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SIMULATION OF TSUNAMI-INDUCED FLOOD IN HINTERLAND OF SEAWALL BY USING PARTICLE METHOD

机译:用粒子法模拟海啸腹地海啸诱发的洪水

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摘要

Complicated characteristics of tsunami induced flood at a vertical seawall, including overflowing jet and run-up over a hinterland are reproduced by the gridless Lagrangian flow model, or the particle method. Detailed behavior of flow, which is characterized by an overflowing jet, circulating flow cell and a hydraulic jump, is simulated on both of a uniform slope and a horizontal bed with bar-type roughness.
机译:无网格拉格朗日流模型或粒子法再现了海啸在垂直海堤上引发的复杂特征,包括溢流和腹地上空上升。在均匀的坡度和具有杆状粗糙度的水平床上,都模拟了详细的流动行为,其特征是溢流,循环流通池和水力跳跃。

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