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Absorption Angstrom exponent (AAE, 470/950 nm) versus scattering Angstrom exponent (SAE, 450/635 nm), color coded by the aerosol absorption coefficient at 880 nm. Dry daily average values are shown (February 2014-June 2018). The classification by aerosol type is based on Cazorla et al. (2013).

Absorption Angstrom exponent (AAE, 470/950 nm) versus scattering Angstrom exponent (SAE, 450/635 nm), color coded by the aerosol absorption coefficient at 880 nm. Dry daily average values are shown (February 2014-June 2018). The classification by aerosol type is based on Cazorla et al. (2013).

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In 2014, Pha Din (1466 m a.s.l.) was established as a Global Atmosphere Watch (GAW) regional station for aerosol and trace gas measurements in northwestern Vietnam. This study presents a five-year climatology of aerosol optical properties derived from nephelometer and aethalometer measurements and a comparison with ground-based remote sensing measu...

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... CO emissions Supplementary Information). In contrast, the lower values in the summer months largely coincide with the SE Asian summer monsoon with more rain and generally more humid conditions. During the time period covered so far by the measurements at Pha Din, a decrease in peak intensity for all parameters is observed between 2014 and 2018. Fig. 3 shows a classification of aerosol types based on AAE and SAE (Cazorla et al., 2013). AAE dry reaches 1.6-2.0 during BB periods, a typical value for BB dominated aerosol in northern Indochina ( Wang et al., 2015). SAE dry is > 1.5, pointing to a dominant contribution of accumulation mode particles to light scattering, as is expected for ...
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... during BB periods, a typical value for BB dominated aerosol in northern Indochina ( Wang et al., 2015). SAE dry is > 1.5, pointing to a dominant contribution of accumulation mode particles to light scattering, as is expected for BB aerosols, and does not indicate a significant influence of coarse mode dust. According to the classification used in Fig. 3, the aerosol detected during high BB episodes is thus characterized as "OC dominated", while for the rest of the year, the major fraction of the data is classified as "EC/OC ...

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... Here we report on long-term observations of CO, ozone (O3) and carbonaceous greenhouse gases (GHG) including carbon dioxide (CO2) and methane (CH4) based on measurements performed at the regional Global Atmosphere Watch (GAW) station Pha Din (PDI) in Northwestern Vietnam. Our study on trace gases complements previous studies at PDI, which focused on aerosol optical properties (Bukowiecki et al., 2019) and carbonaceous aerosol composition (Nguyen et al., 2021). ...
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We investigated concentrations of organic carbon (OC), elemental carbon (EC) and a wide range of particle-bound organic compounds in daily sampled PM2.5 at the remote Pha Din (PDI) – Global Atmosphere Watch (GAW) monitoring station in Northwestern Vietnam during an intense 3-week sampling campaign from 23rd March to 12th April 2015. The site is known to receive trans-regional air masses during large-scale biomass burning episodes, but OC composition studies are missing in the scientific literature. We quantified 51 organic compounds simultaneously by in-situ derivatization thermal desorption gas chromatography time-of-flight mass spectrometry (IDTD-GC-TOFMS). Anhydrosugars, methoxyphenols, n-alkanes, fatty acids, polycyclic aromatic hydrocarbons, oxygenated polycyclic aromatic hydrocarbons, nitrophenols as well as OC were used in a hierarchical cluster analysis highlighting distinctive patterns for periods under low, medium and high biomass burning (BB) influence. The highest particle phase concentration of the typical primary organic aerosol (POA) and possible secondary organic aerosol (SOA) constituents, especially nitrophenols, were found on 5th and 6th April. We linked the trace gases CH4, CO2, CO, O3 mixing ratios to the statistical classification of BB events based on OA composition and found increased CO and O3 levels during medium and high BB influence. Likewise, a backward trajectory analysis indicates different source regions for the identified periods based on the OA cluster, with cleaner air masses arriving from northeast, i.e., mainland China and Yellow sea. The more polluted periods are characterized by trajectories from southwest, with more continental recirculation of the medium cluster, and more westerly advection for the high cluster. These findings highlight that BB activities in Northern Southeast Asia cannot only significantly enhance the regional organic aerosol loading, but also affect the carbonaceous PM2.5 constituents and the trace gases in northwestern Vietnam. The presented analysis adds valuable data on the carbonaceous and in particular OC chemical composition of PM2.5 in a region of scarce data availability.
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