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    Gaussian Quadrature and Its Application to Infrared Radiation

    Source: Journal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 005::page 753
    Author:
    Li, J.
    DOI: 10.1175/1520-0469(2000)057<0753:GQAIAT>2.0.CO;2
    Publisher: 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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      Gaussian Quadrature and Its Application to Infrared Radiation

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    contributor authorLi, J.
    date accessioned2017-06-09T14:36:01Z
    date available2017-06-09T14:36:01Z
    date copyright2000/03/01
    date issued2000
    identifier issn0022-4928
    identifier otherams-22555.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159018
    description abstractThe 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.
    publisherAmerican Meteorological Society
    titleGaussian Quadrature and Its Application to Infrared Radiation
    typeJournal Paper
    journal volume57
    journal issue5
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(2000)057<0753:GQAIAT>2.0.CO;2
    journal fristpage753
    journal lastpage765
    treeJournal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 005
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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