Reduction of aerosol absorption in Beijing since 2007 from MODIS and AERONET

dc.contributor.authorLyapustin, Alexei
dc.contributor.authorSmirnov, A.
dc.contributor.authorHolben, B.
dc.contributor.authorChin, M.
dc.contributor.authorStreets, D. G.
dc.contributor.authorLu, Z.
dc.contributor.authorKahn, R.
dc.contributor.authorSlutsker, I.
dc.contributor.authorLaszlo, I.
dc.contributor.authorKondragunta, S.
dc.contributor.authorTanré, D.
dc.contributor.authorDubovik, O.
dc.contributor.authorGoloub, P.
dc.contributor.authorChen, H.-B.
dc.contributor.authorSinyuk, A.
dc.contributor.authorWang, Yujie
dc.contributor.authorKorkin, Sergey
dc.date.accessioned2024-09-04T19:58:15Z
dc.date.available2024-09-04T19:58:15Z
dc.date.issued2011-05-20
dc.description.abstractAn analysis of the time series of MODIS-based and AERONET aerosol records over Beijing reveals two distinct periods, before and after 2007. The MODIS data from both the Terra and Aqua satellites were processed with the new Multi-Angle Implementation of Atmospheric Correction (MAIAC) algorithm. A comparison of MAIAC and AERONET AOT shows that whereas MAIAC consistently underestimated peak AOT values by 10–20% in the prior period, the bias mostly disappears after mid-2007. Independent analysis of the AERONET dataset reveals little or no change in the effective radii of the fine and coarse fractions and of the Ångström exponent. At the same time, it shows an increasing trend in the single scattering albedo, by ∼0.02 in 9 years. As MAIAC was using the same aerosol model for the entire 2000–2010 period, the decrease in AOT bias after 2007 can be explained only by a corresponding decrease of aerosol absorption caused by a reduction in local black carbon emissions. The observed changes correlate in time with the Chinese government's broad measures to improve air quality in Beijing during preparations for the Summer Olympics of 2008.
dc.description.sponsorshipThe research of A. Lyapustin, Y. Wang and S. Korkin was funded by the NASA Terrestrial Ecology Program (D. Wickland), NASA Applications Program (L. Friedl, B. Doorn) and in part by the NOAA GOES-R program (M. Goldberg). The first author thanks S. Platnick for a helpful discussion on data analysis._x000D_The Editor thanks two anonymous reviewers for their assistance in evaluating this paper.
dc.description.urihttps://onlinelibrary.wiley.com/doi/abs/10.1029/2011GL047306
dc.format.extent5 pages
dc.genrejournal articles
dc.identifierdoi:10.13016/m2mqva-npa4
dc.identifier.citationLyapustin, A., A. Smirnov, B. Holben, M. Chin, D. G. Streets, Z. Lu, R. Kahn, et al. “Reduction of Aerosol Absorption in Beijing since 2007 from MODIS and AERONET.” Geophysical Research Letters 38, no. 10 (2011). https://doi.org/10.1029/2011GL047306.
dc.identifier.urihttps://doi.org/10.1029/2011GL047306
dc.identifier.urihttp://hdl.handle.net/11603/35940
dc.language.isoen_US
dc.publisherAGU
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC GESTAR II
dc.relation.ispartofUMBC Joint Center for Earth Systems Technology (JCET)
dc.relation.ispartofUMBC Faculty Collection
dc.rightsThis work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.
dc.rightsPublic Domain
dc.rights.urihttps://creativecommons.org/publicdomain/mark/1.0/
dc.subjectabsorption
dc.subjectBeijing
dc.subjectaerosol
dc.subjectBC
dc.subjectemissions
dc.titleReduction of aerosol absorption in Beijing since 2007 from MODIS and AERONET
dc.typeText
dcterms.creatorhttps://orcid.org/0000-0003-1105-5739
dcterms.creatorhttps://orcid.org/0000-0002-5576-6711
dcterms.creatorhttps://orcid.org/0000-0001-6514-5233

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