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Westward Intensification of the Mean Circulation on the Bering Sea Shelf
Westward Intensification Mean Circulation Bering Sea Shelf
2009/1/12
Most of the water that eventually flows northward through Bering Strait originates about 500 km south, seaward of the shelfbreak in the Bering Sea. Cumulative observational evidence supports the idea ...
Stommel’s “Westward Intensification” in a Three-Dimensional Similarity Version
Westward Intensification Three-Dimensional Similarity Version Stommel's classical transport
2009/1/5
A special three-dimensional solution of similarity type is given for a meridionally closed ocean with dynamic according to Stommel's classical transport model, and with the density determined by three...