| dc.contributor.author | Johnson, J. A. | |
| dc.contributor.author | Killworth, P. D. | |
| dc.date.accessioned | 2017-06-09T14:44:03Z | |
| dc.date.available | 2017-06-09T14:44:03Z | |
| dc.date.copyright | 1975/01/01 | |
| dc.date.issued | 1975 | |
| dc.identifier.issn | 0022-3670 | |
| dc.identifier.other | ams-25497.pdf | |
| dc.identifier.uri | http://onlinelibrary.yabesh.ir/handle/yetl/4162286 | |
| dc.description.abstract | The theory of Hill and Johnson for upwelling over the shelf break is modified to give agreement with the work of Killworth. It is shown that when upwelling occurs over a discontinuity in bottom slope, this upwelling does not penetrate into the surface Ekman layer. Associated with this upwelling is a strong current along the shelf break in the bottom Ekman layer. | |
| dc.publisher | American Meteorological Society | |
| dc.title | A Bottom Current Along the Shelf Break | |
| dc.type | Journal Paper | |
| dc.journal.volume | 5 | |
| dc.journal.issue | 1 | |
| dc.journal.title | Journal of Physical Oceanography | |
| dc.identifier.doi | 10.1175/1520-0485(1975)005<0185:ABCATS>2.0.CO;2 | |
| dc.journal.fristpage | 185 | |
| dc.journal.lastpage | 188 | |
| dc.tree | Journal of Physical Oceanography:;1975:;Volume( 005 ):;issue: 001 | |
| dc.contenttype | Fulltext | |
