Monitoring the Permafrost Conditions along Pipeline Routes in Central Yakutia, Russia

Pipelines are critical infrastructure for Yakutia, transporting vital supplies to communities in this vast northern region. The pipeline routes in central Yakutia traverse areas of ice-rich permafrost that is sensitive to temperature changes. This study examined the thermal state of permafrost in un...

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Published in:Land
Main Authors: Stepan Varlamov, Pavel Skryabin, Aleksandr Zhirkov, Zhi Wen
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
Subjects:
Ice
Online Access:https://doi.org/10.3390/land11122331
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spelling ftmdpi:oai:mdpi.com:/2073-445X/11/12/2331/ 2023-08-20T03:59:05+02:00 Monitoring the Permafrost Conditions along Pipeline Routes in Central Yakutia, Russia Stepan Varlamov Pavel Skryabin Aleksandr Zhirkov Zhi Wen agris 2022-12-19 application/pdf https://doi.org/10.3390/land11122331 EN eng Multidisciplinary Digital Publishing Institute Land Systems and Global Change https://dx.doi.org/10.3390/land11122331 https://creativecommons.org/licenses/by/4.0/ Land; Volume 11; Issue 12; Pages: 2331 permafrost ground temperature active layer thickness monitoring pipeline climate change anthropogenic effects Text 2022 ftmdpi https://doi.org/10.3390/land11122331 2023-08-01T07:52:29Z Pipelines are critical infrastructure for Yakutia, transporting vital supplies to communities in this vast northern region. The pipeline routes in central Yakutia traverse areas of ice-rich permafrost that is sensitive to temperature changes. This study examined the thermal state of permafrost in undisturbed and disturbed settings along the Lena River to Mundulakh Reservoir water pipeline and the Mastakh to Yakutsk gas pipeline and considered the effects of climatic fluctuations and surface disturbances (forest removal and wildfire) over the monitoring periods of 28 and 18 years, respectively. The geocryological conditions in the study area, as well as the methods of permafrost thermal monitoring, are described. The observation results demonstrated significant increases in the mean annual ground temperature in the upper permafrost layers, as well as in the active-layer thickness following fire and post-fire clearing. At some sites, progressive deepening of the active layer caused the formation of taliks and reached the top of massive ground ice, initiating permafrost degradation. The development of extreme ground temperatures in the layer of annual temperature fluctuations was analyzed according to the combination of seasonal and annual meteorological conditions and the type of anthropogenic impact. The research results can be extrapolated to similar anthropogenic landscapes. Text Active layer thickness Ice lena river permafrost Yakutia Yakutsk MDPI Open Access Publishing Yakutsk Land 11 12 2331
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic permafrost
ground temperature
active layer thickness
monitoring
pipeline
climate change
anthropogenic effects
spellingShingle permafrost
ground temperature
active layer thickness
monitoring
pipeline
climate change
anthropogenic effects
Stepan Varlamov
Pavel Skryabin
Aleksandr Zhirkov
Zhi Wen
Monitoring the Permafrost Conditions along Pipeline Routes in Central Yakutia, Russia
topic_facet permafrost
ground temperature
active layer thickness
monitoring
pipeline
climate change
anthropogenic effects
description Pipelines are critical infrastructure for Yakutia, transporting vital supplies to communities in this vast northern region. The pipeline routes in central Yakutia traverse areas of ice-rich permafrost that is sensitive to temperature changes. This study examined the thermal state of permafrost in undisturbed and disturbed settings along the Lena River to Mundulakh Reservoir water pipeline and the Mastakh to Yakutsk gas pipeline and considered the effects of climatic fluctuations and surface disturbances (forest removal and wildfire) over the monitoring periods of 28 and 18 years, respectively. The geocryological conditions in the study area, as well as the methods of permafrost thermal monitoring, are described. The observation results demonstrated significant increases in the mean annual ground temperature in the upper permafrost layers, as well as in the active-layer thickness following fire and post-fire clearing. At some sites, progressive deepening of the active layer caused the formation of taliks and reached the top of massive ground ice, initiating permafrost degradation. The development of extreme ground temperatures in the layer of annual temperature fluctuations was analyzed according to the combination of seasonal and annual meteorological conditions and the type of anthropogenic impact. The research results can be extrapolated to similar anthropogenic landscapes.
format Text
author Stepan Varlamov
Pavel Skryabin
Aleksandr Zhirkov
Zhi Wen
author_facet Stepan Varlamov
Pavel Skryabin
Aleksandr Zhirkov
Zhi Wen
author_sort Stepan Varlamov
title Monitoring the Permafrost Conditions along Pipeline Routes in Central Yakutia, Russia
title_short Monitoring the Permafrost Conditions along Pipeline Routes in Central Yakutia, Russia
title_full Monitoring the Permafrost Conditions along Pipeline Routes in Central Yakutia, Russia
title_fullStr Monitoring the Permafrost Conditions along Pipeline Routes in Central Yakutia, Russia
title_full_unstemmed Monitoring the Permafrost Conditions along Pipeline Routes in Central Yakutia, Russia
title_sort monitoring the permafrost conditions along pipeline routes in central yakutia, russia
publisher Multidisciplinary Digital Publishing Institute
publishDate 2022
url https://doi.org/10.3390/land11122331
op_coverage agris
geographic Yakutsk
geographic_facet Yakutsk
genre Active layer thickness
Ice
lena river
permafrost
Yakutia
Yakutsk
genre_facet Active layer thickness
Ice
lena river
permafrost
Yakutia
Yakutsk
op_source Land; Volume 11; Issue 12; Pages: 2331
op_relation Land Systems and Global Change
https://dx.doi.org/10.3390/land11122331
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/land11122331
container_title Land
container_volume 11
container_issue 12
container_start_page 2331
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