| contributor author | Welander, Pierre | |
| contributor author | Liu, Cho-Teng | |
| date accessioned | 2017-06-09T14:44:19Z | |
| date available | 2017-06-09T14:44:19Z | |
| date copyright | 1976/07/01 | |
| date issued | 1976 | |
| identifier issn | 0022-3670 | |
| identifier other | ams-25623.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4162427 | |
| description abstract | In a uniform-depth ocean forced by a wind stress and surface heat flux (or surface temperature) which are independent of longitude, there exists a possible thermocline regime with vanishing east-west temperature gradient. The associated meridional-vertical circulation is entirely wind-driven, producing a deep thermal structure at high latitudes, a thin equatorial thermocline, and a vertical thermal front at the latitude of vanishing Ekman downwelling. Some numerical examples are given. | |
| publisher | American Meteorological Society | |
| title | On a Mid-Ocean Thermocline Regime | |
| type | Journal Paper | |
| journal volume | 6 | |
| journal issue | 4 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/1520-0485(1976)006<0592:OAMOTR>2.0.CO;2 | |
| journal fristpage | 592 | |
| journal lastpage | 595 | |
| tree | Journal of Physical Oceanography:;1976:;Volume( 006 ):;issue: 004 | |
| contenttype | Fulltext | |