EGU25-8335, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-8335
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Wednesday, 30 Apr, 10:45–12:30 (CEST), Display time Wednesday, 30 Apr, 08:30–12:30
 
Hall X4, X4.146
Quantifying CME effects on plasma parameters and elemental abundance recovery during a flare event with X-ray spectroscopy
Saara Takala1, Arto Lehtolainen1,2, Emilia Kilpua1, Minna Palmroth1, Jake Mitchell3, Alexander Warmuth3, and Juhani Huovelin2
Saara Takala et al.
  • 1Department of Physics, University of Helsinki, Helsinki, Finland
  • 2Isaware Oy, Helsinki, Finland
  • 3Leibniz-Institut für Astrophysik Potsdam (AIP), Potsdam, Germany

The connection between coronal mass ejections (CMEs) and solar flares has been studied statistically, but the details of this relationship remain largely unknown. Soft X-rays provide us a unique depiction of eruption dynamics due to the coronal first ionization potential (FIP) bias: abundances of low FIP elements are observed to peak at flare onset, and decrease abruptly towards photospheric values during the impulsive phase before recovery. Recovery times have been linked to the time when the plasma is trapped within the magnetic field, suggesting that CMEs delay abundance recovery. This provides a useful tool for studying the characteristics and dynamics of flares and CMEs and their effects on each other.

This study aims to connect flare characteristics to CME properties using soft X-ray spectroscopy and hard X-ray imaging. The temporal evolution of plasma parameters and elemental abundances during the eruption event are analyzed with soft X-ray data from the SUNSTORM 1 X-ray Flux Monitor for CubeSats (XFM-CS). Evolution of the X-ray loop emission source is investigated with a time-series analysis of image reconstructions utilizing The Spectrometer Telescope for Imaging X-rays (STIX) instrument on board Solar Orbiter. CME kinematics are analyzed with a variety of remote-sensing data. The resulting study shows that emission from a post-CME looptop source significantly affects eruption dynamics by slowing down abundance recovery, and relates this evolution to the flare profile. 

How to cite: Takala, S., Lehtolainen, A., Kilpua, E., Palmroth, M., Mitchell, J., Warmuth, A., and Huovelin, J.: Quantifying CME effects on plasma parameters and elemental abundance recovery during a flare event with X-ray spectroscopy, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-8335, https://doi.org/10.5194/egusphere-egu25-8335, 2025.