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    Atmospheric Solar Heating Rate in the Water Vapor Bands

    Source: Journal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 011::page 1532
    Author:
    Chou, Ming-Dah
    DOI: 10.1175/1520-0450(1986)025<1532:ASHRIT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The total absorption of solar radiation by water vapor in clear atmosphere is parameterized as a simple function of the scaled water vapor amount. For applications to cloudy and hazy atmospheres, the flux-weighted k-distribution functions are computed for individual absorption bands and for the total near-infrared region. The parameterization is based upon monochromatic calculations and follows essentially the scaling approximation of Chou and Arking, but the effect of temperature variation with height is taken into account in order to enhance the accuracy. Furthermore, the spectral range is extended to cover the two weak bands centered at 0.72 and 0.82 ?m. Comparisons with monochromatic calculations show that the atmospheric heating rate and the surface radiation can be accurately computed from the parameterization. Comparisons are also made with other parameterizations. It is found that the absorption of solar radiation can be computed reasonably well using the Goody band model and the Curtis-Godson approximation.
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      Atmospheric Solar Heating Rate in the Water Vapor Bands

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4146261
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    contributor authorChou, Ming-Dah
    date accessioned2017-06-09T14:01:25Z
    date available2017-06-09T14:01:25Z
    date copyright1986/11/01
    date issued1986
    identifier issn0733-3021
    identifier otherams-11073.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146261
    description abstractThe total absorption of solar radiation by water vapor in clear atmosphere is parameterized as a simple function of the scaled water vapor amount. For applications to cloudy and hazy atmospheres, the flux-weighted k-distribution functions are computed for individual absorption bands and for the total near-infrared region. The parameterization is based upon monochromatic calculations and follows essentially the scaling approximation of Chou and Arking, but the effect of temperature variation with height is taken into account in order to enhance the accuracy. Furthermore, the spectral range is extended to cover the two weak bands centered at 0.72 and 0.82 ?m. Comparisons with monochromatic calculations show that the atmospheric heating rate and the surface radiation can be accurately computed from the parameterization. Comparisons are also made with other parameterizations. It is found that the absorption of solar radiation can be computed reasonably well using the Goody band model and the Curtis-Godson approximation.
    publisherAmerican Meteorological Society
    titleAtmospheric Solar Heating Rate in the Water Vapor Bands
    typeJournal Paper
    journal volume25
    journal issue11
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1986)025<1532:ASHRIT>2.0.CO;2
    journal fristpage1532
    journal lastpage1542
    treeJournal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 011
    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