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I<br />
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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 />
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295
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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
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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
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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
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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 />
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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
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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.
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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 />
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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
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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
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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
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i,<br />
I<br />
I<br />
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1<br />
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
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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