| contributor author | Louise Rousselet | |
| contributor author | Paola Cessi | |
| contributor author | Matthew R. Mazloff | |
| date accessioned | 2023-04-12T18:30:24Z | |
| date available | 2023-04-12T18:30:24Z | |
| date copyright | 2022/12/22 | |
| date issued | 2022 | |
| identifier other | JPO-D-21-0308.1.pdf | |
| identifier uri | http://yetl.yabesh.ir/yetl1/handle/yetl/4289787 | |
| description abstract | The origins of the upper limb of the Atlantic meridional overturning circulation and the partition among different routes has been quantified with models at eddy-permitting and one eddy-resolving model or with low-resolution models assimilating observations. Here, a step toward bridging this gap is taken by using the Southern Ocean State Estimate (SOSE) at the eddy-permitting 1/6° horizontal resolution to compute Lagrangian diagnostics from virtual particle trajectories advected between 6.7°S and two meridional sections: one at Drake Passage (cold route) and the other from South Africa to Antarctica (warm route). Our results agree with the prevailing concept attributing the largest transport contribution to the warm route with 12.3 Sv (88%) (1 Sv ≡ 10 | |
| publisher | American Meteorological Society | |
| title | What Controls the Partition between the Cold and Warm Routes in the Meridional Overturning Circulation? | |
| type | Journal Paper | |
| journal volume | 53 | |
| journal issue | 1 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/JPO-D-21-0308.1 | |
| journal fristpage | 215 | |
| journal lastpage | 233 | |
| page | 215–233 | |
| tree | Journal of Physical Oceanography:;2022:;volume( 053 ):;issue: 001 | |
| contenttype | Fulltext | |
