COASTAL AND ESTUARINE SEDIMENT DYNAMICS IN THE MEZEN BAY AND ESTUARIES MEZEN AND KULOY
Authors:
1.
FBGU «Gosudarstvennyy okeanograficheskiy institut im. N.N. Zubova, (FBGU «GOIN»)
Russian Federation
Russian Federation
Type:
Сonference article
Published:
24.11.2012
Subject area:
CSCSTI 06.01
BISAK NAT010000 Ecology
BISAK NAT045050 Ecosystems & Habitats / Coastal Regions & Shorelines
BISAK NAT025000 Ecosystems & Habitats / Oceans & Seas
BISAK NAT045030 Ecosystems & Habitats / Polar Regions
BISAK SCI081000 Earth Sciences / Hydrology
BISAK SCI092000 Global Warming & Climate Change
BISAK SCI020000 Life Sciences / Ecology
BISAK SCI039000 Life Sciences / Marine Biology
BISAK SOC053000 Regional Studies
BISAK TEC060000 Marine & Naval
BISAK NAT010000 Ecology
BISAK NAT045050 Ecosystems & Habitats / Coastal Regions & Shorelines
BISAK NAT025000 Ecosystems & Habitats / Oceans & Seas
BISAK NAT045030 Ecosystems & Habitats / Polar Regions
BISAK SCI081000 Earth Sciences / Hydrology
BISAK SCI092000 Global Warming & Climate Change
BISAK SCI020000 Life Sciences / Ecology
BISAK SCI039000 Life Sciences / Marine Biology
BISAK SOC053000 Regional Studies
BISAK TEC060000 Marine & Naval
Language:
Russian, English
Keywords:
SEDIMENT DYNAMICS
Abstract (English):
In the Mezen bay and estuaries Mezen and Kuloy can be high concentrations of mud suspension there, involving the formation at times mobile suspensions and settled mud. Within estuaries the river water is mixed with the sea water by the action of tidal motions, by waves on the sea surface and by the river discharge forcing its way to the sea. Nearly all shallow tidal estuaries, where currents exceed about 1,0m s-1 and where sand is present, have sand waves. Sand waves have a variety of cross-sectional and plan forms.
In the Mezen bay and estuaries Mezen and Kuloy can be high concentrations of mud suspension there, involving the formation at times mobile suspensions and settled mud. Within estuaries the river water is mixed with the sea water by the action of tidal motions, by waves on the sea surface and by the river discharge forcing its way to the sea. Nearly all shallow tidal estuaries, where currents exceed about 1,0m s-1 and where sand is present, have sand waves. Sand waves have a variety of cross-sectional and plan forms.
Keywords:
SEDIMENT DYNAMICS
SEDIMENT DYNAMICS
Эрозионно-аккумулятивные процессы в Мезенском заливе обусловлены приливо-отливными течениями, ветровым волнением, формированием вдольберегового потока наносов. Трансформация вдоль берегового потока происходит вследствие абразии берегов, взмучивания донных отложений, аккумуляции наносов в зонах замедления скоростей течений. Важной причиной изменения вдольберегового переноса наносов является поступление взвешенных наносов из устьев рек Мезени и Кулоя.
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