EGU25-8769, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-8769
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Thursday, 01 May, 16:15–18:00 (CEST), Display time Thursday, 01 May, 14:00–18:00
 
Hall X4, X4.138
Beam-driven evaporation in 2.5D flare simulations with an asymmetric magnetic field configuration
Maxime Dubart1, Malcolm Druett2, and Rony Keppens1
Maxime Dubart et al.
  • 1KU Leuven, Department of Mathematics, Leuven, Belgium (maxime.dubart@kuleuven.be)
  • 2Plasma Dynamics Group, School of Electrical and Electronic Engineering, University of Sheffield, Sheffield, S1 3JD, United Kingdom

The standard flare model is in generally depicted and studied in 2D simulations with an anti-symmetrical magnetic field configuration, symmetrical in magnitude, either side of the polarity inversion line. However, flare observations confirm that most flare have a significantly asymmetrical values of the magnetic field strength. 

Here we present the first multi-dimensional magnetohydrodynamic flare simulation featuring evaporation driven by energetic electron beams in an asymmetrical magnetic field configuration. The simulation conditions that we use are known to rely significantly on those beams of electrons to drive the evaporated plasma upwards from the lower atmosphere (Druett et al. 2023). We study the impact of an asymmetrical configuration on the evolution and geometry of the flare-loop system as well as the impacts on the beam-driven evaporation using the MPI-AMRVAC model.

This results in multiple Hard X-Rays deposition sites in the lower atmosphere, Hard X-Rays sources forming at the top of the flare loop, and a sustained rotating flux rope structure with associated footpoint electron deposition flux.

How to cite: Dubart, M., Druett, M., and Keppens, R.: Beam-driven evaporation in 2.5D flare simulations with an asymmetric magnetic field configuration, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-8769, https://doi.org/10.5194/egusphere-egu25-8769, 2025.