Brief communication: Alternation of thaw zones and deep permafrost in the cold climate conditions of the East Siberian Mountains, Suntar-Khayata Range
The Suntar-Khayata Range includes numerous natural phenomena interacting with 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 for the temperature monitoring of the topm...
Published in: | The Cryosphere |
---|---|
Main Authors: | , , , , |
Format: | Text |
Language: | English |
Published: |
2023
|
Subjects: | |
Online Access: | https://doi.org/10.5194/tc-17-4601-2023 https://tc.copernicus.org/articles/17/4601/2023/ |
id |
ftcopernicus:oai:publications.copernicus.org:tc108954 |
---|---|
record_format |
openpolar |
spelling |
ftcopernicus:oai:publications.copernicus.org:tc108954 2024-09-15T18:29:32+00:00 Brief communication: Alternation of thaw zones and deep permafrost in the cold climate conditions of the East Siberian Mountains, Suntar-Khayata Range Sysolyatin, Robert Serikov, Sergei Kirillin, Anatoly Litovko, Andrey Sivtsev, Maxim 2023-11-03 application/pdf https://doi.org/10.5194/tc-17-4601-2023 https://tc.copernicus.org/articles/17/4601/2023/ eng eng doi:10.5194/tc-17-4601-2023 https://tc.copernicus.org/articles/17/4601/2023/ eISSN: 1994-0424 Text 2023 ftcopernicus https://doi.org/10.5194/tc-17-4601-2023 2024-08-28T05:24:15Z The Suntar-Khayata Range includes numerous natural phenomena interacting with 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 for the temperature monitoring of the topmost 15 m and measurements of a deep permafrost temperature profile in July 2010. The temperature curvature in the upper part has a bend, which is consistent with the upper portion justified 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 the thaw zone's temperature regime. The temperatures down to 6.7 m deep have been monitored at 5 min intervals during heavy rainfall, and the temperature readings have behaved quite peculiarly. The thickness of the seasonal freezing layer reaches 5.7 m; moreover the ground temperature increases to 6 ∘ C at 6.7 m depth by groundwater heat transfer. This study provides some new insights into the permafrost condition at one of the coldest places in the Northern Hemisphere. Text permafrost Copernicus Publications: E-Journals The Cryosphere 17 11 4601 4608 |
institution |
Open Polar |
collection |
Copernicus Publications: E-Journals |
op_collection_id |
ftcopernicus |
language |
English |
description |
The Suntar-Khayata Range includes numerous natural phenomena interacting with 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 for the temperature monitoring of the topmost 15 m and measurements of a deep permafrost temperature profile in July 2010. The temperature curvature in the upper part has a bend, which is consistent with the upper portion justified 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 the thaw zone's temperature regime. The temperatures down to 6.7 m deep have been monitored at 5 min intervals during heavy rainfall, and the temperature readings have behaved quite peculiarly. The thickness of the seasonal freezing layer reaches 5.7 m; moreover the ground temperature increases to 6 ∘ C at 6.7 m depth by groundwater heat transfer. This study provides some new insights into the permafrost condition at one of the coldest places in the Northern Hemisphere. |
format |
Text |
author |
Sysolyatin, Robert Serikov, Sergei Kirillin, Anatoly Litovko, Andrey Sivtsev, Maxim |
spellingShingle |
Sysolyatin, Robert Serikov, Sergei Kirillin, Anatoly Litovko, Andrey Sivtsev, Maxim Brief communication: Alternation of thaw zones and deep permafrost in the cold climate conditions of the East Siberian Mountains, Suntar-Khayata Range |
author_facet |
Sysolyatin, Robert Serikov, Sergei Kirillin, Anatoly Litovko, Andrey Sivtsev, Maxim |
author_sort |
Sysolyatin, Robert |
title |
Brief communication: Alternation of thaw zones and deep permafrost in the cold climate conditions of the East Siberian Mountains, Suntar-Khayata Range |
title_short |
Brief communication: Alternation of thaw zones and deep permafrost in the cold climate conditions of the East Siberian Mountains, Suntar-Khayata Range |
title_full |
Brief communication: Alternation of thaw zones and deep permafrost in the cold climate conditions of the East Siberian Mountains, Suntar-Khayata Range |
title_fullStr |
Brief communication: Alternation of thaw zones and deep permafrost in the cold climate conditions of the East Siberian Mountains, Suntar-Khayata Range |
title_full_unstemmed |
Brief communication: Alternation of thaw zones and deep permafrost in the cold climate conditions of the East Siberian Mountains, Suntar-Khayata Range |
title_sort |
brief communication: alternation of thaw zones and deep permafrost in the cold climate conditions of the east siberian mountains, suntar-khayata range |
publishDate |
2023 |
url |
https://doi.org/10.5194/tc-17-4601-2023 https://tc.copernicus.org/articles/17/4601/2023/ |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
eISSN: 1994-0424 |
op_relation |
doi:10.5194/tc-17-4601-2023 https://tc.copernicus.org/articles/17/4601/2023/ |
op_doi |
https://doi.org/10.5194/tc-17-4601-2023 |
container_title |
The Cryosphere |
container_volume |
17 |
container_issue |
11 |
container_start_page |
4601 |
op_container_end_page |
4608 |
_version_ |
1810470939395096576 |