磁峰中哨声模合唱波的二维传播模型

IF 2.9 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS Journal of Geophysical Research: Space Physics Pub Date : 2024-12-27 DOI:10.1029/2024JA033383
Bopu Feng, Xiongdong Yu, Haimeng Li, Meng Zhou, Rongxin Tang, Zhihai Ouyang, Ying Xiong, An Yuan, Wenqian Zou, Yingqiao Cheng
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引用次数: 0

摘要

近年来的研究表明,基于一维理论和模拟,合唱波可以被磁峰引导。尽管有这些发现,这种内部磁层内的传导传播仍未得到证实。在这项研究中,我们进行了详细的射线追踪模拟,以探索和声波在磁峰特征区域的二维行为。我们的研究结果表明,合唱波确实可以被磁峰引导,在磁峰的两侧反复反射。此外,我们还讨论了导致这些重复反射的物理机制,为这一过程提供了更深入的见解。为了进一步丰富我们的分析,我们进行了参数分析,研究不同的波频率和初始位置对合唱波传播特性的影响。结果提供了一个更全面的理解哨子模式波是如何在磁层中传播的,增强了我们对波粒相互作用和空间等离子体环境动力学的认识。
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Modeling the Two-Dimensional Propagation of Whistler-Mode Chorus Waves in the Magnetic Peaks

Recent studies have shown that chorus waves can be guided by magnetic peaks based on one-dimensional theories and simulations. Despite these findings, such ducting propagation within the inner magnetosphere remains unconfirmed. In this research, we conduct detailed ray tracing simulations to explore the two-dimensional behavior of chorus waves in regions characterized by magnetic peaks. Our findings demonstrate that chorus waves can indeed be guided by magnetic peaks, undergoing repeated reflections on both sides of the peak. Additionally, we discuss the physical mechanisms responsible for these repetitive reflections, offering deeper insights into the process. To further enrich our analysis, we performed a parameter analysis to study how different wave frequencies and initial locations influence the propagation characteristics of chorus waves. The results provide a more comprehensive understanding of how whistler-mode waves propagate within the magnetosphere, enhancing our knowledge of wave-particle interactions and the dynamics of space plasma environments.

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来源期刊
Journal of Geophysical Research: Space Physics
Journal of Geophysical Research: Space Physics Earth and Planetary Sciences-Geophysics
CiteScore
5.30
自引率
35.70%
发文量
570
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