Preprints
https://doi.org/10.5194/nhess-2022-100
https://doi.org/10.5194/nhess-2022-100
 
12 Apr 2022
12 Apr 2022
Status: a revised version of this preprint was accepted for the journal NHESS and is expected to appear here in due course.

Assessing minimum pyroclastic density current mass to impact critical infrastructures: example from Aso Caldera (Japan)

Andrea Bevilacqua1, Alvaro Aravena2, Willy Aspinall3, Antonio Costa4, Sue Mahony3, Augusto Neri1, Stephen Sparks3, and Brittain Hill5 Andrea Bevilacqua et al.
  • 1Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Pisa, Pisa, Italy
  • 2Laboratoire Magmas et Volcans, Université Clermont Auvergne, CNRS, IRD, OPGC, Clermont-Ferrand, France
  • 3University of Bristol, School of Earth Sciences, Bristol, United Kingdom
  • 4Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Bologna, Bologna, Italy
  • 5University of South Florida, School of Geosciences, Tampa, FL, United States

Abstract. We describe a method for calculating the probability that a distal geographic location is impacted by a pyroclastic density current (PDC) of a given size, considering the key related uncertainties. Specifically, we evaluate the minimum volume and mass of a PDC generated at the Aso caldera (Japan) that might affect each of three distal infrastructure (target) sites, with model input parameter uncertainties derived from expert judgement. The three target sites are all located 130–145 km from the caldera, but in well-separated directions and thus, for each, we test the different topographic shielding effects. To inform our probabilistic analysis, we apply alternative kinetic energy assessment approaches, i.e. rock avalanche and density current dynamics. In the latter formulation, the minimum mass needed to reach the targets ranges between median values ~283×1012 kg and ~465×1012 kg (M7.5–7.7), depending on the site. Rock avalanche dynamics modelling indicates ~3-times greater mass would be required to reach the target sites with 50 % probability, while the hypothetical scenario of a relatively dilute distal ash-cloud would require ~3-times less mass. We compare our results with the two largest recorded Aso eruptions, showing that a catastrophic eruption, similar to Aso-4, ≈M8, would present a high conditional probability of PDCs reaching the target sites, i.e. 32 %–96 %, in the density current formulation and contingent on uncertainty in the erupted mass and on target site direction. This said, for Aso the current occurrence probability of such a colossal initiating eruption has been estimated <10-8 in the next 100 years.

Andrea Bevilacqua et al.

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on nhess-2022-100', Shinji Takarada, 28 May 2022
    • AC1: 'Reply on RC1', Andrea Bevilacqua, 18 Aug 2022
  • RC2: 'Additional Comments on nhess-2022-100', Shinji Takarada, 29 May 2022
    • AC2: 'Reply on RC2', Andrea Bevilacqua, 18 Aug 2022
  • RC3: 'Comment on nhess-2022-100', Anonymous Referee #2, 05 Jul 2022
    • AC3: 'Reply on RC3', Andrea Bevilacqua, 18 Aug 2022

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on nhess-2022-100', Shinji Takarada, 28 May 2022
    • AC1: 'Reply on RC1', Andrea Bevilacqua, 18 Aug 2022
  • RC2: 'Additional Comments on nhess-2022-100', Shinji Takarada, 29 May 2022
    • AC2: 'Reply on RC2', Andrea Bevilacqua, 18 Aug 2022
  • RC3: 'Comment on nhess-2022-100', Anonymous Referee #2, 05 Jul 2022
    • AC3: 'Reply on RC3', Andrea Bevilacqua, 18 Aug 2022

Andrea Bevilacqua et al.

Andrea Bevilacqua et al.

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Short summary
We evaluate, through first-order kinetic energy models, the minimum volume and mass of a pyroclastic density current generated at the Aso caldera that might affect any of three infrastructure sites related to the electricity grid of southern Japan. These target sites are all located 130–145 km from the caldera, but in well-separated directions. Our constraints of volume and mass are then compared with the main characteristics of the two largest Aso eruptions, with emphasis on Aso-4.
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