Formation of a Magnetic Flux Rope Prior to the Eruption: Insight from a Radiative MHD Simulation of Active Region Emergence
Can Wang, Takaaki Yokoyama, Feng Chen, Chen Xing, Mingde Ding, Zekun Lu
TL;DR
This study addresses how pre-eruptive magnetic flux ropes form in a realistic solar active region by analyzing a radiative RMHD simulation with self-consistent flux emergence. By quantifying magnetic helicity flux and its decomposition into advection ($\dot{H}_a$) and shear ($\dot{H}_s$) terms, the authors demonstrate that flux cancellation driven by photospheric shear plays the dominant role in flux rope formation, with reconnection above the photosphere enhancing helicity transport at higher altitudes. Height-dependent analysis shows a transition from shear-dominated to advection-driven helicity contributions, linked to magnetic reconnection processes. The work highlights flux cancellation as a robust mechanism for flux rope assembly in complex active regions and provides quantitative diagnostics relevant for predicting solar eruptions in more realistic solar atmospheres.
Abstract
Magnetic flux ropes (MFRs) are fundamental magnetic structures in solar eruptions, whose formation is generally attributed to (1) the emergence of subsurface flux tubes or (2) flux cancellation driven by photospheric horizontal flows and magnetic reconnection. Both mechanisms can operate simultaneously during active region evolution, making their relative contributions challenging to quantify. Here, we analyze the formation of a flux rope in a MURaM radiative magnetohydrodynamic (RMHD) simulation, which formed and evolved for approximately three hours before an M-class flare. The formation process is quantified by magnetic helicity flux, which drives the non-potential evolution of magnetic field, with its advection and shear terms on the photosphere corresponding to the emergence and photospheric horizontal flows, respectively. Examining the helicity injected into the flux rope through the photosphere, we find both terms increase significantly as the eruption approaches, with the shear term prevailing overall. Height-dependent analysis of helicity flux, together with magnetic field and velocity distributions, further reveals a gradual transition from the shear to the advection term with an increasing altitude, which is driven by magnetic reconnection above the photosphere. Our results provide quantitative evidence that flux cancellation governs flux rope formation, arising naturally from magnetic field reorganization during active region evolution: as flux emergence transports magnetic flux upward, photospheric shearing motions adjust magnetic field and inject helicity into solar atmosphere, and magnetic reconnection ultimately assembles the main body of flux ropes.
