EGU22-11386, updated on 18 Sep 2024
https://doi.org/10.5194/egusphere-egu22-11386
EGU General Assembly 2022
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Real-time prediction trace gases from the Fagradalsfjall volcanic eruption

Páll Einarsson1,2, Ólafur Rögnvaldsson1,2, and Haraldur Ólafsson1
Páll Einarsson et al.
  • 1Háskóli Íslands, School of Atmospheric Sciences, Reykjavík, Iceland (palleinarsson.22@gmail.com)
  • 2Belgingur Ltd., Reykjavík, Iceland

During the Fagradalsfjall volcanic eruption in Iceland in 2021, the atmospheric flow was simulated at high-spatial and temporal resolutions with the numerical system WRF, including the WRF-Chem for the simulation of trace gases and aerosols.  The output of the real-time simulations of SO2 has been compared to observations, showing that on time-scales of 12-24 hours, the numerical system has considerable skill, but moving to temporal scales shorter than 6 hours leads to substantial drop in the model performance.  The data and the model output suggest that there may be strong long-lasting horizontal gradients in the trace gases and limited horizontal mixing at times, calling for a more dense network of monitoring of gases from the volcano.  Wind variability on the time scale of minutes up to few hours remains a challenge.

How to cite: Einarsson, P., Rögnvaldsson, Ó., and Ólafsson, H.: Real-time prediction trace gases from the Fagradalsfjall volcanic eruption, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-11386, https://doi.org/10.5194/egusphere-egu22-11386, 2022.