Within Sensors

How Far Can Sky Sounds Really Travel?

Infrasound can record energetic sky events far beyond human hearing, turning distant booms and fireballs into measurable signals.

On this page

  • Why low frequency waves travel so far
  • Meteor blasts as proof of reach
  • What infrasound can and cannot identify
Preview for How Far Can Sky Sounds Really Travel?

Introduction

Some of the most dramatic sounds linked to unusual aerial events are never heard by human ears at all. Powerful meteor airbursts, high-altitude explosions and other energetic disturbances can generate infrasound: extremely low-frequency pressure waves that travel through the atmosphere over vast distances. Modern monitoring networks were built largely to detect atmospheric nuclear tests, yet they routinely record meteors, volcanic eruptions and other sky events thousands of kilometres from their source. For investigations involving reported UFO noises, this matters because a distant aerial explosion can leave a measurable acoustic trace even when witnesses hear little, hear only a delayed boom, or report unusual vibrations rather than conventional sound. The result is a rare form of evidence that can be compared across continents instead of relying solely on local testimony. [CTBTO]ctbto.orgCTBTOThe International Monitoring SystemEighty radionuclide stations to detect radioactive particles or gases from atmospheric explosions… [CTBTO]ctbto.orgOpen source on ctbto.org.

Infrasound illustration 1

How Far Can Sky Sounds Really Travel?

The extraordinary reach of infrasound comes from its frequency. Higher-frequency sounds are absorbed and scattered relatively quickly by the atmosphere. Very low-frequency waves, by contrast, can travel through atmospheric layers that act like giant waveguides, allowing energy to propagate far beyond the horizon.

In practical terms, this means a sufficiently energetic atmospheric event can be detected at distances measured in thousands rather than tens of kilometres. Atmospheric winds, temperature gradients and pressure layers can bend and channel the waves, sometimes allowing them to circle large portions of the globe. Researchers often compare the process to how certain radio frequencies can be guided over long distances by the upper atmosphere, although the physical mechanisms are different. [National Academies]nationalacademies.orgNational AcademiesChapter: Appendix F: InfrasonicsLarger atmospheric nuclear explosions were easily heard at ranges in excess of 10,000 k… [National]nationalacademies.orgNational AcademiesChapter: Appendix F: InfrasonicsLarger atmospheric nuclear explosions were easily heard at ranges in excess of 10,000 k…

The main international system designed to exploit this property is the International Monitoring System operated for the Comprehensive Nuclear-Test-Ban Treaty. Its infrasound component consists of dozens of stations distributed around the world, continuously listening for ultra-low-frequency atmospheric disturbances. Although the network’s primary mission is nuclear-test verification, its sensors also record natural events that release large amounts of energy into the atmosphere. [CTBTO]conferences.ctbto.orgCTBTO Conferences and Workshops (Indico)CTBT: Science and Technology Conference 2025 - SnT2025Explosive volcanic eruptions produce large… [CTBTO]ctbto.orgCTBTOCivil and Scientific ApplicationsIMS data can also help to cast light on plane crashes and other major accidents: infrasound station…

Why distant detection matters for aerial mysteries

When witnesses report an unexplained flash, a sudden sky boom or an apparent explosion, the local sound alone may be misleading. Audible sound depends heavily on distance, terrain and weather conditions. Infrasound offers a different record:

  • It can persist across enormous ranges.
  • It can be measured even when no clear audible recording exists.
  • Multiple stations can compare arrival times to estimate where an event occurred.
  • Signal strength and frequency characteristics can help estimate the energy released. ScienceDirect [MDPI]mdpi.comMDPIGlobal Monitoring and Characterization of Infrasound…by C Pilger · 2020 · Cited by 38 — This study aims at investigating meteoroid…

That does not identify the object responsible, but it can establish that a significant atmospheric event occurred and roughly how powerful it was.

Meteor Blasts Show the Real Reach of Infrasound

Meteor airbursts provide some of the clearest demonstrations of global-scale acoustic detection because they generate intense atmospheric shock waves while remaining relatively well understood scientifically.

The most famous example is the Chelyabinsk meteor, which exploded over Russia on 15 February 2013. The event shattered windows across a wide area and injured more than a thousand people, largely through blast effects rather than direct impact. What made it especially important for infrasound research was the scale of its acoustic signature. CTBTO stations around the world recorded the event, making it the largest meteor-related infrasound detection in the network’s history at that time. CTBTO [AGU Publications]agupubs.onlinelibrary.wiley.comAGU PublicationsThe 2013 Russian fireball largest ever detected by CTBTO…by A Le Pichon · 2013 · Cited by 183 — One of the most energe…

The blast was detected by around twenty infrasound stations, and the most distant confirmed detection came from Antarctica, roughly 15,000 kilometres away. Researchers used those signals to estimate the energy of the airburst and to study how low-frequency waves propagated through the atmosphere on a global scale. [CTBTO]ctbto.orgCTBTORussian Fireball Largest Ever Detected by CTBTO's…Feb 18, 2013 — The blast was detected by 20 infrasound stations in the CTBTO's… [OSTI]osti.govIt is the most energetic…Read mor…

What scientists learned from Chelyabinsk

Chelyabinsk demonstrated several points directly relevant to unusual aerial-event investigations:

  • A brief atmospheric explosion can produce detectable signals across continents.
  • Multiple stations can independently confirm an event.
  • Infrasound can reveal energy release even when visual observations are incomplete.
  • Atmospheric propagation is complex enough that signals may arrive along unexpected paths. [AGU Publications]agupubs.onlinelibrary.wiley.comAGU PublicationsThe 2013 Russian fireball largest ever detected by CTBTO…by A Le Pichon · 2013 · Cited by 183 — One of the most energe… [OSTI]osti.govThe utility of infrasound towards detection and…by EA Silber · 2024 — The Tajikistan bolide was detected by two infrasound stations of…

Researchers continue to use meteor detections as test cases for refining global monitoring methods. Studies of bolides, the exceptionally bright meteors that often explode in the atmosphere, show that infrasound can detect events ranging from relatively modest airbursts to extremely energetic fragmentation episodes. Some detections have been made more than 2,000 kilometres from the source, while larger events can be tracked much farther away. [A&A Online]aanda.orgaa41106 21A&A OnlineInfrasound signals of fireballs detected by the…by T Ott · 2021 · Cited by 13 — The smallest meteoroid recorded by infrasoun… [OSTI]osti.govIt is the most energetic…Read mor…

Infrasound illustration 2

How Infrasound Networks Reconstruct an Explosion

A single station can detect an unusual pressure wave, but a network provides much more information.

Each monitoring site typically uses an array of sensors spread across an area rather than a lone microphone. By comparing the tiny differences in arrival times between sensors, analysts can estimate the direction from which the wave approached. When multiple stations detect the same event, those directional estimates can be combined to infer a likely source region. [ScienceDirect]sciencedirect.comScienceDirectInfrasound detection of meteorsby MN ElGabry · 2017 · Cited by 29 — Sound waves in the atmosphere become audible to humans i…

Scientists also examine:

  • Signal duration.
  • Dominant frequencies.
  • Pressure amplitude.
  • Arrival timing.
  • Changes in waveform shape across different stations. [ScienceDirect]sciencedirect.comScienceDirectInfrasound detection of meteorsby MN ElGabry · 2017 · Cited by 29 — Sound waves in the atmosphere become audible to humans i…

These measurements can help distinguish a compact explosion from a longer atmospheric track such as a meteor travelling through the atmosphere before breaking apart.

One complication is that atmospheric conditions strongly affect propagation. Winds and temperature structures can alter both the apparent direction and the frequency content of a signal. Recent studies show that atmospheric filtering can change how an event appears at different locations, meaning the recorded signature is partly a product of the atmosphere itself, not just the source. [arXiv]arxiv.orgarXivObservational Evidence for Wind-Driven Low-Pass Filtering of Infrasound at Short RangeJanuary 31, 2026…Published: January 31, 2026

What Infrasound Can Identify — and What It Cannot

For readers interested in UFO-related noises, the most important point is that infrasound is excellent at detecting energetic events but much less reliable at identifying their exact cause.

A strong infrasonic signal can indicate that something released substantial energy into the atmosphere. It may reveal:

  • Approximate location.
  • Time of occurrence.
  • Relative size of the disturbance.
  • Whether the source behaved more like a blast or an extended track. [MDPI]mdpi.comMDPIGlobal Monitoring and Characterization of Infrasound…by C Pilger · 2020 · Cited by 38 — This study aims at investigating meteoroid… ScienceDirect What it usually cannot do on its own is answer the question everyone wants answered: what was the object [sciencedirect.com]sciencedirect.comScienceDirectInfrasound detection of meteorsby MN ElGabry · 2017 · Cited by 29 — Sound waves in the atmosphere become audible to humans i…

A meteor airburst, a large explosion, a volcanic eruption, a rocket re-entry and other energetic atmospheric phenomena can all generate low-frequency acoustic signatures. Additional evidence such as optical observations, radar data, satellite detections or recovered debris is normally required for confident identification. CTBTO [NASA Science]science.nasa.govlooking for lightning finding fireballs 149381NASA ScienceLooking for Lightning, Finding Fireballs27 Jan 2022 — Stereo detection allows researchers to reconstruct the trajectories of…

Infrasound illustration 3

Why a mysterious boom is not necessarily a mysterious object

This distinction is especially important in discussions of unexplained aerial reports. A witness may experience:

  • A bright flash followed by delayed shock waves.
  • A distant rumble with no visible source.
  • Vibrations felt through buildings or the ground.
  • A boom reported across a wide region.

Infrasound networks can often confirm whether a significant atmospheric disturbance occurred. However, confirmation of an acoustic event is not confirmation of an exotic craft. In many cases, later investigation links the signal to meteors, atmospheric explosions, rocket debris re-entry or other known causes. CTBTO [Amusing Planet]amusingplanet.comSecret Nuclear TestsDec 29, 2016 — On February 15, 2013, the CTBTO's infrasound monitoring stations detected signals made by a meteor tha…Published: February 15, 2013

The Quiet Value of Global Acoustic Listening

The most significant contribution of infrasound monitoring to aerial-phenomena research is not that it solves mysteries automatically. Its value is that it creates an independent physical record.

Human reports can be distorted by distance, timing, memory and expectation. Infrasound stations record pressure changes whether anyone is watching the sky or not. When a dramatic aerial event occurs, researchers can compare witness accounts against sensor data gathered hundreds or thousands of kilometres away.

For large atmospheric disturbances, the technology has already proven its reach. The same global network built to detect nuclear explosions has repeatedly shown that meteor airbursts and other energetic sky events can leave acoustic fingerprints detectable across continents. In investigations of unusual aerial noises, that capability transforms some otherwise fleeting reports into measurable evidence. [CTBTO]ctbto.orgbeyond nuclear test detection ctbto and hunga tonga hunga haapai eruptionBeyond nuclear test detection: CTBTO and Hunga Tonga-…Jun 24, 2024 — In comparison, the scale of this event dwarfed even the record-br… [CTBTO]ctbto.orghat had entered the atmosphere and disintegrated in the skies over…Read more…

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Endnotes

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