Vol. 14, issue 06-07, article # 35
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Abstract:
Vertical exchange in a water body is modeled using the equations of hydrothermodynamics on eddy resolving scales. The model under study represents an ensemble of convective structures under conditions of density instability of the upper layers of water. The exchange on a subgrid scale is described within the framework of a semi-empirical theory of turbulence. The modeling results on transport of air bubbles and oil emulsions are given as an example.