Regional cooling in the South Pacific sector of the Southern Ocean due to global warming
This study investigates processes leading to regional cooling in global warming experiments conducted with the NCAR fully coupled Community Climate System Model (CCSM3). While several previous studies have investigated regional cooling in the South Pacific sector of the Southern Ocean, the mechanism leading to this response remains unclear. We find that changes in ocean circulation offer the key to understanding the regional cooling. The regional cooling in the South Pacific sector of the Southern Ocean, especially the area north of the Ross Sea, results mainly through an advective mechanism. The ocean topography contributes strongly to the change of ocean circulation through changes in bottom vortex stretching associated with a decrease in the Antarctic Circumpolar Current transport.
document
http://n2t.net/ark:/85065/d7hx1d1w
eng
geoscientificInformation
Text
publication
2016-01-01T00:00:00Z
publication
2005-10-13T00:00:00Z
Copyright 2005 American Geophysical Union.
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