Acoustic waves can travel vast distances in planetary atmospheres. These waves convey information both on the source that generated them as well as the properties of the medium they travel through. On Earth, these acoustic waves typically fall in the "infrasound" range (<20 Hz, the lower limit of human hearing), since higher frequency waves attenuate more quickly. Infrasound waves can circle the globe multiple times given a powerful enough source (Le Pichon et al., 2013;Symons, 1888).A variety of natural and anthropogenic phenomena gives rise to infrasound. Discrete natural events such as bolide airbursts (Ens et al., 2012;Silber et al., 2009), large earthquakes (Le Pichon et al., 2005;Shani-Kadmiel et al., 2021), and volcanic eruptions (Fee & Matoza, 2013) create signals that can travel over regional to global scales. Other activity such as colliding ocean waves (the "ocean microbarom") (Waxler & Gilbert, 2006), wind blowing over mountains (Bedard, 1978;Walterscheid & Hickey, 2005), and severe storms (Goerke & Woodward, 1966) can create long duration signals that comprise much of the Earth's infrasonic background at low frequencies. Regional to local infrasound (and occasionally audible emissions) have been reported from small earthquakes (