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Figure in a journal article
Ash load probability maps for Martinique using the 41-year wind database and considering the 16 eruptive scenarios
Figure 8 in: Michaud-Dubuy, A., Carazzo, G., & Kaminski, E. (2021). Volcanic hazard assessment for tephra fallout in Martinique. Journal of Applied Volcanology, 10(1), 1-20. https://doi.org/10.1186/s13617-021-00106-7.
Figure in a journal article
Ash loading probability maps for the maximum expected eruption scenario
Figure 5 in: Michaud-Dubuy, A., Carazzo, G., & Kaminski, E. (2021). Volcanic hazard assessment for tephra fallout in Martinique. Journal of Applied Volcanology, 10(1), 1-20. https://doi.org/10.1186/s13617-021-00106-7.
Figure in a journal article
Atmospheric dispersion of tephra for a threshold of 2 mg m−3 for all FL for the eruption scenarios of Hekla ERS 1947-type (a, b, c), Katla LLERS (d, e, f) and Askja OES 1875-type (g, h, i)
Figure 13 in: Biass, S., Scaini, C., Bonadonna, C., Folch, A., Smith, K., & Höskuldsson, A. (2014). A multi-scale risk assessment for tephra fallout and airborne concentration from multiple Icelandic volcanoes–Part 1: Hazard assessment. Natural hazards and earth system sciences, 14(8), 2265-2287. https://doi.org/10.5194/nhess-14-2265-2014
Figure in a journal article
BA hazard maps displaying the yearly mean probability of areas being impacted by BA
Figure 8 in: Sandri, L., Thouret, J. C., Constantinescu, R., Biass, S., & Tonini, R. (2014). Long-term multi-hazard assessment for El Misti volcano (Peru). Bulletin of volcanology, 76(2), 771. https://doi.org/10.1007/s00445-013-0771-9
Figure in a journal article
Ballistic vulnerability or probability of casualty assuming an eruption during the time of exposure, along the Tongariro Alpine Crossing
Figure 12 in: Fitzgerald, R. H., Tsunematsu, K., Kennedy, B. M., Breard, E. C. P., Lube, G., Wilson, T. M., Jolly, A.D., Pawson, J., Rosenburg, M.D., & Cronin, S. J. (2014). The application of a calibrated 3D ballistic trajectory model to ballistic hazard assessments at Upper Te Maari, Tongariro. Journal of volcanology and geothermal research, 286, p. 248-262. https://doi.org/10.1016/j.jvolgeores.2014.04.006
Figure in a journal article
Best-guess probability map of vent opening
Figure 2 in: Massaro, S., Rossi, E., Sandri, L., Bonadonna, C., Selva, J., Moretti, R., & Komorowski, J. C. (2022). Assessing hazard and potential impact associated with volcanic ballistic projectiles: The example of La Soufrière de Guadeloupe volcano (Lesser Antilles). Journal of volcanology and geothermal research, 423, 107453. https://doi.org/10.1016/j.jvolgeores.2021.107453
Figure in a journal article
BET_VH Node 8 maps showing the average absolute probability of accumulating ≥10 km m−2 of tephra in the next 1 year from a single Plinian phase resulting from a a basaltic eruption from within the OVC, b a rhyolitic eruption from within the OVC and c either a basaltic or rhyolitic eruption from within the OVC
Figure 7 in: Thompson, M. A., Lindsay, J. M., Sandri, L., Biass, S., Bonadonna, C., Jolly, G., & Marzocchi, W. (2015). Exploring the influence of vent location and eruption style on tephra fall hazard from the Okataina Volcanic Centre, New Zealand. Bulletin of volcanology, 77(5), 38. https://doi.org/10.1007/s00445-015-0926-y
Figure in a journal article
BET_VH Node 8 maps showing the average conditional probability of accumulating ≥10 kg m−2 tephra given a single Plinian phase resulting from a a basaltic eruption from within the Tarawera LVZ; b a rhyolitic eruption from within the Tarawera LVZ; d a basaltic eruption from within the Haroharo LVZ; e a rhyolitic eruption from within the Haroharo LVZ; e a basaltic eruption from Ruawahia Dome, a single vent within the Tarawera LVZ (see star in Fig. 4); and f a rhyolitic eruption from Ruawahia Dome
Figure 8 in: Thompson, M. A., Lindsay, J. M., Sandri, L., Biass, S., Bonadonna, C., Jolly, G., & Marzocchi, W. (2015). Exploring the influence of vent location and eruption style on tephra fall hazard from the Okataina Volcanic Centre, New Zealand. Bulletin of volcanology, 77(5), 38. https://doi.org/10.1007/s00445-015-0926-y
Figure in a journal article
BET_VH Node 8 outputs showing the average absolute probability of accumulating ≥10 kg m−2 of tephra in the next 1 year from a single Plinian phase resulting from a a basaltic eruption and b a rhyolitic eruption, from somewhere within the Tarawera LVZ
Figure 5 in: Thompson, M. A., Lindsay, J. M., Sandri, L., Biass, S., Bonadonna, C., Jolly, G., & Marzocchi, W. (2015). Exploring the influence of vent location and eruption style on tephra fall hazard from the Okataina Volcanic Centre, New Zealand. Bulletin of volcanology, 77(5), 38. https://doi.org/10.1007/s00445-015-0926-y
Official, Map sheet or poster
Campi Flegrei Mappa di Delimitazione della "Zona Gialla"
(Campi Flegrei Delimitation Map of the "Yellow Zone")
Dipartimento della Protezione Civile. (2015). Campi Flegrei Mappa di Delimitazione della "Zona Gialla" - Aggiornamento Pianificazione Nazionale di Emergenza per Rischio Vulcanico.