Da@ Eladmrric Map Dis@sy<br />

Erasable D@ii Ilk<br />

Eladronk Peaitkn Irdkator<br />

Earth Rsswrcas Data Ar@sia Sydam<br />

Earth ,Rasourcas Obaervatien System<br />

Etacfrd<br />

See TEC<br />

Survey Net<br />

Feature Attribute Code<br />

Feature end Attribute Coding Celelog<br />

Faalura/Attrfbule CorXng Standard<br />

Feature Analysis Dats Table<br />

Faat Acsass Fennel<br />

Factory Acceptance Test<br />

Fseture Exiradion Segment<br />

Federal Geographic D@a Committee<br />

Fad&al Inhxaganq Cocdimsling Cornittee on DiK@al Cartography<br />

Feature Iclent”-tbn Data<br />

Fe&ml Infm-metion Processing standards<br />

Fdaral Intonation Ptmeessing Stan&da (FIPS) Pubtikalien<br />

FIREFINDER Oparatknal Data BSSE<br />

Gaodetis and Geophysical<br />

Greenwich Appsmnt Time<br />

Gigebyte<br />

Gacgraphic Bass FilWDual-lndepandent-MapEbing<br />

Greenwich Cwil The<br />

Gsogrephk Reference<br />

Greund Gain Forwmd<br />

Ground Gainad Sideways<br />

Greenwich Hwr Angle<br />

Gaegraphc Information System<br />

Graphu Kemal system<br />

Geelogkal Leng Rsnge Inclined ASDIC<br />

Gravity Model<br />

Greenwich Mean lima<br />

Glcbal Navigsticm Chert<br />

Gaegraphc Names Pmcesaing System<br />

Government Open Systems Interconnection Protocol<br />

Griddad Phot~raph<br />

Glebel Positioning Syetem<br />

Geegmphw Resouroas Analyais Supfmrt System<br />

Gaedetic Referenoe System S0<br />

Greund Scale Diatense; Ground Sample Dktence<br />

Greenwish Siaraal llme<br />

Grsphical Usar Inlerface<br />

287


I<br />

HA<br />

HOOT<br />

HOT<br />

HWS<br />

HHW<br />

HHWf<br />

HIMAN<br />

tirrs<br />

HLW<br />

HLWI<br />

HSOC<br />

HW<br />

HWR6C<br />

Ics<br />

IFOV<br />

IGES<br />

IGSN 71<br />

IHO<br />

ILW<br />

IMC<br />

IMO<br />

IMU<br />

Ioc<br />

1s0<br />

lTD<br />

JNC<br />

JOG<br />

JOGIA<br />

JOGIG<br />

JOWR<br />

KB<br />

KBS<br />

LHW<br />

LHWI<br />

LLW<br />

LOC<br />

LOLA<br />

LORAC<br />

LORAN<br />

LOROP<br />

LW<br />

MACDIF<br />

MAD<br />

MADPC<br />

MB<br />

MBFI<br />

MC6G<br />

MCGFDES<br />

MCS<br />

MGRS<br />

MHHW<br />

MIL-HDBK-850<br />

Haltwr ad ApfxcM3chchart<br />

High Density DQhel Tape<br />

Hiih Density Tape<br />

Hardccpy ~ploiiticm segment<br />

Hiiher High Water<br />

Higher H~h Wafer Interval<br />

HYdwqti h’rf~ti Handiii<br />

Hufl Integrity Test Sie Chart<br />

Higher LOW Water<br />

Higher Low Water Interval<br />

Htgh speed Digiil CharI<br />

High Walaq Hardware<br />

H@ Water Full and Change<br />

Interactive Cen@etiin Sy.dem<br />

Inatantaneaus Fdd of Wew<br />

Iritial Graphic Exchange spacifiition<br />

Infemational Gravity Slandamlizaticm Net 1971<br />

International tiydregraphic Organization<br />

International Low Water<br />

Iwge Motion Cwr@enaa!ien<br />

Intarnalienal Maritime Organization<br />

Inartial Measurement Unit<br />

Initiil operating Capatili<br />

Intematienel Standerds Organization<br />

Interim Terrain Data<br />

Jet Navigation Chad<br />

Joint operations Graplic<br />

Jeint Oparationa GraPhtiAu<br />

Joint operations GraphidGround<br />

Jeint Operatiena GraphkiRedar<br />

Kibbyle<br />

Knowiedge Baaed System<br />

Lower High Watef<br />

Lewar High Water Interval<br />

Imwer Low Water<br />

Lines of Cenwnunicat ien<br />

Leng Line Azimuth<br />

Long Renge Acaracy<br />

Long Range Navigation<br />

Long Range Obliiue Photography<br />

Lew Water<br />

Map end Charl Data Interchange FormaI<br />

Magnetic Anomaly Detection<br />

MAD Planning Chart<br />

Megabyte<br />

Mhimum Boundng Rectangle<br />

Mapping, Charting & Gecdasy<br />

Mapping, Charting, & Gaodeay Feature Data Exchanga Stamdard<br />

Medern Cataleg System<br />

Miliiary Grid Reference System<br />

Maan I+gher High Water<br />

288


I<br />

MHW<br />

MHWS<br />

MIL-STD<br />

MIM<br />

MINI-TOPO<br />

MK S5<br />

MK 90<br />

MLLW<br />

MLLWS<br />

MLW<br />

MLWS<br />

MMSD<br />

MOE<br />

MP<br />

MSI<br />

MSL<br />

MSS<br />

MTL<br />

MUM<br />

NAD 27<br />

NAD S3<br />

NAVINFONET<br />

NCGIA<br />

NFS<br />

NIST<br />

NNSS<br />

NOS<br />

NRL OEf’ SCC<br />

Iswc<br />

NVPUB<br />

ONc<br />

0PARE4<br />

0s<br />

OSA<br />

PAPI<br />

PBM<br />

PBNZC<br />

PC<br />

PDMM<br />

PGIS<br />

PHIGS<br />

!:P<br />

Pws<br />

PMD<br />

Poslx<br />

PPD<br />

PPDB<br />

PPI<br />

PRSL<br />

PSR<br />

PT<br />

MIL-HDBK-850<br />

Mean HQh Waler<br />

Mean High Wnler springs<br />

Mllifary standard<br />

Milii InetaMalian Map<br />

Mir&nal)y Redundant TepobgY<br />

MARK ss<br />

MARK 90<br />

tin Lower Low Wafer<br />

M-n Lewar Low Water ~<br />

Maen bw Water<br />

Mean Low Wafer springs<br />

Metrk Mappiig Supparf Dafa<br />

%k%%md ‘“f=ftiensss<br />

Multiapedral Irnegery<br />

Mean Ses Level<br />

Muf@actd scanner<br />

Maan Tde Level<br />

Multi Use Menuacrf@<br />

North American Datum of 1927<br />

Notih American Datum of 19S2<br />

Navigation Informalien Network<br />

National Center for GeogrepMc Inferrrdon and Anatysie<br />

Navigational Fllrnship<br />

National Institute for Skmdamls and Tschnofogy<br />

Navy Navigation Safelliie System<br />

National Oosan Survey<br />

Navel Reaaarch Leborat~ DetachmerU Stennis Specs CaMer<br />

Non-Subrnatine Cenfecf<br />

Naval Surface Weapons Center<br />

Navigation PL611cafion<br />

Operafbd Navigation Chstl<br />

Cp.srafing Area<br />

Operating Sy6tem<br />

Open S@errra Arcttiiacture<br />

Precise Automatic Phobgrammetris Intervatomafer<br />

Permanent Benchnark<br />

Prec&sa Sathymatric Nav”~atien Zone Chett<br />

Pilotegs Chart Point e( Curvature<br />

Peint of timpeund Curvature<br />

Pulse Ooppl- Map Matching<br />

Prdktnery Deelgn Review<br />

Product Generafiin Segrnerrf<br />

Programrna#a Hterarch~l httarective Greph- System<br />

Peinf of Interwcfii<br />

Precise Inafattdion Prnilion<br />

Prcdudion Management System<br />

Projected Map D@ley<br />

Porlable Operating System Interface<br />

Peinl Positioning Date<br />

Paint Posifiining Data Sss6<br />

Plan Positii Indwtor<br />

Precise Radar Significant Lecation<br />

Pre-Ship Readinaaa Review<br />

Point of Tangency<br />

289


1,<br />

I<br />

I<br />

I<br />

PTADB<br />

Pvc<br />

Pvl<br />

Pvoo<br />

PVT<br />

Pn<br />

R&PRG<br />

RDT6E<br />

:;P<br />

RGB<br />

RIM<br />

~hL<br />

RMP<br />

ROCS<br />

RPS<br />

RfW<br />

RSAC<br />

RSPL<br />

RTAD<br />

SA<br />

SAls<br />

SAGA<br />

SAR<br />

SCP<br />

SDTS<br />

SECOR<br />

SOD<br />

SGML<br />

SHA<br />

SHIRAN<br />

SHORAN<br />

SINS<br />

Sls<br />

SIAR<br />

sl,F<br />

SMAC<br />

SONAR<br />

Sosus<br />

SPIS<br />

SPOT<br />

sol.<br />

SWATH<br />

TAS<br />

TB<br />

TBM<br />

TCOC<br />

TEc<br />

Tt%cotd<br />

TESIEMPS<br />

TIGRIS<br />

TIN<br />

MIL-HDBK-B50<br />

Plsming Tarrein Analysis Data Base<br />

P&d d Vattical CLXVe<br />

Point of Vertlsal Tangan!<br />

~iii Ver’kaf Cbetrudion Dab<br />

Pc4nl ef Vdcel Tangent<br />

Phonographic Zenith Tube<br />

DoD MC6G Rafuwnants and Programs Reviaw GruuP<br />

Rseaarch, Developrnant, Tad and Evaluation<br />

Repreeantatiie Fradion<br />

Radar Fa Point<br />

Rad, Green: Blue<br />

~a =anC@aMaP<br />

Randxn Micdardiculer<br />

Raster Map PrudUd<br />

Range OnJy COrralation System<br />

Ftaater Prcdud standard<br />

Radar ReWrn Coda<br />

Radar Signifiince Analysis Code<br />

Radar Significant Power Line<br />

Rek.eatable Terget Assess.ment Data<br />

Spesial Araa<br />

Saurce Acquisition Sagment<br />

Stori Arc Gaedetis Adjustment<br />

Svnthatic -, - Armrture<br />

Sacondzxy bntrd<br />

Flad9r<br />

Point<br />

SpaIial Date Transler Standard; Spatial Date” Tra=fer Spacificalion<br />

Seouantiel Co/la[ion of Range<br />

Syn+behzed Graphic Date -<br />

Standard Ganeralbd Markup Language<br />

Sidereal Hour Angle<br />

S-Bard High-Pracieion Shert-Range Neviga!ion<br />

Shotl Range Navigation<br />

Ships Inertial Navigation System<br />

Sensor lmaga Simufatoc Sterxtard Indaxing System<br />

Side-Leoking Airberrra Radar<br />

standard Urrear Ferrnat<br />

Soena Matching Area Cerrelator<br />

Sourtd Navigdon<br />

Sound Surveiflanc4 Systems Chart<br />

Seurce Praparatien Segment<br />

Systbme Probatoire dObsarvatfen de fa Terre<br />

Structured Query Language; Standard Ouery Language<br />

SMSll Wettad Area Twin Hull<br />

Terrain Anatyeis<br />

Temain Analysis Producl<br />

Terrain Anafysia Syetem<br />

Tembyte<br />

Temperary Benchmark<br />

Transferee Cylindrical Orlherrrerphk Chart<br />

Topography Engineering Canter<br />

Terrain Coatour Matching<br />

Tefrain Edn S!atforJElevalion Matrix Prosaesing Systam<br />

To@ogically Integrcdad Gaographw and Resource Information System<br />

Triangulated Irregular Network<br />

290


TLM<br />

TM<br />

TMP<br />

Rw<br />

TPR<br />

TS<br />

lTADB<br />

U.S.G.S.<br />

UPS<br />

UR<br />

UFVS<br />

URA<br />

USATEC<br />

USR<br />

UT<br />

UTc<br />

UTM<br />

VABM<br />

VD<br />

Vt3A<br />

VMP<br />

VOD<br />

VPF<br />

VPPDB<br />

VPR<br />

VPS<br />

WDBII<br />

WGS<br />

WMED<br />

WMRM<br />

WORM<br />

Wsc<br />

Wvs<br />

MIL-HDBK-850<br />

Tcpgraphic Iino Map<br />

Thernelic hlappac Topography Me@<br />

Target Materials ~<br />

Turning Pdrd<br />

Tacik4 Pibthge Chart<br />

Terrain Prvfile Recordar<br />

Ta~r# 10 Spirak Tassaialad SharDid<br />

Tactical Terrain Anatyaia Data Base<br />

Tactical Tana”m Data<br />

Us. Geo&gkd Suvay<br />

Univaraal Polar SlaraoUra@c<br />

universai RecWii<br />

Untwrrsal Ractifiar Sagrnard<br />

User RequiremtmI And@<br />

Us. Army T k Enginaaring Canter<br />

Unkmnral firrra Ceodnatad<br />

Urrivw-1 Tre.nsvaraa Marcator<br />

Vert”til Angla 8anchrnark<br />

MO&G Viiao Disc<br />

Vim Graphics Army<br />

Vector Map Product<br />

Vartiml WstrwXiorr Data<br />

vector Product Form91<br />

Viieo Point Podtiining Data Base<br />

Vktusl PPI Refklc=ape<br />

Vactor Prcduct standard<br />

Worid Data Bank II<br />

World Gaodetic System<br />

Wodd Mean Elavation Data<br />

Write Maw, Raad Many<br />

Writa Ones, Read ManY<br />

DM4 Warrim Supptni Cemler<br />

world Vacior Shorama<br />

291


Board on Geographic Na~ti~BGN)-An<br />

agancY d the U.S. Govamrna<br />

astabliahcul by Exacufive Order ‘m 1S90 ard<br />

_ ~~NW Und9r Ptic Law 242.<br />

sO, 2S Jufy 1947. Nina departments and<br />

WWI&S enjoy Beard mambsmf@. DoD .E OIW<br />

of fheaa medmrs; DMA provides the BGN<br />

EX-e SeUSfary and a staff for work cm the<br />

Boards Foreign Narnax committee. Conioinfty<br />

wirhthas acratsryd thelnterior,th esoard<br />

pmvidas for “uniformity in g90graphk<br />

nommclalure and orthography throughout the<br />

Fdsral GmenunantN It develops pollclsa and<br />

remanization systems under whkh names are<br />

derivad and it atandardiiaa gaographw names<br />

for use on maps and in taxfuaf materials.<br />

Committee on Imagery Requirements<br />

and Expfoltntlon (COMfREX)—The U.S.<br />

intelligence community% management<br />

mrnmirfes en imagery requirements and<br />

exploitation.<br />

Ccrmmltteo on the Exchange of Dlgltel<br />

Data (CEDD)-An international hydregraphic<br />

O~nKStiOn working group tasked with<br />

developing sttmdards for the exchange of<br />

hydrogrephii and bathymetric data.<br />

Construction Enghreerlng Research<br />

Laboratory (CERL)-Laboratory under the<br />

U,S. Army Corps of Engineem. CERL<br />

devefopad GRASS, e raster GIS. see else<br />

GRASS; GfS.<br />

Defonso Mapping Agency (DMA)-A<br />

Dspartmamt ef Dekmaa agency “mchsrge of<br />

enlurncing mattil aacurify and supporting the<br />

Offce ef secretary of Defense, Joint Chmfs of<br />

staff, Unfied and Specified @mmsnda, Miliiary<br />

Dagrarimants, and other uaara. DMA produces<br />

and distributes mapping. charting and geodetic<br />

(MC&G) pmducfs, asrvices and training, cmd<br />

adviaaa on such matters. It provides nautical<br />

charts and marine navigational data to<br />

worldwiie merchant marine and privete vessel<br />

opsmtora. Tha agency maintains Iiiiaon with<br />

ctill agencies and national and intemslierml<br />

-Pping, charting and geodetic activities.<br />

Dafenso Mapping School (DMS)—A<br />

MIL-HDBK-850<br />

5. MC&G ORGANIZATIONS<br />

. A_rlc-. .... . .. . . .<br />

(ANSl)-An<br />

ad ktusfry<br />

-.--.---—. Naricmal Stmndm~ds —-— InStffUt.<br />

maectstkm formed by (fosamn’ranl<br />

to produce and d-rude wirfefy<br />

DC4_ Ma@no AOSI’WY ~ -*<br />

trainDoo, diiary, C&&sr-I. and did<br />

in MC&G Wchnii=. pfOCSdum. ~<br />

to<br />

fmramnel<br />

@@s.<br />

used “dustrial standards.<br />

DILA Aorospsc. Canter (DMAAC)--A<br />

DMA woductiorI osnfer located in S1. Louis, MO.<br />

292<br />

DLfA Combat Support Cmntor<br />

(DMACSC~A DMA mmponent responaiie<br />

fm~ Of DMA pfOdUCfS 10 thS USSr<br />

mmmunify. There are several depots located<br />

atcund the vmrbi.<br />

DMA HydrographlcfTopographlc Contor<br />

(DLIAHTC)-A DMA prodstion center located<br />

in Woekmont, MD.<br />

DMA Systems Canter (DfAASC~The<br />

DMA compenent re.sponsibfe for research and<br />

davefcpmsnt issues. including developing and<br />

integmting new MC&G prodwfa and production<br />

syaiems.<br />

DMA Warrior Support Center (WSC)-<br />

The DMA facilii wliih provides an arrvirenment<br />

for current, future, and @entiel MA custernam<br />

to pan’kipate in the defmhiin, devebpmanl. test<br />

and evaluation end appfiilion of DMA MC6G<br />

products and data. The focus ef the WSC ie to<br />

oenducf -rch and davelcprnant and<br />

promtyping activities that promote<br />

inteqambifii and MC&G atsrxlardiiatii.<br />

Adddbnelty, the WSC pM4t10feS the OpfirrWJM<br />

production and use of DMA prcducts, data, and<br />

ssnricas for combat ferces by raqxmding dimctfy<br />

10 their needs.<br />

Dot) MC6G Raqulremanta and Program<br />

Revlow Group (R& PRG)-A Department of<br />

Oafansa (D@) raview group cerrpisad d<br />

mpraaentafivsa from the DoD agancbs arrd the<br />

military sswbs thsl advim Amistan t secretary<br />

d Dafenee (ASD) on MC&G matters.<br />

Federal Geographic Data Commltleo<br />

(FGDC)—The InterAgency afaaring committee<br />

whiih supemaded the FICCDC. The FGDC<br />

previdas oversight and poficy guidance on the<br />

Wlce of Management and Budget’s (OMB)<br />

Circular A-1 6 activities. In perlioufer, the<br />

mmmittee promotes the coordinated<br />

devebpment, use. shering, and diasamlnation<br />

of surveying mapping, and related apatisl data.<br />

CkmLar A-16 assigns responsftilii to various<br />

egencies to provide Ieadarship in the<br />

coordhation of certain categories of surwying,


I<br />

mapping, and rekdad spatial data. See also<br />

Fodeml InterAgency Coordlnatlng<br />

ComrrrNte8 on Digltsl Cartography.<br />

Faderal lntwAgoncy Coordlnstlng<br />

Commlttaa on Dlgltnl Cartography<br />

(FICCDC~Arr InterAgency steering<br />

cornmftfaa eatsbliied in 19S3 by the Offke of<br />

Menagwnant ad Budget. The purpose ie to<br />

ramnvmnd JNocaduras and progrrsme which<br />

weu~ faciliite the ccardheticm of Fadsrd<br />

a- d@f.sl -=fogmphii SUtVhiiS, and<br />

eefsbfkh ad promulgela sfandarda and<br />

epecifiIions for the producfton of dcatkqmphk<br />

data. Nama changed in 1990 to<br />

the Fsderef Geogrsphm Data Cornmilfee. S..<br />

afao Federal Goographlc Data<br />

C0mmltte6.<br />

Intemetional Hydrographlc Orgenlzetlon<br />

({HO)-The cardirrating body for<br />

internetkmal rautksl chaning practices and<br />

prceadurtm. Establishes minimum stendsnis<br />

end epacifutiimr for the production of nsutiil<br />

charts and the collection of mfslad daIa.<br />

Membership is open to all muntries of the wortd<br />

Interrmtlonal Marltimb ~rganlzation<br />

(lMO)-The SpacMiued Agencf For the United<br />

Nakms raafmnsiMe for M9ritkrrs safety and<br />

effciency of navigation. It prev”kkra machinery<br />

for cocperatien among governments in the fiekt<br />

of governmental regulations and practices<br />

relat”ng to Iachnicd matters of afl kinds affecting<br />

shipping engagsd in intemat”bnef trede.<br />

lntarrmtlorml Standards OrQanlzatlon<br />

(lSO)--An Irrtematbnal organization<br />

reeponsibfe for digits} standards for rn.dla,<br />

format, etc.<br />

Natlond Center for Geographic<br />

Information and Anafysle (NCGIA)-A<br />

conaodium of three urrivarsitk (The Whraity<br />

of Catiiornie al Senta Barbara, The State<br />

University of New York at Buffab, and The<br />

Urdvereily d Maine at Omno) receivii furrdhg<br />

frum the Netbnal Sc4srrce Foundmbn (NS~ to<br />

fcwus rasasrch and model aducatbnel<br />

curricufurns in apetial aneiysis and cpetiel<br />

stetistii; epstiil refatkmships and data bass<br />

slructur~ ertifcief infe(ligerroe and axperf<br />

systems; visualization and secial, economic and<br />

institutional issues in the field of gsogrsph~<br />

information systems (GIS).<br />

National Ocean $errrlce (f JOS)-Major<br />

component of NOAA, charged with maintaining<br />

MIL-HDBK-850<br />

Ihe Natiinal Geodetic Reference System;<br />

producing neuticef and aaruneutical drerts end<br />

related publication.s surveying end monitoring<br />

erwirmrnamtal resoumos, ilxiwSing Coastaf<br />

pd!ufii; researching the phy~ dsaracterfatk2s<br />

of the OcOena: and msnagirrg marine asruenas<br />

end sanctuaries. Formerfy Netbnal omen<br />

survey.<br />

Naval Envlronmentel PredictIon<br />

Research Facillty (NEPRF, NOARL)-A<br />

raseimh and davalepmerst orgsnizst”bn under<br />

lha NSW during the 19 f30e. NEPRF, NOROA,<br />

mv.f MO we#s merged to fcmn the Navaf<br />

Oceanographic end Atmospheric Rmearch<br />

IAroratory (NOARL) in 1989.<br />

Nevaf Oceanogrrsphb and Atmosphbrlc<br />

Research Laboratory (NOARL)-The<br />

Na~s Iesd laboratory for rasasrch and<br />

devebpmont in mapping, chsfiing end geodesy<br />

(MC&G). NOARL k scttiety invohmd in applying<br />

digital MC&G deta to the support d neval<br />

W3SP0rrS SYSterTISad in conducting resesmh to<br />

impruve these data. NOARL wss craalad in I<br />

19a9 as a merger of three razaarch units: Neval<br />

Oman Resasrch and Devebpmerrl Activity, the<br />

Institute for Navel @eenography, and the Navel<br />

Environmental Predktion Research %cili.<br />

Naval Surface Warfaro Center (NSWC)--<br />

ArI irdustriaily Iunded Navy tadii ksted in<br />

Whiie Ctak, MO. ard Dahlgren, VA, Aid<br />

conducts research and devebpment in e<br />

variety of vmrfare dii@ines includii MC6G.<br />

Roms Lnboratorlea (RL)-lhe principal<br />

orga~atmn charged with conducting Air pars.<br />

research and development programs relsdad to I<br />

c31 (rnmrn.”d, ccmtml, communications and<br />

intelligence). RL rnis@en areas irrcfude<br />

cernmunicdbns, .Iectmrnagne!k guktenm end<br />

mntrd, surveillance d ground and asmspce<br />

objects, intelligence data handliig, inform.lion<br />

systems fwhnofogy. .Jacfronic relbMy,<br />

rrrsirrtainabilii, and oornpatbilii.<br />

U.S. Army Topographic Englnearing<br />

Cantar (TEC or USATEC~Army<br />

Iaborafories foaled in Feri Belvoir, VA, whiih<br />

support the Army’s mcdem waepons and<br />

wmmsrsd and control systems through research<br />

end devabpment in mapping, charting, Ierrsin<br />

mdysis, geodesy, remote sensing, fmirrt I<br />

pmWoning, surveying and tend navigation. TEC<br />

.1s0 mnducts research on anvironmentel effects<br />

on military equipment, devabping t0p08MphiC<br />

suppert systems, end terrain arrhlysis products.<br />

293


A.2.<br />

Abbfeviatiau. 235<br />

Amnyms, 2ss<br />

!%!<br />

D, 63<br />

E. 79<br />

F: 91<br />

G, 101<br />

H. 116<br />

1,“125<br />

Iniliils, 2S5<br />

J, 135<br />

K, 136<br />

L, 137<br />

M, 151<br />

MC & G Or@nizations, 292<br />

N, 16S<br />

o. 174<br />

P: 162<br />

a, 206<br />

R. 207<br />

s; 223<br />

T. 251<br />

U’, 271<br />

V, 274<br />

W, 279<br />

x, 282<br />

Y. 283<br />

z 2s4<br />

MIL-HDBK-850<br />

INDEX<br />

295


STANDARDIZATION DOCUMENT IMPROVEMENT PROPOSAL<br />

1. Theprqming_ rr2sdc0n@eteb lodc91,2,3.and6. In block l. bolhthe document nuni=.mdr=’ti<br />

letter should be given.<br />

2. The sdwnitterdthbfwm rn@ cm@eteblock4, 5,-6. and 7.<br />

3. Ttwprqarkw adMtynn6t PIwklear#ywUMn 3Ctdayc fmmmcei@dthetom.<br />

NOTE: ~s bn’n tMy MI be US+@ 10t’equeSCOP&d dOCUTIEt’M6, w 10 request VW3ti~S, or clarifkaticm of<br />

requirements on aJrr@ contrads. Canrnentsedrnkted Onttk!sfOml dOnOttitiew k#yauhd2atiito<br />

Wivesny pwtiondthemhmnced docunwd(s) or to 8nlend cordrnclual m@mn=ds.<br />

. REASON FOR RECOMMENDATION<br />

DD Fon’11 1426, OCT 89<br />

1<br />

Fmtiu# dtbn, *M &mJob. ,mm

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