Estuarine turbidity maxima (ETMs) are generated by a large suite of hydrodynamic and
sediment dynamic processes, leading to longitudinal convergence of cross-sectionally …

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 Hangzhou Bay is a macro-tidal bay located to the south of the Changjiang estuary in
China. Along its northern shore, a large-scale tidal channel system has developed, which …

A three‐dimensional wave‐current‐sediment coupled numerical model with wetting and
drying process is developed to understand hydrodynamics and sediment transport dynamics …

Hangzhou Bay is a large, high-turbidity shallow bay located on the southern side of the
Changjiang Estuary, China. The process and dynamic mechanisms of water and sediment …

A three-dimensional, high-resolution tidal model coupled with the UNSW sediment model
(UNSW-Sed) based on Finite Volume Coastal Ocean Model (FVCOM) was set up to study …

Suspended sediment transport and stratification in the entire Changjiang River Estuary were
examined using the field data of sea-surface level, currents, salinity, and suspended …

The lateral bathymetry in the estuary results in different degrees of tidal mixing asymmetry,
which has significant impacts on the longitudinal sediment transport by changing the …

In coastal and estuarine waters, depth-averaged suspended sediment concentration
(DASSC) at a fixed observation site has two sources: local resuspension and advection …

Tidal flat variations (curvature) in macro‐tidal turbid bays highly correlate with sediment
dynamics. Interactions between tidal flats and sediment dynamics in macro‐tidal turbid …