1. Detection of infrasound disturbances from the Earth's stratosphere
- Author
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Courtney Ballard, Emma Young, Martin Heaney, Peter Brown, Ian Thom, Emily Dougherty, Mark Boslough, Michael Von Hendy, Eliot F. Young, Kyle Garner, Connor Dullea, and Kerry Wahl
- Subjects
Infrasound waves ,010504 meteorology & atmospheric sciences ,Wind noise ,Meteorology ,Payload ,Bolide ,Infrasound ,Environmental science ,010502 geochemistry & geophysics ,01 natural sciences ,Stratosphere ,Sound wave ,0105 earth and related environmental sciences - Abstract
Infrasound is usually defined as sound waves below 20 Hz, the nominal limit of human hearing. Infrasound waves propagate over vast distances the Earth's atmosphere: the CTBTO (Comprehensive Nuclear-Test-Ban Treaty Organization) has 48 installed infrasound-sensing stations around the world to detect nuclear detonations and other disturbances. In February 2013, several CTBTO infrasound stations detected infrasound signals from a large bolide that exploded over Chelyabinsk, Russia. Some stations recorded signals that had circumnavigated the Earth, over a day after the original event. A balloon-borne infrasound sensor is expected to have two advantages over ground-based stations: a lack of wind noise and a concentration of infrasound energy in the “stratospheric duct” between roughly 5–50 km altitude. To test these advantages, we have built a small balloon payload with five calibrated microphones. This paper discusses the design, testing and expected sensitivity of the payload. Our current plans call for a launch in August 2016, coordinated with a ground-based explosion and a network of ground-based infrasound sensors.
- Published
- 2016
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