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contributor authorMahadevan, Amala
contributor authorOliger, Joseph
contributor authorStreet, Robert
date accessioned2017-06-09T14:52:14Z
date available2017-06-09T14:52:14Z
date copyright1996/09/01
date issued1996
identifier issn0022-3670
identifier otherams-28583.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4165715
description abstractThe nonhydrostatic model with a free surface is numerically implemented in boundary-fitted curvilinear coordinates to model the mesoscale circulation in an ocean basin with natural topography. A semi-implicit numerical scheme is used, and the directional inhomogeneity in the elliptic equation for pressure is exploited to speed up the computation of its solution while using the multigrid method. The model is used to simulate the circulation in the Gulf of Mexico. We observe the formation of the Loop Current and several eddies. The flow is very strongly controlled by the topography and our numerical experiments reveal that in the bottom layers, the flow along topographic contours is in the opposite direction of the anticyclonic circulation in the top layers.
publisherAmerican Meteorological Society
titleA Nonhydrostatic Mesoscale Ocean Model. Part II: Numerical Implementation
typeJournal Paper
journal volume26
journal issue9
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1996)026<1881:ANMOMP>2.0.CO;2
journal fristpage1881
journal lastpage1900
treeJournal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 009
contenttypeFulltext


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