Journal
RUSSIAN METEOROLOGY AND HYDROLOGY
Volume 44, Issue 4, Pages 283-290Publisher
PLEIADES PUBLISHING INC
DOI: 10.3103/S1068373919040083
Keywords
Central Yamal; cryogenic processes; gas emission crater; thermocirque; seasonal thaw depth; ground temperature
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Funding
- Russian Science Foundation [16-17-10203]
- Arktika Interregional Expedition Center
- Russian Center for Arctic Development
- Russian Science Foundation [16-17-10203] Funding Source: Russian Science Foundation
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Various climatic parameters (average annual, winter, and summer air temperature, winter and summer total precipitation) and their temporal variability are analyzed to explain the activation of cryogenic processes in Central Yamal. The effect of fluctuations of these parameters on the thaw depth and ground temperature is analyzed. The regression analysis is carried out to reconstruct ground temperature during earlier periods of time in the years preceding the activation of thermal denudation and the formation of gas emission craters.
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