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    On the Energy Conversion during Geostrophic Adjustment

    Source: Journal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 012::page 2203
    Author:
    Ou, Hsien Wang
    DOI: 10.1175/1520-0485(1986)016<2203:OTECDG>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: It is found that for a continuously stratified fluid which remains so during the geostrophic adjustment, the energy conversion ratio ? (≡?KE/?PE) is ½, in contrast to the value of ? for a two-layer fluid. Since the two-layer fluid is an asymptotic limit of a continuously stratified fluid, it is deduced that ? decreases smoothly from ½ to ? when density discontinuities are formed during the adjustment. Furthermore, the total energy released during the adjustment is found to be inversely proportional to the dimensionless horizontal scale (scaled by the baroclinic radius of deformation) characterizing the density variation in the initial state.
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      On the Energy Conversion during Geostrophic Adjustment

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    contributor authorOu, Hsien Wang
    date accessioned2017-06-09T14:48:13Z
    date available2017-06-09T14:48:13Z
    date copyright1986/12/01
    date issued1986
    identifier issn0022-3670
    identifier otherams-27116.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164086
    description abstractIt is found that for a continuously stratified fluid which remains so during the geostrophic adjustment, the energy conversion ratio ? (≡?KE/?PE) is ½, in contrast to the value of ? for a two-layer fluid. Since the two-layer fluid is an asymptotic limit of a continuously stratified fluid, it is deduced that ? decreases smoothly from ½ to ? when density discontinuities are formed during the adjustment. Furthermore, the total energy released during the adjustment is found to be inversely proportional to the dimensionless horizontal scale (scaled by the baroclinic radius of deformation) characterizing the density variation in the initial state.
    publisherAmerican Meteorological Society
    titleOn the Energy Conversion during Geostrophic Adjustment
    typeJournal Paper
    journal volume16
    journal issue12
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1986)016<2203:OTECDG>2.0.CO;2
    journal fristpage2203
    journal lastpage2204
    treeJournal of Physical Oceanography:;1986:;Volume( 016 ):;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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