The Non-Linear Transient Response of a Continuously Stratified, Baroclinic Ocean to Stationary and Transitory Axially-Symmetric Atmospheric Cyclones.

The Non-Linear Transient Response of a Continuously Stratified, Baroclinic Ocean to Stationary and Transitory Axially-Symmetric Atmospheric Cyclones.

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A numerical model is developed to simulate circulation and mixing induced in an initially motionless, continuously stratified ocean by imposed axisymmetric hurricanes. Oceanic responses are obtained to (1) a suddenly applied steady wind permitting a...