Assessment of glacial-earthquake source parameters

Glacial earthquakes are slow earthquakes of magnitude M~5 associated with major calving events at near-grounded marine-terminating glaciers. These globally detectable earthquakes provide information on the grounding state of outlet glaciers and the timing of large calving events. Seismic source mode...

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Published in:Journal of Glaciology
Main Authors: STEPHEN A. VEITCH, MEREDITH NETTLES
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2017
Subjects:
Online Access:https://doi.org/10.1017/jog.2017.52
https://doaj.org/article/c929174a564748e19332a47020fad149
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spelling ftdoajarticles:oai:doaj.org/article:c929174a564748e19332a47020fad149 2023-05-15T16:21:14+02:00 Assessment of glacial-earthquake source parameters STEPHEN A. VEITCH MEREDITH NETTLES 2017-10-01T00:00:00Z https://doi.org/10.1017/jog.2017.52 https://doaj.org/article/c929174a564748e19332a47020fad149 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143017000521/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2017.52 0022-1430 1727-5652 https://doaj.org/article/c929174a564748e19332a47020fad149 Journal of Glaciology, Vol 63, Pp 867-876 (2017) calving cryoseismology glacier geophysics ice/ocean interactions remote sensing seismology Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2017 ftdoajarticles https://doi.org/10.1017/jog.2017.52 2023-03-12T01:30:59Z Glacial earthquakes are slow earthquakes of magnitude M~5 associated with major calving events at near-grounded marine-terminating glaciers. These globally detectable earthquakes provide information on the grounding state of outlet glaciers and the timing of large calving events. Seismic source modeling of glacial earthquakes provides information on the size and orientation of forces associated with calving events. We compare force orientations estimated using a centroid-single-force technique with the calving-front orientations of the source glaciers at or near the time of earthquake occurrence. We consider earthquakes recorded at four glaciers in Greenland – Kangerdlugssuaq Glacier, Helheim Glacier, Kong Oscar Glacier, and Jakobshavn Isbræ – between 1999 and 2010. We find that the estimated earthquake force orientations accurately represent the orientation of the calving front at the time of the earthquake, and that seismogenic calving events are produced by a preferred section of the calving front, which may change with time. We also find that estimated earthquake locations vary in a manner consistent with changes in calving-front position, though with large scatter. We conclude that changes in glacial-earthquake source parameters reflect true changes in the geometry of the source glaciers, providing a means for identifying changes in glacier geometry and dynamics that complements traditional remote-sensing techniques. Article in Journal/Newspaper glacier Greenland Jakobshavn Jakobshavn isbræ Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Greenland Jakobshavn Isbræ ENVELOPE(-49.917,-49.917,69.167,69.167) Journal of Glaciology 63 241 867 876
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic calving
cryoseismology
glacier geophysics
ice/ocean interactions
remote sensing
seismology
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle calving
cryoseismology
glacier geophysics
ice/ocean interactions
remote sensing
seismology
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
STEPHEN A. VEITCH
MEREDITH NETTLES
Assessment of glacial-earthquake source parameters
topic_facet calving
cryoseismology
glacier geophysics
ice/ocean interactions
remote sensing
seismology
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description Glacial earthquakes are slow earthquakes of magnitude M~5 associated with major calving events at near-grounded marine-terminating glaciers. These globally detectable earthquakes provide information on the grounding state of outlet glaciers and the timing of large calving events. Seismic source modeling of glacial earthquakes provides information on the size and orientation of forces associated with calving events. We compare force orientations estimated using a centroid-single-force technique with the calving-front orientations of the source glaciers at or near the time of earthquake occurrence. We consider earthquakes recorded at four glaciers in Greenland – Kangerdlugssuaq Glacier, Helheim Glacier, Kong Oscar Glacier, and Jakobshavn Isbræ – between 1999 and 2010. We find that the estimated earthquake force orientations accurately represent the orientation of the calving front at the time of the earthquake, and that seismogenic calving events are produced by a preferred section of the calving front, which may change with time. We also find that estimated earthquake locations vary in a manner consistent with changes in calving-front position, though with large scatter. We conclude that changes in glacial-earthquake source parameters reflect true changes in the geometry of the source glaciers, providing a means for identifying changes in glacier geometry and dynamics that complements traditional remote-sensing techniques.
format Article in Journal/Newspaper
author STEPHEN A. VEITCH
MEREDITH NETTLES
author_facet STEPHEN A. VEITCH
MEREDITH NETTLES
author_sort STEPHEN A. VEITCH
title Assessment of glacial-earthquake source parameters
title_short Assessment of glacial-earthquake source parameters
title_full Assessment of glacial-earthquake source parameters
title_fullStr Assessment of glacial-earthquake source parameters
title_full_unstemmed Assessment of glacial-earthquake source parameters
title_sort assessment of glacial-earthquake source parameters
publisher Cambridge University Press
publishDate 2017
url https://doi.org/10.1017/jog.2017.52
https://doaj.org/article/c929174a564748e19332a47020fad149
long_lat ENVELOPE(-49.917,-49.917,69.167,69.167)
geographic Greenland
Jakobshavn Isbræ
geographic_facet Greenland
Jakobshavn Isbræ
genre glacier
Greenland
Jakobshavn
Jakobshavn isbræ
Journal of Glaciology
genre_facet glacier
Greenland
Jakobshavn
Jakobshavn isbræ
Journal of Glaciology
op_source Journal of Glaciology, Vol 63, Pp 867-876 (2017)
op_relation https://www.cambridge.org/core/product/identifier/S0022143017000521/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2017.52
0022-1430
1727-5652
https://doaj.org/article/c929174a564748e19332a47020fad149
op_doi https://doi.org/10.1017/jog.2017.52
container_title Journal of Glaciology
container_volume 63
container_issue 241
container_start_page 867
op_container_end_page 876
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