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

We now understand that, morphologically, natural tidal marshes are generally near or
progressing rapidly toward dynamic equilibrium with sediment supply, vegetative growth …

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 …

This contribution investigates the morphodynamic equilibrium of funnel‐shaped well‐mixed
estuaries and/or tidal channels. The one‐dimensional de Saint Venant and Exner equations …

Over decades and centuries, the mean depth of estuaries changes due to sea-level rise,
land subsidence, infilling, and dredging projects. These processes produce changes in …

The long‐term morphological evolution of tidal landforms in response to physical and
ecological forcings is a subject of great theoretical and practical importance. Toward the …

The literature on estuarine physical studies is vast, diverse and contains many valuable
case studies in addition to pure, process-based research. This essay is an attempt to …

This study analyzes tide transformation in the Guadalquivir estuary (SW Spain). When fresh
water discharges are less than 40 m3/s, the estuary is tidally‐dominated (flood‐dominated) …

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

This paper describes an analysis of the observed up-river transport of fine sediments in the
Ems River, Germany/Netherlands, using a 1DV POINT MODEL, accounting for turbulence …