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Rossby's (1936) wake stream theory of the Gulf Stream is revived and generalized. Including the β-effect, the volume transport of the Stream should increase faster than predicted by the Tollmien-Rossby formula, in agreement with observations. The idea that the Gulf Stream is forced by the pressure head in the Florida Straits, with the wind-stress curl at the higher latitude playing a secondary role, finds some support from observations.
Rossby's (1936) wake stream theory of the Gulf Stream is revived and generalized. Including the β-effect, the volume transport of the Stream should increase faster than predicted by the Tollmien-Rossby formula, in agreement with observations. The idea that the Gulf Stream is forced by the pressure head in the Florida Straits, with the wind-stress curl at the higher latitude playing a secondary role, finds some support from observations.
| All Time | Past Year | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 267 | 144 | 11 |
| PDF Downloads | 53 | 17 | 0 |
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