Simulation of the 3D Radiative Transfer with Anisotropic Scattering for Convective Trails
Analyse de l'effet d'un nuage "contrail" sur la temperature dans la vallée de Chamonix par simulation numérique des equations du transfert radiatif
Résumé
In two earlier publications we have proposed a numerical algorithm to solve the RTE in 3D based on an integro-differential formulation and iterations using H-matrices to speed-up the computation of the integrals. In this article we show how the method can be extended to handle an important class of non-isotropic scattering for the atmosphere. An application to the Earth atmosphere is given.
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