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dc.contributor.authorJun Taoen_US
dc.contributor.authorVanisa Surapipithen_US
dc.contributor.authorZhiwei Hanen_US
dc.contributor.authorTippawan Prapamontolen_US
dc.contributor.authorSawaeng Kawichaien_US
dc.contributor.authorLeiming Zhangen_US
dc.contributor.authorZhisheng Zhangen_US
dc.contributor.authorYunfei Wuen_US
dc.contributor.authorJiawei Lien_US
dc.contributor.authorJie Lien_US
dc.contributor.authorYihong Yangen_US
dc.contributor.authorRenjian Zhangen_US
dc.date.accessioned2020-10-14T08:31:48Z-
dc.date.available2020-10-14T08:31:48Z-
dc.date.issued2020-11-01en_US
dc.identifier.issn18732844en_US
dc.identifier.issn13522310en_US
dc.identifier.other2-s2.0-85089537470en_US
dc.identifier.other10.1016/j.atmosenv.2020.117821en_US
dc.identifier.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85089537470&origin=inwarden_US
dc.identifier.urihttp://cmuir.cmu.ac.th/jspui/handle/6653943832/70479-
dc.description.abstract© 2020 Elsevier Ltd Southeast Asia is one of the major regions of biomass burning in the world. To investigate the light absorption properties of carbonaceous aerosols produced from biomass burning, mass concentrations of PM2.5 and its major chemical compositions were obtained by filter sampling, and aerosol absorption coefficient (bap) at 370 nm (bap-370nm) and at 880 nm (bap-880nm) were synchronously determined for the sampled filters using a transmissometer in urban Chiang Mai of Northern Thailand during the dry season in 2019. On campaign average, the reconstructed PM2.5 mass from the measured chemical components accounted for 99% of the measured PM2.5 mass, in which organic matters (OM) accounted for 64 ± 10%. Hardwood burning was identified as the dominant source of carbonaceous aerosols. The measured aerosol absorption Ångström exponent (AAE) at 370–880 nm (AAE370–880nm) was 1.71 ± 0.24. Mass absorption efficiency (MAE) of elemental carbon (EC) and organic carbon (OC) was estimated using a multiple linear regression model between bap and mass concentrations of EC and OC, resulting in campaign-average values of 8.11 m2 g−1 and 0.24 m2 g−1 at 880 nm and 21.06 m2 g−1 and 2.57 m2 g−1 at 370 nm, respectively, which were evidently larger than those in other cities worldwide. The contributions of EC to bap in 370–880 nm spectrum region ranged from 49 ± 5% to 79 ± 3%, and those of OC ranged from 51 ± 5% to 21 ± 3%. Results from this study suggested a potentially significant impact of carbonaceous aerosols on direct radiative forcings in the dry season over Southeast Asia and downwind regions.en_US
dc.subjectEarth and Planetary Sciencesen_US
dc.subjectEnvironmental Scienceen_US
dc.titleHigh mass absorption efficiency of carbonaceous aerosols during the biomass burning season in Chiang Mai of northern Thailanden_US
dc.typeJournalen_US
article.title.sourcetitleAtmospheric Environmenten_US
article.volume240en_US
article.stream.affiliationsSouth China Institute Of Environmental Sciencesen_US
article.stream.affiliationsUniversity of Chinese Academy of Sciencesen_US
article.stream.affiliationsJinan Universityen_US
article.stream.affiliationsInstitute of Atmospheric Physics Chinese Academy of Sciencesen_US
article.stream.affiliationsUniversity of Electronic Science and Technology of Chinaen_US
article.stream.affiliationsChiang Mai Universityen_US
article.stream.affiliationsEnvironment Canadaen_US
article.stream.affiliationsNational Astronomical Research Institute of Thailanden_US
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