Monitoring permafrost and thermokarst processes with TanDEM-X DEM time series: Opportunities and limitations
Permafrost soils have been shown to respond rapidly to warming temperatures. When ice-rich permafrost soils thaw, the melting ground ice reduces the volume and stability of the soils, inducing changes in the topography. We monitor surface elevation changes in three test sites in Northern Eurasia usi...
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ftawi:oai:epic.awi.de:43305 2024-09-09T19:44:23+00:00 Monitoring permafrost and thermokarst processes with TanDEM-X DEM time series: Opportunities and limitations Zwieback, Simon Bartsch, Annett Boike, Julia Grosse, Guido Günther, Frank Heim, Birgit Morgenstern, Anne Hajnsek, Irena 2016-11-03 https://epic.awi.de/id/eprint/43305/ http://ieeexplore.ieee.org/document/7729079/ https://hdl.handle.net/10013/epic.49770 unknown IEEE Zwieback, S. , Bartsch, A. , Boike, J. orcid:0000-0002-5875-2112 , Grosse, G. orcid:0000-0001-5895-2141 , Günther, F. orcid:0000-0001-8298-8937 , Heim, B. orcid:0000-0003-2614-9391 , Morgenstern, A. orcid:0000-0002-6466-7571 and Hajnsek, I. (2016) Monitoring permafrost and thermokarst processes with TanDEM-X DEM time series: Opportunities and limitations , 36th IEEE International Geoscience and Remote Sensing Symposium, IGARSS 2016, pp. 332-335 . doi:10.1109/IGARSS.2016.7729079 <https://doi.org/10.1109/IGARSS.2016.7729079> , hdl:10013/epic.49770 info:eu-repo/semantics/openAccess EPIC336th IEEE International Geoscience and Remote Sensing Symposium, IGARSS 2016, IEEE, pp. 332-335 Article peerRev info:eu-repo/semantics/article 2016 ftawi https://doi.org/10.1109/IGARSS.2016.7729079 2024-06-24T04:16:35Z Permafrost soils have been shown to respond rapidly to warming temperatures. When ice-rich permafrost soils thaw, the melting ground ice reduces the volume and stability of the soils, inducing changes in the topography. We monitor surface elevation changes in three test sites in Northern Eurasia using single-pass TanDEM-X Science Phase data with submetre vertical precision. The results indicate the suitability of single-pass InSAR data for monitoring thaw-induced topographic changes (e.g. coastal erosion) but they also reveal the spurious impact of late-lying snow packs and water bodies, both of which are common in lowland permafrost areas. Furthermore, the coherence and hence the precision with which elevation changes can be estimated is found to be limited by the noise level in certain cases. As some of these influences could be mitigated using appropriate mission and acquisition designs, we conclude that single-pass interferometry has considerable potential for monitoring thaw-induced surface elevation changes in permafrost areas, which in turn could contribute to assessing their vulnerability, fate, and climate system feedback in a warming climate. Article in Journal/Newspaper Ice permafrost Thermokarst Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) 2016 IEEE International Geoscience and Remote Sensing Symposium (IGARSS) 332 335 |
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Open Polar |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
language |
unknown |
description |
Permafrost soils have been shown to respond rapidly to warming temperatures. When ice-rich permafrost soils thaw, the melting ground ice reduces the volume and stability of the soils, inducing changes in the topography. We monitor surface elevation changes in three test sites in Northern Eurasia using single-pass TanDEM-X Science Phase data with submetre vertical precision. The results indicate the suitability of single-pass InSAR data for monitoring thaw-induced topographic changes (e.g. coastal erosion) but they also reveal the spurious impact of late-lying snow packs and water bodies, both of which are common in lowland permafrost areas. Furthermore, the coherence and hence the precision with which elevation changes can be estimated is found to be limited by the noise level in certain cases. As some of these influences could be mitigated using appropriate mission and acquisition designs, we conclude that single-pass interferometry has considerable potential for monitoring thaw-induced surface elevation changes in permafrost areas, which in turn could contribute to assessing their vulnerability, fate, and climate system feedback in a warming climate. |
format |
Article in Journal/Newspaper |
author |
Zwieback, Simon Bartsch, Annett Boike, Julia Grosse, Guido Günther, Frank Heim, Birgit Morgenstern, Anne Hajnsek, Irena |
spellingShingle |
Zwieback, Simon Bartsch, Annett Boike, Julia Grosse, Guido Günther, Frank Heim, Birgit Morgenstern, Anne Hajnsek, Irena Monitoring permafrost and thermokarst processes with TanDEM-X DEM time series: Opportunities and limitations |
author_facet |
Zwieback, Simon Bartsch, Annett Boike, Julia Grosse, Guido Günther, Frank Heim, Birgit Morgenstern, Anne Hajnsek, Irena |
author_sort |
Zwieback, Simon |
title |
Monitoring permafrost and thermokarst processes with TanDEM-X DEM time series: Opportunities and limitations |
title_short |
Monitoring permafrost and thermokarst processes with TanDEM-X DEM time series: Opportunities and limitations |
title_full |
Monitoring permafrost and thermokarst processes with TanDEM-X DEM time series: Opportunities and limitations |
title_fullStr |
Monitoring permafrost and thermokarst processes with TanDEM-X DEM time series: Opportunities and limitations |
title_full_unstemmed |
Monitoring permafrost and thermokarst processes with TanDEM-X DEM time series: Opportunities and limitations |
title_sort |
monitoring permafrost and thermokarst processes with tandem-x dem time series: opportunities and limitations |
publisher |
IEEE |
publishDate |
2016 |
url |
https://epic.awi.de/id/eprint/43305/ http://ieeexplore.ieee.org/document/7729079/ https://hdl.handle.net/10013/epic.49770 |
genre |
Ice permafrost Thermokarst |
genre_facet |
Ice permafrost Thermokarst |
op_source |
EPIC336th IEEE International Geoscience and Remote Sensing Symposium, IGARSS 2016, IEEE, pp. 332-335 |
op_relation |
Zwieback, S. , Bartsch, A. , Boike, J. orcid:0000-0002-5875-2112 , Grosse, G. orcid:0000-0001-5895-2141 , Günther, F. orcid:0000-0001-8298-8937 , Heim, B. orcid:0000-0003-2614-9391 , Morgenstern, A. orcid:0000-0002-6466-7571 and Hajnsek, I. (2016) Monitoring permafrost and thermokarst processes with TanDEM-X DEM time series: Opportunities and limitations , 36th IEEE International Geoscience and Remote Sensing Symposium, IGARSS 2016, pp. 332-335 . doi:10.1109/IGARSS.2016.7729079 <https://doi.org/10.1109/IGARSS.2016.7729079> , hdl:10013/epic.49770 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1109/IGARSS.2016.7729079 |
container_title |
2016 IEEE International Geoscience and Remote Sensing Symposium (IGARSS) |
container_start_page |
332 |
op_container_end_page |
335 |
_version_ |
1809914096195207168 |