Thermal state of soils in the Yenisei Arctic
https://doi.org/10.31242/2618-9712-2021-26-3-43-51
Abstract
Results of the experimental studies of the thermal regime in the upper horizons of the cryolithozone under natural conditions and during the development of the region are presented. The structure of radiation-thermal balance over the surface in different natural sub-zones is demonstrated. The effect of snow, vegetation and ground covers on the formation of thermal regime of the soils of annual heat turnover is evaluated quantitatively. The effect of technogenic impact on the thermal regime of soils is estimated on the basis of mathematical modeling. Results of the prediction of changes in the thermal state of soils caused by the development of the northern taiga, forest-tundra and southern tundra territories are described. The major tasks of geothermal monitoring related to the arrangement of observation stations and testing areas in the regions under development are proposed.
Keywords
Yenisei Arctic,
climate,
radiation balance,
thermal balance,
cryolithozone,
soil temperature,
thickness of the active layer,
forecast of thermal regime
Supporting agencies: The research was carried out within the framework of fundamental prospecting research 1.5.12 (Project No. 4 Thermal field and cryogenic layer in the North-East of Russia. Features of formation and dynamics).
About the Author
P. N. Skryabin
Melnikov Permafrost Institute
Russian Federation
Russian Federation
SKRYABIN, Pavel Nikolayevich, Cand. Sci. (Geography), senior researcher
SB RAS, 36 Merzlotnaya st., Yakutsk 677010
ResearcherID: V-9373-2018, Scopus ID: 6508006475
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For citations:
Skryabin P.N. Thermal state of soils in the Yenisei Arctic. Arctic and Subarctic Natural Resources. 2021;26(3):43-51. (In Russ.) https://doi.org/10.31242/2618-9712-2021-26-3-43-51
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