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contributor authorJohnson, J. A.
contributor authorKillworth, P. D.
date accessioned2017-06-09T14:44:03Z
date available2017-06-09T14:44:03Z
date copyright1975/01/01
date issued1975
identifier issn0022-3670
identifier otherams-25497.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162286
description abstractThe theory of Hill and Johnson for upwelling over the shelf break is modified to give agreement with the work of Killworth. It is shown that when upwelling occurs over a discontinuity in bottom slope, this upwelling does not penetrate into the surface Ekman layer. Associated with this upwelling is a strong current along the shelf break in the bottom Ekman layer.
publisherAmerican Meteorological Society
titleA Bottom Current Along the Shelf Break
typeJournal Paper
journal volume5
journal issue1
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1975)005<0185:ABCATS>2.0.CO;2
journal fristpage185
journal lastpage188
treeJournal of Physical Oceanography:;1975:;Volume( 005 ):;issue: 001
contenttypeFulltext


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