Abstract The 2011 March 11 Tohoku-oki great (Mw 9.1) earthquake ruptured the plate
boundary megathrust fault offshore of northern Honshu with estimates of shallow slip of 50 m …

This paper reviews achievements and findings from studies associated with numerical
modeling of tsunami since the 2011 Tohoku earthquake, and addresses challenges for …

Rupture complexity, typically in the form of heterogeneous slip distribution pattern,
significantly affects the local tsunami wave field. However, the effect of rupture complexity is …

In this study, we considered the accurate calculation of far-field tsunami waveforms by using
the shallow water equations and accounting for the effects of Boussinesq dispersion …

A tsunami was triggered in the North Pacific Ocean by the 2021 Alaska earthquake (M 8.2)
on July 29. We studied the source properties and resonance characteristics of the tsunami …

On 15 January 2022, an eruption of Hunga volcano generated an air‐coupled tsunami that
propagated across the Pacific Ocean. The tsunami reached Japan approximately 7 hr after …

Although most tsunamis are generated by the sea‐bottom deformation caused by
earthquakes, some tsunamis are excited by sea‐surface pressure changes. This study …

This article reviews tsunami modeling and its relation to recent developments of deep-ocean
observations. Unlike near-coast observations, deep-ocean observations have enabled the …

The last decade has seen the rapid emergence of nonhydrostatic modeling as an advanced
tool for studies of tsunami processes and source mechanisms that warrants a critical …

One crucial yet unanswered question about the 2011 MW 9.1 Tohoku-Oki earthquake and
tsunami is what generated the largest tsunami (up to 40 m) along the Sanriku coast north of …