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contributor authorPoulin, F. J.
contributor authorFlierl, G. R.
date accessioned2017-06-09T17:17:44Z
date available2017-06-09T17:17:44Z
date copyright2005/05/01
date issued2005
identifier issn0022-3670
identifier otherams-82597.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4225728
description abstractIn this article, the effect shelflike topography has on the stability of a jet that flows along the smooth shelf is addressed. The linear stability problem is solved to determine for which nondimensional parameters a shelf can either destabilize or stabilize a jet. These calculations reveal an intricate dependence of growth rate on topography. In particular, the authors determine that retrograde topography (with the shallow water on the left) always stabilizes the jet (in relation to the flat-bottom equivalent), whereas prograde topography (with the shallow water on the right) can either stabilize or destabilize the jet depending on the particular values of the Rossby number and topographic parameters. For Rossby numbers of order 1 and larger, prograde topography is strictly stabilizing. For small Rossby numbers, small-amplitude topography destabilizes whereas large topography stabilizes. The nonlinear evolution of these instabilities is explored to confirm the predictions from the linear theory and, also, to illustrate how stabilization is directly related to fluid transport across the shelf.
publisherAmerican Meteorological Society
titleThe Influence of Topography on the Stability of Jets
typeJournal Paper
journal volume35
journal issue5
journal titleJournal of Physical Oceanography
identifier doi10.1175/JPO2719.1
journal fristpage811
journal lastpage825
treeJournal of Physical Oceanography:;2005:;Volume( 035 ):;issue: 005
contenttypeFulltext


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