Effusive crises at Piton de la Fournaise 2014–2015: a review of a multi-national response model
Artikel i vetenskaplig tidskrift, 2017
Many active European volcanoes and volcano observatories are island-based and located far from their administrative “mainland”. Consequently, Governments have developed multisite approaches, in which monitoring is performed by a network of individuals distributed across several national research centers. At a transnational level, multinational networks are also progressively emerging. Piton de la Fournaise (La Réunion Island, France) is one such example. Piton de la Fournaise is one of the most active volcanoes of the World, and is located at the greatest distance from its “mainland” than any other vulnerable “overseas” site, the observatory being 9365 km from its governing body in Paris. Effusive risk is high, so that a well-coordinated and rapid response involving near-real time delivery of trusted, validated and operational product for hazard assessment is critical. Here we review how near-real time assessments of lava flow propagation were developed using rapid provision, and update, of key source terms through a dynamic and open integration of near-real time remote sensing, modeling and measurement capabilities on both the national and international level. The multi-national system evolved during the five effusive crises of 2014–2015, and is now mature for Piton de la Fournaise. This review allows us to identify strong and weak points in an extended observatory system, and demonstrates that enhanced multi-national integration can have fundamental implications in scientific hazard assessment and response during an on-going effusive crisis.
Volcano observatory
Lava flow model
Time averaged discharge rates
Effusive crisis
Hazard response
Inundation forecasts
Piton de la Fournaise
Författare
A. J L Harris
Observatoire de Physique du Globe Clermont Ferrand (OPGC)
Universite d' Auvergne Clermont-FD 1
N. Villeneuve
Institut de Physique du Globe de Paris
A. Di Muro
Institut de Physique du Globe de Paris
V. Ferrazzini
Institut de Physique du Globe de Paris
A. Peltier
Institut de Physique du Globe de Paris
D. Coppola
Universita degli Studi di Torino
M. Favalli
Istituto Nazionale Di Geofisica E Vulcanologia, Rome
P. Bachèlery
Observatoire de Physique du Globe Clermont Ferrand (OPGC)
Universite d' Auvergne Clermont-FD 1
J. L. Froger
Universite d' Auvergne Clermont-FD 1
Observatoire de Physique du Globe Clermont Ferrand (OPGC)
L. Gurioli
Observatoire de Physique du Globe Clermont Ferrand (OPGC)
Universite d' Auvergne Clermont-FD 1
S. Moune
Observatoire de Physique du Globe Clermont Ferrand (OPGC)
Universite d' Auvergne Clermont-FD 1
I. Vlastélic
Universite d' Auvergne Clermont-FD 1
Observatoire de Physique du Globe Clermont Ferrand (OPGC)
Bo Galle
Chalmers, Rymd- och geovetenskap, Optisk fjärranalys
Santiago Arellano
Chalmers, Rymd- och geovetenskap, Optisk fjärranalys
Journal of Applied Volcanology
2191-5040 (eISSN)
Vol. 6 1 11Ämneskategorier (SSIF 2011)
Fysik
DOI
10.1186/s13617-017-0062-9