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

The deployment of a seismic network along the Adelie 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...

Full description

Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Barruol, Guilhem, Cordier, Emmanuel, Bascou, Jerome, Fontaine, Fabrice R., Legresy, Benoit, Lescarmontier, Lydie
Format: Article in Journal/Newspaper
Language:English
Published: Amer Geophysical Union 2013
Subjects:
Online Access:https://archimer.ifremer.fr/doc/00244/35567/34098.pdf
https://doi.org/10.1002/2013GL057814
https://archimer.ifremer.fr/doc/00244/35567/
id ftarchimer:oai:archimer.ifremer.fr:35567
record_format openpolar
spelling ftarchimer:oai:archimer.ifremer.fr:35567 2023-05-15T13:50:50+02:00 Tide-induced microseismicity in the Mertz glacier grounding area, East Antarctica Barruol, Guilhem Cordier, Emmanuel Bascou, Jerome Fontaine, Fabrice R. Legresy, Benoit Lescarmontier, Lydie 2013-10 application/pdf https://archimer.ifremer.fr/doc/00244/35567/34098.pdf https://doi.org/10.1002/2013GL057814 https://archimer.ifremer.fr/doc/00244/35567/ eng eng Amer Geophysical Union https://archimer.ifremer.fr/doc/00244/35567/34098.pdf doi:10.1002/2013GL057814 https://archimer.ifremer.fr/doc/00244/35567/ 2013. American Geophysical Union. All Rights Reserved. info:eu-repo/semantics/openAccess restricted use Geophysical Research Letters (0094-8276) (Amer Geophysical Union), 2013-10 , Vol. 40 , N. 20 , P. 5412-5416 icequakes Mertz glacier tide Antarctica cryoseismology Adélie land text Publication info:eu-repo/semantics/article 2013 ftarchimer https://doi.org/10.1002/2013GL057814 2021-09-23T20:25:36Z The deployment of a seismic network along the Adelie 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 Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) 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
institution Open Polar
collection Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer)
op_collection_id ftarchimer
language English
topic icequakes
Mertz glacier
tide
Antarctica
cryoseismology
Adélie land
spellingShingle icequakes
Mertz glacier
tide
Antarctica
cryoseismology
Adélie land
Barruol, Guilhem
Cordier, Emmanuel
Bascou, Jerome
Fontaine, Fabrice R.
Legresy, Benoit
Lescarmontier, Lydie
Tide-induced microseismicity in the Mertz glacier grounding area, East Antarctica
topic_facet icequakes
Mertz glacier
tide
Antarctica
cryoseismology
Adélie land
description The deployment of a seismic network along the Adelie 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.
format Article in Journal/Newspaper
author Barruol, Guilhem
Cordier, Emmanuel
Bascou, Jerome
Fontaine, Fabrice R.
Legresy, Benoit
Lescarmontier, Lydie
author_facet Barruol, Guilhem
Cordier, Emmanuel
Bascou, Jerome
Fontaine, Fabrice R.
Legresy, 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 Amer Geophysical Union
publishDate 2013
url https://archimer.ifremer.fr/doc/00244/35567/34098.pdf
https://doi.org/10.1002/2013GL057814
https://archimer.ifremer.fr/doc/00244/35567/
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 Geophysical Research Letters (0094-8276) (Amer Geophysical Union), 2013-10 , Vol. 40 , N. 20 , P. 5412-5416
op_relation https://archimer.ifremer.fr/doc/00244/35567/34098.pdf
doi:10.1002/2013GL057814
https://archimer.ifremer.fr/doc/00244/35567/
op_rights 2013. American Geophysical Union. All Rights Reserved.
info:eu-repo/semantics/openAccess
restricted use
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_ 1766254134144532480