| contributor author | Niiler, P. P. | |
| contributor author | Simco, E. | |
| contributor author | Larue, R. | |
| date accessioned | 2017-06-09T14:43:30Z | |
| date available | 2017-06-09T14:43:30Z | |
| date copyright | 1971/10/01 | |
| date issued | 1971 | |
| identifier issn | 0022-3670 | |
| identifier other | ams-25278.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4162043 | |
| description abstract | A two-layer model of a mid-oceanic thermocline is developed, and a comparison of the depth and temperature of the thermocline in this model is made with a root-mean-square description of the hydrographic structure of the North Atlantic. It is shown that the Sverdrup balance is maintained within the rms errors, and the entire estimated heat flux from the atmosphere is used to produce the observed density changes along the path of persistent flow. | |
| publisher | American Meteorological Society | |
| title | A Two-Layer Model of the North Atlantic Thermocline | |
| type | Journal Paper | |
| journal volume | 1 | |
| journal issue | 4 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/1520-0485(1971)001<0271:ATLMOT>2.0.CO;2 | |
| journal fristpage | 271 | |
| journal lastpage | 277 | |
| tree | Journal of Physical Oceanography:;1971:;Volume( 001 ):;issue: 004 | |
| contenttype | Fulltext | |
