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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Preparing for the Future Nankai Trough Tsunami: A Data Assimilation and Inversion Analysis From Various Observational Systems
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Preparing for the Future Nankai Trough Tsunami: A Data Assimilation and Inversion Analysis From Various Observational Systems

机译:为未来的南开槽海啸做准备:各种观察系统的数据同化和反演分析

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The future Nankai Trough tsunami is one of the imminent threats to the Japanese coastal communities that could potentially cause a catastrophic event. As a part of the countermeasure efforts for such an occurrence, this study analyzes the efficacy of combining tsunami data assimilation (DA) and waveform inversion (WI). The DA is used to continuously refine a wavefield model whereas the WI is used to estimate the tsunami source. We consider a future scenario of the Nankai Trough tsunami recorded at various observational systems, including ocean bottom pressure (OBP) gauges, global positioning system (GPS) buoys, and ship height positioning data. Since most of the OBP gauges are located inside the source region, the recorded tsunami signals exhibit significant offsets from surface measurements due to coseismic seafloor deformation effects. Such biased data are not applicable to the standard DA, but can be taken into account in the WI. On the other hand, the use of WI for the ship data may not be practical because a considerably large precomputed tsunami database is needed to cope with the spontaneous ship locations. The DA is more suitable for such an observational system as it can be executed sequentially in time and does not require precomputed scenarios. Therefore, the combined approach of DA and WI allows us to concurrently make use of all observational resources. Additionally, we introduce a bias correction scheme for the OBP data to improve the accuracy, and an adaptive thinning of observations to determine the efficient number of observations.
机译:未来南海海槽的海啸是日本沿海社区的迫在眉睫的威胁,可能导致潜在的灾难性事件中的一个。作为用于这种情况的发生的对策的努力的一部分,本研究分析结合数据海啸同化(DA)和波形反演(WI)的功效。该DA被用于不断地改善一个波场模型而WI被用于估计海啸源。我们认为南海海槽的海啸记录在不同的观测系统,包括海底压力(OBP)计,全球定位系统(GPS)浮标,船舶高度定位数据的未来场景。由于大多数OBP规的位于源极区域内,所记录的海啸信号表现出从表面测量显著偏移由于同震海底变形效果。这种偏置数据是不适用的标准DA,但可考虑在WI。在另一方面,因为需要相当大的预先计算的海啸数据库应付自发船舶位置为船舶数据使用WI的可能是不实际。该DA是更适合这样一个观察系统,因为它可以在时间上依次地执行,并且不需要预先计算场景。因此,DA和无线的组合方法使我们能够同时利用所有的观测资源。此外,我们介绍用于OBP数据,以提高精确度的偏差校正方案,和观察的自适应变薄,以确定观察的有效数量。

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