Using a global aerosol model adjoint to unravel the footprint of spatially-distributed emissions on cloud droplet number and cloud albedo

The adjoints of the GEOS‐Chem Chemical Transport Model and a comprehensive cloud droplet parameterization are coupled to study the sensitivity of cloud droplet number concentration (Nd) over US regions and Central Europe to global emissions of anthropogenic fine mode aerosol precursors. Simulations...

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Bibliographic Details
Published inGeophysical research letters Vol. 39; no. 24
Main Authors Karydis, V. A., Capps, S. L., Moore, R. H., Russell, A. G., Henze, D. K., Nenes, A.
Format Journal Article
LanguageEnglish
Published Washington, DC Blackwell Publishing Ltd 28.12.2012
American Geophysical Union
John Wiley & Sons, Inc
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Summary:The adjoints of the GEOS‐Chem Chemical Transport Model and a comprehensive cloud droplet parameterization are coupled to study the sensitivity of cloud droplet number concentration (Nd) over US regions and Central Europe to global emissions of anthropogenic fine mode aerosol precursors. Simulations reveal that the Nd over the midwestern and southeastern US is mostly sensitive to SO2 emissions during August, and to NH3 emissions during February. Over the western US, Nd is mostly sensitivity to SO2 and primary organic aerosol emissions. In Central Europe, Nd is most sensitive to NH3 and NOx emissions. As expected, local emissions strongly affect Nd; long‐range transport, however, is also important for the western US and Europe. Emissions changes projected for the year 2050 are estimated to have the largest impacts on cloud albedo andNd over Central Europe during August (42% and 82% change, respectively) and western US during February (12% and 36.5% change, respectively). Key Points Adjoint modeling unravels the impact of aerosol on cloud properties Long range transport of aerosol has important impacts on clouds Future emissions will impact droplet number mostly central Europe
Bibliography:istex:2420B13342DF0B7EE776BDCD8495D184DC6FD1A1
ArticleID:2012GL053346
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ISSN:0094-8276
1944-8007
DOI:10.1029/2012GL053346