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A two-layer model of the general circulation including wind and thermal forcing is discussed. The flow in each layer is geostrophic, hydrostatic and obeys linear potential vorticity constraints. The e...
In September–October 1988 and in April 1989 two 4-week cruises were organized to study the structure and dynamics of Gulf Stream meanders. The first one focused on an anticyclonic crest, and the secon...
The equatorial deep jets are often modeled as equatorially trapped long waves, either Kelvin or Rossby. Rossby waves perturb potential vorticity but Kelvin waves do not; therefore the potential vortic...

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