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 …

Exchange of material across the nearshore region, extending from the shoreline to a few
kilometers offshore, determines the concentrations of pathogens and nutrients near the …

Marine nepheloid layer is widely distributed in the oceans and marginal seas. The
concentration of suspended particles in the nepheloid layer is significantly higher than that …

Abstract Knowledge of nepheloid layers is important to improve the understanding of
physical, geological, and sedimentary processes from continental shelf to abyssal …

The deformation and evolution of internal solitary waves (ISWs) beneath an ice keel can
enable potential diapycnal mixing and facilitate upper ocean heat transport, despite a poor …

This is Part II of a two-part study focused on Stokes drift and transient rip current (TRC)
effects on the unstratified (Part I) and stratified (this paper) inner shelf. Part I focuses on …

High-resolution three-dimensional large-eddy simulations are used to investigate the effects
of internal solitary waves (ISWs) breaking over a sloping boundary. The lock release method …

Numerical simulations of sediment resuspension due to shoaling internal bores are
performed with a nonhydrostatic model, SUNTANS. Results show strong sediment …

Observations of Nonlinear Internal Wave Run-Up to the Surfzone in: Journal of Physical
Oceanography Volume 48 Issue 3 (2018) Jump to Content Logo Logo Logo Logo Logo …

Abstract The Sulawesi Sea is one of the most active regions where internal solitary waves
(ISWs) are frequently observed through satellite images. These waves that result from the …