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Tsunami detection in the ionosphere by Juliette Artru Caltech Pasadena USA Philippe Lognonné Giovanni Occhipinti François Crespon Raphael Garcia IPGP Paris France Eric Jeansou Noveltis Toulouse France and Makoto Murakami GSI Tsukuba Japan Introduction Tsunamis are surface gravity waves that propagate for great distances in the oceans usually triggered by earthquakes or landslides In the open ocean their long wavelengths typically km long periods minutes and small amplitudes a few to cm for the gigantic event of December make their detection very challenging even with the deployment of GPS buoy systems Gonzalez et al Recently satellite altimetry has proved to be capable of measuring the sea
5 pages
English
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