| contributor author | Liu, Zhengyu | |
| contributor author | Huang, Boyin | |
| date accessioned | 2017-06-09T14:53:06Z | |
| date available | 2017-06-09T14:53:06Z | |
| date copyright | 1998/07/01 | |
| date issued | 1998 | |
| identifier issn | 0022-3670 | |
| identifier other | ams-28905.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4166073 | |
| description abstract | It is suggested that the tritium maximum in the central Pacific is caused by two water pathways across the North Equatorial Countercurrent (NECC), one from the central Pacific and the other from the Mindanao Current. It is argued that an interior pathway exists, by which tritium-rich thermocline waters from the subtropical North Pacific cross the NECC in the central Pacific. The transport in this pathway, however, is small compared with that from the Mindanao Current. | |
| publisher | American Meteorological Society | |
| title | Why Is There a Tritium Maximum in the Central Equatorial Pacific Thermocline? | |
| type | Journal Paper | |
| journal volume | 28 | |
| journal issue | 7 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/1520-0485(1998)028<1527:WITATM>2.0.CO;2 | |
| journal fristpage | 1527 | |
| journal lastpage | 1533 | |
| tree | Journal of Physical Oceanography:;1998:;Volume( 028 ):;issue: 007 | |
| contenttype | Fulltext | |