The deep sea-an oceanic layer below 200 m depths–has important global biogeochemical
and nutrient cycling functions. It also receives organic pollutants from anthropogenic …

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) …

Hyperpycnites record information on sedimentary processes and climate change and play a
significant role in hydrocarbon exploration. However, deep-water hyperpycnites can hardly …

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 …

Nepheloid layers and turbidity currents transport large quantities of detrital sediments to
deep-sea basins. Locally they may control seawater–detrital particle interactions and modify …

Internal waves (IWs) are broadly distributed globally and have significant impacts on
offshore engineering and underwater navigation. The prediction of IW propagation is a …

Internal solitary waves (ISWs) with features such as large amplitude, short period, and fast
speed have great influence on underwater thermohaline structure, nutrient transport, and …

Characteristics and generation of internal waves (IWs) in the Sulu Sea are studied using
Moderate-Resolution Imaging Spectroradiometer (MODIS) and Visible Infrared Imaging …

An analytical solution is developed for studying transient water wave-induced responses
inside an unsaturated poroelastic seabed of finite thickness. The soil skeleton and the pore …