Ocean Basin Geometry and the Salinification of the Atlantic Ocean

• Published in: Journal of Climate
• Main Authors: Nilsson, Johan, Langen, Peter L., Ferreira, David, Marshall, John
• Format: Article in Journal/Newspaper
• Language: English
• Published: Stockholms universitet, Meteorologiska institutionen (MISU) 2013
• Subjects: Atmosphere-ocean interaction; Energy transport; Freshwater; Gyres; Thermohaline circulation; Meteorology and Atmospheric Sciences; Meteorologi och atmosfärforskning; Pacific; Sea ice
• Online Access: http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-93306; https://doi.org/10.1175/JCLI-D-12-00358.1

A coupled atmosphere-sea ice-ocean model is used in an aqua-planet setting to examine the role of the basin geometry for the climate and ocean circulation. The basin geometry has a present-day-like topology with two idealized northern basins and a circumpolar ocean in the south. A suite of experiments is described in which the southward extents of the two (gridpoint wide) continents and the basin widths have been varied. When the two basins have identical shapes, the coupled model can attain a symmetric climate state with northern deep-water formation in both basins as well as asymmetric states, where the deep-water formation occurs only in one of the basins and Atlantic-Pacific-like hydrographic differences develop. A difference in the southward extents of the land barriers can enhance as well as reduce the zonal asymmetries of the atmosphere-ocean circulation. This arises from an interplay between the basin boundaries and the wind-driven Sverdrup circulation, which controls the interbasin exchange of heat and salt. Remarkably, when the short African continent is located near or equatorward of the zero wind line in the Southern Hemisphere, the deep-water formation becomes uniquely localized to the Atlantic-like basin with the long western boundary. In this case, the salinification is accomplished primarily by a westward wind-routed interbasin salt transport. Furthermore, experiments using geometries with asymmetries in both continental extents and basin widths suggest that in the World Ocean these two fundamental basin asymmetries should independently be strong enough for uniquely localizing the Northern Hemisphere deep-water formation to the Atlantic Ocean. AuthorCount:4;