An Equivalent-Barotropic Mode in the Fine Resolution Antarctic ModelSource: Journal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 011::page 1379Author:Killworth, Peter D.
DOI: 10.1175/1520-0485(1992)022<1379:AEBMIT>2.0.CO;2Publisher: American Meteorological Society
Abstract: Both the 6-year time-mean flow and the eddy kinetic energy in the Fine Resolution Antarctic Model are found to be approximately self-similar in the vertical, with the velocity showing a rapid decay with depth. A simple argument is given as to why this would be expected to occur in this and other numerical models, and an analysis is given as to the degree of steering of the mean flow by topography.
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| contributor author | Killworth, Peter D. | |
| date accessioned | 2017-06-09T14:50:29Z | |
| date available | 2017-06-09T14:50:29Z | |
| date copyright | 1992/11/01 | |
| date issued | 1992 | |
| identifier issn | 0022-3670 | |
| identifier other | ams-27946.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4165007 | |
| description abstract | Both the 6-year time-mean flow and the eddy kinetic energy in the Fine Resolution Antarctic Model are found to be approximately self-similar in the vertical, with the velocity showing a rapid decay with depth. A simple argument is given as to why this would be expected to occur in this and other numerical models, and an analysis is given as to the degree of steering of the mean flow by topography. | |
| publisher | American Meteorological Society | |
| title | An Equivalent-Barotropic Mode in the Fine Resolution Antarctic Model | |
| type | Journal Paper | |
| journal volume | 22 | |
| journal issue | 11 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/1520-0485(1992)022<1379:AEBMIT>2.0.CO;2 | |
| journal fristpage | 1379 | |
| journal lastpage | 1387 | |
| tree | Journal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 011 | |
| contenttype | Fulltext |