Magnetic Field Configuration of a Quiescent Prominence Revealed by Large-amplitude Longitudinal Oscillations in End-view Observations
Jun Dai, Ayumi Asai, Dechao Song, Ye Qiu, Zhe Xu
TL;DR
The paper tackles how to infer the 3D magnetic-field geometry of a quiescent solar prominence by exploiting large-amplitude longitudinal oscillations observed from end-view. It combines CHASE/HIS spectroscopic data with SDO/AIA imaging to derive both Doppler and plane-of-sky velocities, then uses three complementary methods—pendulum-model seismology, time-distance-based curvature estimates, and velocity-field/Doppler analyses—to determine the curvature radius and geometry of the supporting magnetic dips. The authors find that the dips are sinusoidal, with a curvature radius that evolves from ~$90$ Mm at the bottom to ~$220$ Mm in the middle and down to ~$10$–$40$ Mm near the top, and a transverse field of about $22$–$25$ G. They also identify a triggering mechanism in which collision and heating of an adjoining hot structure associated with two coronal jets initiates the LAOs, highlighting end-view observations as a powerful tool for prominence seismology and magnetic-field diagnostics.
Abstract
Prominence seismology, applied to the large-amplitude longitudinal oscillation, is used to indirectly diagnose the geometry and strength of the magnetic fields inside the prominence. In this paper, combining imaging and spectroscopic data, the magnetic field configuration of a quiescent prominence is revealed by large-amplitude longitudinal oscillations observed in end view on 2023 December 4. Particularly, the prominence oscillation involved blueshift velocities in Dopplergrams and horizontal motions in extreme-ultraviolet (EUV) images. Originally, the prominence oscillation was triggered by the collision and heating of an adjoining hot structure associated with two coronal jets. The oscillation involved two groups of signals with similar oscillatory parameters, a three-dimensional (3D) initial amplitude of 40 Mm and a 3D velocity amplitude of 48 km/s, both lasting for 4 cycles with a period of 77 minutes, with a phase difference of pi/4. While the angle between 3D velocities and the prominence axis ranges from 10 to 30. Two methods, utilizing time-distance diagrams and velocity fields, are employed to calculate the curvature radius of magnetic dips supporting the prominence materials. Both methods yield similar value ranges and trends from the bottom to the top of magnetic dips, with the curvature radius increasing from 90 Mm to 220 Mm, then decreasing to 10 Mm, with transverse magnetic field strength 25 Gauss. From this, the realistic 3D geometry of the prominence magnetic dips is determined to be sinusoidal. To the best of our knowledge, we present the first accurate calculation of the 3D curvature radius and geometry of the prominence magnetic dips based on longitudinal oscillatory motions.
