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Radiative Forcing and Climate Sensitivity

Lacis, A. A., and M. I. Mishchenko, Climate Forcing, Climate Sensitivity, and Climate Response A Radiative Modeling Perspective on Atmospheric Aerosols, in Aerosol Forcing of Climate (R. J. Charlson and J. Heintzenberg, Eds.), Wiley, New York, 1995. [Pg.836]

The influence of aerosols on radiative forcing depends on the balance between three essential quantities single-scattering albedo, upscatter fraction, and optical depth—all are sensitive functions of the aerosol chemical composition and size distribution in the 0.1 to 1.0 pm range [1,14]. Aerosol climate forcing, AF, depends on geophysical and aerosol parameters and can be expressed as... [Pg.434]

TABLE 21.3 Surface Temperature Changes Using a One-Dimensional Radiative-Convective Model (Assuming No Feedbacks) for a Range of Forcing Mechanisms, Together with the Radiative Forcing at the Tropopause (AF) and the Climate Sensitivity Parameter (Ao)"... [Pg.1103]


See other pages where Radiative Forcing and Climate Sensitivity is mentioned: [Pg.1101]    [Pg.1101]    [Pg.1103]    [Pg.345]    [Pg.406]    [Pg.1101]    [Pg.1101]    [Pg.1103]    [Pg.345]    [Pg.406]    [Pg.1040]    [Pg.2044]    [Pg.493]    [Pg.493]    [Pg.20]    [Pg.2043]    [Pg.2049]    [Pg.1040]    [Pg.1041]    [Pg.1103]    [Pg.152]    [Pg.145]   


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Forcings, climate

Radiative forcing

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