Article ID Journal Published Year Pages File Type
1782515 Planetary and Space Science 2007 7 Pages PDF
Abstract
The diffusely reflected intensity and emergent intensity for the case of coherent anisotropic scattering are derived in the nth approximation from a radiative transfer equation with linear Planck function and planetary phase function. This is then made exact allowing n tending to infinity.
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Physical Sciences and Engineering Earth and Planetary Sciences Geophysics
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Anisotropic coherent scattering with planetary phase function
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