Interplanetary Magnetic Field <i>B</i> <sub> <i>y</i> </sub> Controlled Alfvén Wings at Earth During an Encounter of a Coronal Mass Ejection

Abstract On 24 April 2023, an ICME reached Earth's orbit. The solar wind density dropped to 0.3 amu/cc while the IMF strength was about 25 nT. As a result, the solar wind flow transitions to a sub‐Alfvénic state with an Alfvén Mach number of 0.4. We carry out global magnetohydrodynamic simulations to investigate the responses of Earth's magnetosphere to the ICME ejecta. The results show the formation of Alfvén wings as the solar wind becomes sub‐Alfvénic. Furthermore, the sub‐Alfvénic period was characterized by the dominance of the IMF component, causing the Alfvén wings to extend toward the dawn and dusk flanks. We investigate the global magnetospheric convection of this sub‐ Alfvénic case and find that the overall convection is mediated by the Alfvén wings, while the magnetic field convection in inner magnetosphere is similar to the super‐Alfvénic case.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-03-13
DOI
https://doi.org/10.1029/2024gl113416
Citations
1
Primary Topic
Solar and Space Plasma Dynamics
Type
article
Field-Weighted Citation Impact
1.15

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article

Interplanetary Magnetic Field B y Controlled Alfvén Wings at Earth During an Encounter of a Coronal Mass Ejection

M. Sarantos, Brandon Lee Burkholder, Yuxi Chen, Li‐Jen Chen et al.
1 citations
Geophysical Research Letters
Solar and Space Plasma Dynamics
1.15
article

Interplanetary Magnetic Field B y Controlled Alfvén Wings at Earth During an Encounter of a Coronal Mass Ejection

M. Sarantos, Brandon Lee Burkholder, Yuxi Chen, Li‐Jen Chen, Chuanfei Dong
article en
1 citations

Abstract

Abstract On 24 April 2023, an ICME reached Earth's orbit. The solar wind density dropped to 0.3 amu/cc while the IMF strength was about 25 nT. As a result, the solar wind flow transitions to a sub‐Alfvénic state with an Alfvén Mach number of 0.4. We carry out global magnetohydrodynamic simulations to investigate the responses of Earth's magnetosphere to the ICME ejecta. The results show the formation of Alfvén wings as the solar wind becomes sub‐Alfvénic. Furthermore, the sub‐Alfvénic period was characterized by the dominance of the IMF component, causing the Alfvén wings to extend toward the dawn and dusk flanks. We investigate the global magnetospheric convection of this sub‐ Alfvénic case and find that the overall convection is mediated by the Alfvén wings, while the magnetic field convection in inner magnetosphere is similar to the super‐Alfvénic case.

Geophysical Research LettersVol. 52(6)
Boston University (US), Goddard Space Flight Center (US), University of Michigan (US)
National Aeronautics and Space Administration, Heliophysics Division
Openalex Percentile: Top 21%
Solar and Space Plasma Dynamics
1.15
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Interplanetary Magnetic Field <i>B</i> <sub> <i>y</i> </sub> Controlled Alfvén Wings at Earth During an Encounter of a Coronal Mass Ejection — M. Sarantos, Brandon Lee Burkholder, et al. · Geophysical Research Letters (2025) | TGRS Research Map | TGRS