首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Two-dimensional hybrid simulations of quasi-perpendicular collisionless shock dynamics: Gyrating downstream ion distributions
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Two-dimensional hybrid simulations of quasi-perpendicular collisionless shock dynamics: Gyrating downstream ion distributions

机译:二维混合模拟quasi-perpendicular无碰撞的冲击动力学:旋转下游离子分布

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摘要

Quasi-perpendicular collisionless shocks undergo structural changes with the increase of the Mach number. These changes are related to the increasing role of the reflected ions, which have a highly nongyrotropic distribution. Eventually, it is expected that the shock front becomes nonstationary. At low and moderate Mach numbers, the fraction of reflected ions is small, yet recent observations show the existence of a well-pronounced structure of the postshock magnetic field in the close vicinity of the transition layer. Large amplitude oscillations were earlier interpreted as waves generated by the shock front or passing through the shock in the downstream direction. Here we show, using two-dimensional hybrid simulations of quasi-perpendicular shocks, that the gyration of the directly transmitted ions downstream of the ramp produces the spatial pressure variations, which are accompanied with the observed magnetic oscillations due to the momentum conservation. In a wide range of the upstream ion temperatures, the low and moderate-Mach-number shocks remain stationary and one-dimensional, so that the magnetic and electric field depend only on the coordinate along the shock normal. The downstream ion distributions gradually gyrotropize due to the collisionless mixing of gyrophases. Nonstationary effects in these shocks do not affect noticeably the ion dynamics. However, we find that with the increase of the Mach number, shocks form rippled fronts in the low-β and moderate-β regimes. Key Points Gyration of transmitted ions downstream the shock produces pressure variationsDownstream ion distributions gyrotropize due to collisionless gyrophase mixingIncreased Mach number shock with low- and moderate-beta form rippled fronts
机译:Quasi-perpendicular无碰撞的冲击进行结构变化与马赫数的增加号码。反映离子扮演的角色越来越重要,一个高度nongyrotropic分布。预计,激震前沿不稳定。反映离子的比例很小最近的观察显示的存在well-pronounced postshock的结构磁场接近附近的过渡层。早些时候被解释为波产生的吗激震前沿或穿过的冲击下游方向。二维混合模拟quasi-perpendicular冲击的回转直接传播离子的下游斜坡产生空间压力变化,哪些是伴随着观测到磁振荡由于动量守恒。广泛的上游离子温度,低和moderate-Mach-number冲击依然存在固定和一维,这样磁场和电场只依靠沿着冲击正常的协调。离子分布逐渐gyrotropize由于gyrophases的无碰撞的混合。在这些冲击不不稳定影响影响离子动力学明显。发现与马赫数的增加,危机波及方面低-β和形式中度-β政权。离子传输下游冲击产生压力variationsDownstream离子分布由于无碰撞的gyrotropize gyrophasemixingIncreased马赫数与低收入和冲击波及moderate-beta形式方面

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