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Sentinel-1 SAR interferometry for surface deformation monitoring in low-land permafrost areas

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Resumo:Low-land permafrost areas are subject to intense freeze-thaw cycles and characterized by remarkable surface displacement. We used Sentinel-1 SAR interferometry (InSAR) in order to analyse the summer surface displacement over four spots in the Arctic and Antarctica since 2015. Choosing floodplain or outcrop areas as the reference for the InSAR relative deformation measurements, we found maximum subsidence of about 3 to 10 cm during the thawing season with generally high spatial variability. Sentinel-1 time-series of interferograms with 6–12 day time intervals highlight that subsidence is often occurring rather quickly within roughly one month in early summer. Intercomparison of summer subsidence from Sentinel-1 in 2017 with TerraSAR-X in 2013 over part of the Lena River Delta (Russia) shows a high spatial agreement between both SAR systems. A comparison with in-situ measurements for the summer of 2014 over the Lena River Delta indicates a pronounced downward movement of several centimetres in both cases but does not reveal a spatial correspondence between InSAR and local in-situ measurements. For the reconstruction of longer time-series of deformation, yearly Sentinel-1 interferograms from the end of the summer were considered. However, in order to infer an effective subsidence of the surface through melting of excess ice layers over multi-annual scales with Sentinel-1, a longer observation time period is necessary.
Autores principais:Strozzi, Tazio
Outros Autores:Antonova, Sofia; Günther, Frank; Mätzler, Eva; Vieira, Gonçalo; Wegmüller, Urs; Westermann, Sebastian; Bartsch, Annett
Assunto:Permafrost Arctic Antarctica Subsidence InSAR Sentinel-1
Ano:2018
País:Portugal
Tipo de documento:artigo
Tipo de acesso:acesso aberto
Instituição associada:Universidade de Lisboa
Idioma:inglês
Origem:Repositório da Universidade de Lisboa
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author Strozzi, Tazio
author2 Antonova, Sofia
Günther, Frank
Mätzler, Eva
Vieira, Gonçalo
Wegmüller, Urs
Westermann, Sebastian
Bartsch, Annett
author2_role author
author
author
author
author
author
author
author_facet Strozzi, Tazio
Strozzi, Tazio
Antonova, Sofia
Günther, Frank
Mätzler, Eva
Vieira, Gonçalo
Wegmüller, Urs
Westermann, Sebastian
Bartsch, Annett
Antonova, Sofia
Günther, Frank
Mätzler, Eva
Vieira, Gonçalo
Wegmüller, Urs
Westermann, Sebastian
Bartsch, Annett
author_role author
contributor_name_str_mv Repositório Científico de Acesso Aberto da ULisboa
country_str PT
creators_json_str [{\"Person.name\":\"Strozzi, Tazio\"},{\"Person.name\":\"Antonova, Sofia\"},{\"Person.name\":\"Günther, Frank\"},{\"Person.name\":\"Mätzler, Eva\"},{\"Person.name\":\"Vieira, Gonçalo\",\"Person.identifier.orcid\":\"0000-0001-7611-3464\"},{\"Person.name\":\"Wegmüller, Urs\"},{\"Person.name\":\"Westermann, Sebastian\"},{\"Person.name\":\"Bartsch, Annett\"}]
datacite.contributors.contributor.contributorName.fl_str_mv Repositório Científico de Acesso Aberto da ULisboa
datacite.creators.creator.creatorName.fl_str_mv Strozzi, Tazio
Antonova, Sofia
Günther, Frank
Mätzler, Eva
Vieira, Gonçalo
Wegmüller, Urs
Westermann, Sebastian
Bartsch, Annett
datacite.date.Accepted.fl_str_mv 2018-01-01T00:00:00Z
datacite.date.available.fl_str_mv 2019-07-16T11:55:14Z
datacite.date.embargoed.fl_str_mv 2019-07-16T11:55:14Z
datacite.rights.fl_str_mv http://purl.org/coar/access_right/c_abf2
datacite.subjects.subject.fl_str_mv Permafrost
Arctic
Antarctica
Subsidence
InSAR
Sentinel-1
datacite.titles.title.fl_str_mv Sentinel-1 SAR interferometry for surface deformation monitoring in low-land permafrost areas
dc.contributor.none.fl_str_mv Repositório Científico de Acesso Aberto da ULisboa
dc.creator.none.fl_str_mv Strozzi, Tazio
Antonova, Sofia
Günther, Frank
Mätzler, Eva
Vieira, Gonçalo
Wegmüller, Urs
Westermann, Sebastian
Bartsch, Annett
dc.date.Accepted.fl_str_mv 2018-01-01T00:00:00Z
dc.date.available.fl_str_mv 2019-07-16T11:55:14Z
dc.date.embargoed.fl_str_mv 2019-07-16T11:55:14Z
dc.format.none.fl_str_mv application/pdf
dc.identifier.none.fl_str_mv http://hdl.handle.net/10451/39123
dc.language.none.fl_str_mv eng
dc.publisher.none.fl_str_mv MDPI
dc.rights.cclincense.fl_str_mv http://creativecommons.org/licenses/by/4.0/
dc.rights.none.fl_str_mv http://purl.org/coar/access_right/c_abf2
dc.subject.none.fl_str_mv Permafrost
Arctic
Antarctica
Subsidence
InSAR
Sentinel-1
dc.title.fl_str_mv Sentinel-1 SAR interferometry for surface deformation monitoring in low-land permafrost areas
dc.type.none.fl_str_mv http://purl.org/coar/resource_type/c_6501
description Low-land permafrost areas are subject to intense freeze-thaw cycles and characterized by remarkable surface displacement. We used Sentinel-1 SAR interferometry (InSAR) in order to analyse the summer surface displacement over four spots in the Arctic and Antarctica since 2015. Choosing floodplain or outcrop areas as the reference for the InSAR relative deformation measurements, we found maximum subsidence of about 3 to 10 cm during the thawing season with generally high spatial variability. Sentinel-1 time-series of interferograms with 6–12 day time intervals highlight that subsidence is often occurring rather quickly within roughly one month in early summer. Intercomparison of summer subsidence from Sentinel-1 in 2017 with TerraSAR-X in 2013 over part of the Lena River Delta (Russia) shows a high spatial agreement between both SAR systems. A comparison with in-situ measurements for the summer of 2014 over the Lena River Delta indicates a pronounced downward movement of several centimetres in both cases but does not reveal a spatial correspondence between InSAR and local in-situ measurements. For the reconstruction of longer time-series of deformation, yearly Sentinel-1 interferograms from the end of the summer were considered. However, in order to infer an effective subsidence of the surface through melting of excess ice layers over multi-annual scales with Sentinel-1, a longer observation time period is necessary.
dirty 0
eu_rights_str_mv openAccess
format article
fulltext.url.fl_str_mv https://repositorio.ulisboa.pt/bitstreams/ed3349e9-1088-422a-be25-f1635def62b3/download
id ul_330c50cffc7bb3b5f1eda7db223d4800
identifier.url.fl_str_mv http://hdl.handle.net/10451/39123
instacron_str ul
institution Universidade de Lisboa
instname_str Universidade de Lisboa
language eng
network_acronym_str ul
network_name_str Repositório da Universidade de Lisboa
oai_identifier_str oai:repositorio.ulisboa.pt:10451/39123
organization_str_mv urn:organizationAcronym:ul
person_str_mv Strozzi, Tazio
Antonova, Sofia
Günther, Frank
Mätzler, Eva
Vieira, Gonçalo
Vieira, Gonçalo
https://www.ciencia-id.pt/2519-6583-CAEA
2519-6583-CAEA
http://orcid.org/0000-0001-7611-3464
0000-0001-7611-3464
Wegmüller, Urs
Westermann, Sebastian
Bartsch, Annett
publishDate 2018
publisher.none.fl_str_mv MDPI
reponame_str Repositório da Universidade de Lisboa
repository_id_str urn:repositoryAcronym:ul
service_str_mv urn:repositoryAcronym:ul
spelling engMDPIpt_PTLow-land permafrost areas are subject to intense freeze-thaw cycles and characterized by remarkable surface displacement. We used Sentinel-1 SAR interferometry (InSAR) in order to analyse the summer surface displacement over four spots in the Arctic and Antarctica since 2015. Choosing floodplain or outcrop areas as the reference for the InSAR relative deformation measurements, we found maximum subsidence of about 3 to 10 cm during the thawing season with generally high spatial variability. Sentinel-1 time-series of interferograms with 6–12 day time intervals highlight that subsidence is often occurring rather quickly within roughly one month in early summer. Intercomparison of summer subsidence from Sentinel-1 in 2017 with TerraSAR-X in 2013 over part of the Lena River Delta (Russia) shows a high spatial agreement between both SAR systems. A comparison with in-situ measurements for the summer of 2014 over the Lena River Delta indicates a pronounced downward movement of several centimetres in both cases but does not reveal a spatial correspondence between InSAR and local in-situ measurements. For the reconstruction of longer time-series of deformation, yearly Sentinel-1 interferograms from the end of the summer were considered. However, in order to infer an effective subsidence of the surface through melting of excess ice layers over multi-annual scales with Sentinel-1, a longer observation time period is necessary.application/pdfpt_PTSentinel-1 SAR interferometry for surface deformation monitoring in low-land permafrost areasStrozzi, TazioAntonova, SofiaGünther, FrankMätzler, EvaPersonalVieira, GonçaloDSpacehttp://dspace.org/items/7039fbb2-e1f8-4c3e-80f1-603b12d33c1cDSpacehttp://dspace.org/items/7039fbb2-e1f8-4c3e-80f1-603b12d33c1cBrito Guapo Teles VieiraGonçaloCiência IDhttps://www.ciencia-id.pt2519-6583-CAEAORCIDhttp://orcid.org0000-0001-7611-3464Scopus Author IDhttps://www.scopus.com7005863976Wegmüller, UrsWestermann, SebastianBartsch, AnnettHostingInstitutionOrganizationalRepositório Científico de Acesso Aberto da ULisboae-mailmailto:repositorio@reitoria.ulisboa.ptrepositorio@reitoria.ulisboa.ptISSNIsPartOf2072-4292DOIIsPartOf10.3390/rs100913602019-07-16T11:55:14Z20182018-01-01T00:00:00ZHandlehttp://hdl.handle.net/10451/39123http://purl.org/coar/access_right/c_abf2open accessPermafrostArcticAntarcticaSubsidenceInSARSentinel-117071367 bytesliteraturehttp://purl.org/coar/resource_type/c_6501journal article2018http://creativecommons.org/licenses/by/4.0/http://purl.org/coar/access_right/c_abf2application/pdffulltexthttps://repositorio.ulisboa.pt/bitstreams/ed3349e9-1088-422a-be25-f1635def62b3/downloadRemote Sensing1091360
spellingShingle Sentinel-1 SAR interferometry for surface deformation monitoring in low-land permafrost areas
Sentinel-1 SAR interferometry for surface deformation monitoring in low-land permafrost areas
Strozzi, Tazio
Permafrost
Arctic
Antarctica
Subsidence
InSAR
Sentinel-1
Strozzi, Tazio
Permafrost
Arctic
Antarctica
Subsidence
InSAR
Sentinel-1
status SINGLETON
subject.fl_str_mv Permafrost
Arctic
Antarctica
Subsidence
InSAR
Sentinel-1
title Sentinel-1 SAR interferometry for surface deformation monitoring in low-land permafrost areas
title_full Sentinel-1 SAR interferometry for surface deformation monitoring in low-land permafrost areas
title_fullStr Sentinel-1 SAR interferometry for surface deformation monitoring in low-land permafrost areas
Sentinel-1 SAR interferometry for surface deformation monitoring in low-land permafrost areas
title_full_unstemmed Sentinel-1 SAR interferometry for surface deformation monitoring in low-land permafrost areas
Sentinel-1 SAR interferometry for surface deformation monitoring in low-land permafrost areas
title_short Sentinel-1 SAR interferometry for surface deformation monitoring in low-land permafrost areas
title_sort Sentinel-1 SAR interferometry for surface deformation monitoring in low-land permafrost areas
topic Permafrost
Arctic
Antarctica
Subsidence
InSAR
Sentinel-1
topic_facet Permafrost
Arctic
Antarctica
Subsidence
InSAR
Sentinel-1
url http://hdl.handle.net/10451/39123
visible 1