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Quasi‐hidden Markov model and its applications in cluster analysis of earthquake catalogs

机译:拟隐马尔可夫模型及其在地震目录聚类分析中的应用

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We identify a broad class of models, quasi‐hidden Markov models (QHMMs), which include hidden Markov models (HMMs) as special cases. Applying the QHMM framework, this paper studies how an earthquake cluster propagates statistically. Two QHMMs are used to describe two different propagating patterns. The “mother‐and‐kids” model regards the first shock in an earthquake cluster as “mother” and the aftershocks as “kids,” which occur in a neighborhood centered by the mother. In the “domino” model, however, the next aftershock strikes in a neighborhood centered by the most recent previous earthquake in the cluster, and therefore aftershocks act like dominoes. As the likelihood of QHMMs can be efficiently computed via the forward algorithm, likelihoodbased model selection criteria can be calculated to compare these two models. We demonstrate this procedure using data from the central New Zealand region. For this data set, the mother‐and‐kids model yields a higher likelihood as well as smaller AIC and BIC. In other words, in the aforementioned area the next aftershock is more likely to occur near the first shock than near the latest aftershock in the cluster. This provides an answer, though not entirely satisfactorily, to the question “where will the next aftershock be?”. The asymptotic consistency of the model selection procedure in the paper is duly established, namely that, when the number of the observations goes to infinity, with probability one the procedure picks out the model with the smaller deviation from the true model (in terms of relative entropy rate).
机译:我们确定了一大类模型,即准隐马尔可夫模型(QHMM),其中包括隐马尔可夫模型(HMM)作为特例。运用QHMM框架,研究地震群如何在统计上传播。两个QHMM用于描述两个不同的传播模式。 “母子”模型将地震群中的第一次地震视为“母子”,并将余震视为“子母”,它们发生在以母亲为中心的邻域中。但是,在“多米诺”模式中,下一次余震在附近发生的最近一次地震中发生,该震群以该集群中最近的地震为中心,因此余震的作用就像多米诺骨牌。由于可以通过正向算法有效地计算QHMM的似然性,因此可以计算基于似然性的模型选择标准以比较这两个模型。我们使用来自新西兰中部地区的数据来演示此过程。对于此数据集,母子模型产生的可能性更高,而AIC和BIC则更小。换句话说,在上述区域中,下一次余震比簇中最新的余震更可能发生在第一次冲击附近。这为“下一次余震将在哪里?”这个问题提供了一个答案,尽管并不完全令人满意。适当地建立了模型选择过程的渐近一致性,即当观测数达到无穷大时,该过程选择概率为1的模型选择与真实模型偏差较小的模型(相对熵率)。

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