2015
DOI: 10.5194/nhess-15-2545-2015
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Infrasound array criteria for automatic detection and front velocity estimation of snow avalanches: towards a real-time early-warning system

Abstract: Abstract. Avalanche risk management is strongly related to the ability to identify and timely report the occurrence of snow avalanches. Infrasound has been applied to avalanche research and monitoring for the last 20 years but it never turned into an operational tool to identify clear signals related to avalanches. We present here a method based on the analysis of infrasound signals recorded by a small aperture array in Ischgl (Austria), which provides a significant improvement to overcome this limit. The meth… Show more

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Cited by 44 publications
(46 citation statements)
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“…Detecting a stable source position in case of moving sources is not unexpected and is a consequence of infrasound array analysis that, in case of multiple sources, detects preferentially the most energetic one. Such a behavior has been observed already for snow avalanches (Marchetti et al, ) and pyroclastic density currents (Delle Donne et al, ) passing a discontinuity in the topography where infrasound energy radiation focuses in a stable position. However, snow avalanches and pyroclastic density currents produce a coherent infrasonic signal all along their downhill moving front and array analysis allows to clearly track their movement (Delle Donne et al, ; Marchetti et al, ).…”
Section: Discussionsupporting
confidence: 61%
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“…Detecting a stable source position in case of moving sources is not unexpected and is a consequence of infrasound array analysis that, in case of multiple sources, detects preferentially the most energetic one. Such a behavior has been observed already for snow avalanches (Marchetti et al, ) and pyroclastic density currents (Delle Donne et al, ) passing a discontinuity in the topography where infrasound energy radiation focuses in a stable position. However, snow avalanches and pyroclastic density currents produce a coherent infrasonic signal all along their downhill moving front and array analysis allows to clearly track their movement (Delle Donne et al, ; Marchetti et al, ).…”
Section: Discussionsupporting
confidence: 61%
“…Therefore, array processing is not really useful to track and investigate the flow, unless discontinuity points of the topography, such as change of slopes or dams, result in stable sources of infrasound clearly detectable by the array. We suggest therefore that the mechanism of infrasound radiation by debris flow is different from other density currents like snow avalanches or pyroclastic density currents, where a turbulent head develops radiating elastic energy in the atmosphere, that allows to nicely track the flow evolution through time with an infrasound array (e.g., Delle Donne et al, 2014;Marchetti et al, 2015;Ulivieri et al, 2011). Figure 11 shows the mean power spectral density of seismic and infrasound signals for the three debris flow events.…”
Section: Numerical Simulation Of Infrasound Radiated By An Extended Smentioning
confidence: 99%
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“…However, the usage of infrasound for automatic detection of avalanches was rare (Chritin et al 2003;Scott et al 2007;Ulivieri et al 2011), because infrasound is strongly contaminated by noise produced by natural (wind, earthquakes) and artificial sources (planes, helicopters, industry). But the increasing demand for automated avalanche monitoring systems in order to verify artificial avalanche release and for mitigation efforts at facilities and transportation corridors has led to improvement of sensor set-ups, data processing, and algorithms for infrasound avalanche detections in the recent years (Ulivieri et al 2011Thüring et al 2014;Marchetti et al 2015).…”
Section: Infrasound Signals Of Avalanchesmentioning
confidence: 99%
“…In a final step, we therefore used the MUSIC method to estimate the median back-azimuth path, as suggested by Heck et al (2018b), to further dismiss false detections. Similar approaches were 15 suggested for the automatic detection of avalanches in infrasonic data by Marchetti et al (2015) and Thüring et al (2015). In those studies, the back-azimuth of continuous infrasound data was calculated on the fly using cross-correlation techniques, and only events with slight changes in back-azimuth over a predefined minimal duration were assumed as avalanche events.…”
mentioning
confidence: 99%