Evolution of solar and stellar coronal abundances due to magnetic activity
David H. Brooks, Deborah Baker, David M. Long. Paola Testa, Harry P. Warren
TL;DR
This work investigates how coronal element abundances evolve with magnetic activity across three timescales: active-region lifetimes, the solar cycle, and stellar evolution. It centers on the First Ionization Potential (FIP) effect and its inverse (iFIP), with the ponderomotive force as a key mechanism linking Alfvén-wave dynamics to fractionation and thus to observed coronal compositions. By examining AR evolution (Emergence–Stable–Dissipation phases) and solar-cycle trends, the authors show that coronal abundances reflect a progression from photospheric-like to coronal composition, modulated by heating regimes and external reconnection, culminating in a broader solar–stellar connection. The study extends these insights to other stars, noting iFIP is common in young, active systems while older stars tend toward solar-like FIP, while also outlining observational and modeling challenges that remain to be overcome.
Abstract
We discuss the evolution of solar coronal element abundances over an active region lifetime. Magneto-convection drives the complexity of magnetic fields that emerge above the photosphere. This complexity is dissipated, together with that of the overlying pre-existing fields, through dynamic events such as flares. A period of stable "ordinary" coronal heating ensues, before the concentrated fields are dissipated through interactions with the surrounding environment. The evolution of coronal abundances can be explained by the First Ionisation Potential (FIP) effect operating within this framework. We extend the discussion from magnetic activity on timescales of active region lifetimes (months), to the solar cycle (years), and stellar evolution (eons). The broad picture shows intriguing similarities that may prompt new investigations.
