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Numerical Procedure to Forecast the Tsunami Parameters from a Database of Pre-Simulated Seismic Unit Sources

机译:从模拟地震单元源数据库预测海啸参数的数值过程

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We have implemented a numerical procedure to forecast the parameters of a tsunami, such as the arrival time of the front of the first wave and the maximum wave height in real and virtual tidal stations along the Peruvian coast, with this purpose a database of pre-computed synthetic tsunami waveforms (or Green functions) was obtained from numerical simulation of seismic unit sources (dimension: 50?×?50?km_(2)) for subduction zones from southern Chile to northern Mexico. A bathymetry resolution of 30?arc-sec (approximately 927?m) was used. The resulting tsunami waveform is obtained from the superposition of synthetic waveforms corresponding to several seismic unit sources contained within the tsunami source geometry. The numerical procedure was applied to the Chilean tsunami of April 1, 2014. The results show a very good correlation for stations with wave amplitude greater than 1?m, in the case of the Arica tide station an error (from the maximum height of the observed and simulated waveform) of 3.5% was obtained, for Callao station the error was 12% and the largest error was in Chimbote with 53.5%, however, due to the low amplitude of the Chimbote wave (<1?m), the overestimated error, in this case, is not important for evacuation purposes. The aim of the present research is tsunami early warning, where speed is required rather than accuracy, so the results should be taken as preliminary.
机译:我们已经实施了一个数字过程,以预测海啸的参数,例如第一波前面的到达时间和秘鲁海岸的真实和虚拟潮汐台中的最大波浪高度,其中一个目的是预先的数据库从地震单元来源的数值模拟获得了计算的合成Tsunami波形(或绿色函数)(尺寸:50?×50?×50?KM_(2)),用于北部南部到墨西哥北部的俯冲区。使用30?ARC-SEC(约927μm)的沐浴分辨率。从对应于海啸源几何形状中包含的若干地震单元源的合成波形的叠加获得得到的TSunami波形。该数值程序应用于2014年4月1日的智利海啸。结果对于具有大于1Ω·m的电台的结果,在arica潮汐站的情况下(从最大高度)所观察到的和模拟波形是获得的3.5%,对于CalloO站,误差为12%,最大的误差是脊柱鲸,然而,由于Chimbote Wave(<1μl)的低幅度,高估错误,在这种情况下,对疏散目的并不重要。目前研究的目的是海啸预警,其中速度是必需而不是准确性,因此结果应作为初步初步。

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