Several sources of interest often generate both low‐frequency acoustic and seismic signals
due to energy propagation through the atmosphere and the solid Earth. Seismic and …

Infrasound waveforms generated by natural and anthropogenic phenomena contain
important clues about the size and nature of the event. We show that sensors on balloons in …

Seismoacoustic signals at local distance (<∼ 10 km) are widely used as important
constraints on source parameters for near‐surface events, yet the seismoacoustic wave …

Shallow sediments can respond non‐linearly to large dynamic strains and undergo a
subsequent healing phase as the material gradually recovers following the passing of …

Infrasound generated by earthquakes and explosions is generally detected at receivers at
epicentral distances of hundreds to thousands of kilometers. However, proximal (< 50 km) …

Volcanic explosions can produce large, ash-rich plumes that pose great hazard to aviation,
yet may often have few precursory geophysical signals. Mount Cleveland is one of the most …

We invert infrasonic timeseries produced by a single buried chemical explosion detonated
as part of the Source Physics Experiment phase II Dry Alluvium Geology (DAG). The key to …

The Dry Alluvium Geology (DAG) project was Phase II of the Source Physics Experiment and
consisted of a series of four chemical explosive tests conducted in the same source hole on …

Acoustic source inversions estimate the mass flow rate of volcanic explosions or yield of
chemical explosions and provide insight into potential source directionality. However, the …

Earthquakes have repeatedly been shown to produce inaudible acoustic signals (< 20 Hz),
otherwise known as infrasound. These signals can propagate hundreds to thousands of …