Абстракт
The aim of the work is to calculate the circulation in the Sea Azov under intense wind stress of different directions, including cyclonic and anticyclonic nature. Numerical experiments were carried out using a three-dimensional barotropic model taking into account the real bottom relief, taking into account run-up phenomena, parametrization of variables in the space of turbulent diffusion coefficients, which, together with the flow fields, are input parameters for solving a wide class of problems of impurity transfer to the sea and solving problems related to the assimilation of measurement data, identification of pollution sources and their parameters.
Ключевые слова
Anticyclone, Cyclone, Surges, The Sea of Azov, Wind barotropic currents