[meteorite-list] Microphones Tell Asteroids From A-Bombs
From: Ron Baalke <baalke_at_meteoritecentral.com>
Date: Thu Apr 22 10:00:07 2004 Message-ID: <200207171702.KAA15696_at_zagami.jpl.nasa.gov> http://www.nature.com/nsu/020715/020715-4.html Microphones tell asteroids from A-bombs Detecting low frequency rumbles could avert nuclear war. TOM CLARKE Nature Science Update 17 July 2002 Free data from a global array of microphones could spot nuclear false alarms, averting disastrous retaliation, say scientists[1] and defence experts. The ground-based network will detect the faint, low-frequency rumbles of meteor explosions high in the atmosphere that can look like nuclear explosions to other sensors. Its primary purpose is to help police the Comprehensive Test Ban Treaty (CTBT) that forbids the testing of nuclear bombs. The United States is the only nation with a satellite network and radar sufficiently sophisticated to tell a nuclear blast from a meteorite explosion. It sometimes makes these data available, but they can take months to get hold of. "This network will warn other nations that [a rumble] is just a meteor and not a nuclear detonation," says Edward Tagliaferri, president of aerospace consultants ET Space Systems in Camarillo, California, an expert in the defence implications of asteroid explosions. In with a bang When meteors travelling at 15 to 20 kilometres per second hit the Earth's atmosphere, they explode because of the increased pressure. A meteor 5 metres across can detonate with the force of 10,000 tonnes of TNT - like the bomb that was dropped on Nagasaki, Japan, in 1945. Five or six asteroid explosions of twice this size occur in the atmosphere each year. Like atomic explosions, meteor blasts release electromagnetic pulses that instruments on the ground can detect. "At a distance, an atmospheric nuclear explosion looks like a large meteor," explains Peter Brown, a physicist at the University of Western Ontario in Canada. That is cause for concern, in the current political climate. For example, in November 1990, as the United States prepared to invade Iraq, the Iraqis threatened to fire Scud missiles at Israel, a nuclear power. A meteorite blew up high over Micronesia with the force of 5,000 tonnes of TNT. If it had arrived just a few hours later on the same trajectory, it would have detonated over Tel Aviv. The Israelis might not have known it was an asteroid, Tagliaferri points out. A similar event, over India or Pakistan, say, could also have devastating consequences, a US Senate round-table meeting on asteroids heard last week. "Neither of those nations has the sophisticated sensors we do," Air Force Brigadier General Simon Worden of US Space Command told the hearing. "The resulting panic could have been the spark for nuclear war," he said. Ground control Ground-based groups of microphones, called infrasonic arrays, can distinguish atomic blasts from exploding asteroids up to a few hundred kilometres away, say Brown, Tagliaferri and colleagues1. The arrays pick up the very-low-frequency sounds that penetrate hundreds of kilometres of the Earth's atmosphere. Multiple arrays pinpoint the position and size of a blast almost as accurately as the satellites used by US Space Command, the researchers show. Right now, there are 12 such arrays. Sixty will be built within the next 5 years as part of the CTBT International Monitoring Network. The rules of the treaty dictate that their data must be available to all. A global array should spot meteor explosions from most areas of the world, says Brown. The infrasonic network will also be important for research. Meteorites smaller than 10 metres across are hard to detect with telescopes, so scientists have little idea of how often they breach our atmosphere. An idea of how frequently small asteroids occur is important for estimating the likelihood of larger ones, such as the one that devastated thousands of square kilometres of Siberian forest in Tunguska in 1908. The microphone array, says Matthew Genge of the Natural History Museum in London, UK, "will help us tell just how many Tunguskas we can expect". References 1. Brown, P. G., Whitaker, R. W., ReVelle, D. O. & Tagliaferri, E. Multi-station infrasonic observations of two large bolides: signal interpretation and implications for monitoring of atmospheric explosions. Geophysical Research Letters (2002). Received on Wed 17 Jul 2002 01:02:05 PM PDT |
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