Magnetic Structure and Dynamics of the Erupting Solar Polar Crown Prominence on 2012 March 12

TL;DR

This study investigates the magnetic structure and eruption dynamics of a polar crown prominence on 2012 March 12, using multi-view observations and magnetic modeling to understand the eruption mechanism and magnetic support.

Contribution

It provides observational evidence favoring the twisted flux rope model and links the eruption onset to torus instability and magnetic reconnection processes.

Findings

Flux rope enters torus instability at eruption onset

Reconnection signatures appear about one hour after eruption begins

Dark ribbons in absorption indicate falling filament material

Abstract

We present an investigation of the polar crown prominence that erupted on 2012 March 12. This prominence is observed at the southeast limb by SDO/AIA (end-on view) and displays a quasi vertical-thread structure. Bright U-shape/horn-like structure is observed surrounding the upper portion of the prominence at 171 angstrom before the eruption and becomes more prominent during the eruption. The disk view of STEREO-B shows that this long prominence is composed of a series of vertical threads and displays a half loop-like structure during the eruption. We focus on the magnetic support of the prominence vertical threads by studying the structure and dynamics of the prominence before and during the eruption using observations from SDO and STEREO-B. We also construct a series of magnetic field models (sheared arcade model, twisted flux rope model, and unstable model with hyperbolic flux tube (HFT)). Various observational characteristics appear to be in favor of the twisted flux rope model. We find that the flux rope supporting the prominence enters the regime of torus instability at the onset of the fast rise phase, and signatures of reconnection (post-eruption arcade, new U-shape structure, rising blobs) appear about one hour later. During the eruption, AIA observes dark ribbons seen in absorption at 171 angstrom corresponding to the bright ribbons shown at 304 angstrom, which might be caused by the erupting filament material falling back along the newly reconfigured magnetic fields. Brightenings at the inner edge of the erupting prominence arcade are also observed in all AIA EUV channels, which might be caused by the heating due to energy released from reconnection below the rising prominence.