TO A QUESTION ABOUT THERMAL CONVECTION IN THE COASTAL ZONE OF THE CURONIAN LAGOON
Authors:
1.
Baltiyskiy Federal'nyy Universitet im. I. Kanta
2.
Atlanticheskoe otdelenie IO im. P.P. Shirshova RAN
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:
In the given work the circulation
Abstract (English):
In the given work the circulation caused in the various speed of warming up (cooling) of shallow and deep-water zones of pool (the phenomenon of the thermal bar) is simulated. The thermal bar is formed in the spring at heating a coastal part of a reservoir above +4 °C and in the autumn during cooling below\ +4 °C. Conditions of the thermal bar occurrence and dependence of circulation on specificity of warming up above underwater slopes with different biases are shown. Influence of the thermal bar on ecology system of large lagoons as it divides two zones with different characteristics of water that defines spatial distinctions of plankton populations is considered. It is supposed to analyse in the further influence of parameters on arising circulation and to compare results to experimental data.
In the given work the circulation caused in the various speed of warming up (cooling) of shallow and deep-water zones of pool (the phenomenon of the thermal bar) is simulated. The thermal bar is formed in the spring at heating a coastal part of a reservoir above +4 °C and in the autumn during cooling below\ +4 °C. Conditions of the thermal bar occurrence and dependence of circulation on specificity of warming up above underwater slopes with different biases are shown. Influence of the thermal bar on ecology system of large lagoons as it divides two zones with different characteristics of water that defines spatial distinctions of plankton populations is considered. It is supposed to analyse in the further influence of parameters on arising circulation and to compare results to experimental data.
Keywords:
In the given work the circulation
In the given work the circulation
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