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    Parcel Stability and its Relation to Semigeostrophic Theory

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 009::page 1318
    Author:
    Shutts, G. J.
    ,
    Cullen, M. J. P.
    DOI: 10.1175/1520-0469(1987)044<1318:PSAIRT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The classical concept of hydrodynamic stability is reviewed in the light of recent developments in semigeostrophic theory. A certain Jacobian matrix is required to be positive-definite if solution of the semigeostrophic equations is to be well posed. formally, this gives three conditions which must be satisfied, one of which corresponds to the positivity of the semigeostrophic potential vorticity defined as the determinant of the matrix. The full implications of these stability criteria are sought here, together with some simple expression of the positive-definite requirement. The existence of a minimum energy principle, with respect to virtual parcel displacements which conserve absolute momentum and potential temperature is shown to play a key role, as in the equivalent circular vortex problem studied by Fjörtoft. It also appears to provide the basis for extending semigeostrophic theory to the general geophysical situation in which the gravitation vector and axis of rotation are not colinear.
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      Parcel Stability and its Relation to Semigeostrophic Theory

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4155661
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    contributor authorShutts, G. J.
    contributor authorCullen, M. J. P.
    date accessioned2017-06-09T14:27:17Z
    date available2017-06-09T14:27:17Z
    date copyright1987/05/01
    date issued1987
    identifier issn0022-4928
    identifier otherams-19534.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155661
    description abstractThe classical concept of hydrodynamic stability is reviewed in the light of recent developments in semigeostrophic theory. A certain Jacobian matrix is required to be positive-definite if solution of the semigeostrophic equations is to be well posed. formally, this gives three conditions which must be satisfied, one of which corresponds to the positivity of the semigeostrophic potential vorticity defined as the determinant of the matrix. The full implications of these stability criteria are sought here, together with some simple expression of the positive-definite requirement. The existence of a minimum energy principle, with respect to virtual parcel displacements which conserve absolute momentum and potential temperature is shown to play a key role, as in the equivalent circular vortex problem studied by Fjörtoft. It also appears to provide the basis for extending semigeostrophic theory to the general geophysical situation in which the gravitation vector and axis of rotation are not colinear.
    publisherAmerican Meteorological Society
    titleParcel Stability and its Relation to Semigeostrophic Theory
    typeJournal Paper
    journal volume44
    journal issue9
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1987)044<1318:PSAIRT>2.0.CO;2
    journal fristpage1318
    journal lastpage1330
    treeJournal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 009
    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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