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  4. Particulate absorption of solar radiation: anthropogenic aerosols vs. dust

Particulate absorption of solar radiation: anthropogenic aerosols vs. dust

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Author(s)
Wang, Chien
•
Jeong, Gill-Ran
•
Mahowald, N. M.
Date Issued
March 2009
Journal
Atmospheric Chemistry and Physics Discussions
Publisher
Copernicus Publications on behalf of the European Geophysical Society
Citation
Wang, C., G. R. Jeong, and N. Mahowald. "Particulate absorption of solar radiation: anthropogenic aerosols vs. dust." Atmospheric Chemistry and Physics Discussions, 9, 3935–3945, 2009.
Version
Final published version
Abstract
Particulate solar absorption is a critical factor in determining the value and even sign of the direct radiative forcing of aerosols. The heating to the atmosphere and cooling to the Earth’s surface caused by this absorption are hypothesized to have significant climate impacts. We find that anthropogenic aerosols play an important role around the globe in total particulate absorption of solar radiation. The global-average anthropogenic fraction in total aerosol absorbing optical depth exceeds 65% in all seasons. Combining the potentially highest dust absorption with the lowest anthropogenic absorption within our model range, this fraction would still exceed 47% in most seasons except for boreal spring (36%) when dust abundance reaches its peak. Nevertheless, dust aerosol is still a critical absorbing constituent over places including North Africa, the entire tropical Atlantic, and during boreal spring in most part of Eurasian continent. The equality in absorbing solar radiation of dust and anthropogenic aerosols appears to be particularly important over Indian subcontinent and nearby regions as well as North Africa.
MIT Department
Massachusetts Institute of Technology. Center for Global Change Science
Massachusetts Institute of Technology. Joint Program on the Science & Policy of Global Change
Terms of Use
Creative Commons Attribution 3.0
http://creativecommons.org/licenses/by/3.0
Persistent DSpace Link
http://hdl.handle.net/1721.1/66112
DOI of Published Version
http://www.atmos-chem-phys.net/9/3935/2009/acp-9-3935-2009.pdf
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