The rivers of the Black Sea

Jaoshvili, S (2002) The rivers of the Black Sea. Technical Report. European Environment Agency, Copenhagen, Denmark.

Full text available as:

Preview

PDF - Requires a PDF viewer such as GSview, Xpdf or Adobe Acrobat Reader 370 Kb

Official URL: http://www.eea.eu.int

Summary

The Black Sea is now one of the most studied of all the marine basins on our planet. This has engendered a requirement for more precise data from additional research such as the balance between water and river load, sediment formation and a wide range of other subjects. The situation has been made more complex in recent years by the ever-increasing level of pollution, with its links to the outflow of water and river load from the surrounding landmass. Interest in the Black Sea stems not just from its strategic position and the biological richness of its waters. It is also of great economic significance internationally. The economic role of the Black Sea has increased over recent years since, after the disintegration of the Soviet Union, six Black Sea littoral countries (Bulgaria, Georgia, Russia, Rumania, Turkey, Ukraine) reasserted their interest in these waters. Of prime importance to the Black Sea economy is the transportation of cargo, locally and as part of the ancient Silk Route, and the production and transportation of oil. The need to transport oil has driven the recent expansion of the existing ports and there are plans for new ports to be built. There are many industrial and military sites located around the Black Sea. Moreover, the Black Sea was, in the recent past, an important resort and holiday destination - a fact which must not be lost sight of. While this role diminished throughout the 1990s, the Black Sea resorts and recreational areas have once again begun to attract tourists. The international Black Sea Economic Cooperation Area (BSEC), comprising the six littoral States and Azerbaijan, Albania, Armenia, Greece and Moldova, was set up in 1992 to exert some control over these complex economic issues. All these circumstances give support to the conclusion that a new approach to Black Sea issues is necessary, one which will entail meticulous study of the sea’s biology, all the more urgent now as human life has more and more negative impact on the already poor ecological condition of the sea. This new raft of work will attempt to quantify the amount of river discharge — water and load — disgorging into the Black Sea. Much is expected from a study at this level. The aggregate amount of fresh water entering the sea is still known only approximately; precise information is long overdue. New data from hydrometric observations and research over recent years has enabled more precise figures to be calculated for the amount of river water entering the Black Sea; these calculations have included the effect of artificial control of the flow. River load is the factor least studied, in the Black Sea as in other regions. There are other associated issues here, too, such as erosion of riverbanks, artificial beach formation, pollution of the sea etc. These issues are particularly topical now, when shoreline retreat, caused by a decreasing amount of bank-forming deposits, has become irreversible, and are played out against a background of observable increase in the ocean levels worldwide, with pollution in the Black Sea already reaching threatening level. Accurate quantitative assessments of river load reaching the sea are also necessary for any proper research into current sediment formation processes on the sea bottom. It must also be remembered that the virtually locked water basin of the Black Sea is many ways similar to an ocean, especially in the relation between river load distribution and deposition. Given its more favourable conditions and the less extensive scope of work involved, the Black Sea can be regarded as a natural laboratory (110). In recent years, with ‘new times’ entering the political situation, the spirit of new times has entered the Black Sea research arena, too, and investigations have become international in character. A Black Sea Regional Committee (BSRC) was set up in 1996 under Unesco’s Intergovernmental Oceanographic Commission, tasked with coordinating and intensifying scientific research on the Black Sea. One of its key projects (pilot project 2: Black Sea sediment fluxes) conducts research into flows of river load into the sea, and our document is part of this project.

Library Staff Only: edit this record