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Eddy saturation and frictional control of the Antarctic Circumpolar Current

Marshall, D. P., Ambaum, M. H. P., Maddison, J. R., Munday, D. R. and Novakova, L. (2017) Eddy saturation and frictional control of the Antarctic Circumpolar Current. Geophysical Research Letters, 44 (1). pp. 286-292. ISSN 1944-8007

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To link to this item DOI: 10.1002/2016GL071702

Abstract/Summary

The Antarctic Circumpolar Current is the strongest current in the ocean and has a pivotal impact on ocean stratification, heat content, and carbon content. The circumpolar volume transport is relatively insensitive to surface wind forcing in models that resolve turbulent ocean eddies, a process termed “eddy saturation.” Here a simple model is presented that explains the physics of eddy saturation with three ingredients: a momentum budget, a relation between the eddy form stress and eddy energy, and an eddy energy budget. The model explains both the insensitivity of circumpolar volume transport to surface wind stress and the increase of eddy energy with wind stress. The model further predicts that circumpolar transport increases with increased bottom friction, a counterintuitive result that is confirmed in eddy-permitting calculations. These results suggest an unexpected and important impact of eddy energy dissipation, through bottom drag or lee wave generation, on ocean stratification, ocean heat content, and potentially atmospheric CO2.

Item Type:Article
Refereed:Yes
Divisions:Faculty of Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
ID Code:68869
Uncontrolled Keywords:Analytical modeling and laboratory experiments, Eddies and mesoscale processes, Currents, General circulation, Topographic/bathymetric interactions, ocean eddies, eddy saturation, bottom drag, Antarctic Circumpolar Current, ocean stratification, heat content
Publisher:Wiley

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