The Delta–M Method: Rapid Yet Accurate Radiative Flux Calculations for Strongly Asymmetric Phase FunctionsSource: Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 009::page 1408Author:Wiscombe, W. J.
DOI: 10.1175/1520-0469(1977)034<1408:TDMRYA>2.0.CO;2Publisher: American Meteorological Society
Abstract: The 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.
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| contributor author | Wiscombe, W. J. | |
| date accessioned | 2017-06-09T14:19:44Z | |
| date available | 2017-06-09T14:19:44Z | |
| date copyright | 1977/09/01 | |
| date issued | 1977 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-17347.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4153231 | |
| description abstract | The 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. | |
| publisher | American Meteorological Society | |
| title | The Delta–M Method: Rapid Yet Accurate Radiative Flux Calculations for Strongly Asymmetric Phase Functions | |
| type | Journal Paper | |
| journal volume | 34 | |
| journal issue | 9 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1977)034<1408:TDMRYA>2.0.CO;2 | |
| journal fristpage | 1408 | |
| journal lastpage | 1422 | |
| tree | Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 009 | |
| contenttype | Fulltext |