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    Nonlinear Saturation of Baroclinic Instability. Part III: Bounds on the Energy

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 016::page 2697
    Author:
    Shepherd, Theodore G.
    DOI: 10.1175/1520-0469(1993)050<2697:NSOBIP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Rigorous upper bounds are derived on the saturation amplitude of baroclinic instability in the two-layer model. The bounds apply to the eddy energy and are obtained by appealing to a finite amplitude conservation law for the disturbance pseudoenergy. These bounds are to be distinguished from those derived in Part I of this study, which employed a pseudomomentum conservation law and provided bounds on the eddy potential enstrophy. The bounds apply to conservative (inviscid, unforced) flow, as well as to forced-dissipative flow when the dissipation is proportional to the potential vorticity. Bounds on the eddy energy are worked out for a general class of unstable westerly jets. In the special case of the Phillips model of baroclinic instability, and in the limit of infinitesimal initial eddy amplitude, the bound states that the eddy energy cannot exceed ??2/6F where ? = (U ? Ucrit)/Ucrit is the relative supercriticality. This bound captures the essential dynamical scalings (i.e., the dependence on ?, ?, and F) of the saturation amplitudes predicted by weakly nonlinear theory, as well as exhibiting remarkable quantitative agreement with those predictions, and is also consistent with heuristic baroclinic adjustment estimates.
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      Nonlinear Saturation of Baroclinic Instability. Part III: Bounds on the Energy

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4157295
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    contributor authorShepherd, Theodore G.
    date accessioned2017-06-09T14:31:43Z
    date available2017-06-09T14:31:43Z
    date copyright1993/08/01
    date issued1993
    identifier issn0022-4928
    identifier otherams-21003.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157295
    description abstractRigorous upper bounds are derived on the saturation amplitude of baroclinic instability in the two-layer model. The bounds apply to the eddy energy and are obtained by appealing to a finite amplitude conservation law for the disturbance pseudoenergy. These bounds are to be distinguished from those derived in Part I of this study, which employed a pseudomomentum conservation law and provided bounds on the eddy potential enstrophy. The bounds apply to conservative (inviscid, unforced) flow, as well as to forced-dissipative flow when the dissipation is proportional to the potential vorticity. Bounds on the eddy energy are worked out for a general class of unstable westerly jets. In the special case of the Phillips model of baroclinic instability, and in the limit of infinitesimal initial eddy amplitude, the bound states that the eddy energy cannot exceed ??2/6F where ? = (U ? Ucrit)/Ucrit is the relative supercriticality. This bound captures the essential dynamical scalings (i.e., the dependence on ?, ?, and F) of the saturation amplitudes predicted by weakly nonlinear theory, as well as exhibiting remarkable quantitative agreement with those predictions, and is also consistent with heuristic baroclinic adjustment estimates.
    publisherAmerican Meteorological Society
    titleNonlinear Saturation of Baroclinic Instability. Part III: Bounds on the Energy
    typeJournal Paper
    journal volume50
    journal issue16
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1993)050<2697:NSOBIP>2.0.CO;2
    journal fristpage2697
    journal lastpage2709
    treeJournal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 016
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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