Gaussian Quadrature and Its Application to Infrared RadiationSource: Journal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 005::page 753Author:Li, J.
DOI: 10.1175/1520-0469(2000)057<0753:GQAIAT>2.0.CO;2Publisher: American Meteorological Society
Abstract: The Gaussian integration of moments is systematically discussed. It is shown that the well-known diffusivity-factor approximation is equivalent to a one-node Gaussian quadrature. The limit as the moment power approaches infinity in a one-node Gaussian quadrature produces a diffusivity factor of e1/2 = 1.648?721?3, which is very close to the value of 1.66 suggested by Elsasser. The errors due to the diffusivity-factor approximation are analyzed in a one-dimensional radiative transfer model. Generally, the results cannot be improved by using other one-node Gaussian quadrature schemes with different moments. More accurate results can be obtained by using higher-node Gaussian quadratures. It is found that the limit as the moment power approaches infinity always produces the best results. The computational advantage of the diffusivity-factor approximation is kept in the higher-node Gaussian quadratures. It is, therefore, feasible to implement the higher-node Gaussian quadratures in climate models.
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contributor author | Li, J. | |
date accessioned | 2017-06-09T14:36:01Z | |
date available | 2017-06-09T14:36:01Z | |
date copyright | 2000/03/01 | |
date issued | 2000 | |
identifier issn | 0022-4928 | |
identifier other | ams-22555.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4159018 | |
description abstract | The Gaussian integration of moments is systematically discussed. It is shown that the well-known diffusivity-factor approximation is equivalent to a one-node Gaussian quadrature. The limit as the moment power approaches infinity in a one-node Gaussian quadrature produces a diffusivity factor of e1/2 = 1.648?721?3, which is very close to the value of 1.66 suggested by Elsasser. The errors due to the diffusivity-factor approximation are analyzed in a one-dimensional radiative transfer model. Generally, the results cannot be improved by using other one-node Gaussian quadrature schemes with different moments. More accurate results can be obtained by using higher-node Gaussian quadratures. It is found that the limit as the moment power approaches infinity always produces the best results. The computational advantage of the diffusivity-factor approximation is kept in the higher-node Gaussian quadratures. It is, therefore, feasible to implement the higher-node Gaussian quadratures in climate models. | |
publisher | American Meteorological Society | |
title | Gaussian Quadrature and Its Application to Infrared Radiation | |
type | Journal Paper | |
journal volume | 57 | |
journal issue | 5 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(2000)057<0753:GQAIAT>2.0.CO;2 | |
journal fristpage | 753 | |
journal lastpage | 765 | |
tree | Journal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 005 | |
contenttype | Fulltext |