A damped Ekman model with a Rayleigh drag term reproduces observed flattened Ekman spirals and changes estimates of wind-driven transport and upwelling.
Direct observations of the Ekman balance at 10 N in the Pacific
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Ekman Theory with Damping
A damped Ekman model with a Rayleigh drag term reproduces observed flattened Ekman spirals and changes estimates of wind-driven transport and upwelling.