作者: J. Murray Mitchell
DOI: 10.1175/1520-0450(1971)010<0703:TEOAAO>2.0.CO;2
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摘要: Abstract A generalized model of the effect an optically thin atmospheric aerosol on terrestrial heat budget is proposed, and applied to problem estimating impact temperatures near earth's surface. The distinction between warming cooling surface attributable found basis this depend whether ratio absorption a backscatter b incoming solar radiation by greater or less than critical (a/b)O = C(1−A)(1−Ak)/[D(1+A)−C(1−A)], where albedo, C fraction sensible total (sensible plus latent) heating surface, D that in convective contact with k multiple measures relative backscattering efficiency respect reflected upward from drawn stratospheric (D=0) which generally cools atmosphere surfac...