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


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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.

作者简介

N. Blokhina

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

编辑信件的主要联系方式.
Email: blokhinans@gmail.com
俄罗斯联邦, Moscow, 119991

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