| contributor author | Hsueh, Y. | |
| contributor author | Weatherly, Georges L. | |
| date accessioned | 2017-06-09T14:44:34Z | |
| date available | 2017-06-09T14:44:34Z | |
| date copyright | 1977/05/01 | |
| date issued | 1977 | |
| identifier issn | 0022-3670 | |
| identifier other | ams-25719.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4162533 | |
| description abstract | Because continental margins are inclined, the boundary layer over them is tied to bottom density as well as to the barotropic pressure gradient. Through the no-flux condition at the sea floor, the bottom boundary layer, in turn, constrains the interior density field. The barotropic pressure gradient and the baroclinic velocity are thus coupled. Theoretical analysis in the framework of a model of linear dynamics demonstrates this coupling and resolves it. | |
| publisher | American Meteorological Society | |
| title | The Importance of Density Stratification to Bottom Boundary Layers over Continental Margins | |
| type | Journal Paper | |
| journal volume | 7 | |
| journal issue | 3 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/1520-0485(1977)007<0488:TIODST>2.0.CO;2 | |
| journal fristpage | 488 | |
| journal lastpage | 493 | |
| tree | Journal of Physical Oceanography:;1977:;Volume( 007 ):;issue: 003 | |
| contenttype | Fulltext | |