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    Nonlinear Wave-Activity Conservation Laws and Hamiltonian Structure for the Two-Dimensional Anelastic Equations

    Source: Journal of the Atmospheric Sciences:;1992:;Volume( 049 ):;issue: 001::page 5
    Author:
    Scinocca, J. F.
    ,
    Shepherd, T. G.
    DOI: 10.1175/1520-0469(1992)049<0005:NWACLA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Exact, finite-amplitude, local wave-activity conservation laws are derived for disturbances to steady flows in the context of the two-dimensional anelastic equations. The conservation laws are expressed entirely in terms of Eulerian quantities, and have the property that, in the limit of a small-amplitude, slowly varying, monochromatic wave train, the wave-activity density A and flux F, when averaged over phase, satisfy F = cgA where cg is the group velocity of the waves. For nonparallel steady flows, the only conserved wave activity is a form of disturbance pseudoenergy; when the steady flow is parallel, there is in addition a conservation law for the disturbance pseudomomentum. The above results are obtained not only for isentropic background states (which give the so-called ?deep form? of the anelastic equations), but also for arbitrary background potential-temperature profiles ?0(z) so long as the variation in ?0(z) over the depth of the fluid is small compared with ?0 itself. The Hamiltonian structure of the equations is established in both cases, and its symmetry properties discussed. An expression for available potential energy is also derived that, for the case of a stably stratified background state (i.e., d?0/dz > 0), is locally positive definite; the expression is valid for fully three-dimensional flow. The counterparts to results for the two-dimensional Boussinesq equations are also noted.
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      Nonlinear Wave-Activity Conservation Laws and Hamiltonian Structure for the Two-Dimensional Anelastic Equations

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4156888
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    contributor authorScinocca, J. F.
    contributor authorShepherd, T. G.
    date accessioned2017-06-09T14:30:39Z
    date available2017-06-09T14:30:39Z
    date copyright1992/01/01
    date issued1992
    identifier issn0022-4928
    identifier otherams-20638.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4156888
    description abstractExact, finite-amplitude, local wave-activity conservation laws are derived for disturbances to steady flows in the context of the two-dimensional anelastic equations. The conservation laws are expressed entirely in terms of Eulerian quantities, and have the property that, in the limit of a small-amplitude, slowly varying, monochromatic wave train, the wave-activity density A and flux F, when averaged over phase, satisfy F = cgA where cg is the group velocity of the waves. For nonparallel steady flows, the only conserved wave activity is a form of disturbance pseudoenergy; when the steady flow is parallel, there is in addition a conservation law for the disturbance pseudomomentum. The above results are obtained not only for isentropic background states (which give the so-called ?deep form? of the anelastic equations), but also for arbitrary background potential-temperature profiles ?0(z) so long as the variation in ?0(z) over the depth of the fluid is small compared with ?0 itself. The Hamiltonian structure of the equations is established in both cases, and its symmetry properties discussed. An expression for available potential energy is also derived that, for the case of a stably stratified background state (i.e., d?0/dz > 0), is locally positive definite; the expression is valid for fully three-dimensional flow. The counterparts to results for the two-dimensional Boussinesq equations are also noted.
    publisherAmerican Meteorological Society
    titleNonlinear Wave-Activity Conservation Laws and Hamiltonian Structure for the Two-Dimensional Anelastic Equations
    typeJournal Paper
    journal volume49
    journal issue1
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1992)049<0005:NWACLA>2.0.CO;2
    journal fristpage5
    journal lastpage28
    treeJournal of the Atmospheric Sciences:;1992:;Volume( 049 ):;issue: 001
    contenttypeFulltext
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