| dc.contributor.author | Anna-Lena Deppenmeier | |
| dc.contributor.author | Frank O. Bryan | |
| dc.contributor.author | William S. Kessler | |
| dc.contributor.author | LuAnne Thompson | |
| dc.date.accessioned | 2023-04-12T18:34:06Z | |
| dc.date.available | 2023-04-12T18:34:06Z | |
| dc.date.copyright | 2022/10/21 | |
| dc.date.issued | 2022 | |
| dc.identifier.other | JPO-D-21-0316.1.pdf | |
| dc.identifier.uri | http://yetl.yabesh.ir/yetl1/handle/yetl/4289892 | |
| dc.description.abstract | The equatorial Pacific zonal circulation is composed of westward surface currents, the eastward equatorial undercurrent (EUC) along the thermocline, and upwelling in the eastern cold tongue. Part of this upwelling arises from water flowing along isotherms sloping up to the east, but it also includes water mass transformation and consequent diabatic (cross-isothermal) flow ( | |
| dc.publisher | American Meteorological Society | |
| dc.title | Diabatic Upwelling in the Tropical Pacific: Seasonal and Subseasonal Variability | |
| dc.type | Journal Paper | |
| dc.journal.volume | 52 | |
| dc.journal.issue | 11 | |
| dc.journal.title | Journal of Physical Oceanography | |
| dc.identifier.doi | 10.1175/JPO-D-21-0316.1 | |
| dc.journal.fristpage | 2657 | |
| dc.journal.lastpage | 2668 | |
| dc.page | 2657–2668 | |
| dc.tree | Journal of Physical Oceanography:;2022:;volume( 052 ):;issue: 011 | |
| dc.contenttype | Fulltext | |
