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arXiv 2604.02452physics.space-phastro-ph.EPastro-ph.SRphysics.geo-phphysics.plasm-ph
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行星际激波处质子温度各向异性:基于WIND观测的统计分析

Proton Temperature Anisotropy Across Interplanetary Shocks: A Statistical Analysis with WIND observations

University of Alabama in Huntsville(亨茨维尔阿拉巴马大学);Center for Space Plasma and Aeronomic Research (CSPAR)(空间等离子体与天文研究中心)

Zeping Jin, Lingling Zhao, Xingyu Zhu, Vladimir Flosinski, Gary P. Zank, Jakobus Le Roux, Yiming Jiao, Ashok Silwal, Nibuna S. M. Subashchandar

AI总结:

研究行星际激波对质子温度各向异性的影响,通过统计分析发现激波几何、压缩和距离影响各向异性,揭示非绝热过程的重要性及不稳定性调节机制。

摘要:

行星际(IP)激波有效地改变了太阳风中的质子温度各向异性。分析约800个由Wind航天器观测的IP激波(1997-2024年),我们对上游和下游质子温度各向异性及其对激波几何、压缩和距离的依赖性进行了统计研究。我们发现(1)近垂直激波导致下游垂直温度显著增强(Tperp > Tpara),而平行激波由于通常更强的上游Tpara保持近各向同性;(2)与Chew-Goldberger-Low(CGL)双绝热模型的比较揭示了几何依赖的偏差。CGL在近垂直激波中高估了下游垂直加热和低估了平行加热,而在近平行激波中趋势相反,突显了非绝热过程的重要性;(3)激波驱动的各向异性强烈集中在激波附近,并逐渐向典型太阳风条件放松,随着激波影响的减弱;(4)下游各向异性受动能不稳定性调节,近垂直激波受质子旋磁不稳定性限制,近平行激波受平行火线不稳定性限制。这些结果表明,行星际激波处温度各向异性的演变受激波几何、局部过程和不稳定性驱动调节控制。

英文摘要:

Interplanetary (IP) shocks efficiently modify the proton temperature anisotropy of the solar wind. Analyzing ~800 IP shocks observed by the Wind spacecraft from 1997-2024, we present a statistical study of upstream and downstream proton temperature anisotropy and its dependence on shock geometry, compression, and distance from the shock. We find that (1) quasi-perpendicular shocks produce a pronounced enhancement of perpendicular temperature downstream (Tperp > Tpara), whereas parallel shocks remain near isotropic downstream due to typically stronger upstream Tpara; (2) comparisons with the Chew-Goldberger-Low (CGL) double-adiabatic model reveal geometry-dependent deviations. CGL overestimates downstream perpendicular heating and underestimates parallel heating at quasi-perpendicular shocks, with the opposite trend at quasi-parallel shocks, highlighting the importance of non-adiabatic processes beyond simple compression; (3) Shock-driven anisotropy is strongly localized near the shock and gradually relaxes toward typical solar wind conditions farther downstream as the shock's influence diminishes; and (4) downstream anisotropy is regulated by kinetic instabilities, with quasi-perpendicular shocks constrained by proton cyclotron and mirror instabilities and quasi-parallel shocks limited by the parallel firehose instability. Together, these results show that the evolution of temperature anisotropy at interplanetary shocks is controlled by shock geometry, localized processes, and instability driven regulation.

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