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    A Stratospheric Fountain?

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 012::page 2789
    Author:
    Newell, Reginald E.
    ,
    Gould-Stewart, Sharon
    DOI: 10.1175/1520-0469(1981)038<2789:ASF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A ?stratospheric fountain?, or area where air enters the stratosphere from the troposphere, is postulated based on an analysis of global 100 mb monthly mean temperatures. The temperature threshold is calculated from the observed global stratospheric water mixing ratio and fulfills the requirement of preserving low stratospheric humidity. The fountain occurs over the western tropical Pacific, northern Australia, Indonesia, and Malaysia in the November?March period and over the Bay of Bengal and India during the Monsoon. It is suggested that the major portion of the stratospheric air supply enters through these areas with most of the exchange occurring in the November?March period. Methods are proposed for substantiating the existence of the stratospheric fountain.
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      A Stratospheric Fountain?

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4154250
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    • Journal of the Atmospheric Sciences

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    contributor authorNewell, Reginald E.
    contributor authorGould-Stewart, Sharon
    date accessioned2017-06-09T14:22:45Z
    date available2017-06-09T14:22:45Z
    date copyright1981/12/01
    date issued1981
    identifier issn0022-4928
    identifier otherams-18264.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154250
    description abstractA ?stratospheric fountain?, or area where air enters the stratosphere from the troposphere, is postulated based on an analysis of global 100 mb monthly mean temperatures. The temperature threshold is calculated from the observed global stratospheric water mixing ratio and fulfills the requirement of preserving low stratospheric humidity. The fountain occurs over the western tropical Pacific, northern Australia, Indonesia, and Malaysia in the November?March period and over the Bay of Bengal and India during the Monsoon. It is suggested that the major portion of the stratospheric air supply enters through these areas with most of the exchange occurring in the November?March period. Methods are proposed for substantiating the existence of the stratospheric fountain.
    publisherAmerican Meteorological Society
    titleA Stratospheric Fountain?
    typeJournal Paper
    journal volume38
    journal issue12
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1981)038<2789:ASF>2.0.CO;2
    journal fristpage2789
    journal lastpage2796
    treeJournal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 012
    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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