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arXiv 2408.09003physics.plasm-phphysics.space-ph
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火星前兆超低频波:对火星弓激波粒子加速机制的影响

Foreshock Ultra-Low Frequency Waves at Mars: Consequence on the Particle Acceleration Mechanisms at the Martian Bow Shock

Nahuel Andrés, Norberto Romanelli, Christian Mazelle, Li-Jen Chen, Jacob R. Gruesbeck, Jared R. Espley

AI总结:

本研究基于MAVEN磁强计观测,首次统计分析了火星前兆区超低频波,发现其特征与快磁声波一致,推测由离子-离子右旋共振不稳定性产生,并揭示了行星弓激波中可能存在共同的粒子加速过程。

摘要:

利用火星大气与挥发物演化磁强计的观测数据,我们报告了首个关于火星前兆区超低频(ULF)波的统计研究。所分析的前兆ULF波事件在0.008-0.086 Hz频率范围内被观测到,在航天器参考系中呈现近圆形和椭圆形的左旋极化。这些波沿准平行于环境磁场的方向传播,具有中等波幅。所有这些性质与快磁声波一致,极有可能是通过离子-离子右旋共振不稳定性产生的。此外,我们的结果表明,在太阳风参考系中,相关的共振逆流质子平行于平均磁场的速度是太阳风速度的1.33 ± 0.40倍。我们的结果与其他前兆区的先前报告之间的相似性可能表明,在行星弓激波中存在一种共同的加速过程,并负责这种特定的逆流粒子群。

英文摘要:

Using Mars Atmosphere and Volatile EvolutioN Magnetometer observations, we report the first statistical study of ultra-low frequency (ULF) waves at the Martian foreshock. The analyzed foreshock ULF wave events are observed in the 0.008-0.086 Hz frequency range, with nearly circular and elliptical left-handed polarization in the spacecraft reference frame. These waves are propagated quasi-parallel to the ambient magnetic field, with a moderate wave amplitude. All these properties are consistent with fast magnetosonic waves, most likely generated through the ion-ion right-hand resonant instability. In addition, our results suggest that the associated resonant backstreaming protons' velocities parallel to the mean magnetic field in the solar wind reference frame is $1.33 \pm 0.40$ times the solar wind velocity. The similarity between our results and previous reports at other foreshocks may indicate the presence of a common acceleration process acting in planetary bow shocks and that is responsible for this particular backstreaming population.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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