Internal waves are important physical phenomena on the continental shelf/slope. They are
often very energetic, and their breaking provides an important dissipation and mixing …

Internal waves occur nearly ubiquitously in lakes and oceans yet their sedimentary records
remain largely unrecognized. Waves propagate at the interface between fluids of different …

Active deepening of tidal channels usually results in the alteration of the vertical and the
horizontal tide. This may lead to concurrent significant increases in mean suspended matter …

A detailed energy analysis of the barotropic and baroclinic M 2 tides in the Monterey Bay
area is performed. The authors first derive a theoretical framework for analyzing internal tide …

Two-dimensional, nonlinear and nonhydrostatic field-scale numerical simulations are used
to examine the resuspension, dispersal and transport of mud-like sediment caused by the …

The breaking of fully nonlinear internal solitary waves of depression shoaling upon a
uniformly sloping boundary in a smoothed two-layer density field was investigated using …

A new modelling framework is presented for application to a range of three‐dimensional
(3D) multi‐scale oceanographic problems. The approach is based upon a finite element …

We observed transient stratification and mixing events associated with nearshore internal
bores in southern Monterey Bay using an array of instruments with high spatial and temporal …

The environmental conditions, mechanisms, and processes that resulted in the deposition of
organic-matter-rich sediments during the early Toarcian oceanic anoxic event are still a …

Laboratory observations are presented showing the structure and dynamics of the turbulent
bottom boundary layer beneath nonlinear internal waves (NLIWs) of depression shoaling …