Permafrost Early Deformation Signals before the Norilsk Oil Tank Collapse in Russia

Despite the profound roles of surface deformation monitoring techniques in observing permafrost surface stability, predetermining the approximate location and time of possibly occurring severe permafrost degradation before applying these techniques is extremely necessary, but has received little att...

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Published in:Remote Sensing
Main Authors: Peng Zhang, Yan Chen, Youhua Ran, Yunping Chen
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
Subjects:
Online Access:https://doi.org/10.3390/rs14195036
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spelling ftmdpi:oai:mdpi.com:/2072-4292/14/19/5036/ 2023-08-20T04:08:07+02:00 Permafrost Early Deformation Signals before the Norilsk Oil Tank Collapse in Russia Peng Zhang Yan Chen Youhua Ran Yunping Chen agris 2022-10-09 application/pdf https://doi.org/10.3390/rs14195036 EN eng Multidisciplinary Digital Publishing Institute Environmental Remote Sensing https://dx.doi.org/10.3390/rs14195036 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 14; Issue 19; Pages: 5036 permafrost degradation deformation SBAS-InSAR early warning Text 2022 ftmdpi https://doi.org/10.3390/rs14195036 2023-08-01T06:48:30Z Despite the profound roles of surface deformation monitoring techniques in observing permafrost surface stability, predetermining the approximate location and time of possibly occurring severe permafrost degradation before applying these techniques is extremely necessary, but has received little attention. Taking the oil tank collapse accident in the Norilsk region as a case, we explored this concern by analyzing the permafrost deformation mechanisms and determining early surface deformation signals. Regarding this case, we firstly applied the Small Baseline Subset Interferometric Synthetic Aperture Radar (SBAS-InSAR) technique to obtain its permafrost surface deformation rate, then utilized a sine model to decompose its interannual deformation and seasonal deformation, and finally compared the relationship between the topographic slope and deformation rate. Based on experimental results, we reveal that when the annual average temperature continuously increases at a rate of 2 °C/year for 2∼3 consecutive years, permafrost areas with relatively large topographic slopes (>15°) are more prone to severe surface deformation during the summer thaw period. Therefore, this paper suggests that permafrost areas with large topographic slopes (>15°) should be taken as the key surveillance areas, and that the appropriate monitoring time for employing surface deformation monitoring techniques should be the summer thawing period after a continuous increase in annual average temperature at a rate of 2 °C/year for 2∼3 years. Text norilsk permafrost MDPI Open Access Publishing Norilsk ENVELOPE(88.203,88.203,69.354,69.354) Remote Sensing 14 19 5036
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic permafrost degradation
deformation
SBAS-InSAR
early warning
spellingShingle permafrost degradation
deformation
SBAS-InSAR
early warning
Peng Zhang
Yan Chen
Youhua Ran
Yunping Chen
Permafrost Early Deformation Signals before the Norilsk Oil Tank Collapse in Russia
topic_facet permafrost degradation
deformation
SBAS-InSAR
early warning
description Despite the profound roles of surface deformation monitoring techniques in observing permafrost surface stability, predetermining the approximate location and time of possibly occurring severe permafrost degradation before applying these techniques is extremely necessary, but has received little attention. Taking the oil tank collapse accident in the Norilsk region as a case, we explored this concern by analyzing the permafrost deformation mechanisms and determining early surface deformation signals. Regarding this case, we firstly applied the Small Baseline Subset Interferometric Synthetic Aperture Radar (SBAS-InSAR) technique to obtain its permafrost surface deformation rate, then utilized a sine model to decompose its interannual deformation and seasonal deformation, and finally compared the relationship between the topographic slope and deformation rate. Based on experimental results, we reveal that when the annual average temperature continuously increases at a rate of 2 °C/year for 2∼3 consecutive years, permafrost areas with relatively large topographic slopes (>15°) are more prone to severe surface deformation during the summer thaw period. Therefore, this paper suggests that permafrost areas with large topographic slopes (>15°) should be taken as the key surveillance areas, and that the appropriate monitoring time for employing surface deformation monitoring techniques should be the summer thawing period after a continuous increase in annual average temperature at a rate of 2 °C/year for 2∼3 years.
format Text
author Peng Zhang
Yan Chen
Youhua Ran
Yunping Chen
author_facet Peng Zhang
Yan Chen
Youhua Ran
Yunping Chen
author_sort Peng Zhang
title Permafrost Early Deformation Signals before the Norilsk Oil Tank Collapse in Russia
title_short Permafrost Early Deformation Signals before the Norilsk Oil Tank Collapse in Russia
title_full Permafrost Early Deformation Signals before the Norilsk Oil Tank Collapse in Russia
title_fullStr Permafrost Early Deformation Signals before the Norilsk Oil Tank Collapse in Russia
title_full_unstemmed Permafrost Early Deformation Signals before the Norilsk Oil Tank Collapse in Russia
title_sort permafrost early deformation signals before the norilsk oil tank collapse in russia
publisher Multidisciplinary Digital Publishing Institute
publishDate 2022
url https://doi.org/10.3390/rs14195036
op_coverage agris
long_lat ENVELOPE(88.203,88.203,69.354,69.354)
geographic Norilsk
geographic_facet Norilsk
genre norilsk
permafrost
genre_facet norilsk
permafrost
op_source Remote Sensing; Volume 14; Issue 19; Pages: 5036
op_relation Environmental Remote Sensing
https://dx.doi.org/10.3390/rs14195036
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs14195036
container_title Remote Sensing
container_volume 14
container_issue 19
container_start_page 5036
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