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contributor authorWiscombe, W. J.
date accessioned2017-06-09T14:19:44Z
date available2017-06-09T14:19:44Z
date copyright1977/09/01
date issued1977
identifier issn0022-4928
identifier otherams-17347.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153231
description abstractThe delta?M method represents a natural extension of the recently proposed delta?Eddington approximation to all orders M of angular approximation. It relies essentially on matching the first 2M phase function moments and using a Dirac delta?function representation of forward scattering. Computed fluxes are remarkably accurate at very low orders M of approximation, even when the phase function is strongly asymmetric; thus the associated M ? M matrix computations remain small and manageable. Flux is automatically conserved, making phase function ?renormalization? unnecessary. Phase function truncation is effected in a much more attractive manner than in the past; furthermore, truncation tends to zero as M ? ∞. Errors are shown to oscillate with (roughly) exponentially decreasing amplitude as M increases; which has the curious consequence that increasing M by small amounts does not necessarily reduce error. Mie computations associated with the δ?M method can be considerably reduced, based on a simple technique for phase function moment calculations proposed herein.
publisherAmerican Meteorological Society
titleThe Delta–M Method: Rapid Yet Accurate Radiative Flux Calculations for Strongly Asymmetric Phase Functions
typeJournal Paper
journal volume34
journal issue9
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1977)034<1408:TDMRYA>2.0.CO;2
journal fristpage1408
journal lastpage1422
treeJournal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 009
contenttypeFulltext


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