Effect of ice formation in crevasses to the temperature field in the cold layer of glacier

The work focuses on modeling the warming of a glacier due to heat release during the refreezing of meltwater in glacier crevasses (cryo-hydrologic warming). The simulation is performed for a polythermal Arctic glacier with a regular network of crevasses filled with water at 0 °C, for the1-year perio...

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Bibliographic Details
Main Authors: G. A. Chernyakov, R. A. Chernov
Format: Article
Language:Russian
Published: Nauka 2023-01-01
Series:Лëд и снег
Subjects:
Online Access:https://ice-snow.igras.ru/jour/article/view/1084
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