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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Bibliographic Details
Main Author: Klinck, John M.
Format: Article in Journal/Newspaper
Language:unknown
Published: ODU Digital Commons 1992
Subjects:
Online Access:https://digitalcommons.odu.edu/ccpo_pubs/171
https://digitalcommons.odu.edu/cgi/viewcontent.cgi?article=1176&context=ccpo_pubs