首页> 外文期刊>The Annals of applied statistics >SPATIALLY INHOMOGENEOUS BACKGROUND RATE ESTIMATORS AND UNCERTAINTY QUANTIFICATION FOR NONPARAMETRIC HAWKES POINT PROCESS MODELS OF EARTHQUAKE OCCURRENCES
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SPATIALLY INHOMOGENEOUS BACKGROUND RATE ESTIMATORS AND UNCERTAINTY QUANTIFICATION FOR NONPARAMETRIC HAWKES POINT PROCESS MODELS OF EARTHQUAKE OCCURRENCES

机译:地震发生的非参数霍克斯点过程模型的空间非均匀背景速率估计和不确定性量化

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Space-time Hawkes point process models for the conditional rate of earthquake occurrences traditionally make many parametric assumptions about the form of the triggering function for the rate of aftershocks following an earthquake. As an alternative, Marsan and Lengline [Science 319 (2008) 1076-1079] developed a completely nonparametric method that provides an estimate of a homogeneous background rate for mainshocks, and a histogram estimate of the triggering function. At each step of the procedure the model estimates rely on computing the probability each earthquake is a mainshock or aftershock of a previous event. The focus of this paper is the improvement and assessment ofMarsan and Lengline's method in the following ways: (a) the proposal of novel ways to incorporate a spatially inhomogeneous background rate; (b) adding error bars to the histogram estimates which quantify the sampling variability in the estimation of the underlying seismic process. A simulation study is designed to evaluate and validate the ability of our methods to recover the triggering function and spatially varying background rate. An application to earthquake data from the Tohoku District in Japan is discussed at the end, and the results are compared to a well-established parametric model of seismicity for this region.
机译:传统上,针对条件地震发生率的时空霍克斯点过程模型对地震后余震发生率的触发函数的形式做出了许多参数假设。作为替代方案,Marsan和Lengline [Science 319(2008)1076-1079]开发了一种完全非参数的方法,该方法可提供主震同质背景速率的估计值和触发函数的直方图估计值。在该过程的每个步骤中,模型估计都依赖于计算每次地震是前次地​​震的主震或余震的概率。本文的重点是通过以下几种方式对Marsan和Lengline的方法进行改进和评估:(a)提出一种新的方法来纳入空间上不均匀的背景速率; (b)在直方图估计中添加误差线,以量化潜在地震过程的估计中的采样变异性。仿真研究旨在评估和验证我们的方法恢复触发功能和空间变化背景速率的能力。最后讨论了如何应用日本东北地区的地震数据,并将结果与​​该地区公认的地震参数化模型进行了比较。

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