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Booms Beneath Our Feet and Above Our Heads: The Unlikely Logic of Space Junk Tracking

A new study shows earthquake sensors can detect sonic booms from falling space debris, improving tracking accuracy during atmospheric reentry.

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Olivier Jhonson

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Booms Beneath Our Feet and Above Our Heads: The Unlikely Logic of Space Junk Tracking

On a quiet afternoon, the Earth sometimes shakes — not because of rumbling plates deep below, but due to the fleeting passage of something from far above. In recent years, scientists have discovered a surprising connection between our planet’s sensitive earthquake-monitoring instruments and a growing challenge from space: the reentry of discarded satellites and other space debris.

When pieces of space junk fall back into Earth’s atmosphere, they often exceed the speed of sound. This supersonic descent produces sonic booms — shock waves in the air similar to those trailing behind supersonic jets. Now, researchers have found that those shock waves can be picked up not just by microphones or radar, but by seismic sensors buried in the ground.

A study published in Science took advantage of one such event. In April 2024, a large, uncontrolled piece of orbital debris — the heavy orbital module from China’s Shenzhou-15 spacecraft — tumbled down over Southern California. As it streaked through the atmosphere, the object generated sonic shock waves that propagated outward and downward, enough to register on seismic networks originally built to detect earthquakes.

By analyzing data from more than 120 seismic stations, scientists led by Benjamin Fernando of Johns Hopkins University and Constantinos Charalambous of Imperial College London were able to reconstruct the debris’s path, speed, and altitude during its fiery descent. In fact, their seismic tracking placed the object’s ground track nearly 20 miles south of where radar had predicted — revealing both the promise and limits of traditional tracking systems once debris begins to break apart and re-enter the atmosphere.

This method doesn’t replace existing orbital surveillance, which uses radar and optical telescopes to watch objects while they orbit. Rather, it adds a powerful new layer of situational awareness once these objects begin their final plunge. Knowing more precisely where and how space debris breaks up could help responders anticipate where surviving fragments might fall — a matter of safety if a piece is large enough to pose risks to people or property.

Experts note that the number of satellites and bits of debris in orbit has grown rapidly over the past decade. With more launches for communications constellations, scientific missions, and whatever lies on the horizon, uncontrolled reentries are becoming more common. Tools that can track these events more accurately are increasingly valuable — and sometimes, surprisingly elegant when they repurpose instruments designed for an entirely different purpose.

In reframing how we think about seismic sensors, this research also shows how interconnected Earth systems can be. Instruments meant to listen to the deep murmurs of the planet now help us read the thunderous echoes of objects from beyond — bridging worlds with every boom they detect.

AI Image Disclaimer (Rotated Wording) Visuals are AI-generated illustrations and are not real photographs — they serve only to represent concepts.

Sources

• AP News

• ScienceAlert

• Phys.org

• Mirage News

• WBOC/AP News coverage

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