Internal solitary waves (ISWs) can cause strong seafloor sediment resuspension and induce
nepheloid layers in both shallow and deepwater environments. However, the roles of ISWs …

The widely recognized global phenomena of bottom nepheloid layer (BNL) and intermediate
nepheloid layer (INL) are ubiquitous in the ocean. These phenomena are induced by …

This study investigates three-dimensional semidiurnal internal tide (IT) energetics in the
vicinity of La Jolla Canyon, a steep shelf submarine canyon off the Southern California …

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

Vertical transport caused by mixing is essential for understanding physical processes in
lakes. However, mixing processes in shallow lakes are not well understood because of the …

This combined numerical/laboratory study investigates the effect of stratification form on the
shoaling characteristics of internal solitary waves propagating over a smooth, linear …

Despite suggestions that turbulence can affect the migration of zooplankton, field
observations of such effects are scarce. This is especially the case for bottom‐associated …

This study investigates the dynamics of tidally induced internal waves over a shallow ridge,
the Izu‐Ogasawara Ridge off the Japanese mainland, using a downscaled high‐resolution …

Previous studies have found that internal solitary waves (ISWs) can erode, resuspend and
transport seabed sediments and form intermediate nepheloid layers (INLs) and bottom …

Baroclinic (BC) tidal residual circulation due to internal tides is investigated around islands
over a shallow ridge using a numerical ocean model. Internal tides enhance vertical mixing …