Wave–current ripples that develop on seabeds of mixed non-cohesive sand and cohesive
clay are commonplace in coastal and estuarine environments. While laboratory research on …

Ripples on tidal flats significantly influence bedform roughness and near-bed turbulence, yet
their dynamics in sandy and muddy environments remain incompletely understood. While …

Hummocky cross‐stratification is commonly observed in the marine offshore transition to
lower shoreface environments. However, to date, the origins of hummocky cross …

The critical bed-shear stress (cbs) for erosion of mud–sand bed mixtures was studied in
laboratory and field conditions with currents, waves, and combined currents and waves …

Wave–current ripples that develop on seabeds of mixed non-cohesive sand and cohesive
clay are commonplace in coastal and estuarine environments. However, laboratory research …

River deltas located in the Fluvial-to-Tidal-Transition-Zone (FTTZ) experience a complex
interaction of river and tidal currents, driving the delta morphology. Deltas worldwide face …

The long-term development of ancient and modern coastal distributive fluvial systems
(DFSs) during periods of relative sea-level highstand or fall usually drives net-progradation …