Research news on tsunamis

Tsunamis are long-wavelength, low-amplitude sea waves generated by large, impulsive disturbances of the ocean, most commonly co-seismic seafloor displacement along subduction zones, but also volcanic eruptions, landslides, or submarine mass failures. They propagate as shallow-water gravity waves with phase speeds governed primarily by ocean depth, enabling rapid trans-oceanic travel with minimal energy loss. In deep water they exhibit small surface amplitudes and long periods (minutes to tens of minutes), amplifying dramatically through shoaling, refraction, and resonance effects on continental shelves and in coastal basins. Scientific research focuses on source characterization, wave propagation modeling, inundation mapping, and hazard assessment for early warning and coastal risk mitigation.

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