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    ON THE MERIDIONAL CIRCULATION AND RELEASE OF KINETIC ENERGY IN THE TROPICS

    Source: Journal of Meteorology:;1958:;volume( 015 ):;issue: 003::page 271
    Author:
    Palmén, E.
    ,
    Riehl, Herbert
    ,
    Vuorela, L. A.
    DOI: 10.1175/1520-0469(1958)015<0271:OTMCAR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The mean meridional circulation is computed for the northern hemisphere winter. The equatorward current in the low troposphere has a strength of l?3 mps near 10 to 15 deg lat, and the return current, centered near 200 mb, has about the same speed. An inactive layer without much net poleward or equatorward component extends from 700 to 400 mb. Next, the release of kinetic energy by the meridional circulation is calculated, and it is shown that this release equals the kinetic energy export from the tropics to the middle latitudes. Finally, the mean meridional circulation exports heat from the tropics poleward; at 15 deg lat this heat transport has the right order of magnitude to balance the net heat loss in higher latitudes.
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      ON THE MERIDIONAL CIRCULATION AND RELEASE OF KINETIC ENERGY IN THE TROPICS

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4150003
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    contributor authorPalmén, E.
    contributor authorRiehl, Herbert
    contributor authorVuorela, L. A.
    date accessioned2017-06-09T14:11:54Z
    date available2017-06-09T14:11:54Z
    date copyright1958/06/01
    date issued1958
    identifier issn0095-9634
    identifier otherams-14441.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150003
    description abstractThe mean meridional circulation is computed for the northern hemisphere winter. The equatorward current in the low troposphere has a strength of l?3 mps near 10 to 15 deg lat, and the return current, centered near 200 mb, has about the same speed. An inactive layer without much net poleward or equatorward component extends from 700 to 400 mb. Next, the release of kinetic energy by the meridional circulation is calculated, and it is shown that this release equals the kinetic energy export from the tropics to the middle latitudes. Finally, the mean meridional circulation exports heat from the tropics poleward; at 15 deg lat this heat transport has the right order of magnitude to balance the net heat loss in higher latitudes.
    publisherAmerican Meteorological Society
    titleON THE MERIDIONAL CIRCULATION AND RELEASE OF KINETIC ENERGY IN THE TROPICS
    typeJournal Paper
    journal volume15
    journal issue3
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1958)015<0271:OTMCAR>2.0.CO;2
    journal fristpage271
    journal lastpage277
    treeJournal of Meteorology:;1958:;volume( 015 ):;issue: 003
    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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