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A simple two-state model interprets temporal modulations in eruptive activity and enhances multivolcano hazard quantification.


ABSTRACT: Volcanic activity typically switches between high-activity states with many eruptions and low-activity states with few or no eruptions. We present a simple two-regime physics-informed statistical model that allows interpreting temporal modulations in eruptive activity. The model enhances comprehension and comparison of different volcanic systems and enables homogeneous integration into multivolcano hazard assessments that account for potential changes in volcanic regimes. The model satisfactorily fits the eruptive history of the three active volcanoes in the Neapolitan area, Italy (Mt. Vesuvius, Campi Flegrei, and Ischia) which encompass a wide range of volcanic behaviors. We find that these volcanoes have appreciably different processes for triggering and ending high-activity periods connected to different dominant volcanic processes controlling their eruptive activity, with different characteristic times and activity rates (expressed as number of eruptions per time interval). Presently, all three volcanoes are judged to be in a low-activity state, with decreasing probability of eruptions for Mt. Vesuvius, Ischia, and Campi Flegrei, respectively.

SUBMITTER: Selva J 

PROVIDER: S-EPMC9629722 | biostudies-literature | 2022 Nov

REPOSITORIES: biostudies-literature

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A simple two-state model interprets temporal modulations in eruptive activity and enhances multivolcano hazard quantification.

Selva Jacopo J   Sandri Laura L   Taroni Matteo M   Sulpizio Roberto R   Tierz Pablo P   Costa Antonio A  

Science advances 20221102 44


Volcanic activity typically switches between high-activity states with many eruptions and low-activity states with few or no eruptions. We present a simple two-regime physics-informed statistical model that allows interpreting temporal modulations in eruptive activity. The model enhances comprehension and comparison of different volcanic systems and enables homogeneous integration into multivolcano hazard assessments that account for potential changes in volcanic regimes. The model satisfactoril  ...[more]

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