Numerical modelling of oceanic circulation forced by the stationary wind in a two-layer ocean

A.B. Fedotov

Institute of Natural and Technical Systems, Russian Federation, Sevastopol, Lenin St., 28


UDC 551.465.5


   Using numerical simulation of two-layer ocean under the outer stationary vorticity flux the investigation of the development of a large-scale circulation has been provided. The space and time scales estimates of stream velocity oscillations in numerical experiments have been discussed and compared with the characteristics of large-scale circulation.

Кeywords: synoptic variability, large-scale variability, wind-forced currents.

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