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タイトルClimate forcing by anthropogenic aerosols
著者(英)Hansen, J. E.; Hales, J. M.; Charlson, R. J.; Hofmann, D. J.; Coakley, J. A., Jr.; Schwartz, S. E.; Cess, R. D.
著者所属(英)State Univ. of New York|Brookhaven National Lab.|Washington Univ.|NASA Goddard Inst. for Space Studies|Oregon State Univ.|Pacific Northwest Lab.|National Oceanic and Atmospheric Administration
発行日1992-01-24
言語eng
内容記述Although long considered to be of marginal importance to global climate change, tropospheric aerosol contributes substantially to radiative forcing, and anthropogenic sulfate aerosol, in particular, has imposed a major perturbation to this forcing. Both the direct scattering of short-wavelength solar radiation and the modification of the shortwave reflective properties of clouds by sulfate aerosol particles increase planetary albedo, thereby exerting a cooling influence on the planet. Current climate forcing due to anthropogenic sulfate is estimated to be -1 to -2 watts per square meter, globally averaged. This perturbation is comparable in magnitude to current anthropogenic greenhouse gas forcing but opposite in sign. Thus, the aerosol forcing has likely offset global greenhouse warming to a substantial degree. However, differences in geographical and seasonal distributions of these forcings preclude any simple compensation. Aerosol effects must be taken into account in evaluating anthropogenic influences on past, current, and projected future climate and in formulating policy regarding controls on emission of greenhouse gases and sulfur dioxide. Resolution of such policy issues requires integrated research on the magnitude and geographical distribution of aerosol climate forcing and on the controlling chemical and physical processes.
NASA分類ENVIRONMENT POLLUTION
レポートNO92A22348
権利Copyright
URIhttps://repository.exst.jaxa.jp/dspace/handle/a-is/329785


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