Depth-integrated free-surface flow with a two-layer non-hydrostatic formulation
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Publication:2902521
DOI10.1002/fld.2566zbMath1245.76024OpenAlexW2094005402WikidataQ59715055 ScholiaQ59715055MaRDI QIDQ2902521
Publication date: 20 August 2012
Published in: International Journal for Numerical Methods in Fluids (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1002/fld.2566
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Cites Work
- An arbitrary Lagrangian-Eulerian \(\sigma\) (ALES) model with non-hydrostatic pressure for shallow water flows
- Depth-integrated, non-hydrostatic model with grid nesting for tsunami generation, propagation, and run-up
- Depth-integrated, non-hydrostatic model for wave breaking and run-up
- The runup of solitary waves
- Shallow-water flow solver with non-hydrostatic pressure: 2D vertical plane problems
- A semi-implicit finite difference method for non-hydrostatic, free-surface flows
- An accurate and efficient finite-difference algorithm for non-hydrostatic free-surface flow with application to wave propagation
- A staggered conservative scheme for every Froude number in rapidly varied shallow water flows
- Further experiences with computing non-hydrostatic free-surface flows involving water waves
- Boussinesq-type formulations for fully nonlinear and extremely dispersive water waves: derivation and analysis
- Long waves on a beach
