Caracterización de señales sísmicas del Volcán Cotopaxi utilizando estimadores espectrales clásicos y de máxima entropía
Abstract
RESUMEN
Se presenta un estudio de detección y caracterización de eventos sísmicos del tipo volcano tectónicos y largo periodo de registros sísmicos generados por el volcán Cotopaxi. La estructura secuencial de detección propuesta permite en un registro sísmico maximizar la probabilidad de presencia de un evento y minimizar la ausencia de este. La detección se la realiza en el dominio del tiempo en cuasi tiempo real manteniendo una tasa constante de falsa alarma para posteriormente realizar un estudio del contenido espectral de los eventos mediante el uso de estimadores espectrales clásicos como el periodograma y paramétricos como el método de máxima entropía de Burg, logrando así, categorizar a los eventos detectados como volcano tectónicos, largo periodo y otros cuando no poseen características pertenecientes a los otros dos tipos como son los rayos.
Palabras clave: Detección de eventos sísmicos, test de hipótesis binaria, señales sismo-volcánicas.
ABSTRACT
A study of the detection and characterization of volcano-tectonic seismic type of events, using a long period of records of the Cotopaxi volcano, is presented. The sequential detection structure, proposed as part of this work, allows maximizing the likelihood of the presence of an event and minimizes the absence of this from a seismic record. The detection is performed in the near real time domain, maintaining a constant false alarm rate, enabling in a later stage a more detailed study of the spectral content of the events using classical spectral estimators such as the periodogram and the parametric maximum entropy method by Burg. The approach enabled to categorize phenomenon detected as volcano-tectonic from a long record of observations which even include activities of non-tectonic origin, such as the other two types of lightning.
Keywords: Event detection, binary hypothesis test, volcanic seismic signals.
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