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    The Dynamics of Polar Jet Streams as Depicted by the METEOSAT WV Channel Radiance Field

    Source: Monthly Weather Review:;1981:;volume( 109 ):;issue: 010::page 2164
    Author:
    Ramond, D.
    ,
    Corbin, H.
    ,
    Des̄bois, M.
    ,
    Szejwach, G.
    ,
    Waldteufel, P.
    DOI: 10.1175/1520-0493(1981)109<2164:TDOPJS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A polar jet stream flowing over northern Europe is investigated using both the radiosounding network and the METEOSAT water vapor (WV) channel imagery. A maximum radiance band associated with the polar jet stream is shown to accurately delineate the tropopause break; a major difference in the subtropical jet stream radiative signature is noted, however. An analytic approximation of the radiative transfer equation is established for the METEOSAT WV channel and leads to the conclusion that the radiance field, away from the polar frontal zones, is representative of the temperature field on a water vapor isosteric surface.
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      The Dynamics of Polar Jet Streams as Depicted by the METEOSAT WV Channel Radiance Field

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4200586
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    • Monthly Weather Review

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    contributor authorRamond, D.
    contributor authorCorbin, H.
    contributor authorDes̄bois, M.
    contributor authorSzejwach, G.
    contributor authorWaldteufel, P.
    date accessioned2017-06-09T16:03:36Z
    date available2017-06-09T16:03:36Z
    date copyright1981/10/01
    date issued1981
    identifier issn0027-0644
    identifier otherams-59970.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4200586
    description abstractA polar jet stream flowing over northern Europe is investigated using both the radiosounding network and the METEOSAT water vapor (WV) channel imagery. A maximum radiance band associated with the polar jet stream is shown to accurately delineate the tropopause break; a major difference in the subtropical jet stream radiative signature is noted, however. An analytic approximation of the radiative transfer equation is established for the METEOSAT WV channel and leads to the conclusion that the radiance field, away from the polar frontal zones, is representative of the temperature field on a water vapor isosteric surface.
    publisherAmerican Meteorological Society
    titleThe Dynamics of Polar Jet Streams as Depicted by the METEOSAT WV Channel Radiance Field
    typeJournal Paper
    journal volume109
    journal issue10
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1981)109<2164:TDOPJS>2.0.CO;2
    journal fristpage2164
    journal lastpage2176
    treeMonthly Weather Review:;1981:;volume( 109 ):;issue: 010
    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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