E. S. Eremina
Marine Hydrophysical Institute of RAS, Sevastopol, Russia
* e-mail: shchurova88@gmail.com
Abstract
The paper analyzes the salinity dynamics in the Sivash Bay after the closure of the North-Crimean based on the data from field research carried out by MHI RAS in 2014–2020. Recent field data are compared with the literature data obtained in the period before the commissioning of the North Crimean Canal. Salinity in water samples taken during 18 expeditions to the Eastern and Southern Sivash at over 100 stations was determined using the refractometric method. It was shown that after the closure of the North Crimean Canal in 2014, there was a steep increase in salinity in the Eastern and Southern Sivash. It was determined that in the area of the Sivash Bay, the haline field changes non-uniformly. The data analysis showed that salinity increases from north to south (from the Eastern to Southern Sivash), moreover salinity values in the Southern Sivash can be several times higher than those in the Eastern Sivash. In spring 2014, salinity in the Eastern Sivash varied from 27 to 33 ‰, and in 2020, 6 years after the closure of the Canal, salinity increased significantly at all stations reaching 60–70 ‰. These values are comparable to those obtained before the start of the Canal in the 1950s. The highest salinity values were observed in the South Sivash: in 2013, it was 54 ‰ and in summer 2020, for the first time since the North Crimean Canal became operational, it reached 110 ‰, which almost corresponds to the salinity level observed in 1969.
Keywords
Sivash Bay, Eastern Sivash, Southern Sivash, Sea of Azov, salinity dynamics, North-Crimean Canal
Acknowledgments
The author is grateful to Elena E. Sovga, Dr.Sci. (Geogr.), Leading Research Associate of the Shelf Hydrophysics Department, for setting the research objective and tasks, scientific supervising and work consulting, as well as to Aleksandr A. Latushkin, Junior Research Associate of the Marine Optics and Biophysics Department, for field research organization and assistance with sampling. The work is performed under state task on topic no. 0555-2021-0005.
For citation
Eremina, E.S., 2021. Restoration of Salinity in the Sivash Bay to Natural Levels after the Closure of the North Crimean Canal. Ecological Safety of Coastal and Shelf Zones of Sea, (3), pp. 84–93. doi:10.22449/2413-5577-2021-3-84-93 (in Russian).
DOI
10.22449/2413-5577-2021-3-84-93
References
- Eremina, Е.S. and Evstigneev, V.P., 2020. Inter-Annual Variability of Water Exchange between the Azov Sea and the Sivash Bay through the Tonky Strait. Physical Oceanography, 27(5), pp. 489–500. doi:10.22449/1573-160X-2020-5-489-500
- Kostyushina, V.A. and Fesenko, G.V., eds., 2007. Sivash Region: a Brief Socio-Economic Overview. Kiev: Wetlands International Black Sea Progr., 178 p. (in Russian).
- Shadrin, N.V., Sergeeva, N.G., Latushkin, A.A., Kolesnikova, E.A., Kipriyanova, L.M., Anufriieva, E.V. and Chepyzhenko, A.A., 2016. Transformation of Gulf Sivash (the Sea of Azov) in Conditions of Growing Salinity: Changes of Meiobenthos and other Ecosystem Components (2013–2015). Journal of Siberian Federal University. Biology, 9(4), pp. 452–466. https://doi.org/10.17516/1997-1389-2016-9-4-452-466 (in Russian).
- Soloveva, O.V., Tikhonova, E.A., Alemov, S.V., Burdiyan, N.V., Viter, T.V., Guseva, E.V., Kotelyanets, E.A. and Bogdanova, T.A., 2019. Ecological State of the Southeastern Part of Sivash Bay (Sea of Azov) under Conditions of Changing Salinity. Contemporary Problems of Ecology, 12(2), pp. 179–188. https://doi.org/10.1134/S1995425519020070
- Eremina, E.S., Sovga, E.E., Stanichny, S.V. and Mikhailov, V.A., 2020. Dynamics of Reed Vegetation Area in the Sivash Gulf (Sea of Azov) according to Satellite Data. Ecological Safety of Coastal and Shelf Zones of Sea, (4), pp. 54–65. doi:10.22449/2413-5577-2020-4-54-65 (in Russian).
- Shadrin, N., Kolesnikova, E., Revkova, T., Latushkin, A., Chepyzhenko, A., Dyakov, N. and Anufriieva, E., 2019. Macrostructure of Benthos along a Salinity Gradient: The Case of Sivash Bay (the Sea of Azov), the Largest Hypersaline Lagoon Worldwide. Journal of Sea Research, 154, 101811. https://doi.org/10.1016/j.seares.2019.101811
- Lomakin, P.D., Sovga, E.E., Shchurova, E.S. and Ovsyany, E.I., 2014. [MHI Field Research in the East Sivash in Spring and Autumn 2014]. In: MHI, 2014. Ekologicheskaya Bezopasnost' Pribrezhnykh i Shel'fovykh Zon i Kompleksnoe Ispol'zovanie Resursov Shel'fa [Ecological Safety of Coastal and Shelf Zones and Comprehensive Use of Shelf Resources]. Sevastopol: ECOSI-Gidrofizika. Iss. 28, pp. 138–145 (in Russian).
- Lomakin, P.D., 2020. Oceanological Characteristic of the Coastal Zone of Sivash Gulf (Azov Sea). Geopolitics and Ecogeodynamics of Regions, 6(4), pp. 170–180 (in Russian).
- Sovga, E.E., Eremina, E.S. and Latushkin, A.A., 2020. Research Expeditions Performed by Marine Hydrophysical Institute in the Sivash Bay Waters in Spring and Autumn, 2018. Physical Oceanography, 27(2), pp. 161–170. doi:10.22449/1573-160X-2020-2-161-170
- Krivoguz, D. and Borovskaya, R., 2020. Evaluating Surface Water Salinity Using Remote Sensing Data with Simple and Multiple Linear Regression for Hypersaline Waterbodies. Preprint. 13 p. doi:10.13140/RG.2.2.13836.54402
- Borovskaya, R.V., Zhugaylo, S.S., Krivoguz, D.O. and Shlyakhov, V.A., 2021. Ecological State of the Eastern Sivash Waters in Early Summer of 2020. Ecological Safety of Coastal and Shelf Zones of Sea, (1), pp. 84–98. doi:10.22449/2413-5577-2021-1-84-98 (in Russian).
- Mykhailov, V.A., 2019. Coastal accumulative Forms of Sivash Bay. Scientific Notes of V.I. Vernadsky Crimean Federal University. Geography. Geology, 5(2), pp. 80–88 (in Russian).