| contributor author | Hill, R. B. | |
| contributor author | Johnson, J. A. | |
| date accessioned | 2017-06-09T14:43:48Z | |
| date available | 2017-06-09T14:43:48Z | |
| date copyright | 1974/01/01 | |
| date issued | 1974 | |
| identifier issn | 0022-3670 | |
| identifier other | ams-25408.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4162188 | |
| description abstract | The three-dimensional circulation produced in a homogeneous ocean by a steady wind stress is investigated when the bottom topography contains a discontinuity in gradient, such as occurs at the edge of the continental shelf. A shear layer is formed above the edge of the shelf in which upwelling is significant. The vertical transport in the shear layer can be sufficient to produce a surface convergence zone in the vicinity of the shelf. | |
| publisher | American Meteorological Society | |
| title | A Theory of Upwelling Over the Shelf Break | |
| type | Journal Paper | |
| journal volume | 4 | |
| journal issue | 1 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/1520-0485(1974)004<0019:ATOUOT>2.0.CO;2 | |
| journal fristpage | 19 | |
| journal lastpage | 26 | |
| tree | Journal of Physical Oceanography:;1974:;Volume( 004 ):;issue: 001 | |
| contenttype | Fulltext | |
