Abstract
A numerical simulation has been undertaken to study the process of the transport of small river runoff by alongshore baroclinic sea currents. The study is based on the implementation of the Princeton Ocean Model (POM) under the conditions of a circular stratified basin whose surface is exposed to a transient tangential wind stress to form an alongshore baroclinic current. A baroclinic current of the downwelling type (in the Northern Hemisphere directed to the left to a sea-viewing observer) was shown to provide the carrying out of the river discharge from estuary’s vicinity more effectively than that of the upwelling type (in the Northern Hemisphere directed to the right to a sea-viewing observer).
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Original Russian Text © V.M. Zhurbas, P.O. Zavialov, A.S. Sviridov, D.A. Lyzhkov, E.E. Andrulionis, 2011, published in Okeanologiya, 2011, Vol. 51, No. 3, pp. 440–449.
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Zhurbas, V.M., Zavialov, P.O., Sviridov, A.S. et al. On the transport of small river run off by an alongshore baroclinic sea current. Oceanology 51, 415–423 (2011). https://doi.org/10.1134/S0001437011030234
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DOI: https://doi.org/10.1134/S0001437011030234