Inferring chromospheric velocities in an M3.2 flare using He

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 <ns0:sc>I</ns0:sc> 10830 Å triplet and Ca <ns0:sc>II</ns0:sc> 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 <ns0:sc>I</ns0:sc> and Ca <ns0:sc>II</ns0:sc> lines to recover the atmospheric parameters of the emitting plasma. Different inversion configurations were tested for Ca <ns0:sc>II</ns0:sc>, 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 <ns0:sc>I</ns0:sc> 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 <ns0:sc>I</ns0:sc>, with velocities of up to −10 km s−1. In addition, at the front we found the coexistence of multiple He <ns0:sc>I</ns0:sc> profiles within one pixel. The central part of the ribbon is dominated by He <ns0:sc>I</ns0:sc> and Ca <ns0:sc>II</ns0:sc> redshifted emission profiles. A flare-loop system, visible only in He <ns0:sc>I</ns0:sc> absorption and not in Ca <ns0:sc>II</ns0:sc>, 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 <ns0:sc>II</ns0:sc> 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 <ns0:sc>I</ns0:sc> triplet in the analysis helped resolve the ambiguity between two possible solutions for the plasma velocities detected in the Ca <ns0:sc>II</ns0:sc> line. This highlights the importance of combining multiple chromospheric spectral lines to achieve a more comprehensive understanding of flare dynamics.

Publication Details

Journal
Springer Link (Chiba Institute of Technology)
Published
2025-07-04
DOI
https://doi.org/10.1051/0004-6361/202554798/pdf
Primary Topic
Mycorrhizal Fungi and Plant Interactions
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article
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article

Inferring chromospheric velocities in an M3.2 flare using He

Springer Link (Chiba Institute of Technology)
Mycorrhizal Fungi and Plant Interactions
article

Inferring chromospheric velocities in an M3.2 flare using He

article en

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 <ns0:sc>I</ns0:sc> 10830 Å triplet and Ca <ns0:sc>II</ns0:sc> 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 <ns0:sc>I</ns0:sc> and Ca <ns0:sc>II</ns0:sc> lines to recover the atmospheric parameters of the emitting plasma. Different inversion configurations were tested for Ca <ns0:sc>II</ns0:sc>, 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 <ns0:sc>I</ns0:sc> 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 <ns0:sc>I</ns0:sc>, with velocities of up to −10 km s−1. In addition, at the front we found the coexistence of multiple He <ns0:sc>I</ns0:sc> profiles within one pixel. The central part of the ribbon is dominated by He <ns0:sc>I</ns0:sc> and Ca <ns0:sc>II</ns0:sc> redshifted emission profiles. A flare-loop system, visible only in He <ns0:sc>I</ns0:sc> absorption and not in Ca <ns0:sc>II</ns0:sc>, 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 <ns0:sc>II</ns0:sc> 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 <ns0:sc>I</ns0:sc> triplet in the analysis helped resolve the ambiguity between two possible solutions for the plasma velocities detected in the Ca <ns0:sc>II</ns0:sc> line. This highlights the importance of combining multiple chromospheric spectral lines to achieve a more comprehensive understanding of flare dynamics.

Springer Link (Chiba Institute of Technology)
Openalex Percentile: Top 53%
Mycorrhizal Fungi and Plant Interactions
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