牛顿法确定意大利震中地震危险性的解路径2016年8月24日

P. H. Gunawan, N. B. Prakoso
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引用次数: 2

摘要

本文研究了牛顿法近似地震震中的性质。这里考虑的是2016年8月24日意大利中部的地震。仅采用Pg波地震资料作为准备资料。本文阐述了地震Pg波最小速度、平均速度和最大速度对数值模拟的影响。结果表明,每种情况下的地震轨迹都有不同的方向,初步估计震中为意大利罗马的一个坐标。例如,通过使用最大速度的行为,可以观察到溶液在开始时向其他国家移动,然后立即移动到震中的诺尔西亚。最小、平均和最大速度牛顿法的最终迭代次数分别为12次、10次和13次,公差数为0.01。最小速度、平均速度和最大速度的最终数值误差分别为0.159848、0.099954和0.45736。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Solution path of Newton's method for determining epicenter earthquake hazard in Italy 24 august 2016
This paper is devoted to investigate the behavior of Newton's method for approximating the epicenter of earthquake. Here, the earthquake in center of Italy 24 August 2016 is considered. The seismic data of Pg waves only is used as preparation data. Here, three scenarios which are depend on the minimum, average and maximum velocity of seismic Pg waves for the numerical simulations are elaborated. The results show the trajectories have different directions for each scenarios with initial guess of epicenter is given to be a coordinate of Rome, Italy. For instance, the behavior by using maximum velocity, the solution is observed moves away toward other countries at beginning before it immediately moves back to the epicenter in Norcia. The numbers of final iteration of Newton's method using minimum, average and maximum velocity are obtained 12, 10, and 13 respectively by tolerance number 0.01. Moreover, the final numerical errors for minimum, average and maximum velocity are 0.159848, 0.099954 and 0.45736 respectively.
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