“It came from nowhere, snapping giant ships in two. No one believed the survivors... until
now”—New Scientist magazine cover, June 30, 2001 Rogue waves are the focus of this …

In the first edition, we paid attention not only to tsunami waves, but to related phenomena,
namely, seaquakes, as well, which to a significant extent reflected the interests of the …

In the aftermath of the 26 December, 2004 tsunami, several quantitative predictions of
inundation for historic events were presented at international meetings differing substantially …

We have developed a method to compute the total energy transmitted by tsunami waves, to
the case where the earthquake source is unknown, by using deep‐ocean pressure …

Almost 5 years after the 26 December 2004 Indian Ocean tragedy, the 10 August 2009
Andaman tsunami demonstrated that accurate forecasting is possible using the tsunami …

Tsunami generation from earthquake-induced seafloor deformations has long been
recognized as a major hazard to coastal areas. Strike-slip faulting has generally been …

The National Oceanic and Atmospheric Administration (NOAA) is the federal agency
charged with mitigating tsunami hazards in the United States. NOAA's National Weather …

The modeling of tsunami generation is an essential phase in understanding tsunamis. For
tsunamis generated by underwater earthquakes, it involves the modeling of the sea bottom …

The formation of rogue waves is studied in the framework of nonlinear hyperbolic systems
with an application to nonlinear shallow-water waves. It is shown that the nonlinearity in the …

The problem of tsunami wave shoaling and runup in U-shaped bays (such as fjords) and
underwater canyons is studied in the framework of 1D shallow water theory with the use of …