Weddell Sea anomalies: Excitation, propagation, and possible consequences
Article first published online: 19 JUN 2009
Copyright 2009 by the American Geophysical Union.
Geophysical Research Letters
Volume 36, Issue 12, June 2009
How to Cite
2009), Weddell Sea anomalies: Excitation, propagation, and possible consequences, Geophys. Res. Lett., 36, L12605, doi:10.1029/2009GL038407., , and (
- Issue published online: 19 JUN 2009
- Article first published online: 19 JUN 2009
- Manuscript Accepted: 22 MAY 2009
- Manuscript Received: 28 MAR 2009
- Southern Ocean;
- decadal variability;
- water mass properties
 Antarctic marginal seas are susceptible to significant decadal variability as revealed by the analysis of a 200-year integration of a regional ice-ocean model forced with the atmospheric output of the IPCC climate model ECHAM5-MPIOM. The strongest signal occurs on the southern and western Weddell Sea continental shelf where changes in bottom salinity are initiated by a variable sea ice cover and modification of surface waters near the Greenwich meridian. Related zonal shifts of the western rim current guide deep waters with different temperature out of the Weddell Sea. With a deep boundary current the temperature signal propagates westward through southern Drake Passage and along the upper continental rise in the southeast Pacific thereby influencing the hydrographic conditions on the continental shelf of Bellingshausen, Amundsen, and Ross Seas.