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An Analysis of Glacial Earthquakes

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Symmetric Double Boxcar. Kawakatsu 1989. Fitting Seismic Data ... Calculate Double Boxcar Synthetic Seismograms. Revise Parameters. Guess Initial Location, Time ... – PowerPoint PPT presentation

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Title: An Analysis of Glacial Earthquakes


1
An Analysis of Glacial Earthquakes
  • Victor C. Tsai
  • Göran Ekström
  • Department of Earth and Planetary Sciences
  • Harvard University

2
What are Glacial Earthquakes?
  • Ekström et al., 2003
  • MS 4.6 5.1
  • Away from plate boundaries
  • Lack high freq. radiation
  • Radiation patterns incompatible with standard
    earthquake focal mechanisms
  • Seasonality more events in summer months

1993-2004 Events
3
A Simple Model
Force
Symmetric Double Boxcar
Kawakatsu 1989
4
Fitting Seismic Data
Select Seismograms to Use in Inversion
Guess Initial Location, Time
Calculate Double Boxcar Synthetic Seismograms
Revise Parameters
Invert for best Source Parameters by Minimizing
Misfit
  • Results
  • Improved location and time
  • Force amplitude and direction
  • Massdistance 0.12 2.04 1014 kgm
  • 10 km3 moving 10 m

5
Glacial Earthquake Locations
Before Relocations After Relocations
6
Comparison with Icesheet Velocities
Bamber et al. 2001
7
Detailed Location
Rignot et al. 2004
Region 1 - Kangerdlugssuaq
10 km
8
Force Directions
Rignot et al. 2004
Region 1 - Kangerdlugssuaq
10 km
9
Force Directions
Region 2 - Helheim
Rignot et al. 2004
10 km
10
Why backwards forces?
  • Modeled Force Actual
    Force
  • Modeled Seismogram Data Seismogram

Easy to have 180 phase shift
11
Size Distribution
12
Size Distribution Comparison
13
Conclusions
  • 182 Glacial Earthquakes
  • Occur only in regions of very high ice flow, but
    not in all of these regions
  • Force directions consistent with the sense of
    glacial motion
  • Amplitudes correspond to
  • 10 km3 sliding 10 m
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