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INFLUENCE OF FLOW ON THAWING OF UNDERWATER SLOPES AND THE PACE COASTAL EROSION OF RIVERS, OCCURRING IN THE PERMAFROST ZONE permafrost, depending on the soil type, the initial slope, and the slope angle. It was shown by authors

Influence of rift zones and thermokarst lakes on the formation of subaqueous permafrost and the stability zone of methane hydrates of the Laptev Sea shelf in the Pleistocene
of subaqueous permafrost and zones of stability of methane hydrates for conditions of the Laptev Sea shelf

Influence of seasonal conditions on the deformation of coastal slopes, occuring in the permafrost zoneInfluence of seasonal conditions on the deformation of coastal slopes, occuring in the permafrost

Modeling of pollutant transport in streams with riverbeds deformed due to thawing permafrostModeling of pollutant transport in streams with riverbeds deformed due to thawing permafrost

Long-Term Variability of Anatomic Features of Annual Tree Rings of Larch, Pine and Spruce in the Permafrost Zone in Central Siberia of various species to climate change. This is especially significant in the permafrost zone due to likely

Теплотехнический расчет свайного фундамента на вечномерзлых грунтах and degradation of permafrost soils. Studies carried out in the city of Norilsk show that the degradation

Colloids in thermokarst lakes along a permafrost and climate gradient of permafrost peatlands in Western Siberia using in situ dialysis procedure carbon (ОC), and related elements remain poorly known, especially across the permafrost gradient

Numerical research of heat transfer processes at the drilling wells in permafrost rocks and gas wells in permafrost have been carried out. The influence of flow rate, temperature, drilling fluid

Pollen-based holocene thawing-history of permafrost in Northern Asia and its potential impacts on climate changeAs the recent permafrost thawing of northern Asia proceeds due to anthropogenic climate change

Carbon storage and burial in thermokarst lakes of permafrost peatlandsThermokarst (thaw) lakes of the Western Siberian Lowland (WSL), the World´s largest permafrost

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