Icequake Source Mechanisms for Studying Glacial Sliding ...

Improving our understanding of glacial sliding is crucial for constraining basal drag in ice dynamics models. We use icequakes, sudden releases of seismic energy as the ice slides over the bed, to provide geophysical observations that can be used to aid understanding of the physics of glacial slidin...

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Main Authors: Hudson, TS, Brisbourne, AM, Walter, F, Gräff, D, White, RS, Smith, AM
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union (AGU) 2020
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.59180
https://www.repository.cam.ac.uk/handle/1810/312085
id ftdatacite:10.17863/cam.59180
record_format openpolar
spelling ftdatacite:10.17863/cam.59180 2024-02-04T09:56:03+01:00 Icequake Source Mechanisms for Studying Glacial Sliding ... Hudson, TS Brisbourne, AM Walter, F Gräff, D White, RS Smith, AM 2020 https://dx.doi.org/10.17863/cam.59180 https://www.repository.cam.ac.uk/handle/1810/312085 en eng American Geophysical Union (AGU) open.access All rights reserved http://purl.org/coar/access_right/c_abf2 seismology glaciology cryoseismology icequakes ice dynamics sea level rise Article ScholarlyArticle JournalArticle article-journal 2020 ftdatacite https://doi.org/10.17863/cam.59180 2024-01-05T14:24:00Z Improving our understanding of glacial sliding is crucial for constraining basal drag in ice dynamics models. We use icequakes, sudden releases of seismic energy as the ice slides over the bed, to provide geophysical observations that can be used to aid understanding of the physics of glacial sliding and constrain ice dynamics models. These icequakes are located at the bed of an alpine glacier in Switzerland and the Rutford Ice Stream, West Antarctica, two extremes of glacial settings and spatial scales. We investigate a number of possible icequake source mechanisms by performing full waveform inversions to constrain the fundamental physics and stress release during an icequake stick‐slip event. Results show that double‐couple mechanisms best describe the source for the events from both glacial settings and the icequakes originate at or very near the ice‐bed interface. We also present an exploratory method for attempting to measure the till shear modulus, if indirect reflected icequake radiation is observed. ... Article in Journal/Newspaper Antarc* Antarctica Rutford Ice Stream West Antarctica DataCite Metadata Store (German National Library of Science and Technology) Rutford ENVELOPE(-85.300,-85.300,-78.600,-78.600) Rutford Ice Stream ENVELOPE(-80.000,-80.000,-79.167,-79.167) West Antarctica
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic seismology
glaciology
cryoseismology
icequakes
ice dynamics
sea level rise
spellingShingle seismology
glaciology
cryoseismology
icequakes
ice dynamics
sea level rise
Hudson, TS
Brisbourne, AM
Walter, F
Gräff, D
White, RS
Smith, AM
Icequake Source Mechanisms for Studying Glacial Sliding ...
topic_facet seismology
glaciology
cryoseismology
icequakes
ice dynamics
sea level rise
description Improving our understanding of glacial sliding is crucial for constraining basal drag in ice dynamics models. We use icequakes, sudden releases of seismic energy as the ice slides over the bed, to provide geophysical observations that can be used to aid understanding of the physics of glacial sliding and constrain ice dynamics models. These icequakes are located at the bed of an alpine glacier in Switzerland and the Rutford Ice Stream, West Antarctica, two extremes of glacial settings and spatial scales. We investigate a number of possible icequake source mechanisms by performing full waveform inversions to constrain the fundamental physics and stress release during an icequake stick‐slip event. Results show that double‐couple mechanisms best describe the source for the events from both glacial settings and the icequakes originate at or very near the ice‐bed interface. We also present an exploratory method for attempting to measure the till shear modulus, if indirect reflected icequake radiation is observed. ...
format Article in Journal/Newspaper
author Hudson, TS
Brisbourne, AM
Walter, F
Gräff, D
White, RS
Smith, AM
author_facet Hudson, TS
Brisbourne, AM
Walter, F
Gräff, D
White, RS
Smith, AM
author_sort Hudson, TS
title Icequake Source Mechanisms for Studying Glacial Sliding ...
title_short Icequake Source Mechanisms for Studying Glacial Sliding ...
title_full Icequake Source Mechanisms for Studying Glacial Sliding ...
title_fullStr Icequake Source Mechanisms for Studying Glacial Sliding ...
title_full_unstemmed Icequake Source Mechanisms for Studying Glacial Sliding ...
title_sort icequake source mechanisms for studying glacial sliding ...
publisher American Geophysical Union (AGU)
publishDate 2020
url https://dx.doi.org/10.17863/cam.59180
https://www.repository.cam.ac.uk/handle/1810/312085
long_lat ENVELOPE(-85.300,-85.300,-78.600,-78.600)
ENVELOPE(-80.000,-80.000,-79.167,-79.167)
geographic Rutford
Rutford Ice Stream
West Antarctica
geographic_facet Rutford
Rutford Ice Stream
West Antarctica
genre Antarc*
Antarctica
Rutford Ice Stream
West Antarctica
genre_facet Antarc*
Antarctica
Rutford Ice Stream
West Antarctica
op_rights open.access
All rights reserved
http://purl.org/coar/access_right/c_abf2
op_doi https://doi.org/10.17863/cam.59180
_version_ 1789960403121340416