Early warning system using tsunami airglow signature

Hydro International -

Researchers at the University of Illinois have become the first to record an airglow signature in the upper atmosphere produced by a tsunami using a camera system based in Maui, Hawaii. The signature, caused by the earthquake that on 11th March 2011 devastated Japan, was observed in an airglow layer 250 kilometers above Earth's surface. The findings were recently published in the peer-reviewed Geophysical Research Letters.

The airglow preceded the tsunami by one hour, suggesting that the technology could be used as an early-warning system in the future. The observation confirms a theory developed in the 1970s that the signature of tsunamis could be observed in the upper atmosphere, specifically the ionosphere. "Imaging the response using the airglow is much more difficult because the window of opportunity for making the observations is so narrow, and had never been achieved before," said Jonathan Makela, an associate professor of electrical and computer engineering and researcher in the Coordinated Science Laboratory. "Our camera happened to be in the right place at the right time."

Tsunamis can generate appreciable wave amplitudes in the upper atmosphere, which in this case was the airglow layer. As a tsunami moves across the ocean, it produces atmospheric gravity waves forced by centimeter-level surface undulations. The amplitude of the waves can reach several kilometers where the neutral atmosphere coexists with the plasma in the ionosphere, causing perturbations that can be imaged.

On the night of the tsunami, conditions above Hawaii for viewing the airglow signature were optimal. Along with graduate student Thomas Gehrels, Makela analysed the images and was able to isolate specific wave periods and orientations. In collaboration with researchers at the Institut de Physique du Globe de Paris, CEA-DAM-DIF in France, Instituto Nacional de Pesquisais Espaciais (INPE) in Brazil, Cornell University in Ithaca, NY, and NOVELTIS in France, the researchers found that the wave properties matched those in the ocean-level tsunami measurements. The team also cross-checked their data against theoretical models and measurements made using GPS receivers.

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