We present an investigation into the growth of nearshore, rhythmic patterns. A comprehensive linear stability model of the surf and shoaling zones is used to examine which type of pattern, transverse or crescentic bar, is likely to form under different wave conditions. In contrast to earlier studies we examine normal and near-normal incidence on a plane beach. In doing so we reproduce results of earlier, more restricted studies and thereby identify the physical mechanisms leading to the growth of different patterns. This paper also focuses on the role of random wave height distribution compared with regular waves and identifies conditions likely to lead to pattern growth. To this end, an amended wave height dissipation function is presented...
International audienceNearshore sandbars are often characterized by three-dimensional bed patterns. ...
This paper considers the evolution of steep mobile sediment beaches under random waves and results f...
The formation and development of transverse and crescentic sand bars in the coastal marine environm...
The coupling between topographic irregularities and wave-driven mean water motion in the surf zone i...
A wave of small amplitude is considered which approaches a straight beach normally and which is part...
The coupling between topographic irregularities and wave-driven mean water motion in the surf zone i...
The process of formation of a rip channel/crescentic bar system on a straight, sandy coast is examin...
The process of formation of a rip channel/crescentic bar system on a straight, sandy coast is examin...
Double sandbar systems often characterize the surf zone of wave-dominated beaches and display a vari...
Double sandbar systems often characterize the surf zone of wave-dominated beaches and display a vari...
Nearshore sandbars are often characterized by three-dimensional bed patterns. To analyze the influen...
Nearshore sandbars are often characterized by three-dimensional bed patterns. To analyze the influen...
Double sandbar systems often characterize the surf zone of wave-dominated beaches and display a vari...
The coupling between hydrodynamics and the evolving topography in the surf zone has been theoretical...
The bed forms in the surf zone can grow as a result of natural morphodynamic instabilities, forced b...
International audienceNearshore sandbars are often characterized by three-dimensional bed patterns. ...
This paper considers the evolution of steep mobile sediment beaches under random waves and results f...
The formation and development of transverse and crescentic sand bars in the coastal marine environm...
The coupling between topographic irregularities and wave-driven mean water motion in the surf zone i...
A wave of small amplitude is considered which approaches a straight beach normally and which is part...
The coupling between topographic irregularities and wave-driven mean water motion in the surf zone i...
The process of formation of a rip channel/crescentic bar system on a straight, sandy coast is examin...
The process of formation of a rip channel/crescentic bar system on a straight, sandy coast is examin...
Double sandbar systems often characterize the surf zone of wave-dominated beaches and display a vari...
Double sandbar systems often characterize the surf zone of wave-dominated beaches and display a vari...
Nearshore sandbars are often characterized by three-dimensional bed patterns. To analyze the influen...
Nearshore sandbars are often characterized by three-dimensional bed patterns. To analyze the influen...
Double sandbar systems often characterize the surf zone of wave-dominated beaches and display a vari...
The coupling between hydrodynamics and the evolving topography in the surf zone has been theoretical...
The bed forms in the surf zone can grow as a result of natural morphodynamic instabilities, forced b...
International audienceNearshore sandbars are often characterized by three-dimensional bed patterns. ...
This paper considers the evolution of steep mobile sediment beaches under random waves and results f...
The formation and development of transverse and crescentic sand bars in the coastal marine environm...