Abstract
Tephra fallout associated with renewal of volcanism at the Campi Flegrei caldera is a serious threat to the Neapolitan area. In order to assess the hazards related with tephra loading, we have considered three different eruption scenarios representative of past activity: a high-magnitude event similar to the 4.1 ka Agnano-Monte Spina eruption, a medium-magnitude event, similar to the ∼3.8 ka Astroni 6 eruption, and a low-magnitude event similar to the Averno 2 eruption. The fallout deposits were reconstructed using the HAZMAP computational model, which is based on a semi-analytical solution of the two-dimensional advection–diffusion–sedimentation equation for volcanic tephra. The input parameters into the model, such as total erupted mass, eruption column height, and bulk grain-size and components distribution, were obtained by best-fitting field data. We carried out tens of thousands simulations using a statistical set of wind profiles, obtained from NOAA re-analysis. Probability maps, relative to the considered scenarios, were constructed for several tephra loads, such as 200, 300 and 400 kg/m2. These provide a hazard assessment for roof collapses due to tephra loading that can be used for risk mitigation plans in the area.
Similar content being viewed by others
References
Aitken AC (1935) On least squares and linear combinations of observations. Proc R Soc Edinb 55:42–48
Armienti P, Macedonio G, Pareschi MT (1988) A numerical model for simulation of tephra transport and deposition: Application to May 18, 1980, Mount St. Helens Eruption. J Geophys Res 93:6463–6476
Barberi F, Macedonio G, Pareschi M, Santacroce R (1990) Mapping the tephra fallout risk: an example from Vesuvius (Italy). Nature 344:142–144
Blong RJ (1984) Volcanic hazards: a sourcebook of the effects of eruptions. Academic, Sydney, p 424
Bursik M (2001) Effect of wind on the rise height of volcanic plumes. Geophys Res Lett 18:3621–3624
Carey S, Sparks RSJ (1986) Quantitative models of the fallout and dispersal of tephra from volcanic eruption columns. Bull Volcanol 48:127–141
Casadevall TJ (ed) (1994) Volcanic ash and aviation safety: proceedings of the First International Symposium on Volcanic Ash and Aviation Safety. US Geol Surv Bull 2047
Cioni R, Longo A, Macedonio G, Santacroce R, Sbrana A, Sulpizio R, Andronico D (2003) Assessing pyroclastic fall hazard through field data and numerical simulations: example from Vesuvius. J Geophys Res 108(B2):2063 DOI 10.1029/2001JB000642
Civetta L, Orsi G, Pappalardo L, Fisher RV, Heiken G, Ort M (1997) Geochemical zoning, mingling, eruptive dynamics and depositional processes—the campanian ignimbrite, Campi Flegrei caldera, Italy. J Volcanol Geotherm Res 75:183–219
Deino AL, Orsi G, Piochi M, de Vita S (2004) The age of the Neapolitan Yellow Tuff caldera-forming eruption (Campi Flegrei caldera—Italy) assessed by 40Ar/39Ar dating method. J Volcanol Geotherm Res 133:157–170
Dellino P, Isaia R, La Volpe L, Orsi G (2001) Statistical analysis of textural data from complex pyroclastic sequence: implication for fragmentation processes of the Agnano-Monte Spina eruption (4.1 ka), Phlegraean Fields, southern Italy. Bull Volcanol 63:443–461
Dellino P, Isaia R, La Volpe L, Orsi G (2004) Interference of particles fallout on the emplacement of pyroclastic surge deposits of the Agnano-Monte Spina eruption (Phlegraean Fields, Southern Italy). J Volcanol Geotherm Res 133:193–210
De Vita S, Orsi G, Civetta L, Carandente A, D’Antonio M, Deino A, di Cesare T, Fisher RV, Isaia R, Marotta E, Necco A, Ort MH, Pappalardo L, Piochi M, Southon J (1999) The Agnano-Monte Spina eruption (4100 years B.P.) in the restless Campi Flegrei caldera. J Volcanol Geotherm Res 91:269–301
De Vivo B, Rolandi G, Gans PB, Calvert A, Bohrson WA, Spera FJ, Belkin HE (2001) New constraints on the pyroclastic eruptive history of the Campanian volcanic Plain (Italy). Mineral Petrol 73:47–65
Di Girolamo P, Ghiara MR, Lirer L, Munno R, Rolandi G, Stanzione D (1984) Vulcanologia e petrologia dei Campi Flegrei. Boll Soc Geol It 103:349–413
Di Vito MA, Isaia R, Orsi G, Southon J, de Vita S, D’Antonio M, Pappalardo L, Piochi M (1999) Volcanism and deformation in the past 12 ka at the Campi Flegrei caldera (Italy). J Volcanol Geotherm Res 91:221–246
Di Vito MA, D’Antonio M, Braia G, Arienzo I, Civetta L, Di Renzo V, Isaia R, Orsi G, Piermattei M (2004) The Averno 2 eruption in the Campi Flegrei caldera.IAVCEI General Assembly, Pucon, 14–19 November 2004
Fedele FG, Giaccio B, Isaia R, Orsi G (2003) The Campanian Ignimbrite eruption, Heinrich Event 4, and Palaeolithic change in Europe: a high-resolution investigation. In: Robock A, Oppenheimer C (eds) Volcanism and the Earth’s atmosphere. Am Geophys Un, Gephys Monog Series. vol. 139. American Geophysical Union, Washington, DC, pp 301–325
Fisher RV, Orsi G, Ort M, Heiken G (1993) Mobility of large-volume pyroclastic flow—emplacement of the Campanian Ignimbrite, Italy. J Volcanol Geotherm Res 56:205–220
Isaia R, D’Antonio M, Dell’Erba F, Di Vito MA, Orsi G (2004) The Astroni volcano: the only example of close eruptions within the same vent area in the recent history of the Campi Flegrei caldera (Italy). J Volcanol Geotherm Res 133:171–192
Kalnay E, Kanamitsu M, Kister R, Collins W, Deaven D, Gandin L, Iredell M, Saha SGW, Woollen J, Zhu Y, Chelliah M, Ebisuzaki M, Higgins W, Janowiak J, Mo K, Ropelewski C, Wang, J, Leetmaa A, Reynolds R, Jenne R, Joseph D (1996) The NCEP/NCAR 40-years reanalysis project. Bull Am Meteorol Soc 77:437–470 (http://www.cdc.noaa.gov/cdc/reanalysis/)
Lirer L, Mastrolorenzo G, Rolandi G (1987) Un evento pliniano nell'attività recente dei Campi Flegrei. Boll Soc Geol It 106:461–473
Lirer L, Petrosino P, Alberico I, Postiglione I (2001) Long-term volcanic hazard forecasts based on Somma-Vesuvio past eruptive activity. Bull Volcanol 63:45–60
Macedonio G, Pareschi MT, Santacroce R (1988) A numerical simulation of the Plinian Fall phase of 79 A.D. eruption of Vesuvius. J Geophys Res 93:817–827
Macedonio G, Pareschi MT, 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
Miller TP, Casadevall TJ (2000) Volcanic ash hazards to aviation. In: Sigurdsson H, Houghton BF, McNutt SR, Rymer H, Stix J (eds) Encyclopedia of volcanoes. Academic, San Diego, pp 915–930
Mills MJ (2000) Volcanic aerosol and global atmospheric effects. In: Sigurdsson H, Houghton BF, McNutt SR, Rymer H, Stix J (eds) Encyclopedia of volcanoes. Academic, San Diego, pp 931–943
Orsi G, D'Antonio M, de Vita S, Gallo G (1992) The Neapolitan Yellow Tuff, a large-magnitude trachytic phreatoplinian eruption: eruptive dynamics, magma withdrawal and caldera collapse. J Volcanol Geotherm Res 53:275–287
Orsi G, Civetta L, D'Antonio M, Di Girolamo P, Piochi M (1995) Step-filling and development of a three-layers magma chamber: the Neapolitan Yellow Tuff case history. J Volcanol Geotherm Res 67:291–312
Orsi G, Di Vito M, de Vita S (1996) The restless, resurgent Campi Flegrei Nested Caldera (Italy): constraints on its evolution and configuration. J Volcanol Geotherm Res 74:179–214
Orsi G, Civetta L, Del Gaudio C, de Vita S, Di Vito MA, Isaia R, Petrazzuoli SM, Ricciardi G, Ricco C (1999) Short-term ground deformations and seismicity in the nested Campi Flegrei caldera (Italy): an example of active block-resurgence in a densely populated area. J Volcanol Geotherm Res 91:415–451
Orsi G, de Vita S, Di Vito M, Nave R, Heiken G (2003) Facing volcanic and related hazards in the Neapolitan area. In: Heiken G, Fakundiny R, Sutter J (eds) Earth sciences in the cities: a reader. Am Geophys Un, Sp Publ Series. vol. 56. American Geophysical Union, Washington, DC, pp 121–170
Orsi G, Di Vito MA, Isaia R (2004) Volcanic hazard assessment at the restless Campi Flegrei caldera. Bull Volcanol 66:514–530
Orsi G, di Vito M, Dell’Erba F, Quaglino M, Marzocchi W, Sandri L, Selva J (2007) Assessing volcanic hazards at the restless Campi Flegrei, Italy.Cities on Volcanoes 5, Shimabara, 19–23 November 2007
Ort M, Orsi G, Pappalardo L, Fisher RV (2003) Emplacement processes in a far-traveled dilute pyroclastic current: anisotropy of magnetic susceptibility studies of the Campanian Ignimbrite. Bull Volcanol 65:55–72
Pareschi MT, Cavarra L, Favalli M, Giannini F, Meriggi A (2000) Gis and volcanic risk management. Nat Hazards 21:361–379
Pfeiffer T, Costa A (2004a) A numerical reconstruction of fall deposits from Agnano-Monte Spina (4100 BP) Plinian eruption in the Campi Flegrei area, Italy, Osservatorio Vesuviano-INGV, Naples, Italy, Report (1), Prot. N. 4440 (10.9.2004). http://www.earth-prints.org/handle/2122/2068
Pfeiffer T, Costa A (2004b) Reconstruction and analysis of a sub-Plinian fall deposits from the Astroni volcano (ca. 4100–3800 BP) in the Campi Flegrei area, Italy, Osservatorio Vesuviano-INGV, Naples, Italy, Report (2), Prot. N. 4440 (10.9.2004). 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 140:273–294
Pyle DM (1989) The thickness, volume and grainsize of tephra fall deposits. Bull Volcanol 51:1–15
Rampino MR, Self S (2000) Volcanism and biotic extinctions. In: Sigurdsson H, Houghton BF, McNutt SR, Rymer H, Stix J (eds) Encyclopedia of volcanoes. Academic, San Diego, pp 1083–1091
Rosi M, Santacroce R (1984) Volcanic hazard assessment in the Phlegeran Fields: a contribution based on stratigraphic and historical data. Bull Volcanol 47:359–370
Rosi M, Sbrana A (1987) The Phlegraean Fields. CNR, Quad de “La ricerca Scientifica” 114:1–175
Rosi M, Sbrana A, Principe C (1983) The Phlegraean Fields: Structural evolution, volcanic history and eruptive mechanism. J Volcanol Geotherm Res 17:273–288
Rosi M, Vezzoli L, Aleotti P, De Cenzi M (1996) Interaction between caldera collapse and eruptive dynamics during the Campanian Ignimbrite eruption, Phlegraean Fields, Italy. Bull Volcanol 57:541–554
Selva J, Marzocchi W, Orsi G, di Vito M, Sandri L, Quaglino M, Costa A (2007) The Bayesian event tree for short- and long-term eruption forecasting (BET_EF) at Campi Flegrei, Italy.Cities on Volcanoes 5, Shimabara, 19–23 November 2007
Sparks RSJ (1986) The dimensions and dynamics of volcanic eruption columns. Bull Volcanol 48:3–15
Spence R, Kelman I, Baxter PJ, Zuccaro G, Petrazzuoli S (2005) Residential building and occupant vulnerability to tephra fall. Nat Haz Earth Syst Sci 5:477–494
Tilling RI (1989) Volcanic hazards and their mitigation: progress and problems. Rev Geophys 27:237–269
Wohletz K, Orsi G, de Vita S (1995) Eruptive mechanisms of the Neapolitan Yellow Tuff interpreted from stratigraphic, chemical and granulometric data. J Volcanol Geotherm Res 67:263–290
Acknowledgements
P. Belviso, A. Carandente and M. Tesauro are warmly thanked for the help given in the laboratory work. The research was supported by the Italian Department for Civil Protection within the 2000–2003 and 2004–2006 INGV-DPC Projects. We are also grateful to R. Cioni, C. Hickson and an anonymous referee for their constructive reviews.
Author information
Authors and Affiliations
Corresponding author
Additional information
Editorial responsibility: R Cioni
Rights and permissions
About this article
Cite this article
Costa, A., Dell’Erba, F., Di Vito, M.A. et al. Tephra fallout hazard assessment at the Campi Flegrei caldera (Italy). Bull Volcanol 71, 259–273 (2009). https://doi.org/10.1007/s00445-008-0220-3
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00445-008-0220-3