Eruption type probability and eruption source parameters at Cotopaxi and Guagua Pichincha volcanoes (Ecuador) with uncertainty quantification-Reference-Cited by-同舟云学术

Eruption type probability and eruption source parameters at Cotopaxi and Guagua Pichincha volcanoes (Ecuador) with uncertainty quantification

Published:2021-04-16 Issue:5 Volume:83 Page:
ISSN:0258-8900
Container-title:Bulletin of Volcanology
language:en
Short-container-title:Bull Volcanol

Author:

Tadini Alessandro^ORCID,Roche Olivier^ORCID,Samaniego Pablo^ORCID,Azzaoui Nourddine,Bevilacqua Andrea^ORCID,Guillin Arnaud,Gouhier Mathieu,Bernard Benjamin^ORCID,Aspinall Willy^ORCID,Hidalgo Silvana^ORCID,Eychenne Julia^ORCID,de’ Michieli Vitturi Mattia^ORCID,Neri Augusto^ORCID,Cioni Raffaello^ORCID,Pistolesi Marco^ORCID,Gaunt Elizabeth^ORCID,Vallejo Silvia,Encalada Marjorie,Yepes Hugo^ORCID,Proaño Antonio,Pique Mia

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Link

https://link.springer.com/content/pdf/10.1007/s00445-021-01458-z.pdf

Reference97 articles.

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2. Aspinall WP (2006) Structured elicitation of expert judgment for probabilistic hazard and risk assessment in volcanic eruptions. Statistics in volcanology 1:15–30

3. Aspinall WP, Cooke RM (2013) Quantifying scientific uncertainty from expert judgment elicitation. In: Rougier J, Sparks RSJ, Hill LJ (eds) Risk and uncertainty assessment for natural hazards. Cambridge University Press, New York, pp 64–99. www.cambridge.org/9781107006195

4. Aspinall WP, Woo G (2014) Santorini unrest 2011–2012: an immediate Bayesian belief network analysis of eruption scenario probabilities for urgent decision support under uncertainty. J Appl Volcanol 3:1–12. https://doi.org/10.1186/s13617-014-0012-8

5. Aspinall WP, Carniel R, Jaquet O, Woo G, Hincks T (2006) Using hidden multi-state Markov models with multi-parameter volcanic data to provide empirical evidence for alert level decision-support. J Volcanol Geotherm Res 153:112–124. https://doi.org/10.1016/j.jvolgeores.2005.08.010

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