磁层冷、热质子等离子体中质子消防水带不稳定性的激发:一种拟线性方法

Muhammad Rashid, Muhammad Sarfraz, Muhammad Ahsan Shahzad, Muhammad Bilal, Aman ur-Rehman
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摘要

太阳风和地球磁层中不同带电物质的不稳定状态受集体和碰撞过程的支配。对于这些稀等离子体,由各向异性粒子分布和热通量驱动的微不稳定性的贡献对于定义电子和离子/质子的稳定/平衡状态变得重要。本文强调了质子消防水带不稳定性在调节这些太阳风和磁层环境中温度各向异性不受控制的上升中的关键作用。右旋圆极化质子消防水带模式在T‖p >T⊥p是满足的,其中方向下标表示相对于周围磁场的方向。基于磁层多尺度(MMS)空间任务的观测,我们假设多组分质子等离子体的模型分布具有双麦克斯韦性质。为了研究不稳定模式的时间演化,我们进一步允许冷、热质子温度的时间变化。对于与观测相关的初始条件的选择,我们揭示了与冷/热质子温度各向异性和质子组分的等离子体β相对应的波性质(生长和不稳定波数域)。在质子火水带不稳定性的反向作用中,我们强调了不同初始冷热温度各向异性和等离子体β选择下初始双麦克斯韦分布的时间尺度变化和饱和以及由此产生的波能密度。
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Excitation of proton firehose instability in magnetospheric cold and hot proton plasma: a quasilinear approach
Unstable states of different charged species in the solar wind and Earth’s magnetosphere are governed with the collective and collisional processes. For these dilute plasmas, the contribution of microinstabilities driven by the anisotropic particle distribution and heat flux becomes important in defining the stable/equilibrium states of electrons and ions/protons. The present paper highlights the key role of proton firehose instability to regulate an unchecked rise in the temperature anisotropy in these solar wind and magnetospheric environments. Right-handed circularly polarized proton firehose mode becomes unstable when the temperature condition of T p > T p is satisfied, where the directional subscripts denote directions with respect to the ambient magnetic field. Based on the observations of magnetospheric multi-scale (MMS) space mission, we assume the bi-Maxwellian nature of the model distribution for the multi-component proton plasma. To study the time evolution of the unstable mode, we further allow the time variation in the cold and hot proton temperatures. For the choice of the initial conditions related with observations, we unveil the wave properties (growth and unstable wave number domain) corresponding to the cold/hot proton temperature anisotropy and the plasma betas of constituents proton components. In the back action of proton firehose instability, we highlight the time-scale modifications and saturation of initial bi-Maxwellian distributions and resulting wave-energy densities for various choices of initial cold-hot temperature anisotropy and plasma betas.
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