Silent sounds the Earth makes
The
Earth is an incredibly noisy place. Avalanches roar down mountains,
volcanoes rumble, and hurricanes blast through coastal areas. And while
there's a whole range of sounds that people can hear, there are also
Earth sounds that are too low for the human ear to pick up.
These silent sounds, or infrasounds, are calling to some scientists.
These researchers are using special microphones to eavesdrop on
infrasound created by the world around us. The noisemakers include
volcanoes, tsunamis, hurricanes, and even the turbulence that shakes
airplanes.
"We're learning more about how the planet operates, by listening,"
says Michael A. Hedlin. He studies sounds at the Scripps Institution of
Oceanography in La Jolla, California in USA.
Low notes
Like all types of sound, infrasound travels in waves. The sound waves
have different heights, or amplitudes
(widths), which make them louder or softer. They also have different
wavelengths, measured from the crest of one wave to the top of the next.
And they have different frequencies, measured by the number of crests
that pass by a particular position per second. Short, rapid waves make
high-pitched sounds, like a teapot's whistle. Long, slow waves make
low-pitched sounds, like a bass guitar in a rock band. And below the
lowest note on a bass, below what people can hear, there's infrasound.
Infrasound is created when something, such as a bomb explosion or an
earthquake, sets a large amount of air in motion.
The resulting sound waves travel through the air, sometimes for
thousands of kilometres. Scientists originally started studying
infrasound to make sure faraway countries weren't testing nuclear bombs.
Now, they're using infrasound to check for natural events. "We're
finding all these exotic sources (of infrasound) that we hadn't thought
of before," Hedlin says.
One of those infrasound sources is a gigantic wave called a tsunami.
"We didn't know that a tsunami produces infrasound," says Milton Garces.
He runs the infrasound laboratory at the University of Hawaii, Manoa.
Earthquakes under the ocean can generate tsunamis. Special
instruments on buoys (floating markers anchored in sea) can detect the
resulting waves.
When a massive earthquake occurred off the coast of Indonesia in
December 2004, for example, it sent a deadly wave across the Indian
Ocean. When Garces looked at infrasound data that were recorded near the
tsunami, he found a big signal that corresponded to the wave. "It
produced a wallop (sound or beat)," he says.
In
the last year, Garces and his colleagues have picked up sounds from two
more tsunamis. One was a Japanese tsunami that produced "beautiful
infrasound," he says.
The researchers recently set up a tsunami infrasound project in
Hawaii. "Whenever there's a tsunami, we're going to be looking at it
very carefully," Garces says. The scientists hope to learn how the giant
waves produce infrasound, which is currently a mystery.
Detecting eruptions
Garces and others are also using infrasound to listen in on
volcanoes. On the Sakurajima volcano in Japan, Garces discovered that
stronger and stronger infrasound signals led up to the volcano's
eruption in 1998. If this happens all the time, scientists could use
infrasound patterns to warn people if a nearby volcano is about to blow,
he says.
The eruption of the Fuego volcano in Guatemala in 2003 generated
strong infrasound, mostly below a frequency of 10 hertz (cycles per
second). The pressure readings show that the strength of these sound
waves can reach the equivalent of 120 decibels (roughly the loudness of
an ambulance siren, heavy machinery, or a rock concert).
Detecting volcanic eruptions with infrasound would also be a useful
tool for airplane pilots, because ash from an erupting volcano can
dangerously damage a plane's engines. Infrasound stations are also
keeping an ear on Mount St. Helens in Washington State.
Hedlin can say that gas is bubbling up in the volcano just by looking
at the infrasound recordings. The recordings also detect small
earthquakes inside the volcano that push air around, as well as other
events whose causes are yet unknown. Infrasound gives researchers a more
complete picture of how volcanoes work, Hedlin says.
And scientists are always listening for new things to investigate, he
adds. Hedlin has recorded infrasound coming from sprites, which are
short flashes of light in the atmosphere above thunderclouds.
He's also planning to set up a station to study winds off the coast
of Africa, where hurricanes begin to form. Other researchers are using
infrasound to detect avalanches, the northern lights (auroras), ocean
waves, bumpy air that causes airplane turbulence, and mountains shaking
from earthquakes.
Animal calls
While people are deaf to infrasound, other animals appear to use it
to communicate. When elephants trumpet, for example, they also produce
infrasound that can reach other elephants as far as 10 kilometres away,
researchers discovered.
Elephants might even pick up these low rumblings through their feet,
says Caitlin E. O'Connell-Rodwell. She's a scientist at Stanford
University in California. Other researchers have suggested that whales,
rhinos, and big birds called cassowaries can create or pick up
infrasound. Even some dinosaurs might have had this ability.
A cassowary might pick up ultrasonic signals with its casque, a
mysterious structure on top of its head. No one is yet sure what this
structure is for.
In addition, it's possible that people can detect infrasound in
special ways. When elephants trumpet, "it's such a powerful,
low-frequency sound," O'Connell-Rodwell says. "You really feel it
resonating in your chest". In one experiment, researchers in England
played infrasound during a music performance.
Although listeners couldn't hear the super-low notes, they seemed to
have stronger emotions during the performance than did people who heard
music without infrasound. There certainly seems to be more to infrasound
than meets the ear.
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