Data-constrained Magnetohydrodynamic Simulation for Magnetic Flux Rope Eruptions Driven by Magnetic Reconnection

We conducted data-constrained magnetohydrodynamic (MHD) simulations for solar active region (AR) NOAA AR 11429, which produced two X-class flares within a span of 63 minutes. The simulations were performed using the zero- β MHD approximation, with the initial condition derived from the nonlinear for...

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Published inThe Astrophysical journal Vol. 983; no. 1; pp. 38 - 49
Main Authors Liu, Nian, Inoue, Satoshi, Wang, Ying, Wang, Haimin
Format Journal Article
LanguageEnglish
Published The American Astronomical Society 10.04.2025
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Abstract We conducted data-constrained magnetohydrodynamic (MHD) simulations for solar active region (AR) NOAA AR 11429, which produced two X-class flares within a span of 63 minutes. The simulations were performed using the zero- β MHD approximation, with the initial condition derived from the nonlinear force-free field extrapolated from the photospheric magnetograms taken 2 hr before the first X5.4 flare. During the simulation, we enhanced magnetic reconnection locally by applying anomalous resistivity in the induction equation within the regions of interest. As a result, the simulations successfully reproduced the expansion of two magnetic flux ropes (MFRs) corresponding to the two observed eruptions. The result shows that the difference in stability between the two MFRs is related to the location of the magnetic reconnection that triggers the solar eruptions. Furthermore, comparison with the analysis of failed MFR eruptions indicates that both the initiation reconnection and the subsequent driving mechanism, torus instability, are equally important for a successful eruption. This simulation reveals a new mechanism in which long loops, formed via tether-cutting reconnection, push up the overlying twisted field lines, leading to their destabilization by torus instability.
AbstractList We conducted data-constrained magnetohydrodynamic (MHD) simulations for solar active region (AR) NOAA AR 11429, which produced two X-class flares within a span of 63 minutes. The simulations were performed using the zero- β MHD approximation, with the initial condition derived from the nonlinear force-free field extrapolated from the photospheric magnetograms taken 2 hr before the first X5.4 flare. During the simulation, we enhanced magnetic reconnection locally by applying anomalous resistivity in the induction equation within the regions of interest. As a result, the simulations successfully reproduced the expansion of two magnetic flux ropes (MFRs) corresponding to the two observed eruptions. The result shows that the difference in stability between the two MFRs is related to the location of the magnetic reconnection that triggers the solar eruptions. Furthermore, comparison with the analysis of failed MFR eruptions indicates that both the initiation reconnection and the subsequent driving mechanism, torus instability, are equally important for a successful eruption. This simulation reveals a new mechanism in which long loops, formed via tether-cutting reconnection, push up the overlying twisted field lines, leading to their destabilization by torus instability.
Author Wang, Ying
Inoue, Satoshi
Liu, Nian
Wang, Haimin
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  surname: Liu
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  organization: Institute for Space Weather Sciences , New Jersey Institute of Technology, Newark, NJ 07102-1982, nian.liu@njit.edu USA
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  givenname: Satoshi
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  surname: Inoue
  fullname: Inoue, Satoshi
  organization: Institute for Space Weather Sciences , New Jersey Institute of Technology, Newark, NJ 07102-1982, nian.liu@njit.edu USA
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  surname: Wang
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  organization: Big Bear Solar Observatory , New Jersey Institute of Technology, 40386 North Shore Lane, Big Bear City, CA 92314-9672, USA
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SubjectTerms Magnetohydrodynamical simulations
Magnetohydrodynamics
Solar active region magnetic fields
Solar flares
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Title Data-constrained Magnetohydrodynamic Simulation for Magnetic Flux Rope Eruptions Driven by Magnetic Reconnection
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