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Global observations of magnetospheric high‐m poloidal waves during the 22 June 2015 magnetic storm

机译:2015年6月22日磁暴期间磁层高m倍体波的全球观测

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摘要

We report global observations of high‐m poloidal waves during the recovery phase of the 22 June 2015 magnetic storm from a constellation of widely spaced satellites of five missions including Magnetospheric Multiscale (MMS), Van Allen Probes, Time History of Events and Macroscale Interactions during Substorm (THEMIS), Cluster, and Geostationary Operational Environmental Satellites (GOES). The combined observations demonstrate the global spatial extent of storm time poloidal waves. MMS observations confirm high azimuthal wave numbers (m ~ 100). Mode identification indicates the waves are associated with the second harmonic of field line resonances. The wave frequencies exhibit a decreasing trend as L increases, distinguishing them from the single‐frequency global poloidal modes normally observed during quiet times. Detailed examination of the instantaneous frequency reveals discrete spatial structures with step‐like frequency changes along L. Each discrete L shell has a steady wave frequency and spans about 1 R E, suggesting that there exist a discrete number of drift‐bounce resonance regions across L shells during storm times.
机译:我们报告了在2015年6月22日磁暴的恢复阶段对高m倍体波的全球观测,这些星座由五个任务的宽间隔卫星组成,这些任务包括磁层多尺度(MMS),范艾伦探测,事件时间历史和宏观相互作用亚暴(THEMIS),星团和地球静止运行环境卫星(GOES)。合并的观测结果表明风暴时间极向波的全球空间范围。 MMS观测结果证实了高的方位波数(m〜100)。模式识别表明,这些波与场线共振的二次谐波相关。随着L的增加,波频率呈现出下降的趋势,这使其与通常在安静时期观察到的单频全局极点模式不同。对瞬时频率的详细检查显示出沿L呈阶梯状频率变化的离散空间结构。每个离散L壳都有一个稳定的波频率,跨度约为1 RE,这表明在L壳上存在离散数量的漂移反弹共振区域在暴风雨时期。

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