What the f boom


Sonic Boom Archive — Steve Rowell



Over the course of 18 months, from 2005 - 2007, I recorded all of the sonic booms that occurred above the California Mojave Desert. The airspace of interest is labeled  the “R-2508 Special Use Airspace Complex” by the US Air Force. The equipment array installed was calibrated to autonomously monitor and record any sound above an established decibel threshold, filtering out long moments of (perceived) silence and / or low volume sounds, natural and man-made. The result is an "inverse noise gate". A noise gate being an acoustical engineering term for a device or application which controls, limits the loud volume spikes or peaks of an audio signal. By inverting this filter, my recordings retain the abrupt and loud sounds, thereby capturing the elusive sonic boom-scape of this singularly militarized, supersonic airspace, the largest and most active of its kind in the world.




The research involved a continuous sampling of the skies for sonic booms, a reasonably frequent occurrence, at the Center for Land Use Interpretation’s Desert Research Station (DRS) which is under Edwards Air Force Base’s R-2515 High Altitude Supersonic Corridor air space. A computer at the DRS, connected to a network of microphones, recorded the outdoor sounds continuously, erasing all silence shortly after recording it. When a sound above a certain threshold is detected, the computer preserves it, as well as the moments before and after it. The logged sonic incidents are later transferred to an off site master where they are catalogued, stored, and accessed for use in research and displays. Every sonic boom between January 2006 and August 2007 was recorded and logged.

Sonic booms are the audible effects of shock waves caused by matter moving faster than the speed of sound - approximately 761 MPH at sea level at 59 °F (1,224 KPH @ 15 °C) – through the atmosphere. In this case, the types of “matter” are various supersonic military aircraft that may include the US Air force F-16, F/A-18, F-22, and F-35 fighter jets as well as NASA’s F-5A and F-15B Shaped Sonic Boom Demonstrator jets. These otherwise exotic aircraft are common to the airspace above the Mojave Desert.

These recordings have been exhibited as part of two collaborative installations with SIMPARCH: Gloom & Doom I (Center For Contemporary Art, Cincinnati, OH, May - October 2006) and Gloom & Doom II (Weston Art Gallery, Cincinnati, May - July 2006) where an anechoic "boom chamber" was constructed in the form of a two-story plywood "house", a direct reference to the test-homes NASA and the US Air Force built in the 1950s on a dry lake bed at Edwards AFB. These test homes had embedded microphones and seismometers to detect shockwave impact and structural damage.

See also:
Gloom & Doom I
Gloom & Doom II

An installation featuring a listening station and descriptive poster was exhibited in the group show Aural Indicators at the Contemporary Conflict Institute in Troy, New York, March-May 2010.
An updated iteration of this audio/didactic poster installation, but including a large format (40x80 inch) print was shown in the group show Ecotone at the Actual Size gallery in Los Angeles, March-April 2014.

A short composition of select booms was exhibited in the group show Zeigen: An Audio Tour through Berlin at the Temporäre Kunsthalle Berlin, December 2009 - January 2010.




As of May 2012, a playback of select booms and incidental desert ambiance is being exhibited indefinitely at the CLUI Desert Research Station in the recently activated Sonic Boom Containment Vessel.

Now part of the CLUI Interpretive Walking Trail at the Desert Research Station, providing information about the Harper Lake Basin region... a region which includes the airspace above, classified by the U.S. Air Force as the "R-2508 Special Use Airspace Complex". This restricted, remote airspace, this ‘nether-ether’, is the (un)natural realm of sonic booms, explosions of air pressure generated by, at this time, US supersonic military aircraft. These fighter jets – above one moment, gone the next – and the split-second eruptions of the atmosphere they produce are the subjects, implied and audible, of the Sonic Boom Containment Vessel (SBCV).

The SBCV holds captive 18 months of sonic boom 'events' from 2006-2007. This sound installation consists of a small modular office unit outfitted with powerful audio equipment, where high decibel playback of these recorded booms occur under the same airspace where the recordings were made. The law of Action-Reaction revisited and manifested ad infinitum. Listening to (and feeling) the playback of these infrasonic frequencies can be a visceral experience.

SONIC BOOM CONTAINMENT VESSEL PLAYLIST
CLUI DRS, Hinkley, CA
Installed May 2012
Daily playback from 10am-5pm, indefinitely

Track title ––– hh:mm:ss

SBA text audio voice over pitched.mp3 ––– 00:03:07
Framework radio piece - S Rowell Sonic Booms.mp3 ––– 00:57:00
Sonic Boom Archive composition for CCI Troy.mp3 ––– 00:15:31
Sonic Boom Archive composition TACTILE AIR-WESTON.mp3 ––– 00:20:00
Sonic Boom Archive composition STV01001_hour 01-dove.mp3 ––– 00:32:01
Landing bird chatter F-28s jetnoise and booms. mp3 ––– 00:06:49
Baby bird chirp owl F-35 jetnoise and booms.mp3 ––– 00:12:21
Bird trilling over jetnoise.mp3 ––– 00:01:05
Dog bark whimper dove multiple booms.MP3 ––– 00:04:36
Bird flap.mp3 ––– 00:00:21


Total ––– 02:32:51

All recordings from autonomous Sonic Boom Archive recording sessions, CLUI DRS 2006-07




Earthquake Booms, Seneca Guns, and Other Sounds

By Earthquake Hazards

Reports of unidentified “booms” have emerged from different places around the world for hundreds of years, and although many of the “boom stories” remain a mystery, others have been explained. Most of the booms that people hear or experience are the result of human activity, such as an explosion, a large vehicle going by, nearby construction, or sometimes a sonic boom, but there have been many reports of booms that cannot be explained by man-made sources. Some of those booms are associated with a variety of interesting natural phenomena, including earthquakes.

In the United States most reports of mysterious booms come from the Northeast and along the East Coast, but there have also been observations along the West Coast. Those on the East Coast have not been directly studied and explained, but we can deduce from observations and measurements in West Coast locations that at least some of the East Coast booms are associated with very small earthquakes. Small shallow earthquakes sometimes produce rumbling sounds or booms that can be heard by people who are very close to them. High-frequency vibrations from the shallow earthquake generate the booming sound; when earthquakes are deeper, those vibrations never reach the surface. Sometimes the earthquakes create booming sounds even when no vibrations are felt.

Booms Around the World

Eastern U.S.

The term “Seneca Guns” is commonly used for booms that residents hear near Lake Seneca in the Finger Lakes region of New York. The name has also been applied to similar sounds along the coasts of North Carolina, South Carolina, and Virginia (possible origins of this term). The 1886 Charleston, South Carolina earthquake (approximately M6.9) was accompanied by well-documented booming sounds. The observations describe a roaring sound that was heard as the seismic waves rolled across the region. For several weeks after the Charleston Earthquake, there were many aftershocks that were reportedly accompanied by "loud detonations".

Midwestern U.S.

There are accounts of "artillery"-like sounds that were said to have occurred before or during the New Madrid earthquakes of 1811-1812 (M 7.4-7.9).

Reports of booms throughout the Midwest often coincide with low temperatures of -20 F or colder and are sometimes described as “ice quakes” or “frost quakes” . A frost quake is a result of shallow groundwater freezing, expanding, and then causing surrounding frozen rock and soil to crack. These events are not recorded on seismographs. Another explanation for booms during cold snaps is the expansion and contraction of houses and other structures due to the extreme temperatures.

Western U.S.

In 2001, a swarm of small earthquakes accompanied by booming sounds unnerved the city of Spokane. The shallow location of the earthquakes in Spokane (sometimes only 1-2 miles deep) probably contributed to all the noise heard by residents.

In 1989, USGS seismologists working on Mammoth Mountain in California heard muffled booming sounds but felt no shaking . Seismographs showed that several small, shallow earthquakes (less than magnitude 2) occurred at the same time. Another group of USGS scientists heard low rumbling sounds and felt shaking while they were installing seismic stations in Imperial Valley, CA during an earthquake swarm. During the 1906 San Francisco earthquake (M7.9), many citizens described sounds of all types, from “roaring” to “rushing”.

Outside the U.S.

Historical reports of earthquake sounds in Europe include anecdotes from as early as 1857 from a M6.9 earthquake in Italy. The sounds from that earthquake were described as both “explosive” and “rushing and rolling” by witnesses. Accounts of sounds from small- to moderate-size earthquakes in England from 1880 to 1916 were collected in a publication in 1938. The observations include descriptions of booming, blowing wind, muffled sounds, and “an immense covey of partridges on the wing”, according to one report.

Non-Earthquake Booms

Of course, most booming sounds that people hear are not caused by earthquakes. Some other common and not-so-common natural causes are lightning, storm and tsunami waves, meteors, and sand dunes. Man-made causes include sonic booms, explosions, and construction.

References

  • Dutton, C.E., (1889). The Charleston Earthquake of August 31, 1886, Ninth Annual Report, 1887-88, U.S. Geological Survey, Washington D.C., 203-528.
  • Hill, D.P. (2011). What is That Mysterious Booming Sound? Seism. Res. Lett., v.5.
  • Hill D. P., Fischer, F. G., Lahr, K. M., & Coakley, J. M. (1976). Earthquake sounds generated by body-wave ground motion. Bulletin Seismological Society of America, v. 66, No. 4, 1159-1172.
  • Kitov, I. O., J. R. Murphy, O. P. Kusnetsov, B. W. Barker, & N. I. Nedoshivin, An analysis of seismic and acoustic signals measured from a series of atmospheric and near-surface explosions. (1997). Bull. Seism. Soc. Am. 87, 1553-1562.
  • Stiermann, D.J.(1980). Earthquake sounds and animal cues; some field observations. Bull. Seism. Soc. Am. 70, 639-643.
  • St-Laurent, F.(2000). The Saguenay, Québec, earthquake lights of November 1988-January 1989. Seism. Res. Lett. 71, 160-174.
  • Tosi, P., De Rubeis, V., Tertulliani, A., & Gasparini, C.(2000). Spatial patterns of earthquake sounds and seismic source geometry. Geophys. Res. Lett. 27, 2749-2752.
  • Tsukuda, T.1997). Sizes and some features of luminous sources associated with the 1995 Hyogo ken Nanbu earthquake. J. Phys. Earth 45, 73-82.

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How to cancel a subscription to boom in VK

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    VK Combo subscription in BUM and VKontakte: what is it, how to disable it?

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    VK Combo presents a service that includes the capabilities of the BUM music application created by the popular social network, as well as the Combo functionality promoted by Mail.ru Group since mid-autumn 2019of the year.

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