MORPHOLOGY AND DYNAMICS OF THE LIMANIC BARRIERS ALONG THE BLACK SEA COAST UNDER ACTIVE ANTROPOGENOUS IMPACT
Authors:
1.
Odesskiy nacional'nyy universitet imeni I.I.Mechnikova, Ukraina
Russian Federation
Russian Federation
Type:
Сonference article
Published:
24.11.2012
Subject area:
GRNTI 06.01 Общие вопросы экономических наук
BISAC NAT010000 Ecology
BISAC NAT045050 Ecosystems & Habitats / Coastal Regions & Shorelines
BISAC NAT025000 Ecosystems & Habitats / Oceans & Seas
BISAC NAT045030 Ecosystems & Habitats / Polar Regions
BISAC SCI081000 Earth Sciences / Hydrology
BISAC SCI092000 Global Warming & Climate Change
BISAC SCI020000 Life Sciences / Ecology
BISAC SCI039000 Life Sciences / Marine Biology
BISAC SOC053000 Regional Studies
BISAC TEC060000 Marine & Naval
BISAC NAT010000 Ecology
BISAC NAT045050 Ecosystems & Habitats / Coastal Regions & Shorelines
BISAC NAT025000 Ecosystems & Habitats / Oceans & Seas
BISAC NAT045030 Ecosystems & Habitats / Polar Regions
BISAC SCI081000 Earth Sciences / Hydrology
BISAC SCI092000 Global Warming & Climate Change
BISAC SCI020000 Life Sciences / Ecology
BISAC SCI039000 Life Sciences / Marine Biology
BISAC SOC053000 Regional Studies
BISAC TEC060000 Marine & Naval
Language:
Russian, English
Keywords:
Typical coastal elements
Abstract (English):
Typical coastal elements of limans and lagoons are barriers, that separate limanic aquatories from a Seas. On limanic shores structure of the Black Sea sand barriers represented three longitudinal landscape “zones”: sea beach (“frontal”), dune-aeolian and limanic (“back of the barrier”). They closely interactive between themselves under influence of lithodynamical exchanges of sediment. General tendency of the barriers dynamics is displacement to Land direction.
Typical coastal elements of limans and lagoons are barriers, that separate limanic aquatories from a Seas. On limanic shores structure of the Black Sea sand barriers represented three longitudinal landscape “zones”: sea beach (“frontal”), dune-aeolian and limanic (“back of the barrier”). They closely interactive between themselves under influence of lithodynamical exchanges of sediment. General tendency of the barriers dynamics is displacement to Land direction.
Keywords:
Typical coastal elements
Typical coastal elements
Важным индикатором состояния береговой зоны в пределах любой литодинамической ячейки является морфология пересыпей, ее изменчивость. Как ранее уже было установлено [2], в структуре пересыпи выделяется три элемента (морской пляж, эоловая и лиманная зоны), которые взаимосвязаны и развиваются в неразрывной связи друг с другом.
1. Vyhovanec G.V. Eolovyy process na morskom beregu. Odessa : Astroprint, 2004. 368 s.
2. Shuyskiy Yu.D., Vyhovanec G.V. Ekzogennye processy razvitiya beregov v severo-zapadnoy chasti Chernogo morya. M. : Nedra, 1989. 198 s.
3. Shuyskiy Yu.D., Vyhovanec G.V. Priroda Prichernomorskih limanov. Odessa : Astroprint, 2011. 276 s.
