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Editor's Highlight
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GEOPHYSICAL RESEARCH LETTERS,
VOL. 33,
L06701,
doi:10.1029/2005GL025332,
2006
Simulated changes in the extratropical Southern Hemisphere winds and currents
John C. Fyfe
Canadian Centre for Climate Modelling and Analysis, Meteorological Service of Canada, Victoria, British Columbia, Canada
Oleg A. Saenko
Canadian Centre for Climate Modelling and Analysis, Meteorological Service of Canada, Victoria, British Columbia, Canada
Abstract
The results from 12 global climate models show a remarkably consistent strengthening and poleward shifting of the zonal wind
stress through the 20th and 21st centuries at extratropical Southern Hemisphere latitudes. Changes in the zonal circulation
of the ocean in the region are broadly consistent with the changes in zonal wind stress. In particular, the climate models
simulate a strengthening and a poleward shift of the Antarctic Circumpolar Current. The strengthening of the zonal wind stress
also results in intensifying northward Ekman transport across the Antarctic Circumpolar Current which, in the unblocked latitudes
of Drake Passage, implies increasing southward geostrophic transport in the ocean below about 2000 m. Zonal wind stress changes
such as these may be expected to enhance the mesoscale eddy activity in the Southern Ocean.
Received 28
November
2005;
accepted 30
January
2006;
published 16
March
2006.
Index Terms: 1610 Global Change: Atmosphere (0315, 0325); 1626 Global Change: Global climate models (3337, 4928); 1630 Global Change: Impacts of global change (1225); 1635 Global Change: Oceans (1616, 3305, 4215, 4513).
Read Full Article (file size: 1082952 bytes) Cited by
Citation: Fyfe, J. C., and O. A. Saenko
(2006),
Simulated changes in the extratropical Southern Hemisphere winds and currents,
Geophys. Res. Lett.,
33,
L06701,
doi:10.1029/2005GL025332.
Copyright 2006 by the American Geophysical Union.
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