Changes in the level of the Black Sea (NW Black Sea region) in today's climate change
dc.contributor.author | Lykhodedova, Olha H. | |
dc.date.accessioned | 2012-04-18T09:00:21Z | |
dc.date.available | 2012-04-18T09:00:21Z | |
dc.date.issued | 2011 | |
dc.description | ЗБІРКА ТЕЗ ДОПОВІДЕЙ 7-ї КОНФЕРЕНЦІЇ ТА ПОЛЬОВИХ ЕКСКУРСІЙ ЗА ПРОЕКТОМ INQUA 501 «КАСПІЙСЬКО-ЧОРНОМОРСЬКО-СЕРЕДЗЕМНОМОРСЬКИЙ КОРИДОР УПРОДОВЖ ОСТАННІХ 30 ТИС. РОКІВ: ЗМІНИ РІВНЯ МОРЯ ТА АДАПТАЦІЇ ЛЮДИНИ» (2005-2011)21 -28 серпня, 2011 р., м. Одеса | uk |
dc.description.abstract | Monitoring of the Black Sea level conducted since 1876 showed its drop with a speed 0.14 cm / year in the 20s of the XX century (first period) that was exchanged for its rise with a speed 0.35 cm / year (second period). Accordingly, sea level dropped in average 6.5 cm during first period and rose in 26 cm in course of the second period. The amplitude of sea level change is 37 and 50 cm, respectively. The change of sea level was mainly defined by river discharge, precipitation, evaporation, as well as water exchange with Mediterranean and Azov seas (Альтман, 1990). Changing these parameters in turn is related to changes in both regional and global climatic conditions. | uk |
dc.identifier.citation | Caspian-Black Sea-Mediterranean corridor during last 30 ky: Sealevel change and human adaptive strategies (2005-2011) : VII plenary meeting and field trip INQUA 501 (Odessa, 21–28 August 2011). – Odessa : Astroprint, 2011. | uk |
dc.identifier.uri | https://dspace.onu.edu.ua/handle/123456789/2351 | |
dc.language.iso | en | uk |
dc.publisher | Astroprint | uk |
dc.relation.ispartofseries | ;C.123-127 | |
dc.subject | global temperature | uk |
dc.subject | wavelets | uk |
dc.subject | cyclic recurrence | uk |
dc.subject | sea level | uk |
dc.subject | forecast | uk |
dc.title | Changes in the level of the Black Sea (NW Black Sea region) in today's climate change | uk |
dc.type | Article | uk |
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