Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/15767
Authors: Langer, Horst* 
Falsaperla, Susanna* 
Spampinato, Salvatore* 
Messina, Alfio* 
Title: Fixing Criteria for Volcanic Unrest Warning
Issue Date: 29-Sep-2022
Publisher: MISCELLANEA INGV
URL: http://editoria.rm.ingv.it/miscellanea/2022/miscellanea70/
DOI: https://doi.org/10.13127/misc/70
Keywords: Volcanic tremor
volcano unrest
Etna
volcanic hazard
eruptive activity
forecasting
pattern classification
Subject Classification04.08. Volcanology 
04.06. Seismology 
05.06. Methods 
05.08. Risk 
05.04. Instrumentation and techniques of general interest 
Abstract: In volcanic observatories worldwide, geophysical and geochemical data are usually collected remotely, providing continuous information about the state of volcanoes even in unfavorable conditions with respect to visibility and access to the area of eruptive centers. Early stages of unrest can be detected with high reliability; nonetheless, style and, in particular, intensity of eruptions are diffcult to predict. Consequently, it turns out important to identify critical moments after which the development of a paroxysmal activity becomes highly probable. In this perspective, we exploit a machine learning (ML) method for the analysis of seismic data continuously acquired by the permanent seismic network at Etna, Italy. Threshold criteria, which are based on parameters derived from the ML system and the number of stations where changes are detected, have been established with the scope of automatic alert flagging. As mild unrests may continue for weeks and even months, there is the need to adjust the trigger criteria with respect to style and intensity of the impending phenomenon. Our choice of the criteria was guided by so-called “Receive Operation Characteristics” (ROC) curves. These are based on the trade-off between the rate of False Positives and True Positives. With a more sensitive setting one can flag more paroxysms (True Positives); however, this may have the cost to flag an alert, but no paroxysm occurs. Carrying out various tests considering both the signal characteristics and the number of stations where the thresholds were met, we identified robust configurations allowing us to issue an alert of an impending paroxysm, widely avoiding the risk of false warnings. The system we propose here can provide timely and indicative information on possible eruptive scenarios to Civil Protection and other stakeholders. Also, It can be a guide for fixing onset and end-times of paroxysmal phenomena, which are especially helpful when image-based monitoring is hindered, for instance, by meteorological conditions. Finally, if others the possibility to effectively re-analyze long time spans of data recorded in the past.
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