| contributor author | Wang, Dailin | |
| contributor author | Moore, Dennis W. | |
| contributor author | Rothstein, Lewis M. | |
| date accessioned | 2017-06-09T14:51:10Z | |
| date available | 2017-06-09T14:51:10Z | |
| date copyright | 1994/10/01 | |
| date issued | 1994 | |
| identifier issn | 0022-3670 | |
| identifier other | ams-28203.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4165294 | |
| description abstract | Exact solutions are found for Kawase's linear, two-layer model of mass-driven deep-ocean circulation. It is demonstrated that for strong damping, even though the deep western boundary current (DWBC) bifurcates at the equator as found in Kawase's perturbation solution, the equatorial flow is much weaker and has a much broader scale than the imposed DWBC. It is found that the presence of an eastern boundary is not necessary for the DWBC to cross the equator in the weak damping case. | |
| publisher | American Meteorological Society | |
| title | Exact Solutions to Kawase's Linear Model of Deep Ocean Circulation | |
| type | Journal Paper | |
| journal volume | 24 | |
| journal issue | 10 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/1520-0485(1994)024<2188:ESTKLM>2.0.CO;2 | |
| journal fristpage | 2188 | |
| journal lastpage | 2195 | |
| tree | Journal of Physical Oceanography:;1994:;Volume( 024 ):;issue: 010 | |
| contenttype | Fulltext | |