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    Quantitative Studies of Meteosat Water-Vapor Channel Data

    Source: Journal of Applied Meteorology:;1979:;volume( 019 ):;issue: 007::page 868
    Author:
    Poc, M. M.
    ,
    Roulleau, M.
    ,
    Scott, N. A.
    ,
    Chedin, A.
    DOI: 10.1175/1520-0450(1980)019<0868:QSOMWV>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In this paper, quantitative studies of water vapor Meteosat imagery, based on an accurate transmittance and radiance model are described. Using conventional radiosonde data, a linear relation between cloudless radiances and digital counts is obtained. It is shown that the distribution with altitude of the peak contribution to the radiances varies from about the 550 mb level to about the 450 mb level for pictures acquired in July over the western part of Europe and Mediterranean Sea. The influence of the temperature profile on the altitude of the maximum contribution layer is pointed out. A relation between the radiative field and the water vapor mass above the 600 mb level is found.
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      Quantitative Studies of Meteosat Water-Vapor Channel Data

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4233484
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    • Journal of Applied Meteorology

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    contributor authorPoc, M. M.
    contributor authorRoulleau, M.
    contributor authorScott, N. A.
    contributor authorChedin, A.
    date accessioned2017-06-09T17:40:34Z
    date available2017-06-09T17:40:34Z
    date copyright1980/07/01
    date issued1979
    identifier issn0021-8952
    identifier otherams-9940.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4233484
    description abstractIn this paper, quantitative studies of water vapor Meteosat imagery, based on an accurate transmittance and radiance model are described. Using conventional radiosonde data, a linear relation between cloudless radiances and digital counts is obtained. It is shown that the distribution with altitude of the peak contribution to the radiances varies from about the 550 mb level to about the 450 mb level for pictures acquired in July over the western part of Europe and Mediterranean Sea. The influence of the temperature profile on the altitude of the maximum contribution layer is pointed out. A relation between the radiative field and the water vapor mass above the 600 mb level is found.
    publisherAmerican Meteorological Society
    titleQuantitative Studies of Meteosat Water-Vapor Channel Data
    typeJournal Paper
    journal volume19
    journal issue7
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1980)019<0868:QSOMWV>2.0.CO;2
    journal fristpage868
    journal lastpage876
    treeJournal of Applied Meteorology:;1979:;volume( 019 ):;issue: 007
    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
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