Features of thermal bar and current development in a deep lake in spring


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Resumo

Features of thermal bar development in a fresh water reservoir during ice cover melting are investigated by means of mathematical modeling. It is shown that the presence of water with the temperature of maximum density (4°C) leads to two opposite effects. On the one hand, a thermal bar forms near the shore and moves to the center of the water basin; on the other hand, an eddy arises near the ice edge, which slows down the process.

Sobre autores

N. Blokhina

Faculty of Physics, Department of the Physics of Sea and Inland Waters

Autor responsável pela correspondência
Email: blokhinans@gmail.com
Rússia, Moscow, 119991

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