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Updated: Oct 22, 2025

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Published on: October 13, 2023
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The First Detection of an Earthquake From a Balloon Using Its Acoustic Signature.
Quentin Brissaud1,2, Siddharth Krishnamoorthy3, Jennifer M Jackson1
1Seismological Laboratory California Institute of Technology Pasadena CA USA.
Summary
Scientists detected earthquakes using a balloon-borne microbarometer, proving seismic infrasound can be measured from high altitudes. This opens possibilities for studying Venusian seismic activity from its atmosphere.
Area of Science:
- Planetary Science
- Seismology
- Acoustics
Background:
- Venus's extreme surface conditions challenge ground-based seismology.
- Seismic waves can couple with the atmosphere, theoretically enabling remote detection.
- Earth-based validation of balloon-borne seismic detection is lacking.
Purpose of the Study:
- To demonstrate the feasibility of detecting earthquakes from a balloon-borne platform.
- To analyze the relationship between seismic infrasound and earthquake source parameters.
- To assess the potential for Venusian seismology using atmospheric platforms.
Main Methods:
- Deployment of a balloon-borne microbarometer for seismic infrasound detection.
- Analysis of infrasound signals correlated with a 2019 earthquake near Ridgecrest, CA.
- Detailed study of seismo-acoustic phenomenology, including topography and atmospheric effects.
Main Results:
- First successful detection of an earthquake using a balloon-borne microbarometer.
- Demonstrated dependence of seismic infrasound on earthquake source parameters and local structure.
- Confirmed detectability of seismic activity from high-altitude platforms.
Conclusions:
- Balloon-borne seismic infrasound detection is a viable technique.
- Rayleigh wave-induced infrasound can constrain subsurface velocities.
- This approach paves the way for future seismological studies on Venus.
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