Abstract
Efficient event detection from large infrasound databases gathered in volcanic settings relies on the availability of robust and automated work-flows. While numerous triggering algorithms for event detection have been proposed in the past, they mostly focus on applications to seismological data. Analyses of acoustic infrasound for signal detection is often performed manually or by application of the traditional short-term average/long-term average (STA/LTA) algorithms, which have shown limitations when applied in volcanic environments, or more generally to signals with poor signal-to-noise ratios. Here, we present a new algorithm specifically designed for automated detection of volcanic explosions from acoustic infrasound data streams. The algorithm is based on the characterization of the shape of the explosion signals, their duration, and frequency content. The algorithm combines noise reduction techniques with automatic feature extraction in order to allow confident detection of signals affected by non-stationary noise. We have benchmarked the performances of the new detector by comparison with both the STA/LTA algorithm and human analysts, with encouraging results. In this manuscript, we present our algorithm and make its software implementation available to other potential users.
Highlights
Seismic and acoustic signals are key in monitoring and characterizing volcanic unrest
Automatic event detection and classification work-flows applied to seismic data include an initial segmentation stage, commonly via the application of short-term average/long-term average (STA/LTA) algorithms in order to parse the continuous seismograms into individual earthquake waveforms with varied characteristics and sources (Allen., 1982)
We have introduced Volcanic INfrasound Explosions Detector Algorithm (VINEDA), an infrasound detector which makes extensive use of signal processing techniques in order to characterize continuous volcano acoustic records and extract explosion signals
Summary
Seismic and acoustic signals are key in monitoring and characterizing volcanic unrest. A wealth of new algorithms are constantly published in the literature in order to improve the efficiency of automatic detection and classification procedures for different types of signals, including those associated with tectonic earthquakes (Di Stefano et al, 2006; Álvarez et al, 2013; Bhatti et al, 2016), low-frequency volcano-seismic events (Frank and Shapiro, 2014), avalanches (Marchetti et al, 2015), and debris flows (Schimmel and Hübl, 2016) These algorithms represent an important toolbox for the creation of high-quality research databases
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