The propagation of positive surges in rivers and open channels is a highly unsteady turbulent process, with intensive sediment scouring and mixing. Despite its ecological and engineering significance, systematic physical studies of the unsteady turbulent characteristics of tidal bores remain limited. The present investigation performed ensemble-averaged velocity measurements using an array of two Vectrino II Profilers to investigate the vertical and transverse variability of the instantaneous velocity field during the propagation of breaking bores in open channel flows. Results highlighted satisfactory performances of Vectrino II Profilers in highly unsteady turbulent open channel flows. Rapid longitudinal deceleration, transient recirculat...
A positive surge results from a sudden change in flow that increases the depth. Positive surges are ...
A turbulent flow is characterised by an unpredictable behaviour, a broad spectrum of length and time...
A tidal bore is an abrupt rise in water depth advancing in some estuaries during spring tide conditi...
A positive surge is a sudden rise in water surface elevation in an open channel flow. It is an unste...
A tidal bore is an unsteady flow motion generated by the rapid water level rise at the river mouth d...
A positive surge results from a sudden change in flow that increases the depth, and a geophysical ap...
A sudden rise of the water depth in an open channel flow creates a surge propagating in the channel ...
In an open channel, steady flow conditions may be achieved when the discharge and boundary condition...
A tidal bore is a hydraulic jump in translation, propagating upstream as the tide turns to rising an...
A tidal bore is an unsteady rapidly-varied open channel flow generated by the swift advance of the e...
A tidal bore is an unsteady flow motion generated by the rapid water level rise at the river mouth d...
A tidal bore is a compressive wave of tidal origin, propagating upstream as the tidal flow turns to ...
A tidal bore is a wave propagating upstream as the tidal flow turns to rising. It forms during sprin...
When a river mouth has a flat converging shape with a tidal range exceeding 6 to 9 m, the river may ...
In an estuary, a tidal bore may be generated at the leading edge of the flood tidal wave during the ...
A positive surge results from a sudden change in flow that increases the depth. Positive surges are ...
A turbulent flow is characterised by an unpredictable behaviour, a broad spectrum of length and time...
A tidal bore is an abrupt rise in water depth advancing in some estuaries during spring tide conditi...
A positive surge is a sudden rise in water surface elevation in an open channel flow. It is an unste...
A tidal bore is an unsteady flow motion generated by the rapid water level rise at the river mouth d...
A positive surge results from a sudden change in flow that increases the depth, and a geophysical ap...
A sudden rise of the water depth in an open channel flow creates a surge propagating in the channel ...
In an open channel, steady flow conditions may be achieved when the discharge and boundary condition...
A tidal bore is a hydraulic jump in translation, propagating upstream as the tide turns to rising an...
A tidal bore is an unsteady rapidly-varied open channel flow generated by the swift advance of the e...
A tidal bore is an unsteady flow motion generated by the rapid water level rise at the river mouth d...
A tidal bore is a compressive wave of tidal origin, propagating upstream as the tidal flow turns to ...
A tidal bore is a wave propagating upstream as the tidal flow turns to rising. It forms during sprin...
When a river mouth has a flat converging shape with a tidal range exceeding 6 to 9 m, the river may ...
In an estuary, a tidal bore may be generated at the leading edge of the flood tidal wave during the ...
A positive surge results from a sudden change in flow that increases the depth. Positive surges are ...
A turbulent flow is characterised by an unpredictable behaviour, a broad spectrum of length and time...
A tidal bore is an abrupt rise in water depth advancing in some estuaries during spring tide conditi...