近场地震引起的沿海海啸与海底压力波动关系的数值研究

T. Baba, N. Takahashi, Y. Kaneda
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引用次数: 2

摘要

我们利用在南开海槽的海底压力计(DONET)观测阵列研究了沿海和近海海啸高度之间的相关性。但在静态底压变化中,很难准确地认识近场地震引起的海面波动。这是因为如果发生大的近场地震,海底会同时发生位移。为了避免这一问题,我们制作了海啸时海底压力波动绝对值的平均波形。许多海啸计算是通过改变板块界面上的滑动模型来进行的。我们检查了海底压力的平均绝对值与海岸海啸高度之间的相关性。这两个值之间可以看出明显的相关性。这一结果表明,利用阵列海底压力计数据可以更准确地实时预测海啸高度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A numerical study for relationship between coastal tsunami and bottom pressure fluctuation in the ocean generated from near-field earthquake
We investigated correlation between coastal and offshore tsunami height for our observational array of ocean-bottom pressure gauges, DONET, in the Nankai trough. But it is not easy to know correct sea surface fluctuation generated from near-field earthquakes in static bottom pressure changes. This is because the seafloor is simultaneously displaced in case of great near-field earthquakes occurred. In order to avoid the problem, we made the averaged waveforms of the absolute values of ocean-bottom pressure fluctuations during tsunami. Many tsunami calculations were executed by changing slip models on the plate interface. We checked the correlation between the average absolute of ocean bottom pressure and tsunami height at the coast. A clear correlation can be seen between the two values. This result indicates a possibility of more accurate real-time predicting of tsunami height by using arrayed ocean-bottom pressure gauge data.
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