Notions of scale hierarchy and closure are introduced into the radiative transfer equation, and it is demonstrated how the customary treatment of partial cloudiness based on cloud amount as a weighting parameter is a special form of closure. Another simple example of closure is described which allows for the treatment of spatial inhomogeneities as a new form of optical property. This concept is introduced into a two-stream model to demonstrate, in a gross way, the effects of inhomogeneities on radiative transfer. -from Author
CITATION STYLE
Stephens, G. L. (1988). Radiative transfer through arbitrarily shaped optical media. Part II: group theory and simple closures. Journal of the Atmospheric Sciences, 45(12), 1837–1848. https://doi.org/10.1175/1520-0469(1988)045<1837:rttaso>2.0.co;2
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