Page 5: Research news on tsunami

A tsunami is a long-wavelength, gravity-driven water wave phenomenon typically generated by large, sudden displacements of the seafloor due to subduction-zone earthquakes, but also by submarine landslides, volcanic eruptions, or impact events. In deep ocean, tsunamis travel at jetliner speeds with low amplitudes and very long periods (minutes to an hour), behaving as shallow-water waves whose phase speed depends on water depth. As they shoal on continental shelves, energy conservation forces rapid increases in wave amplitude and reductions in wavelength and speed, producing highly nonlinear run-up, strong nearshore currents, and complex inundation patterns that are central to hazard assessment and numerical modeling.

Studying tsunamis with GPS satellites

On 30 July, a magnitude 8.8 earthquake off Russia's Kamchatka Peninsula triggered a tsunami that spread across the Pacific Ocean.

Cascadia megathrust earthquake could trigger San Andreas fault

When the tectonic subduction zone beneath the Pacific Northwest moves, it does so in dramatic fashion. Not only is ground shaking from a magnitude 9+ earthquake incredibly destructive, the event triggers tsunamis and landslides ...

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