Geophysics · 1998 · 22 citations · 7 references
EngineeringComputational EngineeringAcousticsOcean AcousticsPropagationAcoustic MeasurementArray ProcessingDigital Signal ProcessingHydrophone ArraysNoiseUltrasonicsAcoustic Slowness AnalysisAcoustic Slowness MeasurementArray DesignDispersive MediaNoise Quality AssessmentNoncentral DistributionsReceiver Array DesignSeismic Array Processing
Abstract Semblance provides a quality indicator for beam-former array processing methods such as slowness/time coherence (STC) and dispersive STC (DSTC). Semblance does not indicate the slowness variance because the array design, the processing time-bandwidth parameters, and the signal spectral content are not taken into account. For the classical case of a single propagating wave with added Gaussian noise, semblance is distributed according to the noncentral beta distribution. This distribution is parameterized by the number of receivers, M, the processing time-bandwidth product, BT, and signal-to-noise ratio. Given M and BT, the measured semblance can be inverted to give a high-quality estimate of the signal-to-noise ratio. The Cramer-Rao lower bounds on slowness variance for the classical case of signals in added Gaussian noise depend on the array dimensions, the signal power spectrum, and the signal-to-noise ratio. Estimates of the Cramer-Rao bounds can be calculated from the estimated signal-to-noise ratio and the measured signal power spectrum. Monte-Carlo simulations show that these bounds approximate the actual slowness variance for high, but practical, signal-to-noise ratios. Preliminary results on field data show that error bars based on Cramer-Rao bounds are credible, and that error bars yield slowness standard deviations comparable to those from repeat runs.
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Handbook of Mathematical Functions
Donald A. McQuarrie · American Journal of Physics · 1966 · 40.9K citations
An automatic event detector at the Tonto Forest Seismic Observatory
Robert R. Blandford · Geophysics · 1974 · 126 citations