Under the action of continuous rainfall, the coupling linkage between runoff and seepage
can cause erosion of non-cohesive soil particles on vegetated slopes. A nonlinear turbulent …

In open channel, canals and rivers, a rapid increase in flow depth will induce a positive
surge, also called bore or compression wave. The positive surge is a translating hydraulic …

A detailed field study was carried out on a tidal bore to document the turbulent processes
and sediment entrainment which occurred. The measured bore, within the Arcins Channel of …

ABSTRACT A tidal bore is a compressive wave, advancing upstream in an estuary when the
flood tidal flow starts. It is observed when a macro-tidal flood flow enters the funnel shaped …

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Tidal bore impact can be strong and destructive, placing estuarine infrastructures under
great threat. However, there is a lack of research focusing on accurately estimating the …

Sediment transport is a geophysical phenomenon characterized by the displacement of
sediment particles in both the horizontal and vertical directions due to various forces. Most of …

Tidal bores are sudden discontinuities in water depth, and can be classified as undular and
breaking bores when tidal waves propagate upstream in a river mouth and on beaches. The …

Direct measurement of forces within the rough bed layer have been limited by previous
spatial-averaging shear force studies. A highly sensitive force transducer assembled with a …

A tidal bore is a hydrodynamic shock, propagating upstream as the tidal flow turns to rising,
with macro-tidal conditions in a funnel shaped system with shallow waters. The tidal bore of …