V. V. Efimov, D. A. Iarovaya*, V. S. Barabanov
Marine Hydrophysical Institute of RAS, Sevastopol, Russia
* e-mail: darik777@mhi-ras.ru
Abstract
Using 2-km resolution coupled air-sea mesoscale model NOW (NEMO-OASIS-WRF), we studied a case of upwelling in the Black Sea near the South Coast of Crimea on 24–25 September 2013. The NOW model successfully reproduced a sharp decrease of sea surface temperature (SST) by 10 °C within two days. The high spatial resolution in the model allowed us to describe upwelling features resulting from the orography and shape of the coastline. In particular, we found small-scale areas of low SST near the coast where surface wind is directed along the coast to the right, for example over the sea near the coastal Crimean Mountains. At the same time the upwelling does not occur in the areas where the coastal wind has another direction, for example in the north-western part of Karkinit Bay, near the coast north to Sevastopol, and near the Azov coast. It is shown that there is a vertical circulation cell in the sea caused by the upwelling: a rise of the seasonal thermocline near the shore, outflow of warm water in the upper quasi-homogenous layer and descend of water at the 30–50 km distance from the shore. We found that the coastal current has diurnal variation due to breeze circulation: the velocity component perpendicular to the coast reaches its maximum during the daylight hours, whereas velocity component directed along the coast reaches its maximum with a delay of 4–6 hours.
Keywords
mesoscale coupled modelling, wind upwelling, vertical structure of velocity and temperature fields in sea, seasonal thermocline, Black Sea, South Coast of Crimea
Acknowledgments
The work was performed under project no. 0555-2021-0002 “Fundamental studies of processes of interaction in the ocean – atmosphere system which determine the regional spatial-temporal variability of the natural environment and climate”.
For citation
Efimov, V.V., Iarovaya, D.A. and Barabanov, V.S., 2023. Numerical Modelling of Upwelling near the South Coast of Crimea on 24–25 September 2013. Ecological Safety of Coastal and Shelf Zones of Sea, (1), pp. 6–19. doi:10.29039/2413-5577-2023-1-6-19
DOI
10.29039/2413-5577-2023-1-6-19
References
- Ivanov, V.A. and Mikhaylova, E.N., 2008. [Upwelling in the Black Sea]. Sevastopol: ECOSI-Gidrofizika, 92 p. (in Russian).
- Brink, K.N., 1983. The Near-Surface Dynamics of Coastal Upwelling. Progress in Oceanography, 12(3), pp. 223–257. https://doi.org/10.1016/0079-6611(83)90009-5
- Allen, J.S., 1973. Upwelling and Coastal Jets in a Continuously Stratified Ocean. Journal of Physical Oceanography, 3(3), pp. 245–257. https://doi.org/10.1175/1520-0485(1973)003<0245:UACJIA>2.0.CO;2
- Preller, R. and O’Brien, J.J., 1980. The Influence of Bottom Topography on Upwelling off Peru. Journal of Physical Oceanography, 10(9), pp. 1377–1398. https://doi.org/10.1175/1520-0485(1980)010<1377:TIOBTO>2.0.CO;2
- Philander, S.J.H. and Yoon, J.-H., 1982. Eastern Boundary Currents and Coastal Upwelling. Journal of Physical Oceanography, 12(8), pp. 862–879. https://doi.org/10.1175/1520-0485(1982)012<0862:EBCACU>2.0.CO;2
- Peffley, M.B. and O’Brien, J.J., 1976. A Three-Dimensional Simulation of Coastal Upwelling off Oregon. Journal of Physical Oceanography, 6(2), pp. 164–180. https://doi.org/10.1175/1520-0485(1976)006<0164:ATDSOC>2.0.CO;2
- Androsovich, A.I., Mikhailova, E.N. and Shapiro, N.B., 1995. Numerical Model and Calculation of the Water Circulation in the North-Western Black Sea. Physical Oceanography, 6(5), pp. 351–364. https://doi.org/10.1007/BF02197483
- Kosnyrev, V.N., Mikhailova, E.N. and Stanichny, S.V., 1997. Upwelling in the Black Sea by the Results of Numerical Experiments and Satellite Data. Physical Oceanography, 8(5), pp. 329–340. https://doi.org/10.1007/BF02523759
- Zatsepin, A.G., Silvestrova, K.P., Kuklev, S.B., Piotoukh, V.B. and Podymov, O.I., 2016. Observations of a Cycle of Intense Coastal Upwelling and Downwelling at the Research Site of the Shirshov Institute of Oceanology in the Black Sea. Oceanology, 56(2), pp. 188–199. https://doi.org/10.1134/S0001437016020211
- Ginzburg, A.I., 1995. [On Variable Jet Currents in the Southwest Part of the Black Sea]. Issledovanie Zemli iz Kosmosa, (4), pp. 10–16 (in Russian).
- Ginzburg, A.I., Kostianoy, A.G., Soloviev, D.M. and Stanichny, S.V., 1998. Cyclonic Upwelling Eddies off the South-West Crimea. Issledovanie Zemli iz Kosmosa, (3), pp. 83–88 (in Russian).
- Divinsky, B.V., Kuklev, S.B. and Zatsepin, A.G., 2017. Numerical Simulation of an Intensive Upwelling Event in the Northeastern Part of the Black Sea at the IO RAS Hydrophysical Testing Site. Oceanology, 57(5), pp. 615–620. https://doi.org/10.1134/S0001437017040038
- Polonskii, A.B. and Muzyleva, M.A., 2016. Modern Spatial-Temporal Variability of Upwelling in the North-Western Black Sea and off the Crimea Coast. Izvestiya RAN. Seriya Geograficheskaya, (4), pp. 96–108. (in Russian).
- Stanichnaya, R.R. and Stanichny, S.V., 2021. Black Sea Upwellings. Sovremennye Problemy Distantsionnogo Zondirovaniya Zemli iz Kosmosa, 18(4), pp. 195–207. doi:10.21046/2070-7401-2021-18-4-195-207 (in Russian).
- Iarovaya, D.A., Efimov, V.V., Barabanov, V.S. and Mizyuk, А.А., 2020. Response of the Black Sea Upper Layer to the Cyclone Passage on September 25–29, 2005. Russian Meteorology and Hydrology, 45(10), pp. 701–711. https://doi.org/10.3103/S1068373920100040
- Iarovaia, D.A. and Efimov, V.V., 2021. Development of Cold Sea Surface Temperature Anomalies in the Black Sea. Izvestiya, Atmospheric and Oceanic Physics, 57(4), pp. 413–424. https://doi.org/10.1134/S0001433821040228
- Valcke, S., 2013. The OASIS3 Coupler: A European Climate Modelling Community Software. Geoscientific Model Development, 6(2), pp. 373–388. https://doi.org/10.5194/gmd-6-373-2013
- Rodi, W., 1987. Examples of Calculation Methods for Flow and Mixing in Stratified Fluids. Journal of Geophysical Research: Oceans, 92(C5), pp. 5305–5328. https://doi.org/10.1029/JC092iC05p05305
- Efimov, V.V., 2017. Numerical Simulation of Breeze Circulation over the Crimean Peninsula. Izvestiya, Atmospheric and Oceanic Physics, 53(1), pp. 84–94. doi:10.1134/S0001433817010042