Large-amplitude internal waves induce currents and turbulence in the bottom boundary
layer (BBL) and are thus a key driver of sediment movement on the continental margins …

The mechanisms responsible for sediment resuspension and transport by nonlinear internal
waves (NLIWs) remain poorly understood largely due to a dearth of detailed field …

Numerical and experimental studies of the transit of a mode-2 internal solitary wave over an
isolated ridge are presented. All studies used a quasi-two-layer fluid with a pycnocline …

The instability and vortex shedding in the bottom boundary layer caused by internal solitary
waves of depression propagating along a shallow pycnocline of a fluid are computed by …

The development of a separated bottom boundary layer in the footprint of a large-amplitude
internal solitary wave of depression, propagating against an oncoming barotropic current, is …

Double-diffusive convection in the finger regime is studied using direct numerical
simulations in a confined domain. For narrow (1–4 mm horizontal extent) domains, we …

Internal solitary waves (ISWs) are nonlinear fluctuations in nature that could cause
significant interactions between seawater and the seabed. ISWs have been proven to be an …

We collected high-resolution observations of nonlinear internal waves (NLIWs) at a
persistent upwelling front in the shallow coastal environment (~ 20 m) of northern Monterey …

Understanding the mechanisms of solute transfer across the sediment-water interface plays
a crucial role in water quality prediction and management. In this study, different arranged …

Confined geometries have an effect on hydrodynamic instabilities, and this provides
opportunities for controlling the rate of mixing in flows of engineering relevance. In multi …