Nucleation and seismic tremor associated with the glacial earthquakes of Whillans Ice Stream, Antarctica

The ability to monitor transient motion along faults is critical to improving our ability to understand many natural phenomena such as landslides and earthquakes. Here, we usedata from a GPS and seismometer network that were deployed to monitor the regularly repeating glacial earthquakes of Whillans...

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Main Authors: Winberry, J. Paul, Anandakrishnan, Sridhar, Wiens, Douglas A., Alley, Richard B.
Format: Text
Language:unknown
Published: ScholarWorks@CWU 2013
Subjects:
Online Access:https://digitalcommons.cwu.edu/cotsfac/276
https://digitalcommons.cwu.edu/cgi/viewcontent.cgi?article=1276&context=cotsfac
id ftcwashingtonuni:oai:digitalcommons.cwu.edu:cotsfac-1276
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spelling ftcwashingtonuni:oai:digitalcommons.cwu.edu:cotsfac-1276 2023-05-15T13:47:32+02:00 Nucleation and seismic tremor associated with the glacial earthquakes of Whillans Ice Stream, Antarctica Winberry, J. Paul Anandakrishnan, Sridhar Wiens, Douglas A. Alley, Richard B. 2013-01-30T08:00:00Z application/pdf https://digitalcommons.cwu.edu/cotsfac/276 https://digitalcommons.cwu.edu/cgi/viewcontent.cgi?article=1276&context=cotsfac unknown ScholarWorks@CWU https://digitalcommons.cwu.edu/cotsfac/276 https://digitalcommons.cwu.edu/cgi/viewcontent.cgi?article=1276&context=cotsfac © 2013. American Geophysical Union. All Rights Reserved. All Faculty Scholarship for the College of the Sciences harmonic tremor glacial earthquakes ice stream stick‐slip nucleation Earth Sciences Geomorphology Geophysics and Seismology Glaciology Tectonics and Structure text 2013 ftcwashingtonuni 2022-10-20T20:29:10Z The ability to monitor transient motion along faults is critical to improving our ability to understand many natural phenomena such as landslides and earthquakes. Here, we usedata from a GPS and seismometer network that were deployed to monitor the regularly repeating glacial earthquakes of Whillans Ice Stream, West Antarctica to show that a unique pattern of precursory slip precedes complete rupture along the bed of the ice stream. Additionally, we show that rupture can be independently tracked by increased levels of microseismic activity, including harmonic tremor, that are coincident with the onset of slip at any location, thus providing a remote means of monitoring stress and rupture propagation during the glacial earthquakes. Text Antarc* Antarctica West Antarctica Whillans Ice Stream Central Washington University: ScholarWorks West Antarctica Whillans ENVELOPE(-64.250,-64.250,-84.450,-84.450) Whillans Ice Stream ENVELOPE(-145.000,-145.000,-83.667,-83.667)
institution Open Polar
collection Central Washington University: ScholarWorks
op_collection_id ftcwashingtonuni
language unknown
topic harmonic tremor
glacial earthquakes
ice stream
stick‐slip nucleation
Earth Sciences
Geomorphology
Geophysics and Seismology
Glaciology
Tectonics and Structure
spellingShingle harmonic tremor
glacial earthquakes
ice stream
stick‐slip nucleation
Earth Sciences
Geomorphology
Geophysics and Seismology
Glaciology
Tectonics and Structure
Winberry, J. Paul
Anandakrishnan, Sridhar
Wiens, Douglas A.
Alley, Richard B.
Nucleation and seismic tremor associated with the glacial earthquakes of Whillans Ice Stream, Antarctica
topic_facet harmonic tremor
glacial earthquakes
ice stream
stick‐slip nucleation
Earth Sciences
Geomorphology
Geophysics and Seismology
Glaciology
Tectonics and Structure
description The ability to monitor transient motion along faults is critical to improving our ability to understand many natural phenomena such as landslides and earthquakes. Here, we usedata from a GPS and seismometer network that were deployed to monitor the regularly repeating glacial earthquakes of Whillans Ice Stream, West Antarctica to show that a unique pattern of precursory slip precedes complete rupture along the bed of the ice stream. Additionally, we show that rupture can be independently tracked by increased levels of microseismic activity, including harmonic tremor, that are coincident with the onset of slip at any location, thus providing a remote means of monitoring stress and rupture propagation during the glacial earthquakes.
format Text
author Winberry, J. Paul
Anandakrishnan, Sridhar
Wiens, Douglas A.
Alley, Richard B.
author_facet Winberry, J. Paul
Anandakrishnan, Sridhar
Wiens, Douglas A.
Alley, Richard B.
author_sort Winberry, J. Paul
title Nucleation and seismic tremor associated with the glacial earthquakes of Whillans Ice Stream, Antarctica
title_short Nucleation and seismic tremor associated with the glacial earthquakes of Whillans Ice Stream, Antarctica
title_full Nucleation and seismic tremor associated with the glacial earthquakes of Whillans Ice Stream, Antarctica
title_fullStr Nucleation and seismic tremor associated with the glacial earthquakes of Whillans Ice Stream, Antarctica
title_full_unstemmed Nucleation and seismic tremor associated with the glacial earthquakes of Whillans Ice Stream, Antarctica
title_sort nucleation and seismic tremor associated with the glacial earthquakes of whillans ice stream, antarctica
publisher ScholarWorks@CWU
publishDate 2013
url https://digitalcommons.cwu.edu/cotsfac/276
https://digitalcommons.cwu.edu/cgi/viewcontent.cgi?article=1276&context=cotsfac
long_lat ENVELOPE(-64.250,-64.250,-84.450,-84.450)
ENVELOPE(-145.000,-145.000,-83.667,-83.667)
geographic West Antarctica
Whillans
Whillans Ice Stream
geographic_facet West Antarctica
Whillans
Whillans Ice Stream
genre Antarc*
Antarctica
West Antarctica
Whillans Ice Stream
genre_facet Antarc*
Antarctica
West Antarctica
Whillans Ice Stream
op_source All Faculty Scholarship for the College of the Sciences
op_relation https://digitalcommons.cwu.edu/cotsfac/276
https://digitalcommons.cwu.edu/cgi/viewcontent.cgi?article=1276&context=cotsfac
op_rights © 2013. American Geophysical Union. All Rights Reserved.
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