Current Helicity in Response to Coronal Mass Ejections

Fuente: arXiv
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Main Authors: Sun, Zheng, Li, Ting, Bian, Xinkai, Hou, Yijun, Kontogiannis, Ioannis, Wu, Ziqi
Format: Preprint
Published: 2025
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author Sun, Zheng
Li, Ting
Bian, Xinkai
Hou, Yijun
Kontogiannis, Ioannis
Wu, Ziqi
author_facet Sun, Zheng
Li, Ting
Bian, Xinkai
Hou, Yijun
Kontogiannis, Ioannis
Wu, Ziqi
contents Coronal mass ejections (CMEs), powerful solar eruptions with massive plasma ejected into the interplanetary space, are caused by the release of the magnetic free enengy stored in coronal electric currents. Photospheric current helicity, defined as the integral of the product of vertical electric current density and vertical magnetic field ($H_c=\int j_zB_z\ dS$), serves as a key parameter in understanding the eruptions. Using a 3D magnetohydrodynamic model, we identify a current helicity reversal pattern associated with the eruption: a pre-eruption decrease and a post-eruption increase. This helicity reversal is attributed to the redistribution of electric currents: before the eruption, currents concentrate toward the polarity inversion line (PIL); after the eruption they move away from the PIL, consistent with the flare ribbon separation, which is caused by the upward progression reconnection site. To validate this pattern, we conducted an observational analysis of 50 $\geq$M5.0 eruptive flares. The results reveal that 58\% of cases exhibited a pre-eruption decrease and 92\% showed the post-eruption increase in current helicity. Detailed analysis of two cases with this reversal suggests that they share the same current redistribution pattern, consistent with the mechanism identified in the simulations. Moreover, the pre-eruption decrease could be observed clearly even in the long-term evolution of the two cases. Current helicity can serve as an indicator of when electric currents are built up for the subsequent eruption, and it has the potential to predict CMEs to some extent.
format Preprint
id arxiv_https___arxiv_org_abs_2507_11790
institution arXiv
publishDate 2025
record_format arxiv
spellingShingle Current Helicity in Response to Coronal Mass Ejections
Sun, Zheng
Li, Ting
Bian, Xinkai
Hou, Yijun
Kontogiannis, Ioannis
Wu, Ziqi
Solar and Stellar Astrophysics
Coronal mass ejections (CMEs), powerful solar eruptions with massive plasma ejected into the interplanetary space, are caused by the release of the magnetic free enengy stored in coronal electric currents. Photospheric current helicity, defined as the integral of the product of vertical electric current density and vertical magnetic field ($H_c=\int j_zB_z\ dS$), serves as a key parameter in understanding the eruptions. Using a 3D magnetohydrodynamic model, we identify a current helicity reversal pattern associated with the eruption: a pre-eruption decrease and a post-eruption increase. This helicity reversal is attributed to the redistribution of electric currents: before the eruption, currents concentrate toward the polarity inversion line (PIL); after the eruption they move away from the PIL, consistent with the flare ribbon separation, which is caused by the upward progression reconnection site. To validate this pattern, we conducted an observational analysis of 50 $\geq$M5.0 eruptive flares. The results reveal that 58\% of cases exhibited a pre-eruption decrease and 92\% showed the post-eruption increase in current helicity. Detailed analysis of two cases with this reversal suggests that they share the same current redistribution pattern, consistent with the mechanism identified in the simulations. Moreover, the pre-eruption decrease could be observed clearly even in the long-term evolution of the two cases. Current helicity can serve as an indicator of when electric currents are built up for the subsequent eruption, and it has the potential to predict CMEs to some extent.
title Current Helicity in Response to Coronal Mass Ejections
topic Solar and Stellar Astrophysics
url https://arxiv.org/abs/2507.11790