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Numerical Prediction of Regular Wave Breaking on Very Gentle Slopes

机译:非常轻柔的斜坡常规波断裂的数值预测

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Regular wave deformation and breaking on very gentle slopes is calculated by Mixed-Eulerian-Lagrangian procedure.The velocity potentials and their normal derivatives on the boundary are calculated through the mixed 0-1 boundary elementmethod. The wave elevation and the potentials of time-stepping integration are determined by the 2nd-order Taylor expansionat the nodes of free surface boundary elements. During calculation the x-coordinates of the free surface element nodes aresupposed to remain unchanged, i.e. the partial derivatives of wave elevation and potentials with respect to x are consideredas zero. The numerical results of asymmetric parameters of breaking waves are verified by experimental study. It is shownthat when the wave asymmetry is weak, the maximum horizontal velocity of water particales occurs at the wave peak and, theaverage ratio of this maximum velocity to wave celerity is 0.96. However, when the wave asymmetry is strong, the maximumhorizontal velocity of water particles occurs just before the wave crest, and the average ratio of the maximum velocity to wavecelerity is about 0.98. The numerical results also show that the asymmetry of wave profiles affects the value of the wavebreaking index (H/d)b, that is, when the asymmetric characteristics are weak, the value of wave breaking index coincideswith that given by Coda; on the contrary, when the asymmetry of wave profiles is notable, the value of wave breaking indexis close to Nelson's result. The experimental study gives the same couclusions.
机译:通过混合欧洲拉格朗日程序计算常规波形变形和断裂非常平缓的斜坡。通过混合的0-1边界元素方法计算速度电位及其正常衍生物。通过自由表面边界元件的节点来确定波形升高和时间步进积分的电位。在计算期间,自由表面元件节点的X坐标被覆盖以保持不变,即波升和相对于X的电位的部分衍生物被认为是零。通过实验研究验证了破坏波的不对称参数的数值结果。当波不对称较弱时,当波峰值较弱时,水分的最大水平速度发生,并且这种最大速度与波圆形的灰度比为0.96。然而,当波浪不对称性强时,水颗粒的火山颗粒的火血管速度速度在波浪嵴之前发生,并且波形的最大速度的平均比率为约0.98。数值结果还表明波形谱的不对称性影响了导航指数(H / D)B的值,即当非对称特性较弱时,波断裂指数的值与CODA给出的波浪分数相吻合;相反,当波形轮廓的不对称是值得注意的时,波浪断裂索引的值接近尼尔森的结果。实验研究提供了相同的作用。

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