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    On Spectral Analysis of Mesoscale Eddies. Part II: Nonlinear Analysis

    Source: Journal of Physical Oceanography:;2013:;Volume( 043 ):;issue: 012::page 2528
    Author:
    Berloff, P.
    ,
    Kamenkovich, I.
    DOI: 10.1175/JPO-D-12-0233.1
    Publisher: American Meteorological Society
    Abstract: everal turbulent flow regimes of an idealized ocean circulation model are systematically analyzed in physical and spectral domains. Zonal dispersion properties of transient mesoscale eddies are described by the zonal wavenumber/temporal frequency spectra. The eddy patterns and the corresponding nonlinear eddy forcing exerted on the jets are examined by filtering different parts of the spectra. Comparison of the outcome of this nonlinear analysis with the properties of the linearized solutions (obtained in Part I of this paper) demonstrates that a very substantial part of the flow dynamics is controlled by the underlying linear dynamics. This result supports the hypothesis that it is possible to describe most of the oceanic mesoscale eddies as a wave turbulence phenomenon.
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      On Spectral Analysis of Mesoscale Eddies. Part II: Nonlinear Analysis

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    contributor authorBerloff, P.
    contributor authorKamenkovich, I.
    date accessioned2017-06-09T17:19:48Z
    date available2017-06-09T17:19:48Z
    date copyright2013/12/01
    date issued2013
    identifier issn0022-3670
    identifier otherams-83286.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4226494
    description abstracteveral turbulent flow regimes of an idealized ocean circulation model are systematically analyzed in physical and spectral domains. Zonal dispersion properties of transient mesoscale eddies are described by the zonal wavenumber/temporal frequency spectra. The eddy patterns and the corresponding nonlinear eddy forcing exerted on the jets are examined by filtering different parts of the spectra. Comparison of the outcome of this nonlinear analysis with the properties of the linearized solutions (obtained in Part I of this paper) demonstrates that a very substantial part of the flow dynamics is controlled by the underlying linear dynamics. This result supports the hypothesis that it is possible to describe most of the oceanic mesoscale eddies as a wave turbulence phenomenon.
    publisherAmerican Meteorological Society
    titleOn Spectral Analysis of Mesoscale Eddies. Part II: Nonlinear Analysis
    typeJournal Paper
    journal volume43
    journal issue12
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/JPO-D-12-0233.1
    journal fristpage2528
    journal lastpage2544
    treeJournal of Physical Oceanography:;2013:;Volume( 043 ):;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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