Recent advances in understanding secondary organic aerosol: Implications for global climate forcing
Supporting Files
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2017
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Source Reviews of Geophysics, 55(2), 509-559
Details
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Journal Title:Reviews of Geophysics
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Personal Author:Shrivastava, Manish
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Cappa, Christopher D.
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Fan, Jiwen
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Goldstein, Allen H.
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Guenther, Alex B.
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Jimenez, Jose L.
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Kuang, Chongai
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Laskin, Alexander
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Martin, Scot T.
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Ng, Nga Lee
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Petaja, Tuukka
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Pierce, Jeffrey R.
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Rasch, Philip J.
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Roldin, Pontus
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Seinfeld, John H.
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Shilling, John
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Smith, James N.
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Thornton, Joel A.
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Volkamer, Rainer
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Wang, Jian
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Worsnop, Douglas R.
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Zaveri, Rahul A.
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Zelenyuk, Alla
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Zhang, Qi
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NOAA Program & Office:
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Description:Anthropogenic emissions and land use changes have modi fied atmospheric aerosol concentrations and size distributions over time. Understanding preindustrial conditions and changes in organic aerosol due to anthropogenic activities is important because these features (1) in fluence estimates of aerosol radiative forcing and (2) can confound estimates of the historical response of climate to increases in greenhouse gases. Secondary organic aerosol (SOA), formed in the atmosphere by oxidation of organic gases, represents a major fraction of global submicron-sized atmospheric organic aerosol. Over the pastdecade, signi ficant advances in understanding SOA properties and formation mechanisms have occurred through measurements, yet current climate models typically do not comprehensively include all important
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Source:Reviews of Geophysics, 55(2), 509-559
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DOI:
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ISSN:8755-1209 ; 1944-9208
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Rights Information:Other
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Compliance:Library
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Main Document Checksum:urn:sha256:70b161081a548cc979b074b7414a6a589d9151c5ee13772bc4ab019022cf4cd2
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