title: Two-layer Eddy-resolving Model of Wind Currents in the Black Sea
abstract: Processes of formation and variability of the Black Sea circulation are investigated using a two-layer eddy-resolving model. The wind effect only is considered as an exciting force; energy sink takes place due to horizontal turbulent viscosity, friction between the layers and the bottom friction. The rivers' flowing to the sea and the water exchange through the straits are not taken into account. Numerical approximation requires application of the finite-difference scheme based on the box-method
journal: Physical Oceanography