Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/16921
Authors: Sandri, Laura* 
de' Michieli Vitturi, Mattia* 
Costa, Antonio* 
Di Vito, Mauro Antonio* 
Rucco, Ilaria* 
Doronzo, Domenico Maria* 
Bisson, Marina* 
Gianardi, Roberto* 
de Vita, Sandro* 
Sulpizio, Roberto* 
Title: Lahar events in the last 2000 years from Vesuvius eruptions – Part 3: Hazard assessment over the Campanian Plain
Journal: Solid Earth 
Series/Report no.: 4/15 (2024)
Publisher: Egu-Copernicus
Issue Date: 2024
DOI: 10.5194/se-15-459-2024
Keywords: Lahar
Somma-Vesuvius
Volcanic Hazards
Sub-Plinian eruptions
Subject Classification04.08. Volcanology 
Abstract: In this study we present a novel general methodology for probabilistic volcanic hazard assessment (PVHA) for lahars. We apply the methodology to perform a probabilistic assessment in the Campanian Plain (southern Italy), focusing on syn-eruptive lahars from a reference size eruption from Somma–Vesuvius. We take advantage of new field data relative to volcaniclastic flow deposits in the target region (Di Vito et al., 2024b) and recent improvements in modelling lahars (de' Michieli Vitturi et al., 2024). The former allowed defining proper probability density functions for the parameters related to the flow initial conditions, and the latter allowed computationally faster model runs. In this way, we are able to explore the effects of uncertainty in the initial flow conditions on the invasion of lahars in the target area by sampling coherent sets of values for the input model parameters and performing a large number of simulations. We also account for the uncertainty in the position of lahar generation by running the analysis on 11 different catchments threatening the Campanian Plain. The post-processing of the simulation outputs led to the production of hazard curves for the maximum flow thickness reached on a grid of points covering the Campanian Plain. By cutting the hazard curves at selected threshold values, we produce a portfolio of hazard maps and probability maps for the maximum flow thickness. We also produce hazard surface and probability maps for the simultaneous exceeding of pairs of thresholds in flow thickness and dynamic pressure. The latter hazard products represent, on one hand, a novel product in PVHA for lahars and, on the other hand, a useful means of impact assessment by assigning a probability to the occurrence of lahars that simultaneously have a relevant flow thickness and large dynamic pressure.
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