An Assessment of the Possibility of Restoration and Protection of Territories Disturbed by Thermokarst in Central Yakutia, Eastern Siberia

Rapid permafrost degradation is observed in northern regions as a result of climate change and expanding economic development. Associated increases in active layer depth lead to thermokarst development, resulting in irregular surface topography. In Central Yakutia, significant areas of the land surf...

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Published in:Land
Main Authors: Aleksandr Zhirkov, Maksim Sivtsev, Vasylii Lytkin, Anatolii Kirillin, Antoine Séjourné, Zhi Wen
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Ice
Online Access:https://doi.org/10.3390/land12010197
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spelling ftmdpi:oai:mdpi.com:/2073-445X/12/1/197/ 2023-08-20T04:07:06+02:00 An Assessment of the Possibility of Restoration and Protection of Territories Disturbed by Thermokarst in Central Yakutia, Eastern Siberia Aleksandr Zhirkov Maksim Sivtsev Vasylii Lytkin Anatolii Kirillin Antoine Séjourné Zhi Wen agris 2023-01-07 application/pdf https://doi.org/10.3390/land12010197 EN eng Multidisciplinary Digital Publishing Institute Land Systems and Global Change https://dx.doi.org/10.3390/land12010197 https://creativecommons.org/licenses/by/4.0/ Land; Volume 12; Issue 1; Pages: 197 permafrost ice-rich sediments thermokarst yedoma (ice complex) active layer transition layer permafrost degradation transition layer restoration Text 2023 ftmdpi https://doi.org/10.3390/land12010197 2023-08-01T08:10:58Z Rapid permafrost degradation is observed in northern regions as a result of climate change and expanding economic development. Associated increases in active layer depth lead to thermokarst development, resulting in irregular surface topography. In Central Yakutia, significant areas of the land surface have been deteriorated by thermokarst; however, no mitigation or land rehabilitation efforts are undertaken. This paper presents the results of numerical modeling of the thermal response of permafrost to changes in the active layer hydrothermal regime using field data from the village of Amga, Republic of Sakha (Yakutia), and mathematical analysis. The results suggest that restoring a thick ice-enriched layer will require increasing the pre-winter soil moisture contents in order to increase the effective heat capacity of the active layer. Snow removal or compaction during the winter is recommended to maximize permafrost cooling. The thickness of the restored transition layer varies from 0.3 to 1.3 m depending on soil moisture contents in the active layer. The modeling results demonstrate that damaged lands can be restored through a set of measures to lower the subsurface temperatures. A combination of the insulating layer (forest vegetation) and the high heat capacity layer (transition layer) in the atmosphere–ground system would be more effective in providing stable geocryological conditions. Text Ice permafrost Republic of Sakha Sakha Thermokarst Yakutia Siberia MDPI Open Access Publishing Sakha Land 12 1 197
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic permafrost
ice-rich sediments
thermokarst
yedoma (ice complex)
active layer
transition layer
permafrost degradation
transition layer restoration
spellingShingle permafrost
ice-rich sediments
thermokarst
yedoma (ice complex)
active layer
transition layer
permafrost degradation
transition layer restoration
Aleksandr Zhirkov
Maksim Sivtsev
Vasylii Lytkin
Anatolii Kirillin
Antoine Séjourné
Zhi Wen
An Assessment of the Possibility of Restoration and Protection of Territories Disturbed by Thermokarst in Central Yakutia, Eastern Siberia
topic_facet permafrost
ice-rich sediments
thermokarst
yedoma (ice complex)
active layer
transition layer
permafrost degradation
transition layer restoration
description Rapid permafrost degradation is observed in northern regions as a result of climate change and expanding economic development. Associated increases in active layer depth lead to thermokarst development, resulting in irregular surface topography. In Central Yakutia, significant areas of the land surface have been deteriorated by thermokarst; however, no mitigation or land rehabilitation efforts are undertaken. This paper presents the results of numerical modeling of the thermal response of permafrost to changes in the active layer hydrothermal regime using field data from the village of Amga, Republic of Sakha (Yakutia), and mathematical analysis. The results suggest that restoring a thick ice-enriched layer will require increasing the pre-winter soil moisture contents in order to increase the effective heat capacity of the active layer. Snow removal or compaction during the winter is recommended to maximize permafrost cooling. The thickness of the restored transition layer varies from 0.3 to 1.3 m depending on soil moisture contents in the active layer. The modeling results demonstrate that damaged lands can be restored through a set of measures to lower the subsurface temperatures. A combination of the insulating layer (forest vegetation) and the high heat capacity layer (transition layer) in the atmosphere–ground system would be more effective in providing stable geocryological conditions.
format Text
author Aleksandr Zhirkov
Maksim Sivtsev
Vasylii Lytkin
Anatolii Kirillin
Antoine Séjourné
Zhi Wen
author_facet Aleksandr Zhirkov
Maksim Sivtsev
Vasylii Lytkin
Anatolii Kirillin
Antoine Séjourné
Zhi Wen
author_sort Aleksandr Zhirkov
title An Assessment of the Possibility of Restoration and Protection of Territories Disturbed by Thermokarst in Central Yakutia, Eastern Siberia
title_short An Assessment of the Possibility of Restoration and Protection of Territories Disturbed by Thermokarst in Central Yakutia, Eastern Siberia
title_full An Assessment of the Possibility of Restoration and Protection of Territories Disturbed by Thermokarst in Central Yakutia, Eastern Siberia
title_fullStr An Assessment of the Possibility of Restoration and Protection of Territories Disturbed by Thermokarst in Central Yakutia, Eastern Siberia
title_full_unstemmed An Assessment of the Possibility of Restoration and Protection of Territories Disturbed by Thermokarst in Central Yakutia, Eastern Siberia
title_sort assessment of the possibility of restoration and protection of territories disturbed by thermokarst in central yakutia, eastern siberia
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/land12010197
op_coverage agris
geographic Sakha
geographic_facet Sakha
genre Ice
permafrost
Republic of Sakha
Sakha
Thermokarst
Yakutia
Siberia
genre_facet Ice
permafrost
Republic of Sakha
Sakha
Thermokarst
Yakutia
Siberia
op_source Land; Volume 12; Issue 1; Pages: 197
op_relation Land Systems and Global Change
https://dx.doi.org/10.3390/land12010197
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/land12010197
container_title Land
container_volume 12
container_issue 1
container_start_page 197
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