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contributor authorChapman, David C.
date accessioned2017-06-09T14:47:08Z
date available2017-06-09T14:47:08Z
date copyright1984/07/01
date issued1984
identifier issn0022-3670
identifier otherams-26719.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163644
description abstractA simple two-layer, step-shelf model is used to demonstrate that barotropic (surface) edge waves of substantial amplitude can, in principle, be generated by deep-sea internal waves incident upon the coastal topography. Some qualitative features of the results suggest that this mechanism could amount for the edge-wave ?noise? observed by Munk and others.
publisherAmerican Meteorological Society
titleThe Generation of Barotropic Edge Waves by Deep-Sea Internal Waves
typeJournal Paper
journal volume14
journal issue7
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1984)014<1152:TGOBEW>2.0.CO;2
journal fristpage1152
journal lastpage1158
treeJournal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 007
contenttypeFulltext


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