The effect of Northern Hemisphere winds on the meridional overturning circulation and stratification

TitleThe effect of Northern Hemisphere winds on the meridional overturning circulation and stratification
Publication TypeJournal Article
Year of Publication2018
AuthorsCessi P
JournalJournal of Physical Oceanography
Volume48
Pagination2495-2506
Date Published2018/10
Type of ArticleArticle
ISBN Number0022-3670
Accession NumberWOS:000447718400003
Keywordsantarctic circumpolar current; atlantic; driven; Meridional overturning circulation; Mesoscale eddies; models; oceanography; pacific; southern-ocean; thermohaline circulation; transport; variability
Abstract

The 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.

DOI10.1175/jpo-d-18-0085.1
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