EGU21-14235, updated on 04 Mar 2021
https://doi.org/10.5194/egusphere-egu21-14235
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Ensemble-Based Data Assimilation of volcanic ash clouds from satellite observations: application to the 24 December 2018 Mt.Etna explosive eruption.

Federica Pardini1, Stefano Corradini2, Antonio Costa3, Lorenzo Guerrieri2, Tomaso Esposti Ongaro1, Luca Merucci2, Augusto Neri1, Dario Stelitano2, and Mattia de' Michieli Vitturi4
Federica Pardini et al.
  • 1Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Pisa, Pisa, Italy
  • 2Istituto Nazionale di Geofisica e Vulcanologia (INGV), CNT, Rome, Italy (stefano.corradini@ingv.it)
  • 3stituto Nazionale di Geofisica e Vulcanologia, Sezione di Bologna, Bologna, Italy
  • 4University at Buffalo, Buffalo, NY, United States

Explosive volcanic eruptions release high amounts of ash into the atmosphere. Accurate tracking and forecasting of ash dispersal into the atmosphere and quantification of its uncertainty is of fundamental importance for volcanic hazard mitigation. Numerical models represent a powerful tool to monitor ash clouds in real-time, but limits and uncertainties affect numerical results. A way to improve numerical forecasts is by assimilating satellite observations of ash clouds through Data Assimilation algorithms, such as Ensemble-based Kalman Filters. In this study, we present the implementation of the so-called Local Ensemble Transform Kalman Filters inside a numerical procedure which simulates the release and transport of volcanic ash during explosive eruptions. The numerical procedure consists of the eruptive column model PLUME-MoM coupled with the tephra transport and dispersal model HYSPLIT. When satellite observations are available, ash maps supplied by PLUME-MoM/HYSPLIT are sequentially corrected/modified using ash column loading as retrieved from space. The new volcanic ash state represents the optimal solution with minimized uncertainties with respect to numerical estimates and observations. To test the Data Assimilation procedure, we used satellite observations of the volcanic cloud released during the explosive eruption that occurred at Mt. Etna (Italy) on 24 December 2018. Satellite observations have been carried out by the Spinning Enhanced Visible and InfraRed Imager (SEVIRI) instrument, on board the Meteosat Second Generation (MSG) geostationary satellite. Results show that the assimilation procedure significantly improves the current ash state and the forecast. In addition, numerical tests show that the use of sequential Kalman Filters does not require a precise initialization of the numerical model, being able to improve the forecasts as the assimilation cycles are performed.

How to cite: Pardini, F., Corradini, S., Costa, A., Guerrieri, L., Esposti Ongaro, T., Merucci, L., Neri, A., Stelitano, D., and de' Michieli Vitturi, M.: Ensemble-Based Data Assimilation of volcanic ash clouds from satellite observations: application to the 24 December 2018 Mt.Etna explosive eruption., EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-14235, https://doi.org/10.5194/egusphere-egu21-14235, 2021.

Corresponding displays formerly uploaded have been withdrawn.