Mapping Retrogressive Thaw Slumps Using Single-Pass TanDEM-X Observations ...
Vast areas of the Arctic host ice-rich permafrost, which is becoming increasingly vulnerable to terrain-altering thermokarst in a warming climate. Among the most rapid and dramatic changes are retrogressive thaw slumps. These slumps evolve by a retreat of the slump headwall during the summer months,...
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Online Access: | https://dx.doi.org/10.3929/ethz-b-000426695 http://hdl.handle.net/20.500.11850/426695 |
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ftdatacite:10.3929/ethz-b-000426695 2024-04-28T08:10:44+00:00 Mapping Retrogressive Thaw Slumps Using Single-Pass TanDEM-X Observations ... Bernhard, Philipp Zwieback, Simon Leinss, Silvan Hajnsek, Irena 2020 application/pdf https://dx.doi.org/10.3929/ethz-b-000426695 http://hdl.handle.net/20.500.11850/426695 en eng ETH Zurich info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Abrupt thaw Banks island Digital elevation model DEM differencing DEM generation Interferometry Mackenzie river delta Permafrost Remote sensing Retrogressive thaw slumps RTSs Single-pass radar interferometry Synthetic aperture radar SAR Thermokarst article-journal Text ScholarlyArticle Journal Article 2020 ftdatacite https://doi.org/10.3929/ethz-b-000426695 2024-04-02T12:34:54Z Vast areas of the Arctic host ice-rich permafrost, which is becoming increasingly vulnerable to terrain-altering thermokarst in a warming climate. Among the most rapid and dramatic changes are retrogressive thaw slumps. These slumps evolve by a retreat of the slump headwall during the summer months, making them detectable by comparing digital elevation models over time using the volumetric change as an indicator. Here, we present and assess a method to detect and monitor thaw slumps using time series of elevation models applied on two contrasting study areas in Northern Canada. Our two-step method is tailored to single-pass InSAR observations from the TanDEM-X satellite pair, which have been acquired since 2011. For each acquisition, we derive a digital elevation model and uncertainty estimates. In the first step, we difference digital elevation models and detect the significant elevation changes using a blob-detection algorithm. In the second step, we classify the detections into those due to thaw slumps ... : IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 13 ... Article in Journal/Newspaper Arctic Banks Island Ice Mackenzie river permafrost Thermokarst DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Abrupt thaw Banks island Digital elevation model DEM differencing DEM generation Interferometry Mackenzie river delta Permafrost Remote sensing Retrogressive thaw slumps RTSs Single-pass radar interferometry Synthetic aperture radar SAR Thermokarst |
spellingShingle |
Abrupt thaw Banks island Digital elevation model DEM differencing DEM generation Interferometry Mackenzie river delta Permafrost Remote sensing Retrogressive thaw slumps RTSs Single-pass radar interferometry Synthetic aperture radar SAR Thermokarst Bernhard, Philipp Zwieback, Simon Leinss, Silvan Hajnsek, Irena Mapping Retrogressive Thaw Slumps Using Single-Pass TanDEM-X Observations ... |
topic_facet |
Abrupt thaw Banks island Digital elevation model DEM differencing DEM generation Interferometry Mackenzie river delta Permafrost Remote sensing Retrogressive thaw slumps RTSs Single-pass radar interferometry Synthetic aperture radar SAR Thermokarst |
description |
Vast areas of the Arctic host ice-rich permafrost, which is becoming increasingly vulnerable to terrain-altering thermokarst in a warming climate. Among the most rapid and dramatic changes are retrogressive thaw slumps. These slumps evolve by a retreat of the slump headwall during the summer months, making them detectable by comparing digital elevation models over time using the volumetric change as an indicator. Here, we present and assess a method to detect and monitor thaw slumps using time series of elevation models applied on two contrasting study areas in Northern Canada. Our two-step method is tailored to single-pass InSAR observations from the TanDEM-X satellite pair, which have been acquired since 2011. For each acquisition, we derive a digital elevation model and uncertainty estimates. In the first step, we difference digital elevation models and detect the significant elevation changes using a blob-detection algorithm. In the second step, we classify the detections into those due to thaw slumps ... : IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 13 ... |
format |
Article in Journal/Newspaper |
author |
Bernhard, Philipp Zwieback, Simon Leinss, Silvan Hajnsek, Irena |
author_facet |
Bernhard, Philipp Zwieback, Simon Leinss, Silvan Hajnsek, Irena |
author_sort |
Bernhard, Philipp |
title |
Mapping Retrogressive Thaw Slumps Using Single-Pass TanDEM-X Observations ... |
title_short |
Mapping Retrogressive Thaw Slumps Using Single-Pass TanDEM-X Observations ... |
title_full |
Mapping Retrogressive Thaw Slumps Using Single-Pass TanDEM-X Observations ... |
title_fullStr |
Mapping Retrogressive Thaw Slumps Using Single-Pass TanDEM-X Observations ... |
title_full_unstemmed |
Mapping Retrogressive Thaw Slumps Using Single-Pass TanDEM-X Observations ... |
title_sort |
mapping retrogressive thaw slumps using single-pass tandem-x observations ... |
publisher |
ETH Zurich |
publishDate |
2020 |
url |
https://dx.doi.org/10.3929/ethz-b-000426695 http://hdl.handle.net/20.500.11850/426695 |
genre |
Arctic Banks Island Ice Mackenzie river permafrost Thermokarst |
genre_facet |
Arctic Banks Island Ice Mackenzie river permafrost Thermokarst |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.3929/ethz-b-000426695 |
_version_ |
1797578472523038720 |