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contributor authorMoum, J. N.
contributor authorNash, J. D.
date accessioned2017-06-09T14:54:09Z
date available2017-06-09T14:54:09Z
date copyright2000/08/01
date issued2000
identifier issn0022-3670
identifier otherams-29298.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4166509
description abstractRecent turbulence measurements over a small bank on the continental shelf off Oregon reveal a previously undetected site for intense mixing of the coastal ocean. The flow is hydraulically controlled and turbulence diffusivities over the bank are more than 100 times greater than estimates made on the shelf away from topography. The total drag exerted by the bank on the flow field is a combination of bottom friction plus form drag (analogous to mountain drag) and is comparable to the Coriolis force. This drag is sufficient to decelerate the flow over the bank in a matter of hours.
publisherAmerican Meteorological Society
titleTopographically Induced Drag and Mixing at a Small Bank on the Continental Shelf
typeJournal Paper
journal volume30
journal issue8
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(2000)030<2049:TIDAMA>2.0.CO;2
journal fristpage2049
journal lastpage2054
treeJournal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 008
contenttypeFulltext


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