A tidal bore is an unsteady rapidly-varied open channel flow characterised by a rise in water surface elevation in estuarine zones, under spring tidal conditions. After formation, the bore is traditionally analysed as a hydraulic jump in translation and its leading edge is characterised by a breaking roller for Froude number Fr1 > 1.3–1.5. The roller is a key flow feature characterised by intense turbulence and air bubble entrainment. Detailed unsteady air-water flow measurements were conducted in a breaking bore propagating in a large-size channel, using an array of three dual-tip phase detection probes and photographic camera. The data showed a relatively steep roller, with a short and dynamic bubbly flow region. Air entrainment took plac...
Abstract: A tidal bore is an unsteady flow motion generated by the rapid water level rise at the riv...
In an estuarine system, the flood tidal wave may become a tidal bore during the early flood tide in ...
The sudden transition from a high-velocity, supercritical open channel flow into a slow-moving sub-c...
A tidal bore is an unsteady rapidly-varied open channel flow characterised by a rise in water surfac...
In an estuary, a tidal bore is a hydraulic jump in translation generated at the leading edge of the ...
In an estuary, a tidal bore may be generated at the leading edge of the flood tidal wave during the ...
A positive surge or bore is an unsteady rapidly-varied open channel flow characterised by a rise in ...
In an estuary, a tidal bore is a hydraulic jump in translation generated at the leading edge of the ...
In open channel flows, the transition from a rapid to fluvial flow motion is called a hydraulic jump...
A tidal bore is a hydraulic jump in translation, propagating upstream as the tide turns to rising an...
A tidal bore is an unsteady flow motion generated by the rapid water level rise at the river mouth d...
Breaking surges and bores are observed during flood events, tidal bores and tsunamis propagating in ...
A tidal bore is an unsteady flow motion generated by the rapid water level rise at the river mouth d...
Continuing from the part 1 (Shi et al., 2022) this paper presents an experimental investigation of t...
A tidal bore is a surge of waters propagating upstream in an estuary as the tidal flow turns to risi...
Abstract: A tidal bore is an unsteady flow motion generated by the rapid water level rise at the riv...
In an estuarine system, the flood tidal wave may become a tidal bore during the early flood tide in ...
The sudden transition from a high-velocity, supercritical open channel flow into a slow-moving sub-c...
A tidal bore is an unsteady rapidly-varied open channel flow characterised by a rise in water surfac...
In an estuary, a tidal bore is a hydraulic jump in translation generated at the leading edge of the ...
In an estuary, a tidal bore may be generated at the leading edge of the flood tidal wave during the ...
A positive surge or bore is an unsteady rapidly-varied open channel flow characterised by a rise in ...
In an estuary, a tidal bore is a hydraulic jump in translation generated at the leading edge of the ...
In open channel flows, the transition from a rapid to fluvial flow motion is called a hydraulic jump...
A tidal bore is a hydraulic jump in translation, propagating upstream as the tide turns to rising an...
A tidal bore is an unsteady flow motion generated by the rapid water level rise at the river mouth d...
Breaking surges and bores are observed during flood events, tidal bores and tsunamis propagating in ...
A tidal bore is an unsteady flow motion generated by the rapid water level rise at the river mouth d...
Continuing from the part 1 (Shi et al., 2022) this paper presents an experimental investigation of t...
A tidal bore is a surge of waters propagating upstream in an estuary as the tidal flow turns to risi...
Abstract: A tidal bore is an unsteady flow motion generated by the rapid water level rise at the riv...
In an estuarine system, the flood tidal wave may become a tidal bore during the early flood tide in ...
The sudden transition from a high-velocity, supercritical open channel flow into a slow-moving sub-c...