ТЕРМОХАЛИННАЯ ХАРАКТЕРИСТИКА СРЕДИЗЕМНОМОРСКОЙ ВОДЫ ЗИМОЙ В ПРИБОСФОРСКОМ РАЙОНЕ ЧЕРНОГО МОРЯ
1981
The inflow of the Mediterranean waters into the Black Sea through the Bosporus in the winter period was studied. The detected fluctuations of the 10° isothermal line level are supposed to be attributed to passing of internal waves of different energy carrying frequencies.
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