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首页> 外文期刊>Journal of Volcanology and Geothermal Research >The classification of seismo-volcanic signals using Hidden Markov Models as applied to the Stromboli and Etna volcanoes
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The classification of seismo-volcanic signals using Hidden Markov Models as applied to the Stromboli and Etna volcanoes

机译:使用隐马尔可夫模型对斯特龙博利火山和埃特纳火山进行地震火山信号分类

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摘要

The aim of this work is to apply the Hidden Markov Model (HMM) method to recognise seismic signals belonging to different active volcanoes. We use data obtained from two field surveys carried out in 1997 and 1999 at Stromboli and Etna, respectively. For Stromboli we used two types of seismic signals for recognition purposes: Strombolian explosions and background seismic noise whilst for Etna we used volcanic tremors and tremor bursts. We initially proceeded to visually identify the signals, and to segment the data to obtain a model for each event class. We then applied these models separately to each volcano dataset, finally combining both datasets as a test of the portability of the system. The method analyses the seismograms and compares the characteristics of the data to a number of pre-defined event classes. If a signal is present, the method detects its occurrence and produces a classification. We observed that, to obtain reliable results, a careful and adequate segmentation process is crucial and that each signal type must be represented by its own specific model. Once we had built this model, the success level of the system was high. The success rates obtained indicated that the method was fully able to detect, isolate, and identify signals from raw seismic data. These results imply that, once an adequate training process has been used, this method is particularly appropriate for work in real time, as well as concurrently with the data acquisition system.
机译:这项工作的目的是应用隐马尔可夫模型(HMM)方法来识别属于不同活火山的地震信号。我们使用从1997年和1999年分别在Stromboli和Etna进行的两次现场调查获得的数据。对于Stromboli,我们使用两种类型的地震信号进行识别:Strombolian爆炸和背景地震噪声,而对于Etna,我们使用火山地震和震颤爆发。我们首先着手视觉识别信号,并对数据进行分段以获得每个事件类别的模型。然后,我们将这些模型分别应用于每个火山数据集,最后将这两个数据集组合起来作为对系统可移植性的测试。该方法分析地震图,并将数据特征与许多预定义的事件类别进行比较。如果存在信号,则该方法检测到它的出现并产生分类。我们观察到,为了获得可靠的结果,仔细而充分的分割过程至关重要,并且每种信号类型都必须由其自己的特定模型表示。一旦我们建立了这个模型,系统的成功水平就很高。获得的成功率表明该方法完全能够从原始地震数据中检测,隔离和识别信号。这些结果表明,一旦使用了足够的培训过程,该方法特别适用于实时工作以及与数据采集系统同时进行。

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  • 来源
    《Journal of Volcanology and Geothermal Research 》 |2009年第4期| 218-226| 共9页
  • 作者单位

    Instituto Andaluz de Geofisica. Campus de Cartuja s. Universidad de Granada. 18071 Granada, Spain Departamento de fisica Teorica y del Cosmos. Area de Fiska de la Tierra Universidad de Granada, Spain;

    Departamento de Teoria de la Senal Telematica y Comunicaciones, Escuela Tecnica Superior de Ingenieria Informatica. C/ Periodista Daniel Saucedo Aranda, Universidad de Granada, 18071 Granada, Spain;

    Departamento de Teoria de la Senal Telematica y Comunicaciones, Escuela Tecnica Superior de Ingenieria Informatica. C/ Periodista Daniel Saucedo Aranda, Universidad de Granada, 18071 Granada, Spain;

    Departamento de Teoria de la Senal Telematica y Comunicaciones, Escuela Tecnica Superior de Ingenieria Informatica. C/ Periodista Daniel Saucedo Aranda, Universidad de Granada, 18071 Granada, Spain;

    Instituto Andaluz de Geofisica. Campus de Cartuja s. Universidad de Granada. 18071 Granada, Spain Departamento de fisica Teorica y del Cosmos. Area de Fiska de la Tierra Universidad de Granada, Spain;

    Instituto Andaluz de Geofisica. Campus de Cartuja s. Universidad de Granada. 18071 Granada, Spain Departamento de fisica Teorica y del Cosmos. Area de Fiska de la Tierra Universidad de Granada, Spain;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    volcano-seismology; automatic classification; volcanic tremor; seismic monitoring;

    机译:火山地震学自动分类;火山震颤地震监测;

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