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Lagrangian decomposition of the Deacon Cell
Stockholm University, Faculty of Science, Department of Meteorology.
Stockholm University, Faculty of Science, Department of Meteorology.
2008 (English)In: Journal of Geophysical Research: Oceans, Vol. 113, C07028- p.Article in journal (Refereed) Published
Abstract [en]

The meridional overturning cells in the Southern Ocean are decomposed by Lagrangian tracing using velocity and density fields simulated with an ocean general circulation model. Particular emphasis is given to the Deacon Cell. The flow is divided into four major components: 1) water circling around Antarctica in the Antarctic Circumpolar Current (ACC), 2) water leaving the ACC towards the north into the three world oceans, 3) water coming from the north and joining the ACC, mainly consisting of North Atlantic Deep Water (NADW) and 4) inter-ocean exchange between the three world oceans without circling around Antarctica. The Deacon Cell has an amplitude of 20 Sv, of which 6 Sv can be explained by the the east-west tilt of the ACC, 5 Sv by the east-west tilt of the sub-tropical gyre, and the remaining 9 Sv by the differences of the slope and depth of the southward transport of NADW and its return flow as less dense water. The diabatic or cross-isopycnal Deacon Cell is only 2 Sv.

Place, publisher, year, edition, pages
2008. Vol. 113, C07028- p.
National Category
Oceanography, Hydrology, Water Resources
URN: urn:nbn:se:su:diva-16017DOI: doi:10.1029/2007JC004351ISI: 000257999800004OAI: diva2:182537
Available from: 2009-01-13 Created: 2009-01-13 Last updated: 2011-01-10Bibliographically approved

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Döös, KristoferNycander, Jonas
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