Multi-Annual Kinematics of an Active Rock Glacier Quantified from Very High-Resolution DEMs: An Application-Case in the French Alps
[Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE [ADD1_IRSTEA]Hydrosystèmes et risques naturels International audience Rock glaciers result from the long-term creeping of ice-rich permafrost along mountain slopes. Under warming conditions, deformation is expected to increase, and potential destabilizatio...
Published in: | Remote Sensing |
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Main Authors: | , , , , |
Other Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2018
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Online Access: | https://sde.hal.science/hal-01880573 https://sde.hal.science/hal-01880573/document https://sde.hal.science/hal-01880573/file/pub00060682.pdf https://doi.org/10.3390/rs10040547 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
Inserm: HAL (Institut national de la santé et de la recherche médicale) |
op_collection_id |
ftinserm |
language |
English |
topic |
very high-resolution DEM SFM-MVS TLS ALS rock glacier deformation image correlation surface displacement [SDE.MCG]Environmental Sciences/Global Changes [SDE.BE]Environmental Sciences/Biodiversity and Ecology [SDE.IE]Environmental Sciences/Environmental Engineering [SDE.ES]Environmental Sciences/Environment and Society [SHS.GEO]Humanities and Social Sciences/Geography |
spellingShingle |
very high-resolution DEM SFM-MVS TLS ALS rock glacier deformation image correlation surface displacement [SDE.MCG]Environmental Sciences/Global Changes [SDE.BE]Environmental Sciences/Biodiversity and Ecology [SDE.IE]Environmental Sciences/Environmental Engineering [SDE.ES]Environmental Sciences/Environment and Society [SHS.GEO]Humanities and Social Sciences/Geography Bodin, Xavier Thibert, Emmanuel Sanchez, Olivier Rabatel, Antoine Jaillet, Stéphane Multi-Annual Kinematics of an Active Rock Glacier Quantified from Very High-Resolution DEMs: An Application-Case in the French Alps |
topic_facet |
very high-resolution DEM SFM-MVS TLS ALS rock glacier deformation image correlation surface displacement [SDE.MCG]Environmental Sciences/Global Changes [SDE.BE]Environmental Sciences/Biodiversity and Ecology [SDE.IE]Environmental Sciences/Environmental Engineering [SDE.ES]Environmental Sciences/Environment and Society [SHS.GEO]Humanities and Social Sciences/Geography |
description |
[Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE [ADD1_IRSTEA]Hydrosystèmes et risques naturels International audience Rock glaciers result from the long-term creeping of ice-rich permafrost along mountain slopes. Under warming conditions, deformation is expected to increase, and potential destabilization of those landforms may lead to hazardous phenomena. Monitoring the kinematics of rock glaciers at fine spatial resolution is required to better understand at which rate, where and how they deform. We present here the results of several years of in situ surveys carried out between 2005 and 2015 on the Laurichard rock glacier, an active rock glacier located in the French Alps. Repeated terrestrial laser-scanning (TLS) together with aerial laser-scanning (ALS) and structure-from-motion-multi-view-stereophotogrammetry (SFM-MVS) were used to accurately quantify surface displacement of the Laurichard rock glacier at interannual and pluri-annual scales. Six very high-resolution digital elevation models (DEMs, pixel size <50 cm) of the rock glacier surface were generated, and their respective quality was assessed. The relative horizontal position accuracy (XY) of the individual DEMs is in general less than 2 cm with a co-registration error on stable areas ranging from 20–50 cm. The vertical accuracy is around 20 cm. The direction and amplitude of surface displacements computed between DEMs are very consistent with independent geodetic field measurements (e.g., DGPS). Using these datasets, local patterns of the Laurichard rock glacier kinematics were quantified, pointing out specific internal (rheological) and external (bed topography) controls. The evolution of the surface velocity shows few changes on the rock glacier’s snout for the first years of the observed period, followed by a major acceleration between 2012 and 2015 affecting the upper part of the tongue and the snout |
author2 |
Environnements, Dynamiques et Territoires de Montagne (EDYTEM) Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ) Institut Mondor de recherche biomédicale (IMRB) Institut National de la Santé et de la Recherche Médicale (INSERM)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12) Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ) |
format |
Article in Journal/Newspaper |
author |
Bodin, Xavier Thibert, Emmanuel Sanchez, Olivier Rabatel, Antoine Jaillet, Stéphane |
author_facet |
Bodin, Xavier Thibert, Emmanuel Sanchez, Olivier Rabatel, Antoine Jaillet, Stéphane |
author_sort |
Bodin, Xavier |
title |
Multi-Annual Kinematics of an Active Rock Glacier Quantified from Very High-Resolution DEMs: An Application-Case in the French Alps |
title_short |
Multi-Annual Kinematics of an Active Rock Glacier Quantified from Very High-Resolution DEMs: An Application-Case in the French Alps |
title_full |
Multi-Annual Kinematics of an Active Rock Glacier Quantified from Very High-Resolution DEMs: An Application-Case in the French Alps |
title_fullStr |
Multi-Annual Kinematics of an Active Rock Glacier Quantified from Very High-Resolution DEMs: An Application-Case in the French Alps |
title_full_unstemmed |
Multi-Annual Kinematics of an Active Rock Glacier Quantified from Very High-Resolution DEMs: An Application-Case in the French Alps |
title_sort |
multi-annual kinematics of an active rock glacier quantified from very high-resolution dems: an application-case in the french alps |
publisher |
HAL CCSD |
publishDate |
2018 |
url |
https://sde.hal.science/hal-01880573 https://sde.hal.science/hal-01880573/document https://sde.hal.science/hal-01880573/file/pub00060682.pdf https://doi.org/10.3390/rs10040547 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
ISSN: 2072-4292 Remote Sensing https://sde.hal.science/hal-01880573 Remote Sensing, 2018, 10 (4), pp.14. ⟨10.3390/rs10040547⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.3390/rs10040547 hal-01880573 https://sde.hal.science/hal-01880573 https://sde.hal.science/hal-01880573/document https://sde.hal.science/hal-01880573/file/pub00060682.pdf doi:10.3390/rs10040547 IRSTEA: PUB00060682 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.3390/rs10040547 |
container_title |
Remote Sensing |
container_volume |
10 |
container_issue |
4 |
container_start_page |
547 |
_version_ |
1801376634280869888 |
spelling |
ftinserm:oai:HAL:hal-01880573v1 2024-06-09T07:46:41+00:00 Multi-Annual Kinematics of an Active Rock Glacier Quantified from Very High-Resolution DEMs: An Application-Case in the French Alps Bodin, Xavier Thibert, Emmanuel Sanchez, Olivier Rabatel, Antoine Jaillet, Stéphane Environnements, Dynamiques et Territoires de Montagne (EDYTEM) Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ) Institut Mondor de recherche biomédicale (IMRB) Institut National de la Santé et de la Recherche Médicale (INSERM)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12) Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ) 2018-04 https://sde.hal.science/hal-01880573 https://sde.hal.science/hal-01880573/document https://sde.hal.science/hal-01880573/file/pub00060682.pdf https://doi.org/10.3390/rs10040547 en eng HAL CCSD MDPI info:eu-repo/semantics/altIdentifier/doi/10.3390/rs10040547 hal-01880573 https://sde.hal.science/hal-01880573 https://sde.hal.science/hal-01880573/document https://sde.hal.science/hal-01880573/file/pub00060682.pdf doi:10.3390/rs10040547 IRSTEA: PUB00060682 info:eu-repo/semantics/OpenAccess ISSN: 2072-4292 Remote Sensing https://sde.hal.science/hal-01880573 Remote Sensing, 2018, 10 (4), pp.14. ⟨10.3390/rs10040547⟩ very high-resolution DEM SFM-MVS TLS ALS rock glacier deformation image correlation surface displacement [SDE.MCG]Environmental Sciences/Global Changes [SDE.BE]Environmental Sciences/Biodiversity and Ecology [SDE.IE]Environmental Sciences/Environmental Engineering [SDE.ES]Environmental Sciences/Environment and Society [SHS.GEO]Humanities and Social Sciences/Geography info:eu-repo/semantics/article Journal articles 2018 ftinserm https://doi.org/10.3390/rs10040547 2024-05-16T11:12:46Z [Departement_IRSTEA]Eaux [TR1_IRSTEA]RIVAGE [ADD1_IRSTEA]Hydrosystèmes et risques naturels International audience Rock glaciers result from the long-term creeping of ice-rich permafrost along mountain slopes. Under warming conditions, deformation is expected to increase, and potential destabilization of those landforms may lead to hazardous phenomena. Monitoring the kinematics of rock glaciers at fine spatial resolution is required to better understand at which rate, where and how they deform. We present here the results of several years of in situ surveys carried out between 2005 and 2015 on the Laurichard rock glacier, an active rock glacier located in the French Alps. Repeated terrestrial laser-scanning (TLS) together with aerial laser-scanning (ALS) and structure-from-motion-multi-view-stereophotogrammetry (SFM-MVS) were used to accurately quantify surface displacement of the Laurichard rock glacier at interannual and pluri-annual scales. Six very high-resolution digital elevation models (DEMs, pixel size <50 cm) of the rock glacier surface were generated, and their respective quality was assessed. The relative horizontal position accuracy (XY) of the individual DEMs is in general less than 2 cm with a co-registration error on stable areas ranging from 20–50 cm. The vertical accuracy is around 20 cm. The direction and amplitude of surface displacements computed between DEMs are very consistent with independent geodetic field measurements (e.g., DGPS). Using these datasets, local patterns of the Laurichard rock glacier kinematics were quantified, pointing out specific internal (rheological) and external (bed topography) controls. The evolution of the surface velocity shows few changes on the rock glacier’s snout for the first years of the observed period, followed by a major acceleration between 2012 and 2015 affecting the upper part of the tongue and the snout Article in Journal/Newspaper Ice permafrost Inserm: HAL (Institut national de la santé et de la recherche médicale) Remote Sensing 10 4 547 |