The Effect of Northern Hemisphere Winds on the Meridional Overturning Circulation and Stratification
AbstractThe current paradigm for the meridional overturning cell and the associated middepth stratification is that the wind stress in the subpolar region of the Southern Ocean drives a northward Ekman flow, which, together with the global diapycnal mixing across the lower boundary of the middepth w...
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ftcdlib:oai:escholarship.org/ark:/13030/qt6qp5h1s6 2023-05-15T17:28:59+02:00 The Effect of Northern Hemisphere Winds on the Meridional Overturning Circulation and Stratification Cessi, Paola 2495 - 2506 2018-10-01 application/pdf https://escholarship.org/uc/item/6qp5h1s6 unknown eScholarship, University of California qt6qp5h1s6 https://escholarship.org/uc/item/6qp5h1s6 public JOURNAL OF PHYSICAL OCEANOGRAPHY, vol 48, iss 10 Meridional overturning circulation Oceanography Maritime Engineering article 2018 ftcdlib 2021-01-24T17:37:54Z AbstractThe current paradigm for the meridional overturning cell and the associated middepth stratification is that the wind stress in the subpolar region of the Southern Ocean drives a northward Ekman flow, which, together with the global diapycnal mixing across the lower boundary of the middepth waters, feeds the upper branch of the interhemispheric overturning. The resulting mass transport proceeds to the Northern Hemisphere of the North Atlantic, where it sinks, to be eventually returned to the Southern Ocean at depth. Seemingly, the wind stress in the Atlantic basin plays no role. This asymmetry occurs because the Ekman transport in the Atlantic Ocean is assumed to return geostrophically at depths much shallower than those occupied by the interhemispheric overturning. However, this vertical separation fails in the North Atlantic subpolar gyre region. Using a conceptual model and an ocean general circulation model in an idealized geometry, we show that the westerly wind stress in the northern part of the Atlantic provides two opposing effects. Mechanically, the return of the Ekman transport in the North Atlantic opposes sinking in this region, reducing the total overturning and deepening the middepth stratification; thermodynamically, the subpolar gyre advects salt poleward, promoting Northern Hemisphere sinking. Depending on which mechanism prevails, increased westerly winds in the Northern Hemisphere can reduce or augment the overturning. Article in Journal/Newspaper North Atlantic Southern Ocean University of California: eScholarship Southern Ocean |
institution |
Open Polar |
collection |
University of California: eScholarship |
op_collection_id |
ftcdlib |
language |
unknown |
topic |
Meridional overturning circulation Oceanography Maritime Engineering |
spellingShingle |
Meridional overturning circulation Oceanography Maritime Engineering Cessi, Paola The Effect of Northern Hemisphere Winds on the Meridional Overturning Circulation and Stratification |
topic_facet |
Meridional overturning circulation Oceanography Maritime Engineering |
description |
AbstractThe current paradigm for the meridional overturning cell and the associated middepth stratification is that the wind stress in the subpolar region of the Southern Ocean drives a northward Ekman flow, which, together with the global diapycnal mixing across the lower boundary of the middepth waters, feeds the upper branch of the interhemispheric overturning. The resulting mass transport proceeds to the Northern Hemisphere of the North Atlantic, where it sinks, to be eventually returned to the Southern Ocean at depth. Seemingly, the wind stress in the Atlantic basin plays no role. This asymmetry occurs because the Ekman transport in the Atlantic Ocean is assumed to return geostrophically at depths much shallower than those occupied by the interhemispheric overturning. However, this vertical separation fails in the North Atlantic subpolar gyre region. Using a conceptual model and an ocean general circulation model in an idealized geometry, we show that the westerly wind stress in the northern part of the Atlantic provides two opposing effects. Mechanically, the return of the Ekman transport in the North Atlantic opposes sinking in this region, reducing the total overturning and deepening the middepth stratification; thermodynamically, the subpolar gyre advects salt poleward, promoting Northern Hemisphere sinking. Depending on which mechanism prevails, increased westerly winds in the Northern Hemisphere can reduce or augment the overturning. |
format |
Article in Journal/Newspaper |
author |
Cessi, Paola |
author_facet |
Cessi, Paola |
author_sort |
Cessi, Paola |
title |
The Effect of Northern Hemisphere Winds on the Meridional Overturning Circulation and Stratification |
title_short |
The Effect of Northern Hemisphere Winds on the Meridional Overturning Circulation and Stratification |
title_full |
The Effect of Northern Hemisphere Winds on the Meridional Overturning Circulation and Stratification |
title_fullStr |
The Effect of Northern Hemisphere Winds on the Meridional Overturning Circulation and Stratification |
title_full_unstemmed |
The Effect of Northern Hemisphere Winds on the Meridional Overturning Circulation and Stratification |
title_sort |
effect of northern hemisphere winds on the meridional overturning circulation and stratification |
publisher |
eScholarship, University of California |
publishDate |
2018 |
url |
https://escholarship.org/uc/item/6qp5h1s6 |
op_coverage |
2495 - 2506 |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
North Atlantic Southern Ocean |
genre_facet |
North Atlantic Southern Ocean |
op_source |
JOURNAL OF PHYSICAL OCEANOGRAPHY, vol 48, iss 10 |
op_relation |
qt6qp5h1s6 https://escholarship.org/uc/item/6qp5h1s6 |
op_rights |
public |
_version_ |
1766122292899741696 |