2013
DOI: 10.1016/j.jvolgeores.2011.09.012
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Combining local and remote infrasound recordings from the 2009 Redoubt Volcano eruption

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Cited by 50 publications
(42 citation statements)
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“…Haney et al (2013) take advantage of this low frequency energy to derive a volumetric source depth of 1.9 km below the crater floor for event 12. Fee et al (2013) note that the infrasonic pulses associated with these later events were more impulsive and shorter in duration than earlier events. The nature of the deposits was also different during this period, exhibiting much finer grain-sizes than deposits from the March 23-24 explosion sequence, although the chemical composition remained unchanged (Wallace et al, 2013).…”
Section: Explosion Seismicitymentioning
confidence: 80%
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“…Haney et al (2013) take advantage of this low frequency energy to derive a volumetric source depth of 1.9 km below the crater floor for event 12. Fee et al (2013) note that the infrasonic pulses associated with these later events were more impulsive and shorter in duration than earlier events. The nature of the deposits was also different during this period, exhibiting much finer grain-sizes than deposits from the March 23-24 explosion sequence, although the chemical composition remained unchanged (Wallace et al, 2013).…”
Section: Explosion Seismicitymentioning
confidence: 80%
“…Fee et al (2013) noted a difference in the infrasonic explosion signal characteristics during this same period and attributed it to a change in eruptive style, from the subplinian-type activity observed during the early phase of the eruption to vulcanian activity. Wallace et al (2013) also observed a change in the tephra componentary, finding much finer grainsizes indicative of more explosive activity following the March 27 swarm.…”
Section: March 27 Swarmmentioning
confidence: 84%
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“…Given two sets of data that could represent our experiment for n observations for two trials a and b, (5) the variance of the individual sets of data is calculated as shown below (set a for example), (6) where  is the mean of the vector a.…”
Section: Disseminationmentioning
confidence: 99%
“…Since the natural attenuation of signals traveling through the atmosphere is a function of a signals frequency, infrasound signals can travel very long distances (thousands of kilometers or more, depending on atmospheric conditions) [6]. As Fig.…”
Section: A Backgroundmentioning
confidence: 99%