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Peculiarities of oceanographic processes in the north-western Black Sea

  • Analysis of Observations and Methods of Calculating Oceanic Hydrophysical Fields
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Physical Oceanography

Abstract

The paper examines how various factors affect the intensity of photosynthesis and oxidation reaction in the north-western part of the Black Sea. In the course of the evolution of the basin, natural aspects were widely changing; therefore their role is evaluated by the content of organic matter and diatoms in the bottom sediments. The influence of anthropogenic factors is determined by the current tendencies in the variation of physico-chemical and biological characteristics of the basin. The main factor upsetting steady functioning of the north-western Black Sea ecosystem is the large biogenic influx to the sea. The possible changing of the ecosystem during the nearest few decades is assessed.

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References

  1. Eremeev, V. N., Boguslavsky, S. G. and Zhorov, V. A. Some peculiarities of the Black Sea palaeohydrology in various geological periods.Phys. Oceanogr. (1995)6, 273–281.

    Article  Google Scholar 

  2. Fashchuk, D. Ya., Samyshev, E. Z., Sebakh, L. K.,et al., The forms of man's impact upon the Black Sea ecosystem under the current conditions.Mar. Ecology (1991) No.38, 19–28.

    Google Scholar 

  3. Berlinsky, N. A. The mechanism for the formation of near-bottom hypoxia in shelf ecosystems.Water Resources (1989) No.4, 112–121.

    Google Scholar 

  4. Kolesnikov, A. G. The application of data on O2 distribution for determining the intensity of vertical exchange in the ocean.Okeanologia (1963)3, 260–270.

    Google Scholar 

  5. Kolesnikov, A. G., Ivanova, Z. S. and Boguslavsky, S. G. About the effect of stability of waters upon the intensity of vertical transport in the Atlantic Ocean,Okeanologia (1961)1, 592–599.

    Google Scholar 

  6. Agatova, A. I., Burlakova, Z. P., Eremeeva, L. V.,et al., Dissolved and suspended organic matter in the Black Sea during winter-spring period. In:Multidisciplinary Oceanographic Investigations in the Black Sea. Sevastopol: MHI (1989), pp. 153–164.

    Google Scholar 

  7. Neprochnov, Yu. P. (Ed.).Geological History of the Black Sea as Reconstructed by the Subwater Deep-drilling Data. Moscow: Nauka (1980).

    Google Scholar 

  8. Eremeev, V. N., Boguslavsky, S. G. and Zhorov, V. A. Formation of the New Euxinic basin during Würmian glaciation period.Phys. Oceanogr. (1997)8, 297–304.

    Article  Google Scholar 

  9. Boguslavsky, S. G., Eremeev, V. N., Zhorov, V. A.,et al., The study of the dynamics of the Black Sea hydrogen sulfide zone.Morsk. Gidrofiz. Zh. (1986) No.6, 52–60.

    Google Scholar 

  10. Mozer, L.Contemporary Viniculture. Moscow, Kolos (1971).

    Google Scholar 

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Translated by Vladimir A. Puchkin.

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Boguslavsky, S.G., Zhorov, V.A., Sovga, E.E. et al. Peculiarities of oceanographic processes in the north-western Black Sea. Phys. Oceanogr. 9, 347–352 (1998). https://doi.org/10.1007/BF02522730

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  • DOI: https://doi.org/10.1007/BF02522730

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