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The 2006 large interplate Kurile earthquake proved that the entire plateinterface of the Kurile-Kamchatka subduction zone was strongly coupled fromHokkaido, Japan, to Kamchatka, Russia. The seismic moment of the 2006 Kurileearthquake estimated from ten tsunami waveforms is 3.1×1021 Nm(Mw=8.3). This estimate is consistent with the seismic moment estimated from theseismological data in the Global CMT catalog. The computed tsunamipropagation indicates that scattering of the tsunami waves occurred at theshallow region near the Emperor Ridge. The computed tsunami propagation alsoindicates that large later tsunami waves observed at Crescent City is causedby the shallow region along the Mendocino Fracture Zone. The seismic momentof the 2007 outer-rise Kurile earthquake estimated from tsunami waveforms is1.0×1021 Nm (Mw=8.0). This estimate is also consistent with theseismic moment in the Global CMT catalog

Tsunami waveform analyses of the 2006 underthrust and 2007 outer-rise Kurile earthquakes