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首页> 外文期刊>Proceedings of the Royal Society. Mathematical, physical and engineering sciences >Uncertainties in the 2004 Sumatra-Andaman source through nonlinear stochastic inversion of tsunami waves
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Uncertainties in the 2004 Sumatra-Andaman source through nonlinear stochastic inversion of tsunami waves

机译:2004年Sumatra-Andaman来源的不确定性通过海啸波的非线性随机反演

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摘要

Numerical inversions for earthquake source parameters from tsunami wave data usually incorporate subjective elements to stabilize the search. In addition, noisy and possibly insufficient data result in instability and non-uniqueness in most deterministic inversions, which are barely acknowledged. Here, we employ the satellite altimetry data for the 2004 Sumatra-Andaman tsunami event to invert the source parameters. We also include kinematic parameters that improve the description of tsunami generation and propagation, especially near the source. Using a finite fault model that represents the extent of rupture and the geometry of the trench, we perform a new type of nonlinear joint inversion of the slips, rupture velocities and rise times with minimal a priori constraints. Despite persistently good waveform fits, large uncertainties in the joint parameter distribution constitute a remarkable feature of the inversion. These uncertainties suggest that objective inversion strategies should incorporate more sophisticated physical models of seabed deformation in order to significantly improve the performance of early warning systems.
机译:来自海啸波数据的地震源参数的数值逆,通常包含主观元素来稳定搜索。此外,在大多数确定性反转中,嘈杂和可能不足的数据导致不稳定和非唯一性,这几乎没有被确认。在这里,我们使用2004苏门答腊andaman海啸事件的卫星高度数据数据来反转源参数。我们还包括用于改善海啸生成和传播的描述,尤其是靠近来源的运动参数。使用代表破裂程度和沟槽几何形状的有限故障模型,我们执行单个滑动,破裂速度和上升时间的新型非线性关节反转,并具有最高的先验约束。尽管波形持续良好,但联合参数分布的大不确定性构成了反转的显着特征。这些不确定性表明客观反转策略应纳入更复杂的海底变形的物理模型,以便显着提高预警系统的性能。

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