Numerical modeling of the mount Steller landslide flow history and of the generated long period seismic waves
International audience The rock-ice avalanche that occurred in 2005 on Mount Steller, Alaska and the resulting long period seismic waves have been simulated for different avalanche scenarios (i.e., flow histories), with and without erosion processes taken into account. This 40-60 Mm3 avalanche trave...
Published in: | Geophysical Research Letters |
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Online Access: | https://hal-upec-upem.archives-ouvertes.fr/hal-00728958 https://hal-upec-upem.archives-ouvertes.fr/hal-00728958/document https://hal-upec-upem.archives-ouvertes.fr/hal-00728958/file/Moretti_et_al-2012-Geophysical_Research_Letters.pdf https://doi.org/10.1029/2012GL052511 |
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ftccsdartic:oai:HAL:hal-00728958v1 2023-05-15T16:20:41+02:00 Numerical modeling of the mount Steller landslide flow history and of the generated long period seismic waves Moretti, Laurent Mangeney, Anne Capdeville, Yann Stutzmann, Eléonore Huggel, Christian Schneider, Demian Bouchut, François Sismologie Paris Institut de Physique du Globe de Paris (IPGP) Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-IPG PARIS-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Centre National de la Recherche Scientifique (CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-IPG PARIS-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Centre National de la Recherche Scientifique (CNRS) Laboratoire de Planétologie et Géodynamique UMR 6112 (LPG) Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST) Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) Glaciology, Geomorphodynamics and Geochronology, Physical Geography Division, Department of Geography Universität Zürich Zürich (UZH) Laboratoire d'Analyse et de Mathématiques Appliquées (LAMA) Centre National de la Recherche Scientifique (CNRS)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Fédération de Recherche Bézout-Université Paris-Est Marne-la-Vallée (UPEM) 2012 https://hal-upec-upem.archives-ouvertes.fr/hal-00728958 https://hal-upec-upem.archives-ouvertes.fr/hal-00728958/document https://hal-upec-upem.archives-ouvertes.fr/hal-00728958/file/Moretti_et_al-2012-Geophysical_Research_Letters.pdf https://doi.org/10.1029/2012GL052511 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2012GL052511 hal-00728958 https://hal-upec-upem.archives-ouvertes.fr/hal-00728958 https://hal-upec-upem.archives-ouvertes.fr/hal-00728958/document https://hal-upec-upem.archives-ouvertes.fr/hal-00728958/file/Moretti_et_al-2012-Geophysical_Research_Letters.pdf doi:10.1029/2012GL052511 info:eu-repo/semantics/OpenAccess ISSN: 0094-8276 EISSN: 1944-8007 Geophysical Research Letters https://hal-upec-upem.archives-ouvertes.fr/hal-00728958 Geophysical Research Letters, American Geophysical Union, 2012, 39 (16), pp.L16402. ⟨10.1029/2012GL052511⟩ numerical modeling landslides [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] info:eu-repo/semantics/article Journal articles 2012 ftccsdartic https://doi.org/10.1029/2012GL052511 2021-11-21T02:19:24Z International audience The rock-ice avalanche that occurred in 2005 on Mount Steller, Alaska and the resulting long period seismic waves have been simulated for different avalanche scenarios (i.e., flow histories), with and without erosion processes taken into account. This 40-60 Mm3 avalanche traveled about 10 km down the slope, mainly on top of a glacier, eroding a significant amount of ice. It was recorded by 7 broadband seismic stations. The simulations were compared with the recorded long period seismic signal and with the inverted flow history. The results show that, when erosion processes are taken into account, the simulations reproduce the observed signal at all the stations over a wide range of azimuths and source-station distances (37-623 km). This comparison makes it possible to constrain the rheological parameters involved which should help constrain the volume of eroded material. Because landslides are continuously recorded by seismic networks, this method could significantly broaden quantitative insights into natural flow dynamics. Article in Journal/Newspaper glacier Alaska Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Geophysical Research Letters 39 16 n/a n/a |
institution |
Open Polar |
collection |
Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
numerical modeling landslides [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] |
spellingShingle |
numerical modeling landslides [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] Moretti, Laurent Mangeney, Anne Capdeville, Yann Stutzmann, Eléonore Huggel, Christian Schneider, Demian Bouchut, François Numerical modeling of the mount Steller landslide flow history and of the generated long period seismic waves |
topic_facet |
numerical modeling landslides [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] |
description |
International audience The rock-ice avalanche that occurred in 2005 on Mount Steller, Alaska and the resulting long period seismic waves have been simulated for different avalanche scenarios (i.e., flow histories), with and without erosion processes taken into account. This 40-60 Mm3 avalanche traveled about 10 km down the slope, mainly on top of a glacier, eroding a significant amount of ice. It was recorded by 7 broadband seismic stations. The simulations were compared with the recorded long period seismic signal and with the inverted flow history. The results show that, when erosion processes are taken into account, the simulations reproduce the observed signal at all the stations over a wide range of azimuths and source-station distances (37-623 km). This comparison makes it possible to constrain the rheological parameters involved which should help constrain the volume of eroded material. Because landslides are continuously recorded by seismic networks, this method could significantly broaden quantitative insights into natural flow dynamics. |
author2 |
Sismologie Paris Institut de Physique du Globe de Paris (IPGP) Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-IPG PARIS-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Centre National de la Recherche Scientifique (CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-IPG PARIS-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Centre National de la Recherche Scientifique (CNRS) Laboratoire de Planétologie et Géodynamique UMR 6112 (LPG) Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST) Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) Glaciology, Geomorphodynamics and Geochronology, Physical Geography Division, Department of Geography Universität Zürich Zürich (UZH) Laboratoire d'Analyse et de Mathématiques Appliquées (LAMA) Centre National de la Recherche Scientifique (CNRS)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Fédération de Recherche Bézout-Université Paris-Est Marne-la-Vallée (UPEM) |
format |
Article in Journal/Newspaper |
author |
Moretti, Laurent Mangeney, Anne Capdeville, Yann Stutzmann, Eléonore Huggel, Christian Schneider, Demian Bouchut, François |
author_facet |
Moretti, Laurent Mangeney, Anne Capdeville, Yann Stutzmann, Eléonore Huggel, Christian Schneider, Demian Bouchut, François |
author_sort |
Moretti, Laurent |
title |
Numerical modeling of the mount Steller landslide flow history and of the generated long period seismic waves |
title_short |
Numerical modeling of the mount Steller landslide flow history and of the generated long period seismic waves |
title_full |
Numerical modeling of the mount Steller landslide flow history and of the generated long period seismic waves |
title_fullStr |
Numerical modeling of the mount Steller landslide flow history and of the generated long period seismic waves |
title_full_unstemmed |
Numerical modeling of the mount Steller landslide flow history and of the generated long period seismic waves |
title_sort |
numerical modeling of the mount steller landslide flow history and of the generated long period seismic waves |
publisher |
HAL CCSD |
publishDate |
2012 |
url |
https://hal-upec-upem.archives-ouvertes.fr/hal-00728958 https://hal-upec-upem.archives-ouvertes.fr/hal-00728958/document https://hal-upec-upem.archives-ouvertes.fr/hal-00728958/file/Moretti_et_al-2012-Geophysical_Research_Letters.pdf https://doi.org/10.1029/2012GL052511 |
genre |
glacier Alaska |
genre_facet |
glacier Alaska |
op_source |
ISSN: 0094-8276 EISSN: 1944-8007 Geophysical Research Letters https://hal-upec-upem.archives-ouvertes.fr/hal-00728958 Geophysical Research Letters, American Geophysical Union, 2012, 39 (16), pp.L16402. ⟨10.1029/2012GL052511⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1029/2012GL052511 hal-00728958 https://hal-upec-upem.archives-ouvertes.fr/hal-00728958 https://hal-upec-upem.archives-ouvertes.fr/hal-00728958/document https://hal-upec-upem.archives-ouvertes.fr/hal-00728958/file/Moretti_et_al-2012-Geophysical_Research_Letters.pdf doi:10.1029/2012GL052511 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1029/2012GL052511 |
container_title |
Geophysical Research Letters |
container_volume |
39 |
container_issue |
16 |
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1766008652477497344 |