Estimations of Elemental Abundances During Solar Flares Observed in Soft X-rays by the MinXSS-1 CubeSat Mission
Crisel Suarez, Christopher S. Moore

TL;DR
This study analyzes the elemental abundance variations during solar flares using soft X-ray spectra from the MinXSS-1 CubeSat, revealing depletion patterns consistent with chromospheric evaporation.
Contribution
It provides the first detailed measurements of elemental abundance changes during solar flares using high-resolution soft X-ray spectra from MinXSS-1.
Findings
Elemental abundances of Fe, Ca, S, Si, and Ar are depleted during SXR peak.
Depletion patterns are consistent with chromospheric evaporation.
Observed abundances match theoretical models of flare plasma composition.
Abstract
Solar flares are complex phenomena emitting all types of electromagnetic radiation, and accelerating particles on timescales of minutes, converting magnetic energy to thermal, radiative, and kinetic energy through magnetic reconnections. As a result, local plasma can be heated to temperatures in excess of 20 MK. During the soft X-ray (SXR) solar flare peak, the elemental abundance of low first-ionization potential (FIP) elements are typically observed to be depleted from coronal values. We explored the abundance variations using disk-integrated solar spectra from the Miniature X-ray Solar Spectrometer CubeSat-1 (MinXSS-1). MinXSS-1 is sensitive to the 1-12 keV energy range with an effective 0.25 keV full-width at half-maximum (FWHM) resolution at 5.9 keV. During the year-long mission of MinXSS-1, between May 2016 - May 2017, 21 flares with intermittent data downlinks were observed…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsSolar and Space Plasma Dynamics · Ionosphere and magnetosphere dynamics · Geomagnetism and Paleomagnetism Studies
