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Numerical simulation of solitary waves overtopping on a sloping sea dike using a particle method
Institution:1. Dept.of Hydraulic Eng., Delft University of Technology, Stevinweg 1, 2628 CNDelft, The Netherlands;2. Dept.of Coastal Structures and Waves, Deltares,PO Box 177, 2600 MHDelft, The Netherlands;1. The State Key Laboratory of Coastal and Offshore Engineering, Dalian University of Technology, Dalian 116024, China;2. School of Engineering, Physics and Mathematics, University of Dundee, DD1 4HN, United Kingdom;1. Dept. of Hydraulic Eng., Delft University of Technology, Stevinweg 1, 2628 CN Delft, The Netherlands;2. Dept. of Coastal Structures and Waves, Deltares, PO Box 177, 2600 MH Delft, The Netherlands;3. Flanders Hydraulics Research, Berchemlei 115, 2140 Antwerp, Belgium;4. Ghent University, Technologiepark 904, B-9052 Ghent, Belgium
Abstract:Sea dikes, as a commonly used type of coastal protection structures, are often attacked or damaged by violent waves overtopping under tsunamis and storm surges. In this study, the behavior of solitary waves traveling on a sloping sea dike is simulated, and solitary wave overtopping characteristics are analyzed using a complete Lagrangian numerical method, the moving particle semi-implicit (MPS) method. To better describe the complicated fluid motions during the wave overtopping process, the original MPS method is modified by introducing a new free surface detection method, i.e., the area filling rate identification method, and a modified gradient operator to provide higher precision. Meanwhile, the approximation method for sloping boundaries in particle methods is enhanced, and a smooth slope approximation method is proposed and recommended. To verify the improved MPS method, a solitary wave traveling over a steep sloping bed is studied. The entire solitary wave run-up and run-down processes and exquisite water movements are reproduced well by the present method, and are consistent with the corresponding experimental results. Subsequently, the improved MPS method is applied to investigate the overtopping process of a single solitary wave over a sloping sea dike. The results show that the hydraulic jump phenomenon is also possible to occur during the run-down motion of the solitary wave overtopping. Finally, the characteristics of the propagation and overtopping of two successive solitary waves on a sloping sea dike are discussed. The result manifests that the interaction between adjacent solitary waves affects wave overtopping patterns and overtopping velocities.
Keywords:Particle method  Solitary waves overtopping  Slope approximation  Run-down motion  Hydraulic jump
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