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Comparing source inversion techniques for GPS-based local tsunami forecasting: A case study for the April 2014 M8.1 Iquique, Chile, earthquake

机译:比较基于GPS的当地海啸预报的源反演技术:以2014年4月智利伊基克M8.1级地震为例

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摘要

Real-time GPS is nowadays considered as a valuable component of next generation near-field tsunami early warning systems able to provide fast and reliable source parameters. Looking for optimal methodologies and assessing corresponding uncertainties becomes an important task. We take the opportunity and consider the 2014 Pisagua event as a case study to explore tsunami forecast uncertainty related to the GPS-based source inversion. We intentionally neglect all other sources of uncertainty (observation set, signal processing, wave simulation, etc.) and exclusively assess the effect of inversion technique. In particular, we compare three end-member methods: (1) point-source fastCMT (centroid moment tensor), (2) distributed slip along predefined plate interface, and (3) unconstrained inversion into a single uniform slip finite fault. The three methods provide significantly different far-field tsunami forecast but show surprisingly similar tsunami predictions in the near field.
机译:如今,实时GPS被视为下一代近场海啸预警系统的重要组成部分,能够提供快速,可靠的源参数。寻找最佳方法并评估相应的不确定性成为一项重要任务。我们借此机会,将2014年的比萨山事件作为案例研究,以探索与基于GPS的源反演有关的海啸预报不确定性。我们有意忽略了所有其他不确定性来源(观测集,信号处理,波模拟等),并专门评估了反演技术的效果。特别是,我们比较了三种末端构件方法:(1)点源fastCMT(质心矩张量),(2)沿预定义板界面分布的滑移,以及(3)无约束反演成单个均匀滑移有限断层。三种方法提供的远场海啸预报有很大不同,但在近场中却显示出惊人的相似海啸预报。

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