Publication Date:
2019-07-18
Description:
The light absorption coefficient, Beta(a) of the stratospheric aerosol is an important quantity that determines its radiative effects. When combined with the aerosol scattering coefficient, Beta(a) it becomes possible to evaluate the aerosol single scatter albedo, omega = Beta(s)/(Beta(s) + Beta(a)) which is essential for modeling the overall radiative effects of the stratospheric aerosol. Pollack1 determined that omega = 0.98 is a critical value that separates stratospheric cooling from warming.
Keywords:
Geophysics
Type:
European Aerosol Conference; Sep 14, 1997 - Sep 19, 1997; Hamburg; Germany
Format:
text
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