1. Earth-prints
  2. Affiliation
  3. INGV
  4. Article published / in press
Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6766
DC FieldValueLanguage
dc.contributor.authorallBonasia, R.; Corresponding author. Istituto Nazionale di Geofisica e Vulcanologia, Sezione Osservatorio Vesuviano”, Via Diocleziano, 328, Napoli, Italy.en
dc.contributor.authorallMacedonio, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallCosta, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallMele, D.; CIRISIVU, Dipartimento Geomineralogico, Università degli Studi di Bari, Bari, Italyen
dc.contributor.authorallSulpizio, R.; CIRISIVU, Dipartimento Geomineralogico, Università degli Studi di Bari, Bari, Italyen
dc.date.accessioned2011-01-19T11:07:32Zen
dc.date.available2011-01-19T11:07:32Zen
dc.date.issued2010en
dc.identifier.urihttp://hdl.handle.net/2122/6766en
dc.description.abstractA simple semi-analytical model for ash-fall deposit was applied to reconstruct the tephra deposits of the sub- Plinian 472 AD eruption of Vesuvius, Italy, which is of the scale of the reference eruptive scenario for the emergency planning, at Vesuvius. Applying a novel least-squares method, the bulk grain-size distribution, the total mass, and the eruption column height were obtained by fitting the computed ground load and granulometries with the observed ones. The analysis of the effect of three different weighting factors in the minimization procedure was also performed. Results showed that the statistical weighting factor produced the minimum bias. The best correlation between calculated and measured deposit was found, even though the quantity of the input data was not very high, as it commonly occurs for several ancient eruptions. Model results were also in agreement with estimations provided by other independent methods.en
dc.language.isoEnglishen
dc.publisher.nameelsevieren
dc.relation.ispartofJournal of Volcanology and Geothermal Researchen
dc.relation.ispartofseries/189(2010)en
dc.subjecttephra fallouten
dc.subjectPollena eruptionen
dc.subjectHAZMAP modelen
dc.subjectVesuviusen
dc.titleNumerical inversion and analysis of tephra fallout deposits fromthe 472 ADsub-Plinian eruption at Vesuvius (Italy) through a new best-fit procedureen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber238–246en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.08. Sediments: dating, processes, transporten
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risken
dc.subject.INGV05. General::05.01. Computational geophysics::05.01.03. Inverse methodsen
dc.identifier.doi10.1016/j.jvolgeores.2009.11.009en
dc.relation.referencesAitken, A., 1935. On the least squares and linear combination of observations. Proc. R. Soc. Edinb. 55, 42–48. Armienti, P., Macedonio, G., Pareschi, M., 1988. A numerical model for simulation of tephra transport and deposition: application to May 18, 1980 Mount St. Helens eruption. J. Geophys. Res. 93 (B6), 6463–6476. Arnò, V., Principe, C., Rosi, M., Santacroce, R., Sbrana, A., Sheridan, M., 1987. Eruptive history. Somma-Vesuvius. In: Santacroce, R. (Ed.), Quaderni della Ricerca Scientifica, vol. 114. CNR, Roma, pp. 53–103. Bonadonna, C., Houghton, B., 2005. Total grain-size distribution and volume of tephrafall deposits. Bull. Volcanol. 67, 441–456. Bonadonna, C., Connor, C., Houghton, B., Connor, L., Byrne, M., Laing, A., Hincks, T., 2005. Probabilistic modeling of tephra dispersal: hazard assessment of a multiphase rhyolitic eruption at Tarawera, New Zealand. J. Geophys. Res. 110. Carey, S., Sigurdsson, H., 1982. Influence of particle aggregation on deposition of distal tephra from the May 18, 1980, eruption of Mount St-Helens volcano. J. Geophys. Res. 87 (B8), 7061–7072. Carey, S., Sparks, R., 1986. Quantitative models of the fallout and dispersal of tephra from volcanic eruption columns. Bull. Volcanol. 48, 109–125. Casadevall, T., 1994. Volcanic ash and aviation safety. Proceedings of the First International Symposium on Volcanic Ash and Aviation Safety, U. S. Geological Survay Bullettin, vol. 2047, pp. 1–6. Cioni, R., Longo, A., Macedonio, G., Santacroce, R., Sbrana, A., 2003. Assessing pyroclastic fall hazard through field data and numerical simulations: example from Vesuvius. J. Volcanol. Geotherm. Res. 108, 2063–2073. Cioni, R., Bertagnini, A., Santacroce, R., Andronico, R., 2008. Explosive activity and eruption scenarios of Somma-Vesuvius (Italy): towards a newclassification scheme. J.Volcanol. Geotherm. Res. 178, 331–346. Cornell, W., Carey, S., Sigurdsson, H., 1983. Computer simulation and transport of the Campanian Y-5 ash. J. Volcanol. Geotherm. Res. 17, 89–109. Costa, A., Macedonio, A., Folch, A., 2006. A three-dimensional Eulerian model for transport and deposition of volcanic ashes. Earth Planet. Sci. Lett. 241, 634–647. Costa, A., Dell'Erba, F., Di Vito,M., Isaia, R.,Macedonio, G., Orsi, G., Pfeiffer, T., 2009. Tephra fallout hazard assessment at Campi Flegrei caldera (Italy). Bull. Volcanol. 71 (3), 259–273. Durant, A., Rose, W., Sarna-Wojcicki, A., Carey, S., Volentik, A., 2009. Hydrometeorenhanced tephra sedimentation: constraints from the 18 May 1980 eruption of Mount St. Helens. J. Geophys. Res. 114 (B13). Fierstein, J., Nathenson, M., 1992. Another look at the calculation of tephra fallout volumes. Bull. Volcanol. 54, 156–167. Folch, A., Costa, A., Macedonio, G., 2009. FALL3D: a computational model for transport and deposition of volcanic ash. Comput. Geosci. 35 (6), 1334–1342. Joron, J.,Metrich, N., Rosi,M., Santacroce, R., Sbrana, A., 1987. Chemistry and petrography. Somma-Vesuvius. In: Santacroce, R. (Ed.), Quaderni della Ricerca Scientifica, vol. 114. CNR, Roma, pp. 105–174. Macedonio, G., Pareschi, M., Santacroce, R., 1988. A numerical simulation of the Plinian fall phase of 79 AD eruption of Vesuvius. J. Geophys. Res. 93, 14817–14827. Macedonio, G., Pareschi,M., Santacroce, R., 1990. Renewal of explosive activity at Vesuvius: models for the expected tephra fallout. J. Volcanol. Geotherm. Res. 40, 327–342. Macedonio, G., Costa, A., Longo, A., 2005. A computer model for volcanic ash fallout and assessment of subsequent hazard. Comput. Geosci. 31, 837–845. Macedonio, G., Costa, A., Folch, A., 2008. Ash fallout at Vesuvius: numerical simulations and implication for hazard assessment. J. Volcanol. Geotherm. Res. 178, 366–377. Mele, D., 2003. Studio quantitativo per la ricostruzione dei meccanismi di trasporto e deposizione delle eruzioni esplosive: l'eruzione di Pollena (472 AD) al Vesuvio. Ph.D. Thesis, University of Bari, Italy. Morton, B., Taylor, G., Turner, S., 1956. Turbulent gravitational convection from maintained and instantaneous sources. Proc. R. Soc. Lond. 234, 1–23. Pfeiffer, T., Costa, A., 2004a. A numerical reconstruction of fall deposits from Agnano- Montespina (4100 BP) Plinian eruption in the Campi Flegrei area. Tech. Rep. OV Prot. N. 4440 (10.11.2004), Osservatorio Vesuviano-INGV, http://www.earth-prints.org/ handle/2122/2068. Pfeiffer, T., Costa, A., 2004b. Reconstruction and analysis of a sub-Plinian fall deposit from the Astroni volcano (ca. 4100–3800 BP) in the Campi Flegrei area, Italy. Tech. Rep. OV Prot. N. 4440 (10.11.2004, Osservatorio Vesuviano-INGV, http://www. earth-prints.org/handle/2122/2069. Pfeiffer, T., Costa, A., Macedonio, G., 2005. A model for the numerical simulation of tephra fall deposits. J. Volcanol. Geotherm. Res. 140, 237–294. Pyle, D., 1989. The thickness, volume and grainsize of tephra fall deposits. Bull. Volcanol. 51, 1–5. Rolandi, G., Munno, R., Postiglione, I., 2004. The AD 472 eruption of Somma volcano. J. Volcanol. Geotherm. Res. 129, 291–319. Rose,W., Durant, A., 2009. Fine ash content of explosive eruptions. J. Volcanol. Geotherm. Res. 187 (1–2), 32–39. Rosi, M., Santacroce, R., 1983. The A.D. 472 “Pollena” eruption: volcanological and petrological data from this poorly known Plinian-type event at Vesuvius. J. Volcanol. Geotherm. Res. 17, 249–271. Scollo, S., Tarantola, S., Bonadonna, C., Coltelli, M., Saltelli, A., 2008. Sensitivity analysis and uncertainty estimation for tephra dispersal models. J. Geophys. Res. 113, B06202. doi:10.1029/2006JB004864. Sparks, R., 1986. The dimensions and dynamics of volcanic eruption columns. Bull. Volcanol. 48 (1), 3–15. Sulpizio, R., Mele, D., Dellino, P., La Volpe, L., 2005. A complex Subplinian-type eruption from low-viscosity, phonolitic to tephri-phonolitic magma: the AD 472 (Pollena) eruption of Somma-Vesuvius, (Italy). Bull. Volcanol. 67, 743–767. Suzuki, T., 1983. A theoreticalmodel for dispersion of tephra. In: Shimozuru,D., Yokoyama, I. (Eds.), Volcanism: Physics and Tectonics. Terrapub, Tokyo, pp. 95–113. Woods, A., 1995. The dynamics of explosive volcanic eruptions. Rev. Geophys. 33, 495–530.en
dc.description.obiettivoSpecifico3.5. Geologia e storia dei vulcani ed evoluzione dei magmien
dc.description.obiettivoSpecifico4.3. TTC - Scenari di pericolosità vulcanicaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorBonasia, R.en
dc.contributor.authorMacedonio, G.en
dc.contributor.authorCosta, A.en
dc.contributor.authorMele, D.en
dc.contributor.authorSulpizio, R.en
dc.contributor.departmentCorresponding author. Istituto Nazionale di Geofisica e Vulcanologia, Sezione Osservatorio Vesuviano”, Via Diocleziano, 328, Napoli, Italy.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentCIRISIVU, Dipartimento Geomineralogico, Università degli Studi di Bari, Bari, Italyen
dc.contributor.departmentCIRISIVU, Dipartimento Geomineralogico, Università degli Studi di Bari, Bari, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptCIRISIVU, c/o Dipartimento Geomineralogico, Universita' di Bari-
crisitem.author.orcid0000-0001-6604-1479-
crisitem.author.orcid0000-0002-4987-6471-
crisitem.author.orcid0000-0002-8935-335X-
crisitem.author.orcid0000-0002-3930-5421-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
Appears in Collections:Article published / in press
Files in This Item:
File Description SizeFormat Existing users please Login
bonmac2010.pdf1.48 MBAdobe PDF
Show simple item record

WEB OF SCIENCETM
Citations 20

26
checked on Feb 10, 2021

Page view(s)

138
checked on Apr 17, 2024

Download(s)

27
checked on Apr 17, 2024

Google ScholarTM

Check

Altmetric