On the factors determining the eruptive character of solar flares
arXiv:1712.05106 · doi:10.3847/1538-4357/aaa243
Abstract
We investigated how the magnetic field in solar active regions (ARs) controls flare activity, i.e., whether a confined or eruptive flare occurs. We analyzed 44 flares of GOES class M5.0 and larger that occurred during 2011--2015. We used 3D potential magnetic field models to study their location (using the flare distance from the flux-weighted AR center ) and the strength of the magnetic field in the corona above (via decay index and flux ratio). We also present a first systematic study of the orientation of the coronal magnetic field, using the orientation of the flare-relevant polarity inversion line as a measure. We analyzed all quantities with respect to the size of the underlying dipole field, characterized by the distance between the opposite-polarity centers, . Flares originating from underneath the AR dipole ) tend to be eruptive if launched from compact ARs ( Mm) and confined if launched from extended ARs. Flares ejected from the periphery of ARs () are predominantly eruptive. In confined events the flare-relevant field adjusts its orientation quickly to that of the underlying dipole with height ( until the apex of the dipole field), in contrast to eruptive events where it changes more slowly with height. The critical height for torus instability, , discriminates best between confined ( Mm) and eruptive flares ( Mm). It discriminates better than , implying that the decay of the confining field plays a stronger role than its orientation at different heights.
17 pages, 7 figures, accepted for publication in ApJ
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