Long‐term changes in the ground thermal regime of an artificially drained thaw‐lake basin in the Russian European north

• Published in: Permafrost and Periglacial Processes
• Main Authors: Kaverin, Dmitry A., Melnichuk, Evgeniy B., Shiklomanov, Nikolay I., Kakunov, Nikolay B., Pastukhov, Alexander V., Shiklomanov, Alexey N.
• Other Authors: Western History Association, University of Alaska Fairbanks, George Washington University, National Aeronautics and Space Administration, Boston University, Russian Science Foundation
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2017
• Subjects: Pechora; permafrost; Permafrost and Periglacial Processes; Tundra
• Online Access: http://dx.doi.org/10.1002/ppp.1963; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.1963; https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.1963; https://onlinelibrary.wiley.com/doi/full-xml/10.1002/ppp.1963

Abstract Long‐term (1982–1995) observations of the ground thermal regime of a drained thaw‐lake basin in the Pechora Lowlands of the Russian European north revealed a high spatial and temporal variability in the ground temperature response to artificial drainage. The thermal response was controlled by the atmospheric climate and by evolution of the landsurface following drainage. Observed changes in permafrost conditions were related to three climatic subperiods identified from air and ground temperature trends. The first (1982–1984) was characterized by gradual ground cooling associated with partial formation of permafrost patches under the initial stage of formation of marshy meadows. The second (1985–1987) involved strong ground cooling, resulting in the formation of a subsurface permafrost layer beneath most of the basin. The third (1988–1995) was marked by a gradual increase in annual mean ground temperature, promoting partial permafrost degradation under marshy meadows and willow stands. Initially, newly aggraded permafrost remained under peat mounds and tundra meadows. The spatial pattern of permafrost change can be attributed to heterogeneous landsurface evolution and variable snow thickness. Four distinct ground temperature regimes are distinguished: (i) thawed ground, (ii) deep permafrost, (iii) unstable permafrost and (iv) stable permafrost.