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Fig. 14 | Journal of Applied Volcanology

Fig. 14

From: Effects of eruption source parameter variation and meteorological dataset on tephra fallout hazard assessment: example from Vesuvius (Italy)

Fig. 14

Effect of the terminal settling velocity of the ash particles on the extension of the hazard zone. The hazard zone is represented by the area enclosed by the 5 % probability contour of a deposit loading equal to 300 kg/m2. Eruption column ranges between 16 and 18 km, the diffusion coefficient between 3000 and 5000 m2/s. We use radio-sounding between 1962–1976 (Aeronautica Militare) recorded at Brindisi (BRIN), radio-sounding between 1962–1976 recorded at Pratica di Mare station between 1995–2013 (LIRE), 6-h NOAA-CIRES Reanalysis-2 model between 1991–2010 (NOAA) and of ECMWF ERA-Interim Full Resolution model between 1991–2010 (ERA)

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