首页> 外文会议>Fourteenth Australasian Fluid Mechanics Conference Vol.I Dec 9-14, 2001 Adelaide, Australia >Three-dimensional modelling of a tsunami interacting with real topographical coastline using Smoothed Particle Hydrodynamics
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Three-dimensional modelling of a tsunami interacting with real topographical coastline using Smoothed Particle Hydrodynamics

机译:海浪与真实地形海岸线相互作用的三维模型,使用平滑粒子流体动力学

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This paper presents the simulation of a tsunami wave interacting with a section of real coastline adapted from the US Geological Survey (USGS). The full Navier-Stokes equations are solved using the Smoothed Particle Hydrodynamics (SPH) method. Since the SPH method is mesh free it is well suited to simulating complex free-surface flows of this kind involving wave propagation, splashing, wave refraction and break up. The full three dimensional nature of the simulation allows important features such as the differential breaking of the wave due to variations in the sea bed level, preferential inundation of exposed coastal features and wave reflection and refraction. The paper demonstrates the ability of the SPH method to handle these large geophysical phenomena having length scales of the order of kilometres and to be able to predict information of importance for coastal defence.
机译:本文介绍了根据美国地质调查局(USGS)改编的海啸波与真实海岸线的相互作用的模拟。完整的Navier-Stokes方程使用平滑粒子流体动力学(SPH)方法求解。由于SPH方法是无网格的,因此非常适合于模拟这种复杂的自由表面流动,包括波传播,飞溅,波折射和破裂。模拟的全部三维性质允许使用重要的功能,例如由于海床水位的变化而造成的波的差异性破坏,裸露的沿海特征的优先淹没以及波的反射和折射。本文证明了SPH方法能够处理这些大型地球物理现象,其长度尺度为千米,并能够预测对沿海防御至关重要的信息。

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