In seismology and ocean acoustics, the interface with the atmosphere is typically
represented as a free surface. Similarly, these interfaces are considered as a rigid surface …

Sound propagation predictions for ice-covered ocean acoustic environments do not match
observational data: received levels in nature are less than expected, suggesting that the …

A three-dimensional (3D) geodesic Cartesian parabolic equation model is utilized to study
the propagation of low-frequency underwater sound (5 to 20 Hz), the so-called T-phase …

Numerical simulations based on the Finite Volume Method (FVM) solve the wave equation
directly to provide highly accurate predictions of the sound field in ocean waveguides …

A full-field perturbation approach is modified for an ice-covered ocean and applied to
estimating narrowband long-range reverberation caused by roughness of the ice-water …

Oceanic T-waves are earthquake signals that originate when elastic waves interact with the
fluid–elastic interface at the ocean bottom and are converted to acoustic waves in the ocean …

Parabolic equation (PE) method is an efficient tool for modelling underwater sound
propagation, particularly for problems involving range dependence. Since the PE method …

Normal mode solutions to range-independent seismo-acoustic problems are benchmarked
against elastic parabolic equation solutions and then used to benchmark the shear elastic …

In this paper we consider a general hyperbolic system subject to random perturbations
which models wave propagation in random media. We consider the paraxial white-noise …

The sound propagation in a wedge‐shaped waveguide with perfectly reflecting boundaries
is one of the few range‐dependent problems with an analytical solution. This provides a …