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    Low-Resolution Numerical Simulation of Decaying Two-Dimensional Turbulence

    Source: Journal of the Atmospheric Sciences:;1983:;Volume( 040 ):;issue: 003::page 738
    Author:
    Bennett, Andrew F.
    ,
    Haidvogel, Dale B.
    DOI: 10.1175/1520-0469(1983)040<0738:LRNSOD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Numerical simulations of two-dimensional turbulence show that O(??1) and O(??4) energy spectra?described by Fox and Orszag (1973a) as enstrophy-equipartitioning and strongly dissipating turbulence, respectively?occur independently of the type of dissipation mechanism, and the inclusion of forcing and the ?-effect. In both states the modal decorrelation rate ? depends strongly upon wavenumber in accordance with the equations of a direct interaction approximation (Kraichnan, 1958), but in conflict with the hypothetical wavenumber independence of ? in an enstrophy-caseading inertial similarity range. Implications for geophysical fluid dynamical modeling are discussed.
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      Low-Resolution Numerical Simulation of Decaying Two-Dimensional Turbulence

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4154553
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    contributor authorBennett, Andrew F.
    contributor authorHaidvogel, Dale B.
    date accessioned2017-06-09T14:23:46Z
    date available2017-06-09T14:23:46Z
    date copyright1983/03/01
    date issued1983
    identifier issn0022-4928
    identifier otherams-18537.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154553
    description abstractNumerical simulations of two-dimensional turbulence show that O(??1) and O(??4) energy spectra?described by Fox and Orszag (1973a) as enstrophy-equipartitioning and strongly dissipating turbulence, respectively?occur independently of the type of dissipation mechanism, and the inclusion of forcing and the ?-effect. In both states the modal decorrelation rate ? depends strongly upon wavenumber in accordance with the equations of a direct interaction approximation (Kraichnan, 1958), but in conflict with the hypothetical wavenumber independence of ? in an enstrophy-caseading inertial similarity range. Implications for geophysical fluid dynamical modeling are discussed.
    publisherAmerican Meteorological Society
    titleLow-Resolution Numerical Simulation of Decaying Two-Dimensional Turbulence
    typeJournal Paper
    journal volume40
    journal issue3
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1983)040<0738:LRNSOD>2.0.CO;2
    journal fristpage738
    journal lastpage748
    treeJournal of the Atmospheric Sciences:;1983:;Volume( 040 ):;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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