| contributor author | McPhaden, Michael J. | |
| contributor author | Fine, Rana A. | |
| date accessioned | 2017-06-09T14:49:00Z | |
| date available | 2017-06-09T14:49:00Z | |
| date copyright | 1988/10/01 | |
| date issued | 1988 | |
| identifier issn | 0022-3670 | |
| identifier other | ams-27416.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4164419 | |
| description abstract | The tropical tritium distribution between 1974 and 1981 is characterized by a maximum along the equator centered between 125° and 145°W. It signifies that this region has received the maximum input of high northern latitude water. A dynamical interpretation of the maximum shows that it can be explained by the strength of the Sverdrup circulation in the central equatorial Pacific where there is a strong zonal convergence in the North Equatorial Countercurrent (NECC) and a strong meridional geostrophic flow towards the equator. | |
| publisher | American Meteorological Society | |
| title | A Dynamical Interpretation of the Tritium Maximum in the Central Equatorial Pacific | |
| type | Journal Paper | |
| journal volume | 18 | |
| journal issue | 10 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/1520-0485(1988)018<1454:ADIOTT>2.0.CO;2 | |
| journal fristpage | 1454 | |
| journal lastpage | 1457 | |
| tree | Journal of Physical Oceanography:;1988:;Volume( 018 ):;issue: 010 | |
| contenttype | Fulltext | |
