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    On a Physical Mechanism for Rossby Wave Propagation

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 024::page 4020
    Author:
    Durran, Dale R.
    DOI: 10.1175/1520-0469(1988)045<4020:OAPMFR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A simple class of barotropic Rossby waves are shown to propagate westward as the graphically balanced meridional windfield periodically reverses in response to a small meridional pressure gradient arising from the latitudinal variation of the Coriolis parameter.
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      On a Physical Mechanism for Rossby Wave Propagation

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4156157
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    contributor authorDurran, Dale R.
    date accessioned2017-06-09T14:28:41Z
    date available2017-06-09T14:28:41Z
    date copyright1988/12/01
    date issued1988
    identifier issn0022-4928
    identifier otherams-19981.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4156157
    description abstractA simple class of barotropic Rossby waves are shown to propagate westward as the graphically balanced meridional windfield periodically reverses in response to a small meridional pressure gradient arising from the latitudinal variation of the Coriolis parameter.
    publisherAmerican Meteorological Society
    titleOn a Physical Mechanism for Rossby Wave Propagation
    typeJournal Paper
    journal volume45
    journal issue24
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1988)045<4020:OAPMFR>2.0.CO;2
    journal fristpage4020
    journal lastpage4022
    treeJournal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 024
    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
    yabeshDSpacePersian