Tide-induced microseismicity in the Mertz glacier grounding area, East Antarctica

International audience The deployment of a seismic network along the Adélie and George V coasts in East Antarctica during the period 2009–2012 provides the opportunity to monitor cryoseismic activity and to obtain new insights on the relationship between tidal cycles and coastal glacier dynamics. He...

Full description

Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Barruol, Guilhem, Cordier, Emmanuel, Fontaine, Fabrice R., R., Bascou, Jerôme, Legrésy, Benoit, Lescarmontier, Lydie
Other Authors: Institut de Physique du Globe de Paris (IPGP), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS), Laboratoire GéoSciences Réunion (LGSR), Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris), Laboratoire Magmas et Volcans (LMV), Observatoire de Physique du Globe de Clermont-Ferrand (OPGC), Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS), Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS), Research School of Earth Sciences Canberra (RSES), Australian National University (ANU)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2013
Subjects:
Online Access:https://hal.univ-reunion.fr/hal-01236143
https://hal.univ-reunion.fr/hal-01236143/document
https://hal.univ-reunion.fr/hal-01236143/file/Barruol_Icequakes_Mertz_Glacier_Antarctica_GRL2013.pdf
https://doi.org/10.1002/2013GL057814
id ftinsu:oai:HAL:hal-01236143v1
record_format openpolar
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
topic [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]
spellingShingle [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]
Barruol, Guilhem
Cordier, Emmanuel
Fontaine, Fabrice R., R.
Bascou, Jerôme
Legrésy, Benoit
Lescarmontier, Lydie
Tide-induced microseismicity in the Mertz glacier grounding area, East Antarctica
topic_facet [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]
description International audience The deployment of a seismic network along the Adélie and George V coasts in East Antarctica during the period 2009–2012 provides the opportunity to monitor cryoseismic activity and to obtain new insights on the relationship between tidal cycles and coastal glacier dynamics. Here we focus on records from a seismometer located on a rocky outcrop in the vicinity of the grounding line of the 35 km broad Mertz glacier, a major outflow of this region. We detect numerous icequakes (50,000 events within 10 months and up to 100 events/h) and demonstrate their clear tidal modulation. We suggest that they result from ice friction and fracturing around the rocky peak and from the glacier flexure in response to the falling and rising tides at its grounding area. We propose that such icequake monitoring could be used as a climate proxy since grounding lines are subject to migrate with sea level changes.
author2 Institut de Physique du Globe de Paris (IPGP)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS)
Laboratoire GéoSciences Réunion (LGSR)
Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)
Laboratoire Magmas et Volcans (LMV)
Observatoire de Physique du Globe de Clermont-Ferrand (OPGC)
Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS)
Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS)
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)
Research School of Earth Sciences Canberra (RSES)
Australian National University (ANU)
format Article in Journal/Newspaper
author Barruol, Guilhem
Cordier, Emmanuel
Fontaine, Fabrice R., R.
Bascou, Jerôme
Legrésy, Benoit
Lescarmontier, Lydie
author_facet Barruol, Guilhem
Cordier, Emmanuel
Fontaine, Fabrice R., R.
Bascou, Jerôme
Legrésy, Benoit
Lescarmontier, Lydie
author_sort Barruol, Guilhem
title Tide-induced microseismicity in the Mertz glacier grounding area, East Antarctica
title_short Tide-induced microseismicity in the Mertz glacier grounding area, East Antarctica
title_full Tide-induced microseismicity in the Mertz glacier grounding area, East Antarctica
title_fullStr Tide-induced microseismicity in the Mertz glacier grounding area, East Antarctica
title_full_unstemmed Tide-induced microseismicity in the Mertz glacier grounding area, East Antarctica
title_sort tide-induced microseismicity in the mertz glacier grounding area, east antarctica
publisher HAL CCSD
publishDate 2013
url https://hal.univ-reunion.fr/hal-01236143
https://hal.univ-reunion.fr/hal-01236143/document
https://hal.univ-reunion.fr/hal-01236143/file/Barruol_Icequakes_Mertz_Glacier_Antarctica_GRL2013.pdf
https://doi.org/10.1002/2013GL057814
long_lat ENVELOPE(144.500,144.500,-67.667,-67.667)
ENVELOPE(-126.203,-126.203,57.733,57.733)
geographic East Antarctica
Mertz Glacier
Rocky Peak
geographic_facet East Antarctica
Mertz Glacier
Rocky Peak
genre Antarc*
Antarctica
East Antarctica
Mertz Glacier
genre_facet Antarc*
Antarctica
East Antarctica
Mertz Glacier
op_source ISSN: 0094-8276
EISSN: 1944-8007
Geophysical Research Letters
https://hal.univ-reunion.fr/hal-01236143
Geophysical Research Letters, 2013, ⟨10.1002/2013GL057814⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1002/2013GL057814
hal-01236143
https://hal.univ-reunion.fr/hal-01236143
https://hal.univ-reunion.fr/hal-01236143/document
https://hal.univ-reunion.fr/hal-01236143/file/Barruol_Icequakes_Mertz_Glacier_Antarctica_GRL2013.pdf
doi:10.1002/2013GL057814
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1002/2013GL057814
container_title Geophysical Research Letters
container_volume 40
container_issue 20
container_start_page 5412
op_container_end_page 5416
_version_ 1785532504699043840
spelling ftinsu:oai:HAL:hal-01236143v1 2023-12-17T10:21:18+01:00 Tide-induced microseismicity in the Mertz glacier grounding area, East Antarctica Barruol, Guilhem Cordier, Emmanuel Fontaine, Fabrice R., R. Bascou, Jerôme Legrésy, Benoit Lescarmontier, Lydie Institut de Physique du Globe de Paris (IPGP) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS) Laboratoire GéoSciences Réunion (LGSR) Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris) Laboratoire Magmas et Volcans (LMV) Observatoire de Physique du Globe de Clermont-Ferrand (OPGC) Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS) Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) Research School of Earth Sciences Canberra (RSES) Australian National University (ANU) 2013 https://hal.univ-reunion.fr/hal-01236143 https://hal.univ-reunion.fr/hal-01236143/document https://hal.univ-reunion.fr/hal-01236143/file/Barruol_Icequakes_Mertz_Glacier_Antarctica_GRL2013.pdf https://doi.org/10.1002/2013GL057814 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1002/2013GL057814 hal-01236143 https://hal.univ-reunion.fr/hal-01236143 https://hal.univ-reunion.fr/hal-01236143/document https://hal.univ-reunion.fr/hal-01236143/file/Barruol_Icequakes_Mertz_Glacier_Antarctica_GRL2013.pdf doi:10.1002/2013GL057814 info:eu-repo/semantics/OpenAccess ISSN: 0094-8276 EISSN: 1944-8007 Geophysical Research Letters https://hal.univ-reunion.fr/hal-01236143 Geophysical Research Letters, 2013, ⟨10.1002/2013GL057814⟩ [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] info:eu-repo/semantics/article Journal articles 2013 ftinsu https://doi.org/10.1002/2013GL057814 2023-11-22T17:51:01Z International audience The deployment of a seismic network along the Adélie and George V coasts in East Antarctica during the period 2009–2012 provides the opportunity to monitor cryoseismic activity and to obtain new insights on the relationship between tidal cycles and coastal glacier dynamics. Here we focus on records from a seismometer located on a rocky outcrop in the vicinity of the grounding line of the 35 km broad Mertz glacier, a major outflow of this region. We detect numerous icequakes (50,000 events within 10 months and up to 100 events/h) and demonstrate their clear tidal modulation. We suggest that they result from ice friction and fracturing around the rocky peak and from the glacier flexure in response to the falling and rising tides at its grounding area. We propose that such icequake monitoring could be used as a climate proxy since grounding lines are subject to migrate with sea level changes. Article in Journal/Newspaper Antarc* Antarctica East Antarctica Mertz Glacier Institut national des sciences de l'Univers: HAL-INSU East Antarctica Mertz Glacier ENVELOPE(144.500,144.500,-67.667,-67.667) Rocky Peak ENVELOPE(-126.203,-126.203,57.733,57.733) Geophysical Research Letters 40 20 5412 5416