The Dependence of Southern Ocean Meridional Overturning on Wind Stress
An eddy-resolving numerical model of a zonal flow, meant to resemble the Antarctic Circumpolar Current, is described and analyzed using the framework of J. Marshall and T. Radko. In addition to wind and buoyancy forcing at the surface, the model contains a sponge layer at the northern boundary that...
| Main Authors: | , , |
|---|---|
| Other Authors: | |
| Format: | Article |
| Language: | en_US |
| Published: |
American Meteorological Society
2012
|
| Online Access: | http://hdl.handle.net/1721.1/70089 https://orcid.org/0000-0001-9230-3591 |