On stationary baroclinic planetary dipole-vortices in a continuously- stratified fluid of finite depth

DOI10.1007/BF00991901zbMath0809.76014OpenAlexW2149209137MaRDI QIDQ1338721

Gordon E. Swaters

Publication date: 7 December 1994

Published in: ZAMP. Zeitschrift für angewandte Mathematik und Physik (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1007/bf00991901

zbMATH Keywords

exact solutionbeta-planevertical normal-mode decomposition

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Vortex flows for incompressible inviscid fluids (76B47) Reaction effects in flows (76V05)

Cites Work

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• Hamiltonian formulation of the baroclinic quasigeostrophic fluid equations
• A nonlinear stability theorem for baroclinic quasigeostrophic flow
• An exact local conservation theorem for finite-amplitude disturbances to non-parallel shear flows, with remarks on Hamiltonian structure and on Arnol'd's stability theorems
• Inertial Taylor columns on a beta plane
• A three-dimensional model of inertial currents in a variable-density ocean
• Dynamics of ventilated coherent cold eddies on a sloping bottom

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