Revealing the Local Time Structure of the Alfvén Radius in Jupiter's Magnetosphere Through High-Resolution Simulations

IF 3.9 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Yan Xu, Licia Ray, Zhonghua Yao, Binzheng Zhang, Bertrand Bonfond, Sarah Badman, Denis Grodent, Enhao Feng, Tianshu Qin, Yong Wei
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Abstract

In the context of planetary magnetospheres, the Alfvén radius plays a critical role as the demarcation line where the planet's magnetosphere and ionosphere effectively decouple. This boundary is pivotal in understanding the complex interactions between planetary magnetic fields and space plasma environments. This study presents a dynamic analysis of the Alfvén radius within Jupiter's magnetosphere using high-resolution simulations to capture its temporal variability. Our simulations reveal that the Alfvén radius presents a dynamic behavior, which is strongly modulated by planetary rotation. However, when averaged over one Jovian rotation period, the location of the Alfvén radius displays striking similarities to that described by the statistical models proposed by Jenkins et al. (2024, 10.17635/lancaster/researchdata/661). Specifically, our averaged results highlight a prominent outward bulge in the radius location toward ∼03 local time with a notable absence of the radius between the noon and dusk sectors. The absence of the Alfvén radius suggests the higher Alfvén velocities in the noon-to-dusk sector associated with strong magnetic fields. These results suggest that while short-term dynamics are present, the average position of the Alfvén radius over a rotation period roughly remains consistent with previous steady-state models, providing an enhanced understanding of the long-term behavior exhibited by the magnetospheric plasma environment in Jupiter's magnetosphere. Importantly, the dynamic location of the Alfvén radius and the observed asymmetry after averaging over one rotation period could demonstrate a significant correlation with the complex evolution of the auroral enhancement.

Abstract Image

通过高分辨率模拟揭示木星磁层中阿尔芬半径的局部时间结构
在行星磁层方面,阿尔芬半径作为行星磁层和电离层有效脱钩的分界线起着至关重要的作用。这条分界线对于理解行星磁场和太空等离子体环境之间复杂的相互作用至关重要。本研究利用高分辨率模拟对木星磁层内的阿尔芬半径进行了动态分析,以捕捉其时间变化。我们的模拟显示,阿尔芬半径呈现出一种动态行为,它受到行星自转的强烈调制。然而,当平均到一个木星自转周期时,阿尔芬半径的位置与詹金斯等人提出的统计模型(2024,10.17635/lancaster/researchdata/661)所描述的位置惊人地相似。具体来说,我们的平均结果表明,半径位置在当地时间 ∼03 时有一个明显的向外凸起,而在正午和黄昏扇区之间则明显没有半径。阿尔弗文半径的缺失表明,正午到黄昏扇区的阿尔弗文速度较高,与强磁场有关。这些结果表明,虽然存在短期动态变化,但在一个旋转周期内,阿尔弗文半径的平均位置与之前的稳态模型大致保持一致,从而加深了对木星磁层等离子体环境所表现出的长期行为的理解。重要的是,阿尔弗文半径的动态位置以及在一个自转周期内平均后观测到的不对称现象可能与极光增强的复杂演变有重要关联。
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来源期刊
Journal of Geophysical Research: Planets
Journal of Geophysical Research: Planets Earth and Planetary Sciences-Earth and Planetary Sciences (miscellaneous)
CiteScore
8.00
自引率
27.10%
发文量
254
期刊介绍: The Journal of Geophysical Research Planets is dedicated to the publication of new and original research in the broad field of planetary science. Manuscripts concerning planetary geology, geophysics, geochemistry, atmospheres, and dynamics are appropriate for the journal when they increase knowledge about the processes that affect Solar System objects. Manuscripts concerning other planetary systems, exoplanets or Earth are welcome when presented in a comparative planetology perspective. Studies in the field of astrobiology will be considered when they have immediate consequences for the interpretation of planetary data. JGR: Planets does not publish manuscripts that deal with future missions and instrumentation, nor those that are primarily of an engineering interest. Instrument, calibration or data processing papers may be appropriate for the journal, but only when accompanied by scientific analysis and interpretation that increases understanding of the studied object. A manuscript that describes a new method or technique would be acceptable for JGR: Planets if it contained new and relevant scientific results obtained using the method. Review articles are generally not appropriate for JGR: Planets, but they may be considered if they form an integral part of a special issue.
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