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 …

Strong nonlinear internal waves generate a significant pressure force on the seafloor and
induce a pore-pressure response penetrated in the seabed and are thus an important driver …

We present a semi‐analytical model for predicting the breaking location of internal solitary
waves (ISWs) over a sloping seabed. Our conceptual model is based on laboratory …

Parameterizations for bottom shear stress are required to predict sediment resuspension
from field observations and within numerical models that do not resolve flow within the …

Dissipation of Turbulent Kinetic Energy in the Oscillating Bottom Boundary Layer of a Large
Shallow Lake in: Journal of Atmospheric and Oceanic Technology Volume 37 Issue 3 (2020) …

A series of experiments were conducted beneath simulated partial ice covers to investigate
the turbulent flow behaviour using a particle image velocimetry system. The velocity data …

Breaking nonlinear internal waves (NLIWs) of depression on boundary slopes drive mixing
and mass transport in the coastal ocean. Of the different breaker types, fission is most …

We investigate the dynamics of diurnal coastal-trapped waves and near-inertial waves on
the Tasmanian Eastern Continental Shelf, where the local Coriolis frequency is separable …