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

IF 3
D Gopinathan, M Venugopal, D Roy, K Rajendran, S Guillas, F Dias
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引用次数: 12

Abstract

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.

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2004年苏门答腊-安达曼震源海啸波非线性随机反演的不确定性。
利用海啸波资料进行震源参数的数值反演通常包含主观因素,以稳定搜索结果。此外,在大多数确定性反演中,噪声和可能不足的数据导致不稳定性和非唯一性,这一点很少得到承认。本文利用2004年苏门答腊-安达曼海啸事件的卫星测高数据对震源参数进行反演。我们还包括运动参数,以改进对海啸产生和传播的描述,特别是在震源附近。利用有限断层模型表示破裂程度和沟槽的几何形状,我们在最小的先验约束下对滑动、破裂速度和上升时间进行了一种新型的非线性联合反演。尽管波形拟合一直很好,但联合参数分布的不确定性很大,这是反演的一个显著特征。这些不确定性表明,客观反演策略应纳入更复杂的海底变形物理模型,以显著提高预警系统的性能。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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