Spectroscopic inversions of the Ca ii 8542 {\AA} line in a C-class solar flare

TL;DR

This study uses high-resolution spectral imaging and non-LTE inversions to analyze temperature and velocity changes in the chromosphere during a C-class solar flare, revealing localized heating and downflows.

Contribution

It presents the first detailed spectroscopic inversion analysis of the Ca ii 8542 Å line during a C-class flare, showing temperature and velocity evolution in the flare chromosphere.

Findings

Strong footpoint heating during flare peak

Temperature in flaring footpoints reaches 5-6.5 kK

Flaring chromosphere exhibits weak downflows

Abstract

We study the C8.4 class solar flare SOL2016-05-14T11:34 UT using high-resolution spectral imaging in the Ca ii 8542 {\AA} line obtained with the CRISP imaging spectropolarimeter on the Swedish 1-m Solar Telescope. Spectroscopic inversions of the Ca ii 8542 {\AA} line using the non-LTE code NICOLE are used to investigate the evolution of the temperature and velocity structure in the flare chromosphere. A comparison of the temperature stratification in flaring and non-flaring areas reveals strong footpoint heating during the flare peak in the lower atmosphere. The temperature of the flaring footpoints between continuum optical depth at 500~nm, $\mathrm{log~\tau_{500}~\approx -2.5~and~ -3.5}$ is $\mathrm{\sim5-6.5~kK}$, close to the flare peak, reducing gradually to $\mathrm{\sim5~kK}$. The temperature in the middle and upper chromosphere, between $\mathrm{log~\tau_{500} \approx - 3.5~and~- 5.5}$, is estimated to be $\mathrm{\sim6.5 - 20~kK}$, decreasing to pre-flare temperatures, $\mathrm{\sim5 - 10~kK}$, after approximately 15 minutes. However, the temperature stratification of the non-flaring areas is unchanged. The inverted velocity fields show that the flaring chromosphere is dominated by weak downflowing condensations at the Ca ii 8542 {\AA} formation height.