A primary goal in volcano seismology is to characterize source motions internal to a volcano in terms of their representative forces. In a similar manner, much volcano infrasound research strives to recover eruptive force time histories corresponding to material accelerations occurring at Earth’s free surface. These motions may correspond to explosive emission of gas and pyroclasts (e.g., Banister, 1984), rapid ground distensions of a volcanic dome (e.g., Johnson and Lees, 2010), and/or gravity driven rock fall or pyroclastic flows (e.g., Yamasato, 1997). When free surface motion is unsteady it imposes stresses upon the surrounding atmosphere, which are propagated as acoustic airwaves. Typically, the sounds produced by volcanic phenomena are recorded with low‐frequency infrasound sensitive microphones. The intervening atmosphere is relatively homogeneous and nonattenuating for infrasound propagation of a few kilometers, therefore the recorded excess pressures closely represent volcano source time functions. Such force time histories are equivalent to volumetric accelerations of the atmosphere at or near to the source. Many volcano explosion signals begin with intense, impulsive bipolar pulses (compression followed by rarefaction) with durations of a few seconds or less (e.g., Morrissey and Chouet, 1997). These volcano explosion waveforms are often similar to chemical explosion signals recorded in the far field and are suggestive of a rapid release and expansion of gases (Kitov et al. , 1997). Several volcano infrasound studies have made use of the Lighthill (1978) simple acoustic source to characterize ejection of fluid from the volcanic vent (e.g., Johnson, 2003). Volcanic explosions generate bipolar infrasound pulses with durations of a few seconds (Firstov and Kravchenko, 1996; Johnson, 2003) that have been attributed to simple acoustic sources. A simple acoustic source, or a monopole, corresponds to a point approximation of fluid injection or extraction. Although most volcanic vents possess length scales of tens of meters to …
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