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Statistical emulation of landslide-induced tsunamis at the Rockall Bank NE Atlantic

机译:大西洋东北洛克罗克银行滑坡诱发海啸的统计模拟

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摘要

Statistical methods constitute a useful approach to understand and quantify the uncertainty that governs complex tsunami mechanisms. Numerical experiments may often have a high computational cost. This forms a limiting factor for performing uncertainty and sensitivity analyses, where numerous simulations are required. Statistical emulators, as surrogates of these simulators, can provide predictions of the physical process in a much faster and computationally inexpensive way. They can form a prominent solution to explore thousands of scenarios that would be otherwise numerically expensive and difficult to achieve. In this work, we build a statistical emulator of the deterministic codes used to simulate submarine sliding and tsunami generation at the Rockall Bank, NE Atlantic Ocean, in two stages. First we calibrate, against observations of the landslide deposits, the parameters used in the landslide simulations. This calibration is performed under a Bayesian framework using Gaussian Process (GP) emulators to approximate the landslide model, and the discrepancy function between model and observations. Distributions of the calibrated input parameters are obtained as a result of the calibration. In a second step, a GP emulator is built to mimic the coupled landslide-tsunami numerical process. The emulator propagates the uncertainties in the distributions of the calibrated input parameters inferred from the first step to the outputs. As a result, a quantification of the uncertainty of the maximum free surface elevation at specified locations is obtained.
机译:统计方法是理解和量化控制复杂海啸机制的不确定性的有用方法。数值实验通常可能具有很高的计算成本。这是进行不确定性和灵敏度分析的限制因素,需要进行大量仿真。作为这些仿真器的替代品,统计仿真器可以以更快,计算成本更低的方式提供物理过程的预测。它们可以构成一个杰出的解决方案,以探索成千上万种方案,否则这些方案在数字上会非常昂贵且难以实现。在这项工作中,我们分两个阶段构建了确定性代码的统计仿真器,该确定性代码用于模拟海底滑行和海啸的产生。首先,根据滑坡沉积物的观测值,校准滑坡模拟中使用的参数。该校准是在贝叶斯框架下使用高斯过程(GP)仿真器进行的,以近似滑坡模型以及模型与观测值之间的差异函数。作为校准的结果,获得了校准输入参数的分布。第二步,构建GP仿真器来模拟滑坡-海啸耦合数值过程。仿真器将从第一步推断的校准输入参数分布的不确定性传播到输出。结果,获得了在指定位置处最大自由表面高度的不确定性的量化。

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