A triple deck model of ripple formation and evolution
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Publication:3553995
DOI10.1063/1.1588305zbMath1186.76302OpenAlexW2029822697MaRDI QIDQ3553995
Publication date: 22 April 2010
Published in: Physics of Fluids (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1063/1.1588305
Related Items (9)
Parallelization of a relaxation scheme modelling the bedload transport of sediments in shallow water flow ⋮ Asymptotic derivation and simulations of a non-local Exner model in large viscosity regime ⋮ Self-similar evolution of a body eroding in a fluid flow ⋮ Drop impact on a solid surface: short-time self-similarity ⋮ Stability of bedforms in laminar flows with free surface: from bars to ripples ⋮ Couette flow in channels with wavy walls ⋮ Bedforms in a turbulent stream: formation of ripples by primary linear instability and of dunes by nonlinear pattern coarsening ⋮ Evolution of a model dune in a shear flow ⋮ Towards a new friction model for shallow water equations through an interactive viscous layer
Cites Work
- On physical mechanisms in two– and three–dimensional separations
- Sand ripples under sea waves Part 1. Ripple formation
- A particle model of rolling grain ripples under waves
- On hypersonic self‐induced separation, hydraulic jumps and boundary layers with algebraic growth
- The formation of ripples and dunes on an erodible bed
- On boundary-layer flow past two-dimensional obstacles
- On the High Reynolds Number Theory of Laminar Flows
- Dispersion of suspended particles in turbulent flow
- The standing hydraulic jump: theory, computations and comparisons with experiments
- FLOW THROUGH CONSTRICTED OR DILATED PIPES AND CHANNELS: PART 1
- The hydraulic jump in a viscous laminar flow
- Opposing mixed convection flow in a wall jet over a horizontal plate
- Linear instability mechanisms for sand wave formation
- Instability of a bed of particles sheared by a viscous flow
- Inception of channelization and drainage basin formation: upstream-driven theory
- Viscous resuspension of a sediment within a laminar and stratified flow
- Self-induced separation
- The mechanics of dunes and antidunes in erodible-bed channels
- Separating shear flow past a surface-mounted blunt obstacle
- Removing the marching breakdown of the boundary-layer equations for mixed convection above a horizontal plate
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