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    Ertel's Potential Vorticity in Unstratified Turbulence

    Source: Journal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 001::page 35
    Author:
    Herring, J. R.
    ,
    Kerr, R. M.
    ,
    Rotunno, R.
    DOI: 10.1175/1520-0469(1994)051<0035:EPVIUT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The evolution of Ertel's potential vorticity (PV) is examined in direct numerical simulations (DNS) of decaying turbulence advecting passive scalars and in a generalized Taylor-Green vortex (TGV). It is noted that although PV itself is advected as a passive scalar, its dissipation occurs over all scales and is not concentrated in the velocity or scalar dissipations range. Thus, attempts to invoke cascade arguments to infer an inertial range for PV variance are vitiated. Moreover, for the TGV it is noted that molecular dissipation can create PV from an initial state for which it is everywhere zero. For the random initial value problem, the DNS results suggest a simple characterization of PV dissipation, which implies that for isotropic turbulence (and small Prandtl numbers) PV decays roughly exponentially on a lime scale ? (L/Urms)R?½, L being the integral scale, urms the large rms velocity, and Rrms, the microscale Reynolds number. The statistics of PV are also examined, and it is noted that it is far from Gaussian, even at modest values of Reynolds number R?.
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      Ertel's Potential Vorticity in Unstratified Turbulence

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4157400
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    • Journal of the Atmospheric Sciences

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    contributor authorHerring, J. R.
    contributor authorKerr, R. M.
    contributor authorRotunno, R.
    date accessioned2017-06-09T14:31:59Z
    date available2017-06-09T14:31:59Z
    date copyright1994/01/01
    date issued1994
    identifier issn0022-4928
    identifier otherams-21099.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157400
    description abstractThe evolution of Ertel's potential vorticity (PV) is examined in direct numerical simulations (DNS) of decaying turbulence advecting passive scalars and in a generalized Taylor-Green vortex (TGV). It is noted that although PV itself is advected as a passive scalar, its dissipation occurs over all scales and is not concentrated in the velocity or scalar dissipations range. Thus, attempts to invoke cascade arguments to infer an inertial range for PV variance are vitiated. Moreover, for the TGV it is noted that molecular dissipation can create PV from an initial state for which it is everywhere zero. For the random initial value problem, the DNS results suggest a simple characterization of PV dissipation, which implies that for isotropic turbulence (and small Prandtl numbers) PV decays roughly exponentially on a lime scale ? (L/Urms)R?½, L being the integral scale, urms the large rms velocity, and Rrms, the microscale Reynolds number. The statistics of PV are also examined, and it is noted that it is far from Gaussian, even at modest values of Reynolds number R?.
    publisherAmerican Meteorological Society
    titleErtel's Potential Vorticity in Unstratified Turbulence
    typeJournal Paper
    journal volume51
    journal issue1
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1994)051<0035:EPVIUT>2.0.CO;2
    journal fristpage35
    journal lastpage47
    treeJournal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 001
    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