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Recent Developments in Analyzing Infrasonic Signals Observed at I55US

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Title: Recent Developments in Analyzing Infrasonic Signals Observed at I55US


1
Recent Developments in Analyzing Infrasonic
Signals Observed at I55US
  • Kenneth M. Arnoult, John V. Olson,
  • Charles R. Wilson, C. A. L. Szuberla,
  • and D. Osborne
  • Infrasound Group, University of Alaska Fairbanks

Presented at the Infrasound Technology
Workshop Scripps Research Institute, UC San Diego
2
I55US Windless Bight, Antarctica
I55US, the CTBT infrasound site, is located on
the Ross ice shelf approximately 30 km from
McMurdo base.
3
CTBT Array Geometry
The UAF CTBT installations are constructed using
8 sensors in the form of a pentagram surrounding
a triangle. This provides broad-band coverage of
the k-spectrum. Data are taken at 20 Hz.
4
Previously Explained Signals
  • Strombolian Signals from Erebus
  • Signals from Vee Cliffs
  • Mountain Associated Waves (MAWs) from New Zealand
  • Microbaroms

5
Strombolian signal from Erebus
Mt. Erebus, located approximately 25 km from the
infrasound site, is an active volcano producing
occasional small strombolian eruptions.
6
Strombolian signal from Erebus
  • Statistics for 1 year
  • 182 signals observed
  • ( 1 signal every 2 days)
  • Trace Velocity
  • 320.5 /- 6.32 m/s
  • Azimuth
  • 336.5 /- 0.39o
  • Duration
  • 5 s

Sensors
Overlay
7
Vee Cliffs Ice Avalanche
  • Common Characteristics
  • Trace velocity
  • 327.4 /- 1.5 m/s
  • Azimuth
  • 19.0 /- 2.0o
  • Duration
  • 10s 30s

Sensors
Overlay
8
Mountain Associated Wavesfrom New Zealand
  • Common Characteristics
  • Frequency
  • 0.015 0.100 Hz
  • Duration
  • Hours to Days
  • Low correlation
  • Seasonal Variation

Sensors
Overlay
9
Microbaroms
  • Common Characteristics
  • Frequency
  • 0.2 Hz
  • Low Spatial Correlation
  • Seasonal Variation

Inner 3 Sensors
Overlay
10
Recently Explained Signals
  • Signals from Erebus Tremors
  • Signals from Ice Shelf/Island Interface

11
Signal from Erebus Tremors
  • 4 Signals Observed
  • Trace Velocity
  • 329.5 /- 3.0 m/s
  • Azimuth
  • 340.0 /- 0.78o
  • Average Amplitude
  • 0.01 Pa

Inner 3 Sensors
Overlay
12
Ice Shelf Signal
  • Common Characteristics
  • Azimuth
  • - Highly Variable
  • - Usually Northern
  • Duration
  • 5s 30s
  • Highly Variable Waveforms
  • High Correlation

Sensors
Overlay
13
Locator function
  • Assumptions
  • Spherical wave propagation
  • (Temperature is constant and uniform)
  • No wind
  • Earth is flat
  • Precise Tau Precise Location
  • Sampling Delta Tau Ovals

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Summary
  • Erebus Study
  • Recently Explained Signals
  • Signals from Erebus Tremors
  • Signals from Ice Shelf/Island Interface
  • Near Field Source Locator
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