Effects of Wind, Density, and Bathymetry on a One-Layer Southern Ocean Model
Steady solutions from a one-layer, wind-driven, primitive equation model are analyzed to determine the importance of wind forcing, pressure gradient force due to the climatological density distribution and bottom form drag on circulation in the Southern Ocean. Five simulations are discussed: three w...
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Format: | Article in Journal/Newspaper |
Language: | unknown |
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ODU Digital Commons
1992
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Online Access: | https://digitalcommons.odu.edu/ccpo_pubs/171 https://digitalcommons.odu.edu/cgi/viewcontent.cgi?article=1176&context=ccpo_pubs |