Tracking volcanic explosions using Shannon entropy at Volcán de Colima.


Journal

Scientific reports
ISSN: 2045-2322
Titre abrégé: Sci Rep
Pays: England
ID NLM: 101563288

Informations de publication

Date de publication:
17 Jun 2023
Historique:
received: 21 03 2023
accepted: 13 06 2023
medline: 18 6 2023
pubmed: 18 6 2023
entrez: 17 6 2023
Statut: epublish

Résumé

The main objective of this work is to show that Shannon Entropy (SE) calculated on continuous seismic signals can be used in a volcanic eruption monitoring system. We analysed three years of volcanic activity of Volcán de Colima, México, recorded between January 2015 and May 2017. This period includes two large explosions, with pyroclastic and lava flows, and intense activity of less energetic explosion, culminating with a period of quiescence. In order to confirm the success of our results, we used images of the Visual Monitoring system of Colima Volcano Observatory. Another of the objectives of this work is to show how the decrease in SE values can be used to track minor explosive activity, helping Machine Learning algorithms to work more efficiently in the complex problem of distinguishing the explosion signals in the seismograms. We show that the two big eruptions selected were forecasted successfully (6 and 2 days respectively) using the decay of SE. We conclude that SE could be used as a complementary tool in seismic volcano monitoring, showing its successful behaviour prior to energetic eruptions, giving time enough to alert the population and prepare for the consequences of an imminent and well predicted moment of the eruption.

Identifiants

pubmed: 37330531
doi: 10.1038/s41598-023-36964-x
pii: 10.1038/s41598-023-36964-x
pmc: PMC10276871
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

9807

Subventions

Organisme : Ministerio de Ciencia e Innovación
ID : PID2019-106260GB-I00

Informations de copyright

© 2023. The Author(s).

Références

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pubmed: 33286427
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pubmed: 32713974

Auteurs

Pablo Rey-Devesa (P)

Department of Theoretical Physics and Cosmos, Science Faculty, University of Granada, Avd. Fuentenueva s/n, 18071, Granada, Spain. pablord@ugr.es.
Andalusian Institute of Geophysics, Campus de Cartuja, University of Granada, C/Profesor Clavera 12, 18071, Granada, Spain. pablord@ugr.es.

Janire Prudencio (J)

Department of Theoretical Physics and Cosmos, Science Faculty, University of Granada, Avd. Fuentenueva s/n, 18071, Granada, Spain.
Andalusian Institute of Geophysics, Campus de Cartuja, University of Granada, C/Profesor Clavera 12, 18071, Granada, Spain.

Carmen Benítez (C)

Department of Signal Theory, Telematics and Communication, Informatics and Telecommunication School, University of Granada, 18071, Granada, Spain.

Mauricio Bretón (M)

Centro Universitario de Estudios Vulcanológicos (CUEV), Observatorio Vulcanológico, Universidad de Colima, Colima, Mexico.

Imelda Plasencia (I)

Centro Universitario de Estudios Vulcanológicos (CUEV), Observatorio Vulcanológico, Universidad de Colima, Colima, Mexico.

Zoraida León (Z)

Centro Universitario de Estudios Vulcanológicos (CUEV), Observatorio Vulcanológico, Universidad de Colima, Colima, Mexico.

Félix Ortigosa (F)

Centro Universitario de Estudios Vulcanológicos (CUEV), Observatorio Vulcanológico, Universidad de Colima, Colima, Mexico.

Ligdamis Gutiérrez (L)

Department of Theoretical Physics and Cosmos, Science Faculty, University of Granada, Avd. Fuentenueva s/n, 18071, Granada, Spain.
Andalusian Institute of Geophysics, Campus de Cartuja, University of Granada, C/Profesor Clavera 12, 18071, Granada, Spain.

Raúl Arámbula-Mendoza (R)

Centro Universitario de Estudios Vulcanológicos (CUEV), Observatorio Vulcanológico, Universidad de Colima, Colima, Mexico.

Jesús M Ibáñez (JM)

Department of Theoretical Physics and Cosmos, Science Faculty, University of Granada, Avd. Fuentenueva s/n, 18071, Granada, Spain.
Andalusian Institute of Geophysics, Campus de Cartuja, University of Granada, C/Profesor Clavera 12, 18071, Granada, Spain.

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