Hazard assessment of explosive volcanism at Somma‐Vesuvius
Language
English
Obiettivo Specifico
4.3. TTC - Scenari di pericolosità vulcanica
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Journal of Geophysical Research
Issue/vol(year)
/115(2010)
Publisher
The American Geophysical Union
Pages (printed)
B12212
Date Issued
2010
Abstract
A probabilistic approach based on the available volcanological data on past
Somma‐Vesuvius eruptions has been developed to produce hazard‐zone maps for fallout,
pyroclastic density currents (PDCs), and secondary mass flows by using numerical
simulations. The hazard maps have been incorporated in a GIS, making them accessible to
casual and expert users for risk mitigation and education management. The results allowed
us to explore the hazard related to different scenarios from all possible eruptions,
ranked according to volcanic explosivity index (VEI) class, in the Vesuvius area and its
surroundings including Naples. Particularly, eruptions with VEI ≤ 3 would produce a
fallout hazard within about 10 km mostly east of the volcano and a PDC hazard within
about 2 km from the crater. Large‐scale events (4 ≤ VEI ≤ 5) would produce a fallout
hazard up to 80 km from the vent and a PDC hazard at distances exceeding 15 km.
Particularly, the territory northwest of Vesuvius, including metropolitan Naples, featuring
a low hazard level for fallout accumulation, is exposed to PDCs also consistent with field
evidence and archeological findings. Both volcano flanks and surrounding plains, hills,
and mountains are exposed to a moderate–high level of hazard for the passage of
secondary mass flows. With the present level of uncertainty in forecasting future eruption
type and size on the basis of statistical analysis as well as precursory activity, our results
indicate that the reference scenario in the emergency plan should carefully match the
worst‐case VEI 5 probabilistic scenario.
Somma‐Vesuvius eruptions has been developed to produce hazard‐zone maps for fallout,
pyroclastic density currents (PDCs), and secondary mass flows by using numerical
simulations. The hazard maps have been incorporated in a GIS, making them accessible to
casual and expert users for risk mitigation and education management. The results allowed
us to explore the hazard related to different scenarios from all possible eruptions,
ranked according to volcanic explosivity index (VEI) class, in the Vesuvius area and its
surroundings including Naples. Particularly, eruptions with VEI ≤ 3 would produce a
fallout hazard within about 10 km mostly east of the volcano and a PDC hazard within
about 2 km from the crater. Large‐scale events (4 ≤ VEI ≤ 5) would produce a fallout
hazard up to 80 km from the vent and a PDC hazard at distances exceeding 15 km.
Particularly, the territory northwest of Vesuvius, including metropolitan Naples, featuring
a low hazard level for fallout accumulation, is exposed to PDCs also consistent with field
evidence and archeological findings. Both volcano flanks and surrounding plains, hills,
and mountains are exposed to a moderate–high level of hazard for the passage of
secondary mass flows. With the present level of uncertainty in forecasting future eruption
type and size on the basis of statistical analysis as well as precursory activity, our results
indicate that the reference scenario in the emergency plan should carefully match the
worst‐case VEI 5 probabilistic scenario.
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method for the calculation of the impact parameters of dilute pyroclastic
density currents based on deposit particle characteristics, J. Geophys.
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C. Cavazzoni, G. Erbacci, and P. J. Baxter (2008), Transient 3D simulation
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Geology, failure conditions, and implications of seismogenie avalanches
of the 1944 eruption at Vesuvius, Italy, J. Volcanol. Geotherm. Res., 47,
249–264.
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Power Stations, HMSO, London.
Kelfoun, K., P. Samaniego, P. Palacios, and D. Barba (2009), Testing the
suitability of frictional behaviour for pyroclastic flow simulation by
comparison with a well‐constrained eruption at tungurahua volcano
(Ecuador), Bull. Volcanol., 71, 1057–1075, doi:10.1007/s00445-009-
0286-6.
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Geol., 81, 11–16.
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