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Generation of thermal convection in the moss-snow layer on the coast of the Gulf of Grenfjord (West Svalbard)

The significant part of the Arctic soils is covered by vegetation all year round, to which a layer of snow is added in winter. Both layers have a similar structure, consisting of a skeleton (organic and ice, respectively) and air-saturated pores, and, thus, form a unified system with high heat-insul...

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Hlavní autoři: P. V. Bogorodskiy, V. Yu. Kustov, V. V. Movchan, K. A. Ermokhina
Médium: Artigo
Jazyk:Russo
Vydáno: Nauka 2021-05-01
Edice:Лëд и снег
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On-line přístup:https://ice-snow.igras.ru/jour/article/view/891
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