Thaw Subsidence of a Yedoma Landscape in Northern Siberia, Measured In Situ and Estimated from TerraSAR-X Interferometry ...

In permafrost areas, seasonal freeze-thaw cycles result in upward and downward movements of the ground. For some permafrost areas, long-term downward movements were reported during the last decade. We measured seasonal and multi-year ground movements in a yedoma region of the Lena River Delta, Siber...

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Main Authors: Antonova, Sofia, Sudhaus, Henriette, Strozzi, Tazio, Zwieback, Simon, Kääb, Andreas, Heim, Birgit, Langer, Moritz, Bornemann, Niko, Boike, Julia
Format: Text
Language:English
Published: Humboldt-Universität zu Berlin 2018
Subjects:
Online Access:https://dx.doi.org/10.18452/20455
https://edoc.hu-berlin.de/handle/18452/21223
id ftdatacite:10.18452/20455
record_format openpolar
spelling ftdatacite:10.18452/20455 2024-09-30T14:38:15+00:00 Thaw Subsidence of a Yedoma Landscape in Northern Siberia, Measured In Situ and Estimated from TerraSAR-X Interferometry ... Antonova, Sofia Sudhaus, Henriette Strozzi, Tazio Zwieback, Simon Kääb, Andreas Heim, Birgit Langer, Moritz Bornemann, Niko Boike, Julia 2018 https://dx.doi.org/10.18452/20455 https://edoc.hu-berlin.de/handle/18452/21223 en eng Humboldt-Universität zu Berlin Creative Commons Attribution 4.0 International (CC BY 4.0) Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 permafrost thaw subsidence in situ measurements DInSAR TerraSAR-X Lena River Delta yedoma 620 Ingenieurwissenschaften und zugeordnete Tätigkeiten Text article article-journal ScholarlyArticle 2018 ftdatacite https://doi.org/10.18452/20455 2024-09-02T08:57:59Z In permafrost areas, seasonal freeze-thaw cycles result in upward and downward movements of the ground. For some permafrost areas, long-term downward movements were reported during the last decade. We measured seasonal and multi-year ground movements in a yedoma region of the Lena River Delta, Siberia, in 2013–2017, using reference rods installed deep in the permafrost. The seasonal subsidence was 1.7 ± 1.5 cm in the cold summer of 2013 and 4.8 ± 2 cm in the warm summer of 2014. Furthermore, we measured a pronounced multi-year net subsidence of 9.3 ± 5.7 cm from spring 2013 to the end of summer 2017. Importantly, we observed a high spatial variability of subsidence of up to 6 cm across a sub-meter horizontal scale. In summer 2013, we accompanied our field measurements with Differential Synthetic Aperture Radar Interferometry (DInSAR) on repeat-pass TerraSAR-X (TSX) data from the summer of 2013 to detect summer thaw subsidence over the same study area. Interferometry was strongly affected by a fast phase ... Text lena river permafrost Siberia DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic permafrost
thaw subsidence
in situ measurements
DInSAR
TerraSAR-X
Lena River Delta
yedoma
620 Ingenieurwissenschaften und zugeordnete Tätigkeiten
spellingShingle permafrost
thaw subsidence
in situ measurements
DInSAR
TerraSAR-X
Lena River Delta
yedoma
620 Ingenieurwissenschaften und zugeordnete Tätigkeiten
Antonova, Sofia
Sudhaus, Henriette
Strozzi, Tazio
Zwieback, Simon
Kääb, Andreas
Heim, Birgit
Langer, Moritz
Bornemann, Niko
Boike, Julia
Thaw Subsidence of a Yedoma Landscape in Northern Siberia, Measured In Situ and Estimated from TerraSAR-X Interferometry ...
topic_facet permafrost
thaw subsidence
in situ measurements
DInSAR
TerraSAR-X
Lena River Delta
yedoma
620 Ingenieurwissenschaften und zugeordnete Tätigkeiten
description In permafrost areas, seasonal freeze-thaw cycles result in upward and downward movements of the ground. For some permafrost areas, long-term downward movements were reported during the last decade. We measured seasonal and multi-year ground movements in a yedoma region of the Lena River Delta, Siberia, in 2013–2017, using reference rods installed deep in the permafrost. The seasonal subsidence was 1.7 ± 1.5 cm in the cold summer of 2013 and 4.8 ± 2 cm in the warm summer of 2014. Furthermore, we measured a pronounced multi-year net subsidence of 9.3 ± 5.7 cm from spring 2013 to the end of summer 2017. Importantly, we observed a high spatial variability of subsidence of up to 6 cm across a sub-meter horizontal scale. In summer 2013, we accompanied our field measurements with Differential Synthetic Aperture Radar Interferometry (DInSAR) on repeat-pass TerraSAR-X (TSX) data from the summer of 2013 to detect summer thaw subsidence over the same study area. Interferometry was strongly affected by a fast phase ...
format Text
author Antonova, Sofia
Sudhaus, Henriette
Strozzi, Tazio
Zwieback, Simon
Kääb, Andreas
Heim, Birgit
Langer, Moritz
Bornemann, Niko
Boike, Julia
author_facet Antonova, Sofia
Sudhaus, Henriette
Strozzi, Tazio
Zwieback, Simon
Kääb, Andreas
Heim, Birgit
Langer, Moritz
Bornemann, Niko
Boike, Julia
author_sort Antonova, Sofia
title Thaw Subsidence of a Yedoma Landscape in Northern Siberia, Measured In Situ and Estimated from TerraSAR-X Interferometry ...
title_short Thaw Subsidence of a Yedoma Landscape in Northern Siberia, Measured In Situ and Estimated from TerraSAR-X Interferometry ...
title_full Thaw Subsidence of a Yedoma Landscape in Northern Siberia, Measured In Situ and Estimated from TerraSAR-X Interferometry ...
title_fullStr Thaw Subsidence of a Yedoma Landscape in Northern Siberia, Measured In Situ and Estimated from TerraSAR-X Interferometry ...
title_full_unstemmed Thaw Subsidence of a Yedoma Landscape in Northern Siberia, Measured In Situ and Estimated from TerraSAR-X Interferometry ...
title_sort thaw subsidence of a yedoma landscape in northern siberia, measured in situ and estimated from terrasar-x interferometry ...
publisher Humboldt-Universität zu Berlin
publishDate 2018
url https://dx.doi.org/10.18452/20455
https://edoc.hu-berlin.de/handle/18452/21223
genre lena river
permafrost
Siberia
genre_facet lena river
permafrost
Siberia
op_rights Creative Commons Attribution 4.0 International
(CC BY 4.0) Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.18452/20455
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