The 3d problem of the calculation of Azov sea hydrodynamic

The description of the three-dimensional problem of the Azov sea and Taganrog bay hydrodynamic parameters determination is given. The sea water movement is imitated by the movement of a two-layer fluid, where the width of a high layer is determined by the value of the water level oscillation. The problem is solved by finite difference methods on the uniform rectangular grid. The results of the test calculations for some wind situations are given.