Spatial Structure of Sea Currents in the Sea of Azov Based on Numerical Modeling Data
B. V. Divinsky
Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russian Federation
divin@ocean.ru
Abstract
Purpose. The purpose of the study is to obtain climatic spatial fields of currents in the Sea of Azov.
Methods and Results. The parameters of sea currents in the Sea of Azov were calculated for a 45-year climatic period (January 1979 – December 2023) using mathematical modeling and a combined hydrodynamic model that accounts for the interaction between currents and wind waves in shallow water conditions. The model was verified against available experimental data on current parameters, wind waves and sea level. The three-dimensional spatial structure of surface and bottom currents in the Sea of Azov has been established. The main feature is a large cyclonic gyre occupying the entire water column in the central part of the sea. In the western part of the sea, surface currents form local eddy structures with a general water transport directed toward the Arabat Spit, while bottom currents form an anticyclonic eddy with a general transport from the Arabat Spit northeastward. The areas of the most intense currents were identified: the Dolzhansky Strait connecting the main basin with Taganrog Bay, Taganrog Bay itself, the tips of the spits along the northern coast, and the southern part of the sea adjacent to the Kerch Strait. In these areas, the maximum speed of surface currents reaches ~ 1.2 m/s (up to 1.5 m/s in the strait), and that of bottom currents reaches 0.6–0.7 m/s.
Conclusions. The study has made it possible, for the first time, to obtain separate climatic fields of surface and bottom currents in the Sea of Azov and to reveal the complex vertical structure of its circulation. The results provide a basis for solving both fundamental and applied problems, including navigation safety, assessment of bottom sediment transport, and environmental monitoring.
Keywords
Sea of Azov, numerical modeling, climatic fields of currents, water circulation
Acknowledgements
The formation of the sea current parameters database and the setup of the numerical model were carried out within the framework of state assignments of IO RAS FMWE-2024-0027 and 8.5. The problem was formulated, and the results were processed and analyzed with the support of Russian Science Foundation Grant No. 25-17-00104, https://rscf.ru/project/25-17-00104.
Original russian text
Original Russian Text © B. V. Divinsky, 2025, published in MORSKOY GIDROFIZICHESKIY ZHURNAL, Vol. 41, Iss. 6, pp. 843-854 (2025)
For citation
Divinsky, B.V., 2025. Spatial Structure of Sea Currents in the Sea of Azov Based on Numerical Modeling Data. Physical Oceanography, 32(6), pp. 861-870.
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