Changes of Magnetic Energy and Helicity in Solar Active Regions from Major Flares

TL;DR

This study analyzes the evolution of magnetic energy and helicity in solar active regions around major flares, revealing post-flare decreases and subsequent replenishment, with differences between eruptive and confined events.

Contribution

It provides a comprehensive analysis of magnetic energy and helicity changes in 21 X-class flares using advanced observational and modeling techniques, highlighting differences between eruptive and confined flares.

Findings

Magnetic energy and helicity decrease after eruptions

Eruptive events show increased twist in photospheric fields

Energy and helicity are replenished within 12 hours after flares

Abstract

Magnetic free energy powers solar flares and coronal mass ejections (CMEs), and the buildup of magnetic helicity might play a role in the development of unstable structures that subsequently erupt. To better understand the roles of energy and helicity in large flares and eruptions, we have characterized the evolution of magnetic energy and helicity associated with 21 X-class flares from 2010 to 2017. Our sample includes both confined and eruptive events, with 6 and 15 in each category, respectively. Using HMI vector magnetic field observations from several hours before to several hours after each event, we employ (a) the Differential Affine Velocity Estimator for Vector Magnetograms (DAVE4VM) to determine the photospheric fluxes of energy and helicity, and (b) non-linear force-free field (NLFFF) extrapolations to estimate the coronal content of energy and helicity in source-region fields. Using Superposed Epoch analysis (SPE), we find, on average: (1) decreases in both magnetic energy and helicity, in both photospheric fluxes and coronal content, that persist for a few hours after eruptions, but no clear changes, notably in relative helicity, for confined events; (2) significant increases in the twist of photospheric fields in eruptive events, with twist uncertainties too large in confined events to constrain twist changes (and lower overall twist in confined events); and (3) on longer time scales (event time +12 hours), replenishment of free magnetic energy and helicity content to near pre-event levels for eruptive events. For eruptive events, magnetic helicity and free energy in coronal models clearly decrease after flares, with the amounts of decrease proportional to each region's pre-flare content.