| contributor author | Smith, Neville R. | |
| contributor author | Fandry, C. B. | |
| date accessioned | 2017-06-09T14:44:11Z | |
| date available | 2017-06-09T14:44:11Z | |
| date copyright | 1976/01/01 | |
| date issued | 1976 | |
| identifier issn | 0022-3670 | |
| identifier other | ams-25565.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4162362 | |
| description abstract | A simple, frictional, linear model is used to study the motion of the Gull Stream over the continental shelf. It is found that the combination of frictional and topographic effects may provide a further mechanism by which the observed separation of the Gulf Stream may be achieved. The model predicts separation in the form of a classical separated boundary layer and interrelates the slope of the bottom with the position of separation. Counter-circulations northwest of the stream and increased northward transport of the current are also predicted. | |
| publisher | American Meteorological Society | |
| title | A Simple Topographic Model of Gulf Stream Separation | |
| type | Journal Paper | |
| journal volume | 6 | |
| journal issue | 1 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/1520-0485(1976)006<0022:ASTMOG>2.0.CO;2 | |
| journal fristpage | 22 | |
| journal lastpage | 28 | |
| tree | Journal of Physical Oceanography:;1976:;Volume( 006 ):;issue: 001 | |
| contenttype | Fulltext | |
