Brief communication: Alternation of thaw zones and deeppermafrost in the cold climate conditions of the East SiberianMountains, Suntar-Khayata Range

The Suntar-Khayata Range include numerous natural phenomena interacting or depending on permafrost conditions. Here, we examine some patterns of deep permafrost and talik zones on adjacent sites. A 210 m deep borehole in siltstone bedrock was equipped in July 2010 for temperature monitoring of the t...

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Main Authors: Sysolyatin, Robert, Serikov, Sergei, Kirillin, Anatoly, Litovko, Andrey, Sivtcev, Maxim
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2023-49
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-49/
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spelling ftcopernicus:oai:publications.copernicus.org:egusphere108954 2023-05-15T17:56:30+02:00 Brief communication: Alternation of thaw zones and deeppermafrost in the cold climate conditions of the East SiberianMountains, Suntar-Khayata Range Sysolyatin, Robert Serikov, Sergei Kirillin, Anatoly Litovko, Andrey Sivtcev, Maxim 2023-03-20 application/pdf https://doi.org/10.5194/egusphere-2023-49 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-49/ eng eng doi:10.5194/egusphere-2023-49 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-49/ eISSN: Text 2023 ftcopernicus https://doi.org/10.5194/egusphere-2023-49 2023-03-27T16:23:13Z The Suntar-Khayata Range include numerous natural phenomena interacting or depending on permafrost conditions. Here, we examine some patterns of deep permafrost and talik zones on adjacent sites. A 210 m deep borehole in siltstone bedrock was equipped in July 2010 for temperature monitoring of the topmost 15 m and measurements of a deep permafrost temperature profile. The temperature curvature in the upper part has a bend which is consistent with at upper portion justify by climate warming and shows a steady-state linear geothermal profile below 85 m depth with a high geothermal heat flux. A shallow borehole situated at the river floodplain was used to investigate thaw zones temperature regime. Temperatures down to 6.7 m has been monitored at 5-min intervals during heavy rainfall and has had quite peculiar way. The thickness of the season freezing layer reach to 5.7 m, moreover ground temperature increases to 6 °C at 6.7 m depth by groundwater heat transfer. This study provides some new insight on the permafrost condition at one of the coldest places of Northern Hemisphere. Text permafrost Copernicus Publications: E-Journals Suntar ENVELOPE(141.502,141.502,63.318,63.318) Talik ENVELOPE(146.601,146.601,59.667,59.667)
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The Suntar-Khayata Range include numerous natural phenomena interacting or depending on permafrost conditions. Here, we examine some patterns of deep permafrost and talik zones on adjacent sites. A 210 m deep borehole in siltstone bedrock was equipped in July 2010 for temperature monitoring of the topmost 15 m and measurements of a deep permafrost temperature profile. The temperature curvature in the upper part has a bend which is consistent with at upper portion justify by climate warming and shows a steady-state linear geothermal profile below 85 m depth with a high geothermal heat flux. A shallow borehole situated at the river floodplain was used to investigate thaw zones temperature regime. Temperatures down to 6.7 m has been monitored at 5-min intervals during heavy rainfall and has had quite peculiar way. The thickness of the season freezing layer reach to 5.7 m, moreover ground temperature increases to 6 °C at 6.7 m depth by groundwater heat transfer. This study provides some new insight on the permafrost condition at one of the coldest places of Northern Hemisphere.
format Text
author Sysolyatin, Robert
Serikov, Sergei
Kirillin, Anatoly
Litovko, Andrey
Sivtcev, Maxim
spellingShingle Sysolyatin, Robert
Serikov, Sergei
Kirillin, Anatoly
Litovko, Andrey
Sivtcev, Maxim
Brief communication: Alternation of thaw zones and deeppermafrost in the cold climate conditions of the East SiberianMountains, Suntar-Khayata Range
author_facet Sysolyatin, Robert
Serikov, Sergei
Kirillin, Anatoly
Litovko, Andrey
Sivtcev, Maxim
author_sort Sysolyatin, Robert
title Brief communication: Alternation of thaw zones and deeppermafrost in the cold climate conditions of the East SiberianMountains, Suntar-Khayata Range
title_short Brief communication: Alternation of thaw zones and deeppermafrost in the cold climate conditions of the East SiberianMountains, Suntar-Khayata Range
title_full Brief communication: Alternation of thaw zones and deeppermafrost in the cold climate conditions of the East SiberianMountains, Suntar-Khayata Range
title_fullStr Brief communication: Alternation of thaw zones and deeppermafrost in the cold climate conditions of the East SiberianMountains, Suntar-Khayata Range
title_full_unstemmed Brief communication: Alternation of thaw zones and deeppermafrost in the cold climate conditions of the East SiberianMountains, Suntar-Khayata Range
title_sort brief communication: alternation of thaw zones and deeppermafrost in the cold climate conditions of the east siberianmountains, suntar-khayata range
publishDate 2023
url https://doi.org/10.5194/egusphere-2023-49
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-49/
long_lat ENVELOPE(141.502,141.502,63.318,63.318)
ENVELOPE(146.601,146.601,59.667,59.667)
geographic Suntar
Talik
geographic_facet Suntar
Talik
genre permafrost
genre_facet permafrost
op_source eISSN:
op_relation doi:10.5194/egusphere-2023-49
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-49/
op_doi https://doi.org/10.5194/egusphere-2023-49
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