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    ABSORPTION OF ATMOSPHERIC RADIATION BY WATER FILMS AND WATER CLOUDS

    Source: Journal of Meteorology:;1960:;volume( 017 ):;issue: 002::page 232
    Author:
    McDonald, James E.
    DOI: 10.1175/1520-0469(1960)017<0232:AOARBW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Spectrally averaged infrared absorptivities of thin water films are computed using recent spectrometric results. A water film 5 µ thick irradiated at normal incidence with 0C blackbody radiation is found to have a total absorptivity of 0.49, while, for thicknesses of 10, 50, and 100 µ, the absorptivities are 0.67, 0.92, and 0.95, respectively. Spectrally averaged reflectivity at normal incidence for bulk water is 0.04. Change in the shape of the blackbody emission curve with a change in temperature from 0C to 40C produces negligibly small effect on the spectrally averaged absorptivity and reflectivity. A simple bulk-water method yields infrared cloud absorption half-depths of 17 m for 0.25 g m?3 (and 5 m for 1 g m?3) liquid water content. Only 0.5 per cent is transmitted deeper than 400 m for 0.25 g m?3 or deeper than 100 m for 1 g m?3. Evidence for concluding that Mie-theory effects will tend to reduce these absorption depths to still lower values is presented.
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      ABSORPTION OF ATMOSPHERIC RADIATION BY WATER FILMS AND WATER CLOUDS

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4150197
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    contributor authorMcDonald, James E.
    date accessioned2017-06-09T14:12:19Z
    date available2017-06-09T14:12:19Z
    date copyright1960/04/01
    date issued1960
    identifier issn0095-9634
    identifier otherams-14616.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150197
    description abstractSpectrally averaged infrared absorptivities of thin water films are computed using recent spectrometric results. A water film 5 µ thick irradiated at normal incidence with 0C blackbody radiation is found to have a total absorptivity of 0.49, while, for thicknesses of 10, 50, and 100 µ, the absorptivities are 0.67, 0.92, and 0.95, respectively. Spectrally averaged reflectivity at normal incidence for bulk water is 0.04. Change in the shape of the blackbody emission curve with a change in temperature from 0C to 40C produces negligibly small effect on the spectrally averaged absorptivity and reflectivity. A simple bulk-water method yields infrared cloud absorption half-depths of 17 m for 0.25 g m?3 (and 5 m for 1 g m?3) liquid water content. Only 0.5 per cent is transmitted deeper than 400 m for 0.25 g m?3 or deeper than 100 m for 1 g m?3. Evidence for concluding that Mie-theory effects will tend to reduce these absorption depths to still lower values is presented.
    publisherAmerican Meteorological Society
    titleABSORPTION OF ATMOSPHERIC RADIATION BY WATER FILMS AND WATER CLOUDS
    typeJournal Paper
    journal volume17
    journal issue2
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1960)017<0232:AOARBW>2.0.CO;2
    journal fristpage232
    journal lastpage238
    treeJournal of Meteorology:;1960:;volume( 017 ):;issue: 002
    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