360 likes | 477 Views
Array Geometry and Signal Observations. David A McCormack Head of Monitoring and Analysis Geological Survey of Canada, Ottawa, Canada. Topics. IMS design array response for ‘realistic’ signals – how bad is bad? Initial studies of signal coherence as an indicator of maximum source distance.
E N D
Array Geometry and Signal Observations David A McCormack Head of Monitoring and Analysis Geological Survey of Canada, Ottawa, Canada Infrasound Workshop, Kona
Topics • IMS design array response for ‘realistic’ signals – how bad is bad? • Initial studies of signal coherence as an indicator of maximum source distance Infrasound Workshop, Kona
Array Response • Brown(2000) and Christie(2001) have illustrated problem of significant sidelobes in response pattern of 4-element infrasound array. Christie described response of various geometries with more elements and demonstrated superior characteristics of 7 and 8 element arrays. Infrasound Workshop, Kona
Brown(2000) - 1 0.125 Hz 0.5 Hz Spatial Aliasing: DLIAR Array Infrasound Workshop, Kona
Brown (2000) – 2 1.0 Hz Spatial Aliasing: DLIAR Array 2.0 Hz Infrasound Workshop, Kona
Array Geometry Infrasound Workshop, Kona
SHUTTLE - time Infrasound Workshop, Kona
Shuttle Infrasound Workshop, Kona
Brown(2000) - 3 N IS10 Winnipeg, Canada December 16, 1999 to September 1, 2000 Approximately 4200 detections microbaroms, Hudson Bay ? Local blasting, Too small to register on local seismic ? W E Local blasting Thunder Bay area, too small to register on local seismic mining activity, Minnesota, registers strongly on local seismic microbaroms, Pacific Ocean (?) S Infrasound Workshop, Kona
Sine – 4 elements Infrasound Workshop, Kona
Sine – 7 elements Infrasound Workshop, Kona
Synthetic Signals • Difficult to find narrowband real signals • Synthetic Signals • Bandlimited white noise – identical on each channel – perfectly coherent • Superimposed on a bandlimited white background incoherent between channels • S/N adjustable, duration adjustable Infrasound Workshop, Kona
Synth 0.25-1,4 Infrasound Workshop, Kona
Synth 0.25-1,7 Infrasound Workshop, Kona
Synth 0.4-0.6,4 Infrasound Workshop, Kona
Synth 0.4-0.6,7 Infrasound Workshop, Kona
Summary I • Even for narrow-band signals, side lobes are not large • Suggests more analysis of real events is required before final decisions on cost/benefit of densification should be made Infrasound Workshop, Kona
Signal Coherence • Grew out of studies of optimal array aperture for detection/location • Coherence as a routinely calculated intrinsic parameter of an observed signal Infrasound Workshop, Kona
Local – time series Infrasound Workshop, Kona
Local – freq content Infrasound Workshop, Kona
Local - coherence Infrasound Workshop, Kona
MINNTAC - time Infrasound Workshop, Kona
MINNTAC – freq content Infrasound Workshop, Kona
MINNTAC - coherence Infrasound Workshop, Kona
SHUTTLE - time Infrasound Workshop, Kona
Shuttle – freq content Infrasound Workshop, Kona
Shuttle - coherence Infrasound Workshop, Kona
Pacific Freq Infrasound Workshop, Kona
Pacific Bolide Coherence Infrasound Workshop, Kona
Alberta Freq Infrasound Workshop, Kona
Alberta Bolide Coherence Infrasound Workshop, Kona
Recorded sources Infrasound Workshop, Kona
Processing • Noise corrected under assumption of incoherent noise • Interpolate to 1.5 km station spacing • Ignore differences between radial and transverse coherence (this is wrong) Infrasound Workshop, Kona
Coherence vs distance Infrasound Workshop, Kona
Ms 7.4 Hector Mine, California Earthquake - Acoustic Arrival Infrasound Workshop, Kona
Summary II • Contributions to coherence from source and path • General trend of maximum coherence vs. distance • May be useful for to establish maximum distance to observed source Infrasound Workshop, Kona