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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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