Volcanoes can produce tsunamis by means of earthquakes, caldera and flank collapses,
pyroclastic flows or underwater explosions,,–. These mechanisms rarely displace enough …

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 …

Flexural-gravity wave characteristics are analysed, in the presence of a compressive force
and a two-layer fluid, under the assumption of linearized water wave theory and small …

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 …

The overall system of interest is an infinite half-space in which a compressible ocean is the
top layer and an elastic seafloor (together with the crust beneath) forms a semi-infinite …

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 development of offshore observation technology will provide researchers with tsunami
records from within an earthquake focal area, but this will create new problems. Because …

The propagation of waves from a vertical uplift of a slender rectangular fault in a sea of
constant depth is discussed, accounting for water compressibility, gravity and seabed …

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 …

In the present paper, we aim to reduce the discrepancies between tsunami arrival times
evaluated from tsunami models and real measurements considering the role of ocean …