Uncertainty analysis of a model of wind-blown volcanic plumes

• Published in: Bulletin of Volcanology
• Main Authors: Woodhouse, Mark J., Hogg, Andrew J., Phillips, Jeremy C., Rougier, Jonathan C.
• Format: Text
• Language: English
• Published: Springer Berlin Heidelberg 2015
• Subjects: Research Article; Eyjafjallajökull; Iceland
• Online Access: http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4610681/; https://doi.org/10.1007/s00445-015-0959-2

Mathematical models of natural processes can be used as inversion tools to predict unobserved properties from measured quantities. Uncertainty in observations and model formulation impact on the efficacy of inverse modelling. We present a general methodology, history matching, that can be used to investigate the effect of observational and model uncertainty on inverse modelling studies. We demonstrate history matching on an integral model of volcanic plumes that is used to estimate source conditions from observations of the rise height of plumes during the eruptions of Eyjafjallajökull, Iceland, in 2010 and Grímsvötn, Iceland, in 2011. Sources of uncertainty are identified and quantified, and propagated through the integral plume model. A preliminary sensitivity analysis is performed to identify the uncertain model parameters that strongly influence model predictions. Model predictions are assessed against observations through an implausibility measure that rules out model inputs that are considered implausible given the quantified uncertainty. We demonstrate that the source mass flux at the volcano can be estimated from plume height observations, but the magmatic temperature, exit velocity and exsolved gas mass fraction cannot be accurately determined. Uncertainty in plume height observations and entrainment coefficients results in a large range of plausible values of the source mass flux. Our analysis shows that better constraints on entrainment coefficients for volcanic plumes and more precise observations of plume height are required to obtain tightly constrained estimates of the source mass flux.