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dc.contributor.authorAndrew M. Sayeren_US
dc.contributor.authorN. Christina Hsuen_US
dc.contributor.authorTa Chih Hsiaoen_US
dc.contributor.authorPeter Pantinaen_US
dc.contributor.authorFerret Kuoen_US
dc.contributor.authorChang Feng Ou-Yangen_US
dc.contributor.authorBrent N. Holbenen_US
dc.contributor.authorSerm Janjaien_US
dc.contributor.authorSomporn Chantaraen_US
dc.contributor.authorShen Hsiang Wangen_US
dc.contributor.authorAdrian M. Loftusen_US
dc.contributor.authorNeng Huei Linen_US
dc.contributor.authorSi Chee Tsayen_US
dc.date.accessioned2018-09-05T03:02:26Z-
dc.date.available2018-09-05T03:02:26Z-
dc.date.issued2016-11-01en_US
dc.identifier.issn20711409en_US
dc.identifier.issn16808584en_US
dc.identifier.other2-s2.0-84994111922en_US
dc.identifier.other10.4209/aaqr.2015.08.0500en_US
dc.identifier.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=84994111922&origin=inwarden_US
dc.identifier.urihttp://cmuir.cmu.ac.th/jspui/handle/6653943832/55858-
dc.description.abstract© Taiwan Association for Aerosol Research. The spring 2015 deployment of a suite of instrumentation at Doi Ang Khang (DAK) in northwestern Thailand enabled the characterization of air masses containing smoke aerosols from burning predominantly in Myanmar. Aerosol Robotic Network (AERONET) Sun photometer data were used to validate Moderate Resolution Imaging Spectroradiometer (MODIS) Collection 6 ‘Deep Blue’ aerosol optical depth (AOD) retrievals; MODIS Terra and Aqua provided results of similar quality, with correlation coefficients of 0.93–0.94 and similar agreement within expected uncertainties to globalaverage performance. Scattering and absorption measurements were used to compare surface and total column aerosol single scatter albedo (SSA); while the two were well-correlated, and showed consistent positive relationships with moisture (increasing SSA through the season as surface relative humidity and total columnar water vapor increased), insitu surface-level SSA was nevertheless significantly lower by 0.12–0.17. This could be related to vertical heterogeneity and/or instrumental issues. DAK is at ~1,500 m above sea level in heterogeneous terrain, and the resulting strong diurnal variability in planetary boundary layer depth above the site leads to high temporal variability in both surface and column measurements, and acts as a controlling factor to the ratio between surface particulate matter (PM) levels and column AOD. In contrast, while some hygroscopic effects were observed relating to aerosol particle size and Ångström exponent, relative humidity variations appear to be less important for the PM:AOD ratio here.en_US
dc.subjectEnvironmental Scienceen_US
dc.titleIn-situ and remotely-sensed observations of biomass burning aerosols at Doi Ang Khang, Thailand during 7-SEAS/BASELInE 2015en_US
dc.typeJournalen_US
article.title.sourcetitleAerosol and Air Quality Researchen_US
article.volume16en_US
article.stream.affiliationsUniversities Space Research Associationen_US
article.stream.affiliationsNASA Goddard Space Flight Centeren_US
article.stream.affiliationsNational Central University Taiwanen_US
article.stream.affiliationsScience Systems and Applications, Inc.en_US
article.stream.affiliationsSilpakorn Universityen_US
article.stream.affiliationsChiang Mai Universityen_US
article.stream.affiliationsUniversity of Marylanden_US
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