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Turbulence and Transport During Guide Field Reconnection at the Magnetopause

机译:湍流和运输期间指导领域在磁重联

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摘要

We analyze the development and influence of turbulence in three-dimensional particle-in-cell simulations of guide field magnetic reconnection at the magnetopause with parameters based on observations from the Magnetospheric Multiscale (MMS) mission. Along the separatrices the turbulence is a variant of the lower-hybrid-drift instability (LHDI) that produces electric field fluctuations with amplitudes much greater than the reconnection electric field. The turbulence controls the scale length of the density and current profiles while enabling significant transport across the magnetopause, despite the electrons remaining frozen-in to the magnetic field. Transport of the out-of-plane current density exceeds that of the particle density. Near the X-line the electrons are not frozen-in and the turbulence, which differs from the LHDI, makes a significant net contribution to the generalized Ohm's law through an anomalous viscosity. The characteristics of the turbulence and associated particle transport are consistent with fluctuation amplitudes in the MMS observations. However, for this event the simulations suggest that the MMS spacecraft were not close enough to the core of the electron diffusion region to identify the region where anomalous viscosity is important.
机译:我们分析的发展和影响力在三维湍流particle-in-cell指导现场的模拟磁重联基于磁层的参数从磁性层的多尺度观测(MMS)的使命。湍流是一个lower-hybrid-drift的变体不稳定(LHDI)产生电场波动振幅大于重新连接的电场。控制的长度密度和规模当前配置文件而使意义重大运输在磁层,尽管电子剩余磁冻结字段。密度超过了粒子的密度。在x轴电子不冻结在附近和动荡,这不同于LHDI,使一个重要的净贡献通过一个异常广义欧姆定律粘度。和相关的粒子运输是一致的在MMS与波动振幅观察。模拟表明,MMS飞船不足够接近的核心电子扩散区域识别的区域反常粘滞性是很重要的。

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