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    Water Budget of a Mesoscale Convective System in the Tropics

    Source: Journal of the Atmospheric Sciences:;1983:;Volume( 040 ):;issue: 007::page 1835
    Author:
    Gamache, John F.
    ,
    Houze, Robert A.
    DOI: 10.1175/1520-0469(1983)040<1835:WBOAMC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A squall-line cloud cluster observed in the Global Atmospheric Research Program's Atlantic Tropical Experiment (GATE) is studied as an example of a mesoscale convective system in the tropics. The system is divided into convective and stratiform regions. Composite wind, vertical motion, humidity, radar and satellite data fields have been derived for the system and are used to calculate the components of the water budgets of each region. Particular attention is devoted to understanding the sources of condensate for the stratiform region. The mesoscale updraft in the stratiform cloud accounts for 25?40% of the condensate making up the stratiform cloud, while the remaining 60?75% is supplied by horizontal transfer to the stratiform region of condensate generated in the cumulonimbus towers of the convective region.
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      Water Budget of a Mesoscale Convective System in the Tropics

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4154644
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    • Journal of the Atmospheric Sciences

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    contributor authorGamache, John F.
    contributor authorHouze, Robert A.
    date accessioned2017-06-09T14:24:03Z
    date available2017-06-09T14:24:03Z
    date copyright1983/07/01
    date issued1983
    identifier issn0022-4928
    identifier otherams-18619.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154644
    description abstractA squall-line cloud cluster observed in the Global Atmospheric Research Program's Atlantic Tropical Experiment (GATE) is studied as an example of a mesoscale convective system in the tropics. The system is divided into convective and stratiform regions. Composite wind, vertical motion, humidity, radar and satellite data fields have been derived for the system and are used to calculate the components of the water budgets of each region. Particular attention is devoted to understanding the sources of condensate for the stratiform region. The mesoscale updraft in the stratiform cloud accounts for 25?40% of the condensate making up the stratiform cloud, while the remaining 60?75% is supplied by horizontal transfer to the stratiform region of condensate generated in the cumulonimbus towers of the convective region.
    publisherAmerican Meteorological Society
    titleWater Budget of a Mesoscale Convective System in the Tropics
    typeJournal Paper
    journal volume40
    journal issue7
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1983)040<1835:WBOAMC>2.0.CO;2
    journal fristpage1835
    journal lastpage1850
    treeJournal of the Atmospheric Sciences:;1983:;Volume( 040 ):;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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