
© Marcelo Hernandez/dpa/Corbis
Researchers hope measuring atmospheric waves will improve early warning of big tsunamis such as the one generated by a February earthquake in Chile.
The signals of GPS satellites could be used to monitor tsunamis as they sweep across the ocean. In the most detailed study to date of the effect, scientists have shown that even though open ocean tsunami waves are only a few centimetres high, they are powerful enough to create atmospheric vibrations extending all the way to the ionosphere, 300 kilometres up in the atmosphere.
The finding, the researchers hope, could hugely improve tsunami early-warning systems.
In a study published online on 1 September in
Geophysical Research Letters1, a team of French geophysicists was able to use these ionospheric effects to trace the progress of three recent tsunamis, including the one triggered by the 27 February earthquake in Chile, which had a magnitude of 8.8. The researchers showed that the strength of the ionospheric effects increased with the height of the wave.
The maximum height of that tsunami, which swept across the Pacific, was only 10 centimetres in mid-ocean, but low-lying tsunami waves can be more than 100 kilometres long. During a tsunami, hundreds of square kilometres of ocean rise and fall, nearly in unison. This produces a rhythmic movement in the atmosphere, generating a vertically propagating wave known as an internal gravity wave. The thinning air causes the wave to spread out vertically and the air movements become larger.
"At around 300 - 350 kilometres of altitude, the atmospheric wave has been amplified by a factor of 10,000 or more," says Lucie Rolland, a graduate student at the Paris Institute of Geophysics, whose PhD work spearheaded the study. "This means that a 10-centimetre tsunami wave at ocean level will induce atmospheric displacement reaching 1 kilometre."