Abstract

Assessment of volcanic hazards is necessary for risk mitigation. Typically, hazard assessment is based on one or a few, subjectively chosen representative eruptive scenarios, which use a specific combination of eruptive sizes and intensities to represent a particular size class of eruption. While such eruptive scenarios use a range of representative members to capture a range of eruptive sizes and intensities in order to reflect a wider size class, a scenario approach neglects to account for the intrinsic variability of volcanic eruptions, and implicitly assumes that inter-class size variability (i.e. size difference between different eruptive size classes) dominates over intra-class size variability (i.e. size difference within an eruptive size class), the latter of which is treated as negligible. So far, no quantitative study has been undertaken to verify such an assumption. Here, we adopt a novel Probabilistic Volcanic Hazard Analysis (PVHA) strategy, which accounts for intrinsic eruptive variabilities, to quantify the tephra fallout hazard in the Campania area. We compare the results of the new probabilistic approach with the classical scenario approach. The results allow for determining whether a simplified scenario approach can be considered valid, and for quantifying the bias which arises when full variability is not accounted for.

Highlights

  • Recent literature on tephra fallout hazard assessment[5,13,14,15,16] accounts for eruptive size and intensity variability by assuming a few “representative eruptive scenarios”, where one scenario is used to represent a sub-range of eruptive sizes, intensities, and vent position

  • While the spatial uncertainty of the vent position was taken into account by considering several (700) potential vent positions across the caldera, the four eruptive sizes were chosen based on volcanological parameters which characterised four specific past events of the Campi Flegrei, which we call representative members

  • We split the eruptive size range into a few classes that can be linked to representative members similar to the classical approach used in past studies

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Summary

Introduction

Recent literature on tephra fallout hazard assessment[5,13,14,15,16] accounts for eruptive size and intensity variability by assuming a few “representative eruptive scenarios”, where one scenario is used to represent a sub-range of eruptive sizes, intensities, and vent position. While the spatial uncertainty of the vent position was taken into account by considering several (700) potential vent positions across the caldera, the four eruptive sizes were chosen based on volcanological parameters which characterised four specific past events of the Campi Flegrei, which we call representative members. These representative members were assumed to be representative for the whole spectrum of possible eruptive magnitudes and intensities of potential future events at this volcano. These classes ideally span the general range continuosly, whereas representative members, by definition, discretize it;

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