Nonlinear Wave-Activity Conservation Laws and Hamiltonian Structure for the Two-Dimensional Anelastic EquationsSource: Journal of the Atmospheric Sciences:;1992:;Volume( 049 ):;issue: 001::page 5DOI: 10.1175/1520-0469(1992)049<0005:NWACLA>2.0.CO;2Publisher: 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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| contributor author | Scinocca, J. F. | |
| contributor author | Shepherd, T. G. | |
| date accessioned | 2017-06-09T14:30:39Z | |
| date available | 2017-06-09T14:30:39Z | |
| date copyright | 1992/01/01 | |
| date issued | 1992 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-20638.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4156888 | |
| description 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. | |
| publisher | American Meteorological Society | |
| title | Nonlinear Wave-Activity Conservation Laws and Hamiltonian Structure for the Two-Dimensional Anelastic Equations | |
| type | Journal Paper | |
| journal volume | 49 | |
| journal issue | 1 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1992)049<0005:NWACLA>2.0.CO;2 | |
| journal fristpage | 5 | |
| journal lastpage | 28 | |
| tree | Journal of the Atmospheric Sciences:;1992:;Volume( 049 ):;issue: 001 | |
| contenttype | Fulltext |