Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/11599
Authors: Bevilacqua, A.* 
Isaia, Roberto* 
Neri, Augusto* 
Vitale, S.* 
Aspinall, W. P.* 
Bisson, Marina* 
Flandoli, F.* 
Baxter, P. J.* 
Bertagnini, Antonella* 
Esposti Ongaro, Tomaso* 
Iannuzzi, Enrico* 
Pistolesi, Marco* 
Rosi, Mauro* 
Title: Quantifying volcanic hazard at Campi Flegrei caldera (Italy) with uncertainty assessment: 1. Vent opening maps
Journal: Journal of Geophysical Research: Solid Earth 
Series/Report no.: /120 (2015)
Issue Date: 2015
DOI: 10.1002/2014JB011775
Keywords: vent opening probability maps
expert judgment
Campi Flegrei caldera
Abstract: Campi Flegrei is an active volcanic area situated in the Campanian Plain (Italy) and dominated by a resurgent caldera. The great majority of past eruptions have been explosive, variable in magnitude, intensity, and in their vent locations. In this hazard assessment study we present a probabilistic analysis using a variety of volcanological data sets to map the background spatial probability of vent opening conditional on the occurrence of an event in the foreseeable future. The analysis focuses on the reconstruction of the location of past eruptive vents in the last 15 ka, including the distribution of faults and surface fractures as being representative of areas of crustal weakness. One of our key objectives was to incorporate some of the main sources of epistemic uncertainty about the volcanic system through a structured expert elicitation, thereby quantifying uncertainties for certain important model parameters and allowing outcomes from different expert weighting models to be evaluated. Results indicate that past vent locations are the most informative factors governing the probabilities of vent opening, followed by the locations of faults and then fractures. Our vent opening probability maps highlight the presence of a sizeable region in the central eastern part of the caldera where the likelihood of new vent opening per kilometer squared is about 6 times higher than the baseline value for the whole caldera. While these probability values have substantial uncertainties associated with them, our findings provide a rational basis for hazard mapping of the next eruption at Campi Flegrei caldera.
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