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Inferring chromospheric velocities in an M3.2 flare using He i 1083.0 nm and Ca ii 854.2 nm

Kuckein, C; Collados, M; Asensio Ramos, A; Diaz Baso, CJ; Felipe, T; Quintero Noda, C; Kleint, L; ... Matthews, S; + view all (2025) Inferring chromospheric velocities in an M3.2 flare using He i 1083.0 nm and Ca ii 854.2 nm. Astronomy & Astrophysics , 699 , Article A121. 10.1051/0004-6361/202554798. Green open access

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Abstract

Aims. Our aim was to study the chromospheric line-of-sight (LOS) velocities during the GOES M3.2 flare (SOL2013-05-17T08:43) using simultaneous high-resolution ground-based spectroscopic data of the He I 10830 Å triplet and Ca II 8542 Å line. A filament was present in the flaring area. Methods. The observational data were acquired with the Vacuum Tower Telescope (VTT, Tenerife, Spain) and covered the pre-flare, flare, and post-flare phases. Spectroscopic inversion techniques (HAZEL and STiC) were applied individually to He I and Ca II lines to recover the atmospheric parameters of the emitting plasma. Different inversion configurations were tested for Ca II, and two families of solutions were found to explain the red-asymmetry of the profiles: a redshifted emission feature or a blueshifted absorption feature. These solutions could explain two different flare scenarios (condensation vs. evaporation). The ambiguity was solved by comparing these results to the He I inferred velocities. Results. At the front of the flare ribbon, we observed a thin short-lived blueshifted layer. This is seen in both spectral regions, but is much more pronounced in He I, with velocities of up to −10 km s−1. In addition, at the front we found the coexistence of multiple He I profiles within one pixel. The central part of the ribbon is dominated by He I and Ca II redshifted emission profiles. A flare-loop system, visible only in He I absorption and not in Ca II, becomes visible in the post-flare phase and shows strong downflows at the footpoints of up to 39 km s−1. In the flare the Ca II line represents lower heights compared to the quiet Sun, with peak sensitivity shifting from log τ≃−5.2 to log τ≃−3.5. The loop system's downflows persist for over an hour in the post-flare phase. Conclusions. The inferred LOS velocities support a cool-upflow scenario at the leading edge of the flare, with rapid transition from blueshifts to redshifts likely to occur within seconds to tens of seconds. Although the flare had a significant impact on the surrounding atmosphere, the solar filament in the region remained stable throughout all flare phases. The inclusion of the He I triplet in the analysis helped resolve the ambiguity between two possible solutions for the plasma velocities detected in the Ca II line. This highlights the importance of combining multiple chromospheric spectral lines to achieve a more comprehensive understanding of flare dynamics.

Type: Article
Title: Inferring chromospheric velocities in an M3.2 flare using He i 1083.0 nm and Ca ii 854.2 nm
Open access status: An open access version is available from UCL Discovery
DOI: 10.1051/0004-6361/202554798
Publisher version: https://doi.org/10.1051/0004-6361/202554798
Language: English
Keywords: Science & Technology, Physical Sciences, Astronomy & Astrophysics, methods: data analysis, techniques: spectroscopic, Sun: activity, Sun: chromosphere, Sun: flares, ANGSTROM LINE, MAGNETIC-FIELD, SOLAR, REGION, SPECTROPOLARIMETRY, EMISSION, EVAPORATION, INVERSIONS, EVOLUTION, ABUNDANCE
UCL classification: UCL
UCL > Provost and Vice Provost Offices > UCL BEAMS
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences > Dept of Space and Climate Physics
URI: https://discovery.ucl.ac.uk/id/eprint/10211698
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