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Foreshock bubbles and their global magnetospheric impacts

机译:前震泡沫和全球磁性层的影响

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We employ 2.5-D electromagnetic, hybrid simulations that treat ions kinetically via particle-in-cell methods and electrons as a massless fluid to study the formation and properties of a new structure named the foreshock bubble upstream from the bow shock. This structure forms due to changes in the interplanetary magnetic field (IMF) associated with solar wind discontinuities and their interaction with the backstreaming ions in the foreshock prior to these discontinuities encountering the bow shock. The leading edge of the foreshock bubble consists of a fast magnetosonic shock and the compressed and heated plasma downstream of the shock. The leading edge surrounds the core which consists of a less-dense and hotter plasma and lower magnetic field strength. Ultra low frequency turbulence is present in both the outer and core regions of the foreshock bubbles. The size of the foreshock bubble transverse to the flow direction scales with the width of the ion foreshock and at Earth corresponds to tens of RE. The size along the flow depends on the age of the bubble and grows with time. Although they expand sunward, foreshock bubbles are carried antisunward by the solar wind, and for small IMF cone angles (angle between IMF and solar wind flow) when the foreshock lies upstream of the dayside magnetosphere they collide with the bow shock. This collision is shown to have significant magnetospheric impacts. Upon encountering the bow shock, the low pressures within the core of the bubble result in the reversal of the magnetosheath flow from antisunward to sunward direction. This in turn results in the outward motion of the magnetopause and expansion of the dayside magnetosphere. The interaction is found to noticeably impact the density and energy of trapped radiation belt ions and plasma injection into the cusp. Foreshock bubbles are found to be highly effective sites for ion reflection and acceleration to high energies via first- and second-order Fermi acceleration. The interaction of the foreshock bubble with the bow shock results in the release of energetic ions into the magnetosheath. Some of these ions are subsequently injected into the cusp.
机译:我们采用2.5 - d电磁,混合动力车活动通过模拟治疗离子作为一个particle-in-cell方法和电子无质量的流体形成和学习一个新结构命名为“前震的属性泡沫从弓形激波上游。结构形式的变化行星际磁场(IMF)相关联太阳风不连续和他们交互的逆流离子前震前这些不连续遇到弓形激波。前震泡沫由一个快magnetosonic冲击和压缩和加热等离子体下游的冲击。围绕的核心由密度较低热等离子体和低磁场的力量。同时呈现在外层和核心区域的前震泡沫。泡沫横向尺度流动方向与离子前震的宽度和在地球对应的再保险的大小流量取决于泡沫的年龄和生长随着时间的推移。前震泡沫antisunward携带的太阳风,和国际货币基金组织对小锥角(角国际货币基金组织(IMF)和太阳风流动)之间前震谎言的光面的上游磁气圈碰撞弓形激波。显示了这种冲突明显磁性层的影响。休克、低压力的核心泡沫导致的反转磁鞘流antisunward朝着太阳方向。运动的磁层和扩张的光面磁场。的密度和能量明显影响困辐射带离子和等离子体注入尖端。高效离子反射和网站加速通过一线和高能量二阶费米加速。与弓形激波前震的泡沫导致能量的释放离子进入磁鞘。随后注入到尖端。

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