The linear stability of a planar and a barred coast is studied with a complex process-based model. By applying either the Engelund and Hansen or the Bailard sediment transport formulation, and a wave angle of approximately 5 ° in the breaker zone, the sensitivity of the linear stability characteristics to the sediment transport formulation is explored. Applying Engelund and Hansen to planar beaches, no fastest growing mode is found since the growth rate continuously increases with increasing wavelength. The corresponding bed perturbations are very oblique, down-current oriented bars. With Bailard, on the contrary, the growth rate increases with decreasing wavelength, suggesting that the preferred wavelength is somewhere between 0 and 300 m....
The present study investigates longshore sediment transport for a variety of bathymetric and wave co...
AbstractmAn initially uniform longshore current on a plane erodible beach is considered and a linear...
Field measurements of the local time-varying suspended sediment flux across a barred shoreface demon...
The initial growth of bed perturbations on planar sloping beaches under the forcing of obliquely inc...
The coupling between topography, waves and currents in the surf zone may self-organize to produce th...
The process of formation of a rip channel/crescentic bar system on a straight, sandy coast is examin...
The development and evolution of crescentic patterns in double-barred systems is explored using a mo...
A nonlinear numerical model based on a wave- and depth-averaged shallow water equation solver with w...
ABSTRACT: In this work, a recently developed numerical model, capable of solving the hydro- and morp...
An idealised model is presented to study the formation of sorted bed forms generated by a wind-drive...
In the scope of NOURTEC, an EEC project, efforts are made to simulate the behaviour of executed fore...
An idealised model is presented to study the formation of sorted bed forms generated by a wind-drive...
In shallow water, any two waves of the same frequency are shown to produce complex patterns of drift...
A wave of small amplitude is considered which approaches a straight beach normally and which is part...
Large scale patterns in the seabed often occur in the nearshore zone of sandy beaches. A widely occu...
The present study investigates longshore sediment transport for a variety of bathymetric and wave co...
AbstractmAn initially uniform longshore current on a plane erodible beach is considered and a linear...
Field measurements of the local time-varying suspended sediment flux across a barred shoreface demon...
The initial growth of bed perturbations on planar sloping beaches under the forcing of obliquely inc...
The coupling between topography, waves and currents in the surf zone may self-organize to produce th...
The process of formation of a rip channel/crescentic bar system on a straight, sandy coast is examin...
The development and evolution of crescentic patterns in double-barred systems is explored using a mo...
A nonlinear numerical model based on a wave- and depth-averaged shallow water equation solver with w...
ABSTRACT: In this work, a recently developed numerical model, capable of solving the hydro- and morp...
An idealised model is presented to study the formation of sorted bed forms generated by a wind-drive...
In the scope of NOURTEC, an EEC project, efforts are made to simulate the behaviour of executed fore...
An idealised model is presented to study the formation of sorted bed forms generated by a wind-drive...
In shallow water, any two waves of the same frequency are shown to produce complex patterns of drift...
A wave of small amplitude is considered which approaches a straight beach normally and which is part...
Large scale patterns in the seabed often occur in the nearshore zone of sandy beaches. A widely occu...
The present study investigates longshore sediment transport for a variety of bathymetric and wave co...
AbstractmAn initially uniform longshore current on a plane erodible beach is considered and a linear...
Field measurements of the local time-varying suspended sediment flux across a barred shoreface demon...