Report on Piton de la Fournaise (France)

2021 ◽  
Vol 46 (7) ◽  
Author(s):  
Keyword(s):  
Piton De La Fournaise

Hydrologic and thermal modeling of an active volcano: the Piton de la Fournaise, Reunion

1997 ◽  
Vol 191 (1-4) ◽  
pp. 37-63 ◽  
Author(s):  
Sophie Violette ◽  
Emmanuel Ledoux ◽  
Patrick Goblet ◽  
Jean-Pierre Carbonnel
Keyword(s):  
Thermal Modeling ◽  
Active Volcano ◽  
Piton De La Fournaise

scholarly journals Locating rockfalls using inter-station ratios of seismic energy at Dolomieu crater, Piton de la Fournaise volcano

2020 ◽  
Author(s):  
Julian Kuehnert ◽  
Anne Mangeney ◽  
Yann Capdeville ◽  
Jean-Pierre Vilotte ◽  
Eleonore Stutzmann ◽  
...  
Keyword(s):  
Seismic Energy ◽  
Piton De La Fournaise

March 1986 eruptive episodes at Piton de la Fournaise volcano (Reunion Island)

1989 ◽  
Vol 36 (1-3) ◽  
pp. 199-208 ◽  
Author(s):  
H. Delorme ◽  
P. Bachèlery ◽  
P.A. Blum ◽  
J.L. Cheminée ◽  
J.F. Delarue ◽  
...  
Keyword(s):  
Reunion Island ◽  
Piton De La Fournaise ◽  
Réunion Island

scholarly journals Large scale modeling of the transport, chemical transformation and mass budget of the sulfur emitted during the April 2007 eruption of Piton de la Fournaise

2011 ◽  
Vol 11 (9) ◽  
pp. 4533-4546 ◽  
Author(s):  
P. Tulet ◽  
N. Villeneuve
Keyword(s):  
Dry Deposition ◽  
Large Scale ◽  
Temporal Evolution ◽  
Active Period ◽  
General Shape ◽  
So2 Emission ◽  
Piton De La Fournaise ◽  
Scale Modeling ◽  
The Indian Ocean ◽  
Large Scale Modeling

Abstract. In April 2007, the Piton de la Fournaise volcano (Réunion island) entered into its biggest eruption recorded in the last century. Due to the absence of a sensors network in the vicinity of the volcano, an estimation of degassing during the paroxysmal phase of the event has not been performed. Nevertheless, the SO2 plume and aerosols have been observed by the OMI and CALIOP space sensors, respectively. The mesoscale chemical model MesoNH-C simulates the observed bulk mass of SO2 and the general shape of the SO2 plume spreading over the Indian Ocean. Moreover, an analysis of the SO2 plume budget estimates a total SO2 release of 230 kt, among of which 60 kt have been transformed into H2SO4. 27 kt of SO2 and 21 kt of H2SO4 have been deposited at the surface by dry deposition. With this top down approach, the temporal evolution of the SO2 emission has been estimated during the most active period of the eruption. The peak of degassing was estimated at 1800 kg s−1 in the morning of 6~April. The temporal evolution of SO2 emission presented here can also be used for local studies.

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