VERTICAL THERMAL STRUCTURE AND HEAT EXCHANGE IN ICE COVERED LAKE

In the present study the effect of under ice warming is analyzed on the basis of observed data from the Karelian Isthmus and lakes of Karelia. A simple 1D parameterized mathematical model of the phenomenon was developed. The heat fluxes in the “ice – water column – sediments” system were quantified....

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Bibliographic Details
Published in:Proceedings of the Karelian Research Centre of the Russian Academy of Sciences
Main Authors: Sergey Golosov, Il'ya Zverev, Arkady Terzhevik
Format: Article in Journal/Newspaper
Language:English
Russian
Published: Karelian Research Centre of the Russian Academy of Sciences 2017
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Q
Online Access:https://doi.org/10.17076/lim464
https://doaj.org/article/22ab36a8a7934eb9a22997b0cd71daf3
Description
Summary:In the present study the effect of under ice warming is analyzed on the basis of observed data from the Karelian Isthmus and lakes of Karelia. A simple 1D parameterized mathematical model of the phenomenon was developed. The heat fluxes in the “ice – water column – sediments” system were quantified.