Tsunami: Better Safe Than Sorry

Scientists can do a very good job of tracking theas typically happens along the San Andreas fault --
progression of a tsunami and predicting when it willthey won't displace large volumes of water and there
arrive, but they have much more difficulty predictingwill be essentially no tsunami.
how big it will be.But if one plate dives under the other, which is
That disparity has become apparent following theprobably what occurred early Saturday off the coast
massive magnitude-8.8 earthquake off the coast ofof Chile, it will displace "a huge column of water," Yim
Chile. Researchers from the Pacific Tsunami Warningsaid.
Center in Hawaii predicted to within a few minutesThat is precisely what happened with the 2004 Indian
when the tsunami -- a massive influx of water ratherOcean earthquake that devastated parts of
like a flash flood -- would arrive at Hilo. They alsoIndonesia.
predicted that the wave height would range from 2Yim noted that researchers would not know exactly
to 8 feet, and they were correct. But when thewhat happened seismically for a few days, when
waves proved to be at the low end of the range,they can send scanners to look at the ocean floor
they were widely perceived as having blown theand determine how it was reshaped.
prediction.A wave created by an earthquake can travel across
Tsunami expert Harry Yeh of Oregon Statethe ocean at 450 to 600 mph, about 10 to 100 times
University said the forecasters had to err on the sideas fast as a wind-driven wave. In deep water, the
of caution. "Even if they knew deep in their heartwave will only be a few inches to a foot high.
that it probably wouldn't be large, it could be large,"Buoys spaced across the ocean monitor these small
he said. "If they lost one life [because theyincreases in ocean height so researchers can track
underestimated the size of the tsunami], that wouldthe wave's progress and predict when it will strike
be a problem."land. But they provide little or no information about
The biggest problem in predicting the size of amagnitude.
tsunami is in determining exactly how much energyWhen the tsunami reaches shallower water, the
was put into the ocean by an earthquake, and that iswave slows down, the energy is compressed and
something that cannot be determined in thethe wave can get much higher. A large tsunami could
immediate aftermath of the event.be 35 to 40 feet high and move at a speed of 35
Chile's 8.8 quake occurred at the junction of twomph.
massive tectonic plates: the South American plate,Topography plays a big role in how high the wave will
which sits under most of the continent, and thegrow. Hilo harbor "attracts wave energy," Yim said,
Nazca plate, which lies under much of the Pacificbecause the headlands on both sides of the bay tend
Ocean. The Nazca plate is attempting to slip underto focus the incoming energy. That is why there is
the South American plate, but is largely held in placegenerally good surfing there. "If not for the
by friction. Every so often, however, the geologicheadlands, [the tsunami] would have been even
forces overcome friction and the two plates slip. Thissmaller," he said.
time, the slippage occurred over a stretch of theUnderwater geography off the coast of Japan is
juncture about 400 miles long.capable of focusing the energy even more, and
The size of a tsunami depends on how that slippageexperts there were predicting waves of up to 9 feet
occurs, said Solomon Yim, also a tsunami expert ata full day after the Chile quake. Initial waves that hit
Oregon State. If the slippage is mostly horizontal andoutlying islands, however, were not threatening.
the two plates slide side to side against each other --