A.B. Fedotov
Institute of Natural and Technical Systems, Russian Federation, Sevastopol, Lenin St., 28
E-mail: fedotov57@mail.ru
DOI: 10.33075/2220-5861-2017-4-96-101
UDC 551.465.553
Abstract:
Using numerical simulation of two-layer ocean with the layer depths corresponding to real oceanic conditions under the outer stationary vorticity flux and constant dissipation factors the investigation of the development of a large-scale circulation has been provided. There have been analyzed the timescales characters of large-scale circulation oscillation.
Кeywords: synoptic variability, large-scale variability, wind-forced currents.
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