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

J. Paul Winberry, Sridhar Anandakrishnan, Douglas A. Wiens, Richard B. Alley

Research output: Contribution to journalArticle

32 Citations (Scopus)

Abstract

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.

Original languageEnglish (US)
Pages (from-to)312-315
Number of pages4
JournalGeophysical Research Letters
Volume40
Issue number2
DOIs
StatePublished - Jan 28 2013

Fingerprint

tremors
ice stream
Antarctic regions
nucleation
rupture
ice
earthquakes
earthquake
stress propagation
slip
landslides
seismographs
seismograph
beds
landslide
GPS
harmonics
propagation
monitoring
Antarctica

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Earth and Planetary Sciences(all)

Cite this

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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.

In: Geophysical Research Letters, Vol. 40, No. 2, 28.01.2013, p. 312-315.

Research output: Contribution to journalArticle

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