Thunderquakes enable seismic imaging of Earth's shallow subsurface
Seismic waves produced by thunderstorms, called thunderquakes, can be used as a novel source for seismic imaging, according to a new study led by researchers at Penn State.
A seismic wave is an elastic disturbance that propagates through the Earth or along its surface as a result of sudden stress changes, typically from fault rupture, volcanic activity, or anthropogenic sources such as explosions. Governed by the equations of elastodynamics, seismic waves are categorized into body waves (P and S waves) and surface waves (Rayleigh and Love waves), each with distinct particle motion, dispersion, and attenuation characteristics. Their propagation properties—velocity, amplitude, frequency content, and scattering—are strongly controlled by the elastic moduli, density, anisotropy, and heterogeneity of the medium, making seismic waves a primary observational phenomenon in seismology and Earth structure studies.
Seismic waves produced by thunderstorms, called thunderquakes, can be used as a novel source for seismic imaging, according to a new study led by researchers at Penn State.
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