Evolution of Interplanetary Small Magnetic Flux Ropes Across Earth's Bow Shock: Global Hybrid Modeling

Abstract Previous studies indicate that small magnetic flux ropes occupy ∼one third of solar‐wind intervals, yet their appearance in the magnetosheath remains unclear. We use the AuburN Global hybrid CodE in three Dimension (ANGIE3D) to investigate their evolution as they cross Earth's bow shock. We find that the ropes are compressed in the ram direction but retain their transverse dimensions. During shock crossing, backstreaming ions from the trailing edge of the flux rope produce foreshock signatures. In the magnetosheath, significant parallel temperature enhancement occurs within a thin layer on the flux rope's surface. From these results we derive observational signatures to aid identification of interplanetary SFRs in the magnetosheath. These results advance our understanding of coherent‐structure evolution and identification in magnetosheath.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-11-06
DOI
https://doi.org/10.1029/2025gl118529
Primary Topic
Solar and Space Plasma Dynamics
Type
article
Field-Weighted Citation Impact
0.00

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article

Evolution of Interplanetary Small Magnetic Flux Ropes Across Earth's Bow Shock: Global Hybrid Modeling

Y. D. Jia, Y. Lin, H. Y. Wei, Terry Z. Liu et al.
Geophysical Research Letters
Solar and Space Plasma Dynamics
article

Evolution of Interplanetary Small Magnetic Flux Ropes Across Earth's Bow Shock: Global Hybrid Modeling

Y. D. Jia, Y. Lin, H. Y. Wei, Terry Z. Liu, Xueyi Wang, Kun Zhang, Xiaolei Li
article en

Abstract

Abstract Previous studies indicate that small magnetic flux ropes occupy ∼one third of solar‐wind intervals, yet their appearance in the magnetosheath remains unclear. We use the AuburN Global hybrid CodE in three Dimension (ANGIE3D) to investigate their evolution as they cross Earth's bow shock. We find that the ropes are compressed in the ram direction but retain their transverse dimensions. During shock crossing, backstreaming ions from the trailing edge of the flux rope produce foreshock signatures. In the magnetosheath, significant parallel temperature enhancement occurs within a thin layer on the flux rope's surface. From these results we derive observational signatures to aid identification of interplanetary SFRs in the magnetosheath. These results advance our understanding of coherent‐structure evolution and identification in magnetosheath.

Geophysical Research LettersVol. 52(21)
Planetary Science Institute (US), University of California, Los Angeles (US), Auburn University (US)
National Aeronautics and Space Administration, Nuclear Safety and Security Commission, Ames Research Center
Openalex Percentile: Top 77%
Solar and Space Plasma Dynamics
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Evolution of Interplanetary Small Magnetic Flux Ropes Across Earth's Bow Shock: Global Hybrid Modeling — Y. D. Jia, Y. Lin, et al. · Geophysical Research Letters (2025) | TGRS Research Map | TGRS