Runup and boundary layers on sloping beaches
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Publication:5249335
DOI10.1063/1.4773327zbMath1310.76057OpenAlexW2070104140MaRDI QIDQ5249335
Atle Jensen, Erik Lindström, G. Sælevik, A. F. Bertelsen, D. Laskovski, Geir Pedersen
Publication date: 4 May 2015
Published in: Physics of Fluids (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1063/1.4773327
Experimental work for problems pertaining to fluid mechanics (76-05) Boundary-layer theory, separation and reattachment, higher-order effects (76D10)
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Cites Work
- Simulation of spilling breaking waves using a two phase flow CFD model
- An efficient surface integral algorithm applied to unsteady gravity waves
- Swash overtopping a truncated plane beach
- Surf and run-up on a beach: a uniform bore
- Water waves of finite amplitude on a sloping beach
- Boundary layer flow and bed shear stress under a solitary wave
- The interaction between a solitary wave and a submerged semicircular cylinder
- Evolution of the turbulence structure in the surf and swash zones
- Coherent structures in wave boundary layers. Part 1. Oscillatory motion
- Coherent structures in wave boundary layers. Part 2. Solitary motion
- Turbulent boundary layer under a solitary wave
- Run-up of solitary waves
- The stability of solitary waves
- The runup of solitary waves
- Linear and nonlinear stability of the Blasius boundary layer
- An experimental study of wave run-up at a steep beach
- Non-breaking and breaking solitary wave run-up
- Viscous effects on transient long-wave propagation
- The motion of an internal solitary wave of depression over a fixed bottom boundary in a shallow, two-layer fluid
- Solitary wave breaking on sloping beaches: 2-D two-phase flow numerical simulation by SL-VOF method
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