Title: Location and Characterization of Infrasonic Events
1Location and Characterization of Infrasonic
Events
- Roger Bowman1, Greg Beall1, Doug Drob2, Milton
Garces3, Claus Hetzer3, Michael OBrien1, Gordon
Shields1 - 1. Science Applications International Corporation
- 2. Naval Research Laboratory
- 3. University of Hawaii
- Infrasound Technology Workshop
- University of California, San Diego
- October 27-30, 2003
2Outline
- Challenges
- Approach
- Data sets
- Atmospheric models
- Travel-time tables
- Characterization and visualization
- Ongoing work
- Summary
3Challenges in Infrasound Monitoring
Propagation
Source
Receiver
4Location Approach
Stations
Signal observations
HWM/ MSISE models
Ray tracing (tau-p)
Travel-time tables
Location algorithm
Event locations
Uncertainty estimation
NRL G2S models
Travel-time tables
Ray tracing (tau-p)
Arrival times Azimuths
Canonical location data set
Location evaluation
Event times
5Project Network
- All stations available in June 2003
6Canonical Location Data Set
- Focuses on signals with ground truth locations
- Waveforms and arrivals
- Multiple station detections
- For assessing location, azimuth, and travel-time
estimates - Chemical explosions GT1-101 (3 events)
- Moving sources GT100 (3 events)
- Single station detection
- For assessing azimuth and travel-time estimates
- Mining explosions GT10-15 (5 events)
- Chemical explosions GT1-20 (5 events)
- Gas pipe explosion GS1 (1 events)
- Earthquakes GT5-10 (2 events)
1. Ground Truth with accuracy of 1 km 10 km
7Atmospheric Models
8Atmospheric Models (2)
- Meridional winds for a location in the southwest
United States - 0000 UT for January 1-25, 2003
9Travel-Time Tables PIDC
- Prototype International Data Center (PIDC) ca.
2001 - Use HWM and MSISE climatological models
- Horizontal Wind Model (HWM)
- Mass Spectrometer, Incoherent Scatter Extended
(MSISE) - Use David Browns ray tracing program
- Include travel times for I phase only
- Depend on azimuth and season
- 1o azimuthal resolution 1.8o radial resolution
- Use uncertainties based on possible phase
misidentification
10Travel-Time Tables Automatic Processing
- Use HWM/MSISE climatological models
- Use Milton Garces tau-p ray tracing program
- Include travel times for stratospheric (Is),
thermospheric (It) and undetermined (I) phases - Depend on azimuth, month and time of day
- 19 stations x 4 times of day x 12 months x 3
phases 2,736 tables! - 1o azimuthal resolution 1.5o radial resolution
- 0o-120o range
- Use uncertainties based on variability of G2S
models for each month
11HWM/MSISE Travel-Time Table DLIAR
- January
- 0000 UT
- Back-azimuth 200o
- 2 out of 33,840 curves
12HWM/MSISE Travel-Time Table DLIAR
- 0000 UT
- Is phases do not exist for some azimuths
- Longer travel times westbound from source to
receiver
13HWM Travel-Time Uncertainties
- Non-Gaussian distribution of predicted travel
times - Scatter in modeled travel times increases
monotonically with range
- Characterize uncertainty by standard deviation at
two ranges - Interpolate for other ranges
14Accounting for Range Dependence
- Accounts for variation of atmospheric model along
range - Use 1-D ray tracing for four models along profile
- Final curve is 4th degree polynomial
15Travel-Time Tables Interactive Analysis
- Use Naval Research Laboratorys Ground-to-Space
(G2S) models - Dependent on azimuth, date and time of day
- Tables calculated for stations as needed
- Include travel times for stratospheric (Is),
thermospheric (It) and undetermined (I) phases - Use uncertainties based on variability of
travel-time with take off angle for G2S models
for each month
16G2S Travel-Time Table DLIAR
- 1000 km range
- January 23, 2003
- 2000 UT
- Similar to HWM travel times
17HWM and G2S Travel Time Tables
- 2000 km range
- January 23, 2003 2000 UT.
- January, 1800 UT
- Azimuth range for existence of Is phases differs
- All G2S travel times are larger than HWM in this
example
18Source-Size Estimation
- Implemented Brown (1999) formula in libmagnitude
- M log10P 1.36log10R 0.019v
- Where
- P is pressure
- R is range
- v is wind velocity
- Preliminary version uses wind at infrasound
stations from G2S model
19Visualization Tools for Characterization
- libinfra
- libPMCC
- Spectrograms
Feature Plotting
Infra Event Mapping
Array Tool
Analyst Review Station
Feature Animation
- Seismic
- Hydroacoustic
- Infrasound
- Frequency
- Apparent velocity
- Azimuth
20Infra Mapping Tool
- Supports tip-and-queue processing
- Integrated with Analyst Review Station (ARS)
- Arrival information sent back and forth
- Zoom capability
- Topography resolution varies with map scale
21Array Tool - Features
- Watusi explosion at NTS
- libPMC features
- libinfra features
- Waveforms
22Array Tool - Spectrograms
- Watusi explosion at NTS
- Standard spectrogram
- Coherence spectrogram separates coherent signal
from incoherent noise - Waveforms
Array Tool
23Feature Animation Tool
- Maps features to
- x-axes
- y-axes
- Color
- Saturation
- Animation sequence
- Supports 3-D animations
24Feature Animation Tool (2)
can animate over any variable
0.8 Hz
4.8 Hz
25Ongoing Work
- Location
- Test location algorithm using new travel time
curves - Complete travel-time tables for location event
data set - Quantify changes in capability to estimate
location and azimuth - Characterization
- Validate feature measurements
- Complete prototype analysis tool
26Summary
- Data sets
- Assembled a database of ground-truth events for
use in evaluating infrasound source location
estimates - Location
- Defined a framework for using climatological and
meteorological atmospheric models for location
estimation - Calculated travel-time tables based on HWM/MSISE
for each station, month and 4 times/day - Calculated travel-time tables based on G2S for
each event/station in the location data set - Enhanced location programs to accept
station/date/time dependent travel times
26
27Summary (2)
- Characterization and Visualization
- Implemented source-size estimation (strongly
dependent on wind) - Developed prototype visualization tools for
infrasound data feature analysis
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