Triggering mechanism and material transfer of a failed solar filament eruption

TL;DR

This study investigates the trigger mechanisms and material transfer processes of a failed solar filament eruption using high-resolution solar observations, revealing magnetic reconnection and filament dynamics that enhance understanding of filament eruptions.

Contribution

The paper provides detailed observational evidence of magnetic reconnection triggering a failed filament eruption and tracks material transfer, advancing knowledge of filament eruption mechanisms.

Findings

Magnetic reconnection triggered the filament eruption.

Eruptive threads exhibited untwisting motion.

Material transfer occurred into overlying magnetic loops.

Abstract

Soar filament eruptions are often associated with solar flares and coronal mass ejections (CMEs), which are the major impacts on space weather. However, the fine structures and the trigger mechanisms of solar filaments are still unclear. To address these issues, we studied a failed solar active-region filament eruption associated with a C-class flare by using high-resolution H$\alpha$ images from the New Vacuum Solar Telescope (NVST), supplemented by EUV observations of the Solar Dynamical Observatory (SDO). Before the filament eruption, a small bi-pole magnetic field emerged below the filament. And then magnetic reconnection between the filament and the emerging bi-pole magnetic field triggered the filament eruption. During the filament eruption, the untwisting motion of the filament can be clearly traced by the eruptive threads. Moreover, the foot-points of the eruptive threads are determined by tracing the descending filament materials. Note that the filament twisted structure and the right part of the eruptive filament threads cannot be seen before the filament eruption. These eruptive threads at the right part of the filament are found to be rooting in the weak negative polarities near the main negative sunspot. Moreover, a new filament formed in the filament channel due to material injection from the eruptive filament. The above observations and the potential field extrapolations are inclined to support that the filament materials were transferred into the overlying magnetic loops and the nearby filament channel by magnetic reconnection. These observations shed light on better understanding on the complexity of filament eruptions.