Article ID Journal Published Year Pages File Type
5430560 Journal of Quantitative Spectroscopy and Radiative Transfer 2008 20 Pages PDF
Abstract

Rates of radiative heating and cooling of the non-scattering planetary atmosphere and scattering underlying surface are analytically linearized with respect to the atmospheric and surface parameters. Resulting expressions for sensitivities of radiative heating and cooling rates are used to formulate the linearized 1D radiative model of atmospheric dynamics which directly incorporates the relevant linearized atmospheric and surface parameters. Applications to more sophisticated models of atmospheric dynamics, as well as extension to the case of presence of atmospheric scattering, are briefly discussed.

Related Topics
Physical Sciences and Engineering Chemistry Spectroscopy
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