Radiative hydrodynamic simulations of FIP fractionation in solar flares
Jeffrey W. Reep, Luke Fushimi Benavitz, Andy S. H. To, David H. Brooks, J. Martin Laming, Patrick Antolin, David M. Long, Deborah Baker
TL;DR
Addresses variability of elemental abundances in solar flares and tests how depth of footpoint fractionation and evaporation shape coronal composition. Introduces a spatiotemporal abundance factor $f(s,t)$ and couples it to radiative losses via CHIANTI in HYDRAD, then tests two fractionation-depth scenarios with footpoint spikes (100 km narrow, 500 km wide) and impulsive electron-beam heating. Hydrodynamic simulations of a 50 Mm loop heated by an electron beam ($E_c=15$ keV, $δ=5$), across four energy fluxes, show that narrow spikes produce apex-localized $f$ enhancements and coronal rain across heating rates, while wide spikes can fully fractionate the corona at low heating and require stronger heating to induce localized rain. The work predicts a direct link between coronal rain and the combination of fractionation depth and flare heating, offering testable observational strategies and, importantly, providing publicly available simulation data on Zenodo.
Abstract
Elemental abundances in solar flares are observed to vary both spatially and temporally, but the underlying mechanisms remain poorly understood. There is an interplay between advection and the preferential acceleration of low first ionization potential (FIP) elements that likely shapes the observed abundance distributions. Models of the FIP effect predict enhancements near loop footpoints that diffuse upward over time. We simulate strong evaporation events that advect this low-FIP enhancement into the corona. When the enhancement is sharply peaked, the corona does not become fractionated, exhibiting only a localized abundance peak near the loop apex that facilitates coronal rain formation. In contrast, a broad enhancement with relatively weak heating yields a uniformly fractionated corona, which is not sufficient for coronal rain formation. As the heating rate increases, the low-FIP enhanced plasma is increasingly compressed toward the loop apex, and rain is able to form. These results suggest a potential observational correlation between the presence and amount of coronal rain, the strength of flare heating, and the fractionation process itself.
