Experimental studies of the deep turbid layer in the Black Sea
Data compiled in the course of hydro-optical studies are reported. The main interest is focused on the problem of the existence of a deep turbid layer (DTL) over the continental slope, where it is better pronounced than in the central Black Sea. Analysis of the collected data allows a supposition as to the relationship between the DTL structure and the peculiarities of water dynamics.
KeywordsClimate Change Experimental Study Environmental Physic Continental Slope Main Interest
Unable to display preview. Download preview PDF.
- 1.Voskresensky, V.N., Krasheninnikov, B.N. and Prokhorenko, Yu.A., Determination of the upper boundary of the anoxic zone by the vertical profile of the light attenuation index of a hydrogen medium. In:Improvement of the Recreational System Management. Deposit. Manuscript No. 5804 B-87. Part 2. Moscow: VINITI (1987), pp. 282–293.Google Scholar
- 2.Neuymin, G.G. Optical studies of Black Sea waters.Proc. All-Union Symp. on the Black Sea and Mediterranean Sea, 1973. Kiev: Naukova Dumka (1973), pp. 81–88.Google Scholar
- 3.Neuymin, G.G. A steady, deep turbid layer in the Black Sea.Morsk. Gidrofiz. Issled. (1970) No. 1, 178–191.Google Scholar
- 4.Ovchinnikov, I.M. and Titov, V.B., The anticyclonic vorticity of currents in the Black Sea coastal zone.Dokl. Akad. Nauk SSSR (1990)314, 1236–1239.Google Scholar