Clustering and classification of infrasonic events atMount Etna using pattern recognition techniques
Author(s)
Language
English
Obiettivo Specifico
1.4. TTC - Sorveglianza sismologica delle aree vulcaniche attive
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Issue/vol(year)
/185 (2011)
Publisher
wiley
Pages (printed)
253-264
Date Issued
2011
Abstract
Active volcanoes generate sonic and infrasonic signals, whose investigation provides useful information for both monitoring purposes and the study of the dynamics of explosive phenomena.
At Mt. Etna volcano (Italy), a pattern recognition system based on infrasonic waveform
features has been developed. First, by a parametric power spectrum method, the features
describing and characterizing the infrasound events were extracted: peak frequency and quality factor. Then, together with the peak-to-peak amplitude, these features constituted a 3-D ‘feature space’; by Density-Based Spatial Clustering of Applications with Noise algorithm
(DBSCAN) three clusters were recognized inside it. After the clustering process, by using a common location method (semblance method) and additional volcanological information
concerning the intensity of the explosive activity, we were able to associate each cluster to a
particular source vent and/or a kind of volcanic activity. Finally, for automatic event location,
clusters were used to train a model based on Support Vector Machine, calculating optimal
hyperplanes able to maximize the margins of separation among the clusters. After the training phase this system automatically allows recognizing the active vent with no location algorithm and by using only a single station.
At Mt. Etna volcano (Italy), a pattern recognition system based on infrasonic waveform
features has been developed. First, by a parametric power spectrum method, the features
describing and characterizing the infrasound events were extracted: peak frequency and quality factor. Then, together with the peak-to-peak amplitude, these features constituted a 3-D ‘feature space’; by Density-Based Spatial Clustering of Applications with Noise algorithm
(DBSCAN) three clusters were recognized inside it. After the clustering process, by using a common location method (semblance method) and additional volcanological information
concerning the intensity of the explosive activity, we were able to associate each cluster to a
particular source vent and/or a kind of volcanic activity. Finally, for automatic event location,
clusters were used to train a model based on Support Vector Machine, calculating optimal
hyperplanes able to maximize the margins of separation among the clusters. After the training phase this system automatically allows recognizing the active vent with no location algorithm and by using only a single station.
Type
article
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