Lagrangian modelling of nonlinear viscous waves generated by moving seabed deformation
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Publication:2699395
DOI10.1016/j.euromechflu.2023.01.002OpenAlexW4316039402MaRDI QIDQ2699395
Publication date: 26 April 2023
Published in: European Journal of Mechanics. B. Fluids (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1016/j.euromechflu.2023.01.002
Cites Work
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- Enhancement of performance and stability of MPS mesh-free particle method for multiphase flows characterized by high density ratios
- Enhancement of stability and accuracy of the moving particle semi-implicit method
- Optimal shape of an underwater moving bottom generating surface waves ruled by a forced Korteweg-de Vries equation
- An enhanced weakly-compressible MPS method for free-surface flows
- Transient waves generated by a moving bottom obstacle: a new near-field solution
- On water waves generated by a bottom obstacle translating at a subcritical speed
- Hydro-acoustic precursors of gravity waves generated by surface pressure disturbances localised in space and time
- Landslide tsunamis propagating along a plane beach
- Landslide tsunamis propagating around a conical island
- A weakly compressible MPS method for modeling of open-boundary free-surface flow
- Generation of upstream advancing solitons by moving disturbances
- On solitary waves forced by underwater moving objects
- Weakly nonlinear theory for dispersive waves generated by moving seabed deformation
- Review of smoothed particle hydrodynamics: towards converged Lagrangian flow modelling
- Effects of the sound speed vertical profile on the evolution of hydroacoustic waves
- A First Course in Computational Fluid Dynamics
- Computational Wave Dynamics
- Generation of solitary waves by transcritical flow over a step
- Runup and rundown generated by three-dimensional sliding masses
- Theory and Applications of Smoothed Particle Hydrodynamics
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