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Federal Science Research on the Role of Aerosols in Climate Change. Sylvia A. Edgerton * National Science Foundation. Workshop on Secondary Organic Aerosols, Reno NV February 5, 2002.
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Federal Science Research on the Role of Aerosols in Climate Change Sylvia A. Edgerton* National Science Foundation Workshop on Secondary Organic Aerosols, Reno NV February 5, 2002 * Thanks to Dr. Joel Levy, Atmospheric Chemistry Program Manager at NOAA, for preparing many of the slides related to aerosols and climate.
Aerosols and Climate • Aerosols are intimately and significantly linked to the workings of the climate system • Historical view understates the role of aerosols in climate • Aerosols exert very large regional effects not reflected in global averages • Aerosols significantly influence surface energy flux budgets • Aerosols may significantly influence precipitation • Focused aerosol/climate research is an essential for operational climate prediction • Critically selected measurements are required • Research must be targeted at conceptual breakthroughs
Aerosol Radiative Forcing Mechanisms • Direct Effect • Light Scattering and Absorption ==> surface cooling, atmospheric warming • 1st Indirect Effect (Twomey Effect) • Decreased cloud droplet size • Increased cloud droplet concentrations ==> brighter clouds • 2nd Indirect Effect (feedback?) • Increased cloud lifetime and/or thickness ==> suppression of drizzle • Semi-Direct Effect (feedback?) • Cloud burning due to atmospheric heating
IPCC(2001) Global and Annual Mean Radiative Forcing What’s not in this picture? • Aerosol 2nd indirect effect omitted • Aerosol semi-direct effect omitted • Regional character of aerosol forcing not represented • Aerosol models are largely unvalidated
What are aerosol indirect effects? Aerosol-forced perturbations in cloud optical properties, resulting from changes in cloud drop concentration, physical thickness, effective radius, and horizontal extent (cloud fraction) that lead to a change in the earth's cloud radiative forcing
IPCC (1995) - Invoked aerosol cooling to offset GCM overestimates of greenhouse warming Crude Aerosol Model • Sulfate only • Light-scattering only phenomenon included • Impact on albedo computed off-line
Radiative Forcing by Species Hansen (2001)
Optical Properties of Aerosols Data courtesy of Quinn Hegg et al (1997)
Results from recent field programs suggest that regional aerosol-induced surface cooling is large!
Large-scale observational evidence for suppression of precipitation by aerosols Aerosol 2nd Indirect Effect ==> Small droplets coalesce less efficiently than large droplets • AVHRR image over Australia shows pollution tracks from • power plant (5), smelter (6), port (7), refinery (8) • Yellow denotes smaller cloud droplets • Co-located measurements from TRMM/PR show • precipitation outside pollution tracks • no precipitation inside pollution tracks • Similar observations have been made for biomass smoke and dust D. Rosenfeld, Science 287, 1793 (2000)
Recommendations for future research from a recent workshop on aerosol-climate interactionsScripps Institution of Oceanography January 2002 • Characterize the sources, distribution, and properties of aerosols and their influence on cloud formation and rainfall, globally and a region-by-region basis • Represent aerosol impacts in climate models by linking their representation to these observations • Quantify the relative importance of aerosols and greenhouse gases for global warming
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