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dc.contributor.authorallGouhier, M.-
dc.contributor.authorallHarris, A. J. L.-
dc.contributor.authorallCalvari, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia-
dc.contributor.authorallLabazuy, P.-
dc.contributor.authorallGuéhenneux, Y.-
dc.contributor.authorallDonnadieu, F.-
dc.contributor.authorallValade, S.-
dc.description.abstractIn the paper by Gouhier, M., Harris, A., Calvari, S., Labazuy, P., Guéhenneux, Y., Donnadieu, F., Valade, S, entitled “Lava discharge during Etna’s January 2011 fire fountain tracked using MSG-SEVIRI” (Bull Volcanol (2012) 74:787–793, DOI 10.1007/s00445-011-0572-y), we present data from a Doppler radar (VOLDORAD 2B). This ground-based Lband radar has been monitoring the eruptive activity of the summit craters of Mt. Etna in real-time since July 2009 from a site about 3.5 km SSE of the craters. Examples of applications of this type of radar are reviewed by Donnadieu (2012) and shown on the VOLDORAD website (http://wwwobs. Although designed and owned by the Observatoire de Physique du Globe in Clermont-Ferrand (OPGC), France, VOLDORAD 2B is operated jointly with the INGV-Catania (Italy) in the framework of a technical and scientific collaboration agreement between the INGV of Catania, the French CNRS and the OPGC-Université Blaise Pascal in Clermont- Ferrand. The system also utilizes a dedicated micropatch antenna designed at the University of Calabria (Boccia et al. 2010) and owned by INGV. The objective of the joint acquisition of the radar data by INGV-Catania and the OPGC is twofold: (1) to mitigate volcanic risks at Etna by better assessing the hazards arising from ash plumes and (2) to allow detailed study of volcanic activity and its environmental impact. In the paper by Gouhier et al. (2012), we failed to highlight this important collaboration between the INGV Catania and the OPGC; a cooperation essential for the past, current and future generation of such valuable data sets. Specifically we wish to acknowledge the roles of Mauro Coltelli, Michele Prestifilippo and Simona Scollo for their important input into this project, and pivotal role in setting up, and maintaining, this collaborative deployment.en_US
dc.publisher.nameSpringer Berlin Heidelbergen_US
dc.relation.ispartofBulletin of volcanologyen_US
dc.subjectEtna volcanoen_US
dc.subjectlava fountainen_US
dc.titleErratum to: Lava discharge during Etna’s January 2011 fire fountain tracked using MSG-SEVIRIen_US
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoringen_US
dc.relation.referencesBoccia L, Di Massa G, Venneri I (2010) L-Band array for groundbased remote sensing of volcanic eruptions. IET Microw Antennas Propag 4(12):2062–2068 Donnadieu F (2012) Volcanological applications of Doppler radars: A review and examples from a transportable pulse radar in L-band. In: Bech J, Chau JL (eds) Doppler Radar Observations - weather radar, wind profiler, Ionospheric radar, and other advanced applications. ISBN: 978-953-51-0496-4, InTech, pp 409–446en_US
dc.description.obiettivoSpecifico1.5. TTC - Sorveglianza dell'attività eruttiva dei vulcanien_US
dc.description.journalTypeJCR Journalen_US
dc.contributor.authorGouhier, M.-
dc.contributor.authorHarris, A. J. L.-
dc.contributor.authorCalvari, S.-
dc.contributor.authorLabazuy, P.-
dc.contributor.authorGuéhenneux, Y.-
dc.contributor.authorDonnadieu, F.-
dc.contributor.authorValade, S.-
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia-
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