Vortex Generation Through Balanced AdjustmentSource: Journal of Physical Oceanography:;1988:;Volume( 018 ):;issue: 008::page 1178Author:McWilliams, James C.
DOI: 10.1175/1520-0485(1988)018<1178:VGTBA>2.0.CO;2Publisher: American Meteorological Society
Abstract: The problem of geostrophic adjustment, originally considered by C.G. Rossby, is solved in an axisymmetric geometry for a continuously stratified fluid, where the adjusted final state is in hydrostatic, gradient-wind balance. This problem is relevant to the generation of submesoscale coherent vortices in the ocean: diapycnal mixing events can create a local anomaly of less strongly stratified fluid, which then develops a balancing circulation through adjustment. An analytical solution is obtained for a few uniform-density layers, and this is compared with numerical solutions for continuous stratification. In both representations, two-dimensional solutions are compared with axisymmetric ones.
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contributor author | McWilliams, James C. | |
date accessioned | 2017-06-09T14:48:57Z | |
date available | 2017-06-09T14:48:57Z | |
date copyright | 1988/08/01 | |
date issued | 1988 | |
identifier issn | 0022-3670 | |
identifier other | ams-27397.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4164397 | |
description abstract | The problem of geostrophic adjustment, originally considered by C.G. Rossby, is solved in an axisymmetric geometry for a continuously stratified fluid, where the adjusted final state is in hydrostatic, gradient-wind balance. This problem is relevant to the generation of submesoscale coherent vortices in the ocean: diapycnal mixing events can create a local anomaly of less strongly stratified fluid, which then develops a balancing circulation through adjustment. An analytical solution is obtained for a few uniform-density layers, and this is compared with numerical solutions for continuous stratification. In both representations, two-dimensional solutions are compared with axisymmetric ones. | |
publisher | American Meteorological Society | |
title | Vortex Generation Through Balanced Adjustment | |
type | Journal Paper | |
journal volume | 18 | |
journal issue | 8 | |
journal title | Journal of Physical Oceanography | |
identifier doi | 10.1175/1520-0485(1988)018<1178:VGTBA>2.0.CO;2 | |
journal fristpage | 1178 | |
journal lastpage | 1192 | |
tree | Journal of Physical Oceanography:;1988:;Volume( 018 ):;issue: 008 | |
contenttype | Fulltext |