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arXiv 2408.08159physics.space-phastro-ph.SRphysics.plasm-ph
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无碰撞激波下游超阿尔文流的形成研究

On the Formation of Super-Alfvénic Flows Downstream of Collisionless Shocks

Adnane Osmane, Savvas Raptis

AI总结:

本研究针对地球弓激波下游超阿尔文射流的形成问题,提出火hose不稳定性涨落与压缩加热的驱动机制,结合流体模型估算与MMS观测数据验证,为磁鞘射流演化的动力学过程研究提供新依据。

摘要:

动能密度显著高于太阳风的超阿尔文射流,在高、低β等离子体条件下均普遍生成于地球弓激波下游。本研究提出理论证据,表明这类动能增强的流动由无碰撞等离子体环境中的firehose(火 hose)不稳定性涨落与压缩加热共同驱动。我们采用纳入压强各向异性的流体形式体系,估算得出无碰撞等离子体激波的下游流动在firehose不稳定性压缩并饱和后,可被加速至原速度的2至4倍。通过分析Magnetospheric Multiscale(磁层多尺度,MMS)任务原位观测到的准平行磁鞘射流,我们发现这些射流中约11%的等离子体测量结果呈现firehose不稳定涨落特征。我们的发现解释了低β(β<1)与高β(β>1)等离子体中快速下游流的独特生成机制,并为动力学过程对准确描述磁鞘射流的形成与演化至关重要提供了新证据。

英文摘要:

Super-Alfvénic jets, with kinetic energy densities significantly exceeding that of the solar wind, are commonly generated downstream of Earth's bow shock under both high and low beta plasma conditions. In this study, we present theoretical evidence that these enhanced kinetic energy flows are driven by firehose-unstable fluctuations and compressive heating within collisionless plasma environments. Using a fluid formalism that incorporates pressure anisotropy, we estimate that the downstream flow of a collisionless plasma shock can be accelerated by a factor of 2 to 4 following the compression and saturation of firehose instability. By analyzing quasi-parallel magnetosheath jets observed in situ by the Magnetospheric Multiscale (MMS) mission, we find that approximately 11\% of plasma measurements within these jets exhibit firehose-unstable fluctuations. Our findings offer an explanation for the distinctive generation of fast downstream flows in both low ($β<1$) and high ($β>1$) beta plasmas, and provide new evidence that kinetic processes are crucial for accurately describing the formation and evolution of magnetosheath jets.

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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