Albedo-shift method in the problem of anisotropic light scattering in a plane atmosphere.

Details Albedo-shift method in the problem of anisotropic light scattering in a plane atmosphere. Albedo-shift method in the problem of anisotropic light scattering in a plane atmosphere.

Oct 1998

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1998ap.....41..408i&link_type=abstract

Astrophysics, Volume 41, Issue 4, pp.408-426

Astronomy and Astrophysics

Astrophysics

Radiative Transfer: Scattering

Scientific paper

A standard problem of radiative transfer theory — calculating the diffuse reflection and transmission of radiation by a plane scattering atmosphere — is considered. The recently proposed albedoshift method is used to calculate the X and Y functions (and the H function) for the case of anisotropic scattering with a Henyey-Greenstein indicatrix. The method enables one to “suppress” scattering and obtain iterative solutions of high accuracy in only a few iterations, even when the mean number of photon scatterings in the atmosphere is very large.

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