This report presents the experimental methods used in, and tabulates the data obtained from, experiments in the Pulsating Water Tunnel at HR Wallingford. They were made over an immobile gravel rough bed, to investigate the hydrodynamics of wave-current boundary-layer interaction, and over a fine sand bed, to investigate the pick-up, suspension and transport of sediment by combined waves and currents
A series of sand bed experiments was carried out in the Large Wave Flume in Hannover, Germany as a c...
Coastal changes occur mostly as a result of changes in sediment transport along the coast. If at cro...
The evolution and utilization of estuarine and coastal regions are greatly restricted by sediment pr...
Two series of experiments were carried out in the Large Oscillating Water Tunnel of Delft Hydraulics...
A series of experiments were carried out in the Large Oscillating Water Tunnel of Delft Hydraulics i...
SIGLEAvailable from British Library Document Supply Centre- DSC:D75926/87 / BLDSC - British Library ...
The present report contains a description of an experimental program, as a follow up of experiments ...
Measurements are presented of the conditions for the initial motion of sediment under combined stead...
This study set out to investigate the shear stress behaviour at the bed under combined wave and curr...
An experimental study of the turbulent boundary layer, where waves propagate with a current, is pres...
Ripple formation and evolution as well as vortex separation along the bedform profile strongly influ...
Important changes in the coastal profile can appear in a few hours during storm conditions. During t...
The motivation to develop a transport formulation for the combination of waves and current has been ...
For the general purposes of morphodynamic computations in coastal zones, simple formula-based models...
Especially during storms the coast-profile can change dramatically. During storms large waves cause ...
A series of sand bed experiments was carried out in the Large Wave Flume in Hannover, Germany as a c...
Coastal changes occur mostly as a result of changes in sediment transport along the coast. If at cro...
The evolution and utilization of estuarine and coastal regions are greatly restricted by sediment pr...
Two series of experiments were carried out in the Large Oscillating Water Tunnel of Delft Hydraulics...
A series of experiments were carried out in the Large Oscillating Water Tunnel of Delft Hydraulics i...
SIGLEAvailable from British Library Document Supply Centre- DSC:D75926/87 / BLDSC - British Library ...
The present report contains a description of an experimental program, as a follow up of experiments ...
Measurements are presented of the conditions for the initial motion of sediment under combined stead...
This study set out to investigate the shear stress behaviour at the bed under combined wave and curr...
An experimental study of the turbulent boundary layer, where waves propagate with a current, is pres...
Ripple formation and evolution as well as vortex separation along the bedform profile strongly influ...
Important changes in the coastal profile can appear in a few hours during storm conditions. During t...
The motivation to develop a transport formulation for the combination of waves and current has been ...
For the general purposes of morphodynamic computations in coastal zones, simple formula-based models...
Especially during storms the coast-profile can change dramatically. During storms large waves cause ...
A series of sand bed experiments was carried out in the Large Wave Flume in Hannover, Germany as a c...
Coastal changes occur mostly as a result of changes in sediment transport along the coast. If at cro...
The evolution and utilization of estuarine and coastal regions are greatly restricted by sediment pr...