Drift velocity of radiating quasigeostrophic vortices

Drift velocity of radiating quasigeostrophic vortices

Because of the beta effect, quasigeostrophic monopole vortices propagate westward and excite Rossby waves. This wave radiation depletes the vortex energy, and causes cyclones to drift northward and anticyclones southward. Explicit solutions describing such radiating vortices are found by perturbatio...

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Veröffentlicht in:Journal of physical oceanography 2001-01, Vol.31 (8), p.2178-2185
1. Verfasser: NYCANDER, J
Format: Artikel
Sprache:eng
Schlagworte:
Anticyclones
Dynamics of the ocean (upper and deep oceans)
Earth, ocean, space
Exact sciences and technology
External geophysics
Ocean currents
Oceanography
Oceans
Physics of the oceans
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container_title Journal of physical oceanography
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creator NYCANDER, J
description Because of the beta effect, quasigeostrophic monopole vortices propagate westward and excite Rossby waves. This wave radiation depletes the vortex energy, and causes cyclones to drift northward and anticyclones southward. Explicit solutions describing such radiating vortices are found by perturbation analysis.
doi_str_mv 10.1175/1520-0485(2001)031<2178:dvorqv>2.0.co;2
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source American Meteorological Society; EZB-FREE-00999 freely available EZB journals
subjects Anticyclones
Dynamics of the ocean (upper and deep oceans)
Earth, ocean, space
Exact sciences and technology
External geophysics
Ocean currents
Oceanography
Oceans
Physics of the oceans
title Drift velocity of radiating quasigeostrophic vortices
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