Thaw-Season InSAR Surface Displacements and Frost Susceptibility Mapping to Support Community-Scale Planning in Ilulissat, West Greenland

In permafrost regions, ground surface deformations induced by freezing and thawing threaten the integrity of the built environment. Mapping the frost susceptibility of the ground at a high spatial resolution is of practical importance for the construction and planning sectors. We processed Sentinel-...

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Published in:Remote Sensing
Main Authors: Johanna Scheer, Rafael Caduff, Penelope How, Marco Marcer, Tazio Strozzi, Annett Bartsch, Thomas Ingeman-Nielsen
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Ice
Online Access:https://doi.org/10.3390/rs15133310
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spelling ftmdpi:oai:mdpi.com:/2072-4292/15/13/3310/ 2023-08-20T03:59:06+02:00 Thaw-Season InSAR Surface Displacements and Frost Susceptibility Mapping to Support Community-Scale Planning in Ilulissat, West Greenland Johanna Scheer Rafael Caduff Penelope How Marco Marcer Tazio Strozzi Annett Bartsch Thomas Ingeman-Nielsen agris 2023-06-28 application/pdf https://doi.org/10.3390/rs15133310 EN eng Multidisciplinary Digital Publishing Institute Remote Sensing in Geology, Geomorphology and Hydrology https://dx.doi.org/10.3390/rs15133310 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 15; Issue 13; Pages: 3310 InSAR permafrost active layer Arctic infrastructure ice content Text 2023 ftmdpi https://doi.org/10.3390/rs15133310 2023-08-01T10:39:28Z In permafrost regions, ground surface deformations induced by freezing and thawing threaten the integrity of the built environment. Mapping the frost susceptibility of the ground at a high spatial resolution is of practical importance for the construction and planning sectors. We processed Sentinel-1 Interferometric Synthetic Aperture Radar (InSAR) data from thawing seasons 2015 to 2019, acquired over the area of Ilulissat, West Greenland. We used a least-squares inversion scheme to retrieve the average seasonal displacement (S) and long-term deformation rate (R). We secondly investigated two different methods to extrapolate active layer thickness (ALT) measurements, based on their statistical relationship with remotely sensed surface characteristics. A generalized linear model (GLM) was first implemented, but the model was not able to fit the data and represent the ALT spatial variability over the entire study domain. ALT were alternatively averaged per vegetation class, using a land cover map derived by supervised classification of Sentinel-2 images. We finally estimated the active layer ice content and used it as a proxy to map the frost susceptibility of the ground at the community scale. Fine-grained sedimentary basins in Ilulissat were typically frost susceptible and subject to average seasonal downward displacements of 3 to 8 cm. Areas following a subsiding trend of up to 2.6 cm/yr were likely affected by permafrost degradation and melting of ground ice below the permafrost table. Our approach enabled us to identify frost-susceptible areas subject to severe seasonal deformations, to long-term subsidence induced by degrading permafrost, or to both. Used in combination with traditional site investigations, InSAR maps provide valuable information for risk management and community planning in the Arctic. Text Active layer thickness Arctic Greenland Ice Ilulissat permafrost MDPI Open Access Publishing Arctic Greenland Ilulissat ENVELOPE(-51.099,-51.099,69.220,69.220) Remote Sensing 15 13 3310
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic InSAR
permafrost
active layer
Arctic infrastructure
ice content
spellingShingle InSAR
permafrost
active layer
Arctic infrastructure
ice content
Johanna Scheer
Rafael Caduff
Penelope How
Marco Marcer
Tazio Strozzi
Annett Bartsch
Thomas Ingeman-Nielsen
Thaw-Season InSAR Surface Displacements and Frost Susceptibility Mapping to Support Community-Scale Planning in Ilulissat, West Greenland
topic_facet InSAR
permafrost
active layer
Arctic infrastructure
ice content
description In permafrost regions, ground surface deformations induced by freezing and thawing threaten the integrity of the built environment. Mapping the frost susceptibility of the ground at a high spatial resolution is of practical importance for the construction and planning sectors. We processed Sentinel-1 Interferometric Synthetic Aperture Radar (InSAR) data from thawing seasons 2015 to 2019, acquired over the area of Ilulissat, West Greenland. We used a least-squares inversion scheme to retrieve the average seasonal displacement (S) and long-term deformation rate (R). We secondly investigated two different methods to extrapolate active layer thickness (ALT) measurements, based on their statistical relationship with remotely sensed surface characteristics. A generalized linear model (GLM) was first implemented, but the model was not able to fit the data and represent the ALT spatial variability over the entire study domain. ALT were alternatively averaged per vegetation class, using a land cover map derived by supervised classification of Sentinel-2 images. We finally estimated the active layer ice content and used it as a proxy to map the frost susceptibility of the ground at the community scale. Fine-grained sedimentary basins in Ilulissat were typically frost susceptible and subject to average seasonal downward displacements of 3 to 8 cm. Areas following a subsiding trend of up to 2.6 cm/yr were likely affected by permafrost degradation and melting of ground ice below the permafrost table. Our approach enabled us to identify frost-susceptible areas subject to severe seasonal deformations, to long-term subsidence induced by degrading permafrost, or to both. Used in combination with traditional site investigations, InSAR maps provide valuable information for risk management and community planning in the Arctic.
format Text
author Johanna Scheer
Rafael Caduff
Penelope How
Marco Marcer
Tazio Strozzi
Annett Bartsch
Thomas Ingeman-Nielsen
author_facet Johanna Scheer
Rafael Caduff
Penelope How
Marco Marcer
Tazio Strozzi
Annett Bartsch
Thomas Ingeman-Nielsen
author_sort Johanna Scheer
title Thaw-Season InSAR Surface Displacements and Frost Susceptibility Mapping to Support Community-Scale Planning in Ilulissat, West Greenland
title_short Thaw-Season InSAR Surface Displacements and Frost Susceptibility Mapping to Support Community-Scale Planning in Ilulissat, West Greenland
title_full Thaw-Season InSAR Surface Displacements and Frost Susceptibility Mapping to Support Community-Scale Planning in Ilulissat, West Greenland
title_fullStr Thaw-Season InSAR Surface Displacements and Frost Susceptibility Mapping to Support Community-Scale Planning in Ilulissat, West Greenland
title_full_unstemmed Thaw-Season InSAR Surface Displacements and Frost Susceptibility Mapping to Support Community-Scale Planning in Ilulissat, West Greenland
title_sort thaw-season insar surface displacements and frost susceptibility mapping to support community-scale planning in ilulissat, west greenland
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/rs15133310
op_coverage agris
long_lat ENVELOPE(-51.099,-51.099,69.220,69.220)
geographic Arctic
Greenland
Ilulissat
geographic_facet Arctic
Greenland
Ilulissat
genre Active layer thickness
Arctic
Greenland
Ice
Ilulissat
permafrost
genre_facet Active layer thickness
Arctic
Greenland
Ice
Ilulissat
permafrost
op_source Remote Sensing; Volume 15; Issue 13; Pages: 3310
op_relation Remote Sensing in Geology, Geomorphology and Hydrology
https://dx.doi.org/10.3390/rs15133310
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs15133310
container_title Remote Sensing
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