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 present study case examined the capability of Artificial Neural Network (ANN), Adaptive
Neuro-Fuzzy Inference System (ANFIS), M5P, and Random Forest (RF) soft-computing …

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 …

The submarine canyon was the main channel for the transport of sediment to the deep sea,
but the transport process in submarine canyon induced by internal solitary waves (ISWs) …

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 interaction between internal solitary waves (ISWs) and the seabed has been extensively
studied, so do the energy loss, sediment resuspension, parameterization criterion and near …

Evidences of sedimentation affected by oceanic circulation, such as nepheloid layers and
contourites are often observed along continental slopes. However, the oceanographic …

Lombok Strait is one of the main exit passages of the Indonesian throughflow (ITF),
connecting the interior Indonesian seas with the Indian Ocean. Satellite images have shown …

Cold-water corals (CWCs) are important ecosystem engineers in the deep sea that provide
habitat for numerous species and can form large coral mounds. These mounds influence …

Using direct numerical simulations (DNS), we investigate the structure and energetics of
breaking internal waves on slopes. We employ a Navier–Stokes code in an idealized three …