Journal
ASTROPHYSICAL JOURNAL
Volume 912, Issue 1, Pages -Publisher
IOP PUBLISHING LTD
DOI: 10.3847/1538-4357/abec46
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Funding
- Spanish Ministry of Economy, Industry, and Competitiveness (MINECO) [AYA2014-55078-P, PGC2018-095832-B-I00, SEV-2015-0548]
- European Research Council [810218, ERC-2018-SyG]
- NASA High-End Computing (HEC) Program, via the NASA Center for Climate Simulation (NCCS) at Goddard Space Flight Center
- MINECO via the Ramon y Cajal fellowship [RYC2018-026129-I]
- International Space Sciences Institute (ISSI) via team 413 on Large-Amplitude Oscillations as a Probe of Quiescent and Erupting Solar Prominences
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Observational evidence suggests that coronal jets can interact with prominences, leading to large-amplitude oscillations in some areas. 2.5D MHD numerical experiments are conducted to study this process. The jets generate multiple reconnection processes, resulting in the emission of perturbations and plasma jets which cause oscillations in the prominence. The observed oscillation amplitudes and periods generally match the simulations in two different height scenarios above the parasitic bipolar region.
Observational evidence shows that coronal jets can hit prominences and set them in motion. The impact leads to large-amplitude oscillations (LAOs) in the prominence. In this paper, we attempt to understand this process via 2.5D MHD numerical experiments. In our model, the jets are generated in a sheared magnetic arcade above a parasitic bipolar region located in one of the footpoints of the filament channel (FC) supporting the prominence. The shear is imposed at velocities not far above the observed photospheric values; this leads to a multiple reconnection process, as obtained in previous jet models. Both a fast Alfvenic perturbation and a slower supersonic front preceding a plasma jet are issued from the reconnection site; in the later phase, a more violent (eruptive) jet is produced. The perturbation and jets run along the FC; they are partially reflected at the prominence, and partially transmitted through it. This results in a pattern of counter-streaming flows along the FC, and oscillations in the prominence. The oscillations are LAOs (i.e., with amplitudes above 10 km s(-1)) in some areas of the prominence, both in the longitudinal and transverse directions. In some field lines, the impact is so strong that the prominence mass is brought out of the dip and down to the chromosphere along the FC. Two cases are studied, with respect to arcades at different heights above the parasitic bipolar region, leading to different heights for the region of the prominence perturbed by the jets. The obtained oscillation amplitudes and periods are in general agreement with the observations.
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