Assessing the detection capability of the International Monitoring System infrasound network
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Transcript of Assessing the detection capability of the International Monitoring System infrasound network
Page 1British Crown Copyright 2008/MOD
Assessing the detection capability of the International Monitoring System infrasound network
David Green and David Bowers
AWE Blacknest
Page 2British Crown Copyright 2008/MOD
Assessing the detection capability of the International Monitoring System infrasound network
AWE Blacknest
Talk Outline
David Green and David Bowers
1. Previous Models
2. Extensions - Noise
- Array Processing
- Stratospheric Wind
- Frequency Dependence
3. Results
4. Comparison to observed: Gerdec Explosions
Page 3British Crown Copyright 2008/MOD
Previous Work
IMS infrasound network
• 60 stations when complete
• 37 arrays as of July 2007
+( )
( )
Previous models:• incorporate Yield vs. Amplitude relationships• incorporate noise measurements• no wind incorporated
(e.g., Clauter and Blandford, 1998, Stevens et al. 2002)
(following Stevens et al. 2002)
Page 4British Crown Copyright 2008/MOD
Extended Model Components
Noise
(Bowman et. al, 2007)
Array Processing
SNR enhancements
Amplitude dependence on:
1. Yield
2. Stratospheric Wind Conditions
(Whitaker et al. 2003)
Frequency Dependence
(Noise Models and Yield Relationships)
Network Completeness
Detection Capability
Page 5British Crown Copyright 2008/MOD
The Model
• Calculate the probability, Pijk, that a signal will be detected at station i for an event k occurring at location j.
• Assume that noise distribution is taken as log-normal (after e.g., Clauter and Blandford, 1998)
• We define the detection threshold as the yield at which the probability of detecting an event at two or more stations in the network exceeds 0.9.
Pdetect = 1 − Pno detect − Pone detec
Prob. of detection Probability of no detectionacross network
Probability of detection atonly one station across network
Page 6British Crown Copyright 2008/MOD
The Model
The probability that a signal will be detected at station i for an event k occurring at location j.
Station reliability
Uncertainities in signaland noise amplitude
The predicted signal-to-noiseratio at the station.
The signal-to-noise level atwhich a detection can bemade divided by signal-to-noise improvement from beamforming.
We use a single channel signal-to-noise ratio = 1 for thecalculations shown.
(log10-log10)
Page 7British Crown Copyright 2008/MOD
Noise Models Used
(Bowman et. al, 2007)
• Used noise models from Bowman et. al, 2007
• An analysis of 39 stations (34 IMS)- 44 months of data used
• Figure to right shows median spectra (solid line) and the 5th and 95th percentile spectra (dotted lines).
• In our detection capability models we assume time-independent, station-independent noise model
Extending to time and location dependent models is anecessary future improvement (already implemented byLe Pichon et al, 2008).
Page 8British Crown Copyright 2008/MOD
Array Processing: Signal-to-Noise Improvements
Neyshabur Train Explosion recorded at I31KZ (1 to 5 Hz)
Christmas Island BolideRecorded at I04AU (0.1 to 0.5Hz)
Beam
Single Channel
Signal Window Pre-event noise
• A study of 6 events showed gains of between 0.7 and 1.1 x √n (where n = no. of array elements)
• For all modelling, used value of 0.9√n
Page 9British Crown Copyright 2008/MOD
Frequency Dependence
• At what frequency should we take our noise estimates?
• Are different size sources going to be preferentially observed at different frequencies?
or
e.g., AFTAC Yield (Y) vs. Period (t) Equation
Source to Receiverrange = 1000km
• Can combine with the Whitaker Yield vs. Amplitude relation to give Frequency vs. Amplitude relation.
Page 10British Crown Copyright 2008/MOD
Adding the Stratospheric Wind: 59 Station Network
90% Detection Threshold (2 station)for the 59 station network.Noise from Bowman (2007) model,taken at 0.1Hz.
Page 11British Crown Copyright 2008/MOD
37 Station Network (Operational in 2007)
90% Detection Threshold (2 stat.)for the 37 station network.Noise from Bowman (2007) model, taken at 0.1Hz.
Page 12British Crown Copyright 2008/MOD
Comparing 37 and 59 Station Networks
New York, 37 Stat.
New York, 59 Stat.Nov. Zemlya, 59 Stat.
Nov. Zemlya, 37 Stat.
• Incomplete network – decrease detection prob. at specific locations value dependent upon: 1. the completeness of the regional network 2. the influence of the dominant wind directions.
Solid lines: with wind
Dotted lines: without wind
Page 13British Crown Copyright 2008/MOD
Location Capability : Influence of Stratospheric Wind
With less wind - the angle of separation of the two detecting stations tends to be greater - the source to second receiver distance tends to be less
No Wind High Wind
Including wind – better detection capability, but apparently harder to locate source
Page 14British Crown Copyright 2008/MOD
Frequency Dependence
(Noise from AFTAC relation – indicates that the frequency at which the noise is taken from theBowman et. al (2007) model is determined using the AFTAC yield vs. period relation).
If noise variation with frequency is taken into account:- at low yields, achieve better global detections because of lower noise- if comparing with a single noise value (at 0.1Hz), only at the microbarom peak does the variable noise model perform less well than the frequency varying noise
Equivalent
diagrams
Page 15British Crown Copyright 2008/MOD
Comparison with Gerdec Explosion Observations
Dom.SignalFreq.
Gerdec, Albania:• 2 large munitions dump explosions• 15th March 2008• Highest SNR ~ 0.5Hz• Signal Power down to periods of ~30s
Future IMS station
Detecting IMS station
Detecting non-IMS
Non-detecting non-IMS
Decreasingyield
=Decreasingprobability ofsingle stationdetection.
Page 16British Crown Copyright 2008/MOD
Comparison with Gerdec Explosion Observations
Green and Bowers, 2008
Le Pichon et al., 2008
Tons (TNT)
(see Alexis’ talk)
Two independent models. Converge to very similar results.
Adapted to incorporate:• ECMWF wind model• measured noise levels
Uncertainties reduced tosimulate deterministicapproach.
A more deterministicapproach.
Can compare and contrast techniques; underlying empirical models are identical
Page 17British Crown Copyright 2008/MOD
Conclusions
• Inclusion of stratospheric wind makes detection capability time dependent.
• Inclusion of stratospheric wind tends to improve detection capability, but hinders location capability for low yield explosions.
• The completeness of the IMS network is vital for ensuring global coverage.
• The frequencies of interest should be considered when calculating the network detection capability.
• Model presented here is relatively simple in design; future improvements will include:
• More accurate atmospheric parameterisation
• Array-dependent wind noise
• Improved understanding of 1. Yield vs. Pressure2. Yield vs. Period
Page 18British Crown Copyright 2008/MOD
References and Acknowledgements
Acknowledgements
Fruitful discussions with Alexis Le Pichon, Lars Ceranna, Laslo Evers and JulienVergoz helped improve this work, and highlighted possible avenues for future work.
We thank Roger Bowman (SAIC) for providing us with the noise model across theIMS infrasound network.
Green, D. N., Assessing the detection capability of the International Monitoring System infrasound network AWE Report 629/08 (2008) (Available on request, [email protected])
Le Pichon, A. et al. Assessing the performance of the International Monitoring System infrasound network: Geographical coverage and temporal variabilities JGR – Atmospheres (in press, 2008)
Bowman, J. R. et al. Infrasound Station Ambient Noise Estimates and Models: 2003-2006Infrasound Technology Workshop, Tokyo, November 2007
Clauter, D. and Blandford, R. Capability Modelling of the Proposed International Monitoring System 60-Station Infrasonic Network. In Infrasound Workshop for CTBT, pages 215–225, Santa Fe, New Mexico, USA, August 25-28, 1997, (1998) LANL. LA-UR-98-56.
Stevens, J.L., Divnov, I.I., Adams, D.A., Murphy, J.R., and Bourchik, V.N. Constraints on Infrasound Scalingand Attenuation Relations from Soviet Explosion Data. Pageoph, 159, 1045–1062, (2002).Whitaker, R. W., Sondoval, T. D., and Mutschlecner, J. P. Recent Infrasound Analysis. In Proceedings of the 25th Annual Seismic Research Symposium in Tuscon, AZ, pages 646–654, (2003).
Page 19British Crown Copyright 2008/MOD
From Probabilistic to Deterministic
When comparing Le Pichon et al. (2008), and Green and Bowers (2008)
‘We are confident that we can predict noise levels and stratospheric wind values’
and
‘We are confident that our empirical models provide the correct yield/pressure relationship’
Problem: how to correctly assess the uncertainties.
By moving towards the deterministic model, we are saying: