Vertical Mixing in the Main Pycnocline of the Black Sea in Summer

A. N. Morozov

Marine Hydrophysical Institute of RAS, Sevastopol, Russian Federation

e-mail: anmorozov@mhi-ras.ru

Abstract

Purpose. The study is aimed at assessing the parameters of vertical turbulent mixing in the main pycnocline of the Black Sea based on the data on current velocity and density measured by standard hydrological instruments.

Methods and Results. The data collected during six summer cruises of R/V Professor Vodyanitsky in the central sector of the northern sea area in 2016–2021 were used in the research. Temperature, salinity and current velocity profiles were measured by the CTD/LADCP probes. The vertical turbulent diffusion coefficient was calculated with the G03 parameterization. The applied relations are given. The values of the required parameters on the isopycnal surface with the conditional density value 15 kg/m3 are used as the initial data. Their filtered dependencies on its depth are substituted into the calculated relations. It is found that a well-pronounced maximum of specific kinetic energy is observed on average when the isopycnal depth is 77 m. The values of the shear/strain ratio and the canonical internal wave spectrum are close. The average value of the measured shear constitutes about one third of the value of the canonical internal wave spectrum. The average value of the vertical turbulent diffusion coefficient is 10−6 m2/s. Its value in the central sea area is comparable to the heat molecular diffusion coefficient. At the isopycnal depth 90 m the maximum value reaching 1.6·10−6 m2/s, is shifted to the right relatively the Rim Current at a horizontal distance of about 26 km. The average value of the turbulent kinetic energy dissipation rate is 2·10−9 W/kg.

Conclusions. The value of the vertical turbulent diffusion coefficient calculated based on the data collected with a depth resolution of about 10 m agrees well with the estimates obtained from the data of microstructure probes. However, the results of the study should be considered preliminary; in order to obtain a more convincing confirmation of their correctness, it is advisable to conduct synchronous measurements using the microstructure probes and standard hydrological instruments.

Keywords

Black Sea, main pycnocline, vertical turbulent mixing, Rim Current, current velocity shear, strain

Acknowledgements

The study was carried out as part of the state assignment theme FSBSI FRC MHI FNNN-2024-0012, titled “Operational Oceanology”.

Original russian text

Original Russian Text © A. N. Morozov, 2025, published in MORSKOY GIDROFIZICHESKIY ZHURNAL, Vol. 41, Iss. 3, pp. 251–263 (2025)

For citation

Morozov, A.N., 2025. Vertical Mixing in the Main Pycnocline of the Black Sea in Summer. Physical Oceanography, 32(3), pp. 271-282.

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