Annotation
The turbulent vertical-exchange coefficient and the heat-flow coefficient in the surface layer of the sea are calculated on the basis of experimental data and an extension of Fjeldstad's method. The amplitudes and phases of the radiative and turbulent heat flows and their ratios are estimated.
© 2016 Publisher M.V.Lomonosov Moscow State University
Authors
A.A. Pivovarov, E.P. Anisimova, and L.A. Bukina
Department of Maritime and Inland-Water Physics
Department of Maritime and Inland-Water Physics
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