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Numerical characterisation and efficient prediction of landslide-tsunami propagation over a wide range of idealised bathymetries

机译:广泛理想沐浴盆地山体滑艇 - 海啸传播的数值表征及高效预测

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摘要

Landslide-tsunamis are generated by masses, such as landslides or icebergs, impacting into water bodies. Such tsunamis resulted in major catastrophes in the recent past. Generic research into landslide-tsunamis has widely been conducted in idealised water body geometries at uniform water depths. However, varying bathymetries can significantly alter landslide-tsunamis. This article investigates this effect in a 2D flume using selected idealised bathymetries to provide methods to predict the transformed wave characteristics downwave of each feature. The selected bathymetries are: (a) linear beach bathymetries, (b) submerged positive and negative Gaussian bathymetric features and (c) submerged positive and negative step bathymetries. The hydrodynamic model SWASH, based on the non-hydrostatic non-linear shallow water equations, was used to simulate 9 idealised landslidetsunamis (1 approximate linear, 2 Stokes, 2 cnoidal and 4 solitary waves), for a total of 184 tests. The analysed parameters include the free water surface, wave height and amplitude. Shoaling in (a) is represented by either Green's law or the Boussinesq's adiabatic approximation up to wave breaking with an accuracy of -7% to +10% for cnoidal and solitary waves, respectively. The results are then analysed with an (i) Artificial Neural Network and (ii) a regression analysis. (i) shows a smaller Mean Square Error (MSE) of 0.0027 than (ii) (MSE = 0.024) and good generalisation in predicting the transformed wave characteristics and, after defining the best dimensionless parameters, (ii) provides empirical equations to predict transformed waves. In addition, simulations were conducted in a 3D basin to investigate the combined effect of the bathymetry and geometry. The efficient use of the developed prediction methods is demonstrated with the 2014 Lake Askja landslide-tsunami where a good accuracy is achieved compared to available numerical simulations.
机译:Landslide-Tsunamis由群众产生,例如山体滑坡或冰山,影响水体。此类海啸导致最近的过去灾难。在均匀的水深在理想的水体几何形状中广泛地进行了普通岩石 - 海啸的仿制研究。然而,不同的沐浴玻璃可以显着改变滑坡 - 海啸。本文使用所选择的理想化浴剂调查2D水槽中的这种效果,以提供预测每个特征的转换的变换波特性的方法。所选的浴室是:(a)线性海滩浴,(b)浸没的正和阴性高斯碱基特征和(c)浸没正面和负面步骤浴。基于非静液压非线性浅水方程的流体动力模型旋转模拟9个理想化的Landslidetsunis(1个近似线性,2个斯托克,2个Cnoidal和4个孤立的波浪),总共184个测试。分析的参数包括自由水表面,波浪高度和幅度。 (a)中的浅层划分由绿色的法律或Boussinesq的绝热近似,分别为CNOIDAL和孤波的精度为-7%至+ 10%的波浪。然后用(i)人工神经网络和(ii)分析结果进行回归分析。 (i)示出了0.0027的较小均方误差(MSE)而不是(ii)(MSE = 0.024),并且在预测变换的波特性方面的良好推广,并且在定义最佳无量纲参数之后,(ii)提供了经验方程以预测变换波浪。此外,在3D盆地进行模拟,以研究沐浴碱和几何形状的组合效果。通过2014湖Askja Landslide-Tsunami对发达的预测方法进行了有效的使用,其中与可用的数值模拟相比,实现了良好的准确性。

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