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Influence of transparency of the surface 1-metre-depth layer of the ocean on heat and mass exchange between ocean and atmosphere

The calculations show that the absorption of the direct solar radiation in the surface 1-meter layer of the ocean depending on the transparence of the water can result in the change of the heat-and-mass exchange in it. Two new regimes of the heat and mass exchange are described, found experimentally in situ with the help of microthermoprobe. Data on the intensity of heat- and-mass exchange of the ocean and atmosphere are given.