Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/15767
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dc.date.accessioned2022-10-28T07:19:01Z-
dc.date.available2022-10-28T07:19:01Z-
dc.date.issued2022-09-29-
dc.identifier.urihttp://hdl.handle.net/2122/15767-
dc.description.abstractIn 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.en_US
dc.description.sponsorshipThis work was designed within the project IMPACT (A multidisciplinary Insight on the kinematics and dynamics of Magmatic Processes at Mt. Etna Aimed at identifying preCursor phenomena and developing early warning sysTems). IMPACT belongs to the Progetti Dipartimentali INGV [DIP7], https://progetti.ingv.it/index.php/it/progetti-dipartimentali/vulcani/impact#informazioni-sul-progetto.en_US
dc.language.isoEnglishen_US
dc.relation.ispartof5a Conferenza Rittmannen_US
dc.subjectVolcanic tremoren_US
dc.subjectvolcano unresten_US
dc.subjectEtnaen_US
dc.subjectvolcanic hazarden_US
dc.subjecteruptive activityen_US
dc.subjectforecastingen_US
dc.subjectpattern classificationen_US
dc.titleFixing Criteria for Volcanic Unrest Warningen_US
dc.typeConference paperen_US
dc.description.statusPublisheden_US
dc.identifier.URLhttp://editoria.rm.ingv.it/miscellanea/2022/miscellanea70/en_US
dc.subject.INGV04.08. Volcanologyen_US
dc.subject.INGV04.06. Seismologyen_US
dc.subject.INGV05.06. Methodsen_US
dc.subject.INGV05.08. Risken_US
dc.subject.INGV05.04. Instrumentation and techniques of general interesten_US
dc.identifier.doihttps://doi.org/10.13127/misc/70en_US
dc.description.ConferenceLocationCatania (Italy)en_US
dc.description.obiettivoSpecifico8T. Sismologia in tempo reale e Early Warning Sismico e da Tsunamien_US
dc.publisherMISCELLANEA INGVen_US
dc.contributor.authorLanger, Horst-
dc.contributor.authorFalsaperla, Susanna-
dc.contributor.authorSpampinato, Salvatore-
dc.contributor.authorMessina, Alfio-
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen_US
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen_US
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen_US
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italiaen_US
item.openairetypeConference paper-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia-
crisitem.author.orcid0000-0002-2508-8067-
crisitem.author.orcid0000-0002-1071-3958-
crisitem.author.orcid0000-0002-1954-1080-
crisitem.author.orcid0000-0002-3358-7210-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent05. General-
crisitem.classification.parent05. General-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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