Lykhodedova, Olha H.Konikov, Yevhenii G.2014-03-222014-03-222007Black Sea-Mediterranean corridor during the last 30 ky: sea level change and human adaptation (2005–2009) : joint meeting and field trip, IGCP 521 (Gelendzhik; Kerch, 8–17 Sept., 2007). – Moscow : Rosselkhozakademiya Printing House, 2007https://dspace.onu.edu.ua/handle/123456789/4727Black Sea-Mediterranean corridor during the last 30 ky: sea level change and human adaptation (2005-2009) joint meeting and field trip, IGCP 521 (2007), Gelendzhik; Kerch Extended abstracts, 8-17 Sept., 2007 / Black Sea-Mediterranean corridor during the last 30 ky: sea level change and human adaptation (2005-2009) joint meeting and field trip, IGCP 521 (2007), Gelendzhik; Kerch ; Dating Caspian Sea level change (2003-2007),joint meeting and field trip IGCP 481 (2007); Gelendzhik; Kerch, RAS, P.P. Shirshov Institute of Oceanology . – Moscow : Rosselkhozakademiya Printing House, 2007 . – XXII, 178 p. : Fig. – (UNESCO-IUGS-IGCP-INQUA) .In actuality, the study of the dynamics of Black Sea level has implications for the development of the coastal zone, as well as economic and ecologic issues. The longest period of instrumental observations of sea-level (Odessa) spans 140 years (beginning in 1876). The majority of investigators hols a view of eustatic character of Black Sea level changes during the period of interest (Fomicheva 1986; Altman 1990). A significant role is attributed to the discharge of freshwater (fluvial, atmospheric precipitation) into the Black Sea. The leading role in this influx is the fluvial water discharge in the northwestern part of the basin - Danube, Dnieper, and Dniester (approximately 85% of the total discharge).enspectral analysisatmospheric circulationdrainage basinArticle