The Generation of Barotropic Edge Waves by Deep-Sea Internal WavesSource: Journal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 007::page 1152Author:Chapman, David C.
DOI: 10.1175/1520-0485(1984)014<1152:TGOBEW>2.0.CO;2Publisher: American Meteorological Society
Abstract: A 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.
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| contributor author | Chapman, David C. | |
| date accessioned | 2017-06-09T14:47:08Z | |
| date available | 2017-06-09T14:47:08Z | |
| date copyright | 1984/07/01 | |
| date issued | 1984 | |
| identifier issn | 0022-3670 | |
| identifier other | ams-26719.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4163644 | |
| description abstract | A 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. | |
| publisher | American Meteorological Society | |
| title | The Generation of Barotropic Edge Waves by Deep-Sea Internal Waves | |
| type | Journal Paper | |
| journal volume | 14 | |
| journal issue | 7 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/1520-0485(1984)014<1152:TGOBEW>2.0.CO;2 | |
| journal fristpage | 1152 | |
| journal lastpage | 1158 | |
| tree | Journal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 007 | |
| contenttype | Fulltext |