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    Estimates for Infrared Transfer in Finite Clouds

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 004::page 378
    Author:
    O'Brien, D. M.
    DOI: 10.1175/1520-0469(1986)043<0378:EFITIF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Upper and lower bounds are computed for the infrared radiance within a cloud of finite size. The bounds are established by an iterative procedure, analogous to the iterative solution of the radiative transfer equation, except that at every iteration the angular integration in the scattering term of the radiative transfer equation is restricted to a fixed conical region. The estimates are not restricted to clouds of any particular shape, temperature distribution, or radiance field incident upon the cloud. The absorption approximation, in which the albedo is set to zero and scattering is neglected, is shown to lie between the upper and lower bounds. As an illustration, estimates are derived for a cubic cloud (Deirmendjian's C1, 10 ?m) to obtain cheeks on numerical solutions of the radiative transfer equation (RTE) computed by various authors. For the cubic cloud, it is observed that the absorption approximation is in reasonable agreement with the results of a Monte-Carlo simulation.
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      Estimates for Infrared Transfer in Finite Clouds

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4155329
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    contributor authorO'Brien, D. M.
    date accessioned2017-06-09T14:26:15Z
    date available2017-06-09T14:26:15Z
    date copyright1986/02/01
    date issued1986
    identifier issn0022-4928
    identifier otherams-19235.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155329
    description abstractUpper and lower bounds are computed for the infrared radiance within a cloud of finite size. The bounds are established by an iterative procedure, analogous to the iterative solution of the radiative transfer equation, except that at every iteration the angular integration in the scattering term of the radiative transfer equation is restricted to a fixed conical region. The estimates are not restricted to clouds of any particular shape, temperature distribution, or radiance field incident upon the cloud. The absorption approximation, in which the albedo is set to zero and scattering is neglected, is shown to lie between the upper and lower bounds. As an illustration, estimates are derived for a cubic cloud (Deirmendjian's C1, 10 ?m) to obtain cheeks on numerical solutions of the radiative transfer equation (RTE) computed by various authors. For the cubic cloud, it is observed that the absorption approximation is in reasonable agreement with the results of a Monte-Carlo simulation.
    publisherAmerican Meteorological Society
    titleEstimates for Infrared Transfer in Finite Clouds
    typeJournal Paper
    journal volume43
    journal issue4
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1986)043<0378:EFITIF>2.0.CO;2
    journal fristpage378
    journal lastpage387
    treeJournal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian