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Uncertainties in the 2004 Sumatra–Andaman source through nonlinear stochastic inversion of tsunami waves

机译:海啸波的非线性随机反演中2004年苏门答腊-安达曼水源的不确定性

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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震源参数的数值反演通常包含主观因素以稳定搜索。此外,嘈杂的数据(可能还不足)会导致大多数确定性反演中的不稳定和不唯一性,这几乎没有得到承认。在这里,我们使用2004年苏门答腊-安达曼海啸事件的卫星测高数据来反演源参数。我们还包括运动学参数,可以改善对海啸发生和传播(特别是在震源附近)的描述。使用代表断裂程度和沟槽几何形状的有限断层模型,我们以最小的先验约束执行了新型的滑移,断裂速度和上升时间非线性联合反演。尽管始终具有良好的波形拟合,但联合参数分布中的较大不确定性构成了反演的显着特征。这些不确定性表明,客观的反演策略应纳入更复杂的海床变形物理模型,以便显着提高预警系统的性能。

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