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 ben nye sienna powder 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-insulating properties.But, with th