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    Infrared Radiative Transfer Through a Regular Array of Cuboidal Clouds

    Source: Journal of the Atmospheric Sciences:;1982:;Volume( 039 ):;issue: 002::page 431
    Author:
    Harshvardhan
    ,
    Weinman, James A.
    DOI: 10.1175/1520-0469(1982)039<0431:IRTTAR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A study has been made of infrared radiative transfer through a regular array of cuboidal clouds which considers the interaction of the sides of the clouds with each other and the ground. The theory is developed for black clouds and is extended to scattering clouds using a variable azimuth two-stream (VATS) approximation (Harshvardhan et al., 1981). It is shown that geometrical considerations often dominate over the microphysical aspects of radiative transfer through the clouds. For example, the difference in simulated 10 ?m brightness temperature between black isothermal cubic clouds and cubic clouds of optical depth 10, is <2 K for zenith angles <50° for all cloud fractions when viewed parallel to the array. The results show that serious errors are made in flux and cooling rate computations if broken clouds are modeled as planiform. Radiances computed by the usual practice of area-weighting cloudy- and clear-sky radiances are in error by 2?8 K in brightness temperature for cubic clouds over a wide range of cloud fractions and zenith angles. It is also shown that the lapse rate does not markedly affect the exiting radiances for cuboidal clouds of unit aspect ratio and optical depth 10.
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      Infrared Radiative Transfer Through a Regular Array of Cuboidal Clouds

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4154287
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    contributor authorHarshvardhan
    contributor authorWeinman, James A.
    date accessioned2017-06-09T14:22:52Z
    date available2017-06-09T14:22:52Z
    date copyright1982/02/01
    date issued1982
    identifier issn0022-4928
    identifier otherams-18298.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154287
    description abstractA study has been made of infrared radiative transfer through a regular array of cuboidal clouds which considers the interaction of the sides of the clouds with each other and the ground. The theory is developed for black clouds and is extended to scattering clouds using a variable azimuth two-stream (VATS) approximation (Harshvardhan et al., 1981). It is shown that geometrical considerations often dominate over the microphysical aspects of radiative transfer through the clouds. For example, the difference in simulated 10 ?m brightness temperature between black isothermal cubic clouds and cubic clouds of optical depth 10, is <2 K for zenith angles <50° for all cloud fractions when viewed parallel to the array. The results show that serious errors are made in flux and cooling rate computations if broken clouds are modeled as planiform. Radiances computed by the usual practice of area-weighting cloudy- and clear-sky radiances are in error by 2?8 K in brightness temperature for cubic clouds over a wide range of cloud fractions and zenith angles. It is also shown that the lapse rate does not markedly affect the exiting radiances for cuboidal clouds of unit aspect ratio and optical depth 10.
    publisherAmerican Meteorological Society
    titleInfrared Radiative Transfer Through a Regular Array of Cuboidal Clouds
    typeJournal Paper
    journal volume39
    journal issue2
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1982)039<0431:IRTTAR>2.0.CO;2
    journal fristpage431
    journal lastpage439
    treeJournal of the Atmospheric Sciences:;1982:;Volume( 039 ):;issue: 002
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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