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 …

The time-domain motion of a finite depth ocean subject to an arbitrary (in both time and
space) imposed displacement of the bottom is studied under the assumption of linear theory …

To estimate tsunami hazards, it is first necessary to have reliable data relating to the rupture
characteristics, such as epicenter, fault geometry, uplift speed, and duration. We made use …

Tsunamis can propagate thousands of kilometres across the ocean. Precise calculations of
arrival times are essential for reliable early warning systems, determination of source and …

The sudden generation of wave disturbances in the ocean is associated with a change in
the pressure field in the liquid layer. Consequently, compression-type of waves, known as …

A submarine earthquake that generates a tsunami sends a family of acoustic signals that
carry information on the fault dynamics and geometry. These signals travel at the speed of …

The propagation of wave disturbances from a complex multi-fault submarine earthquake of
slender rectangular segments in a sea of constant depth is discussed, accounting for both …

The effect of the compressibility of the ocean and its role in generating progressive
compression-type waves (acoustic-gravity waves) are revisited. Originally, Longuet-Higgins …

The steady-state interaction of acoustic–gravity waves in an ocean of uniform depth is
researched theoretically by means of the homotopy analysis method (HAM), an analytic …

We present a novel analytical model for the evolution of hydroacoustic waves in weakly
compressible fluids characterised by depth variations of the sound speed profile. Using a …