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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Simultaneous Observations of Electromagnetic Ion Cyclotron (EMIC) Waves and Pitch Angle Scattering During a Van Allen Probes Conjunction
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Simultaneous Observations of Electromagnetic Ion Cyclotron (EMIC) Waves and Pitch Angle Scattering During a Van Allen Probes Conjunction

机译:同时观察电磁离子回旋/(EMIC)波和俯视艾伦探头结合期间的俯仰角散射

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On 22 December 2015, the two Van Allen Probes observed two sets of electromagnetic ion cyclotron (EMIC) wave bursts during a close conjunction when both Probe A and Probe B were separated by 0.57 to 0.68 RE. The EMIC waves occurred during an active period in the recovery phase of a coronal mass ejection-driven geomagnetic storm. Both spacecraft observed EMIC wave bursts that had similar spatial structure within a 1-2 min time delay. The EMIC waves occurred outside the plasmasphere, within ΔL ≈ 1-2 of the plasmapause and within a few degrees in magnetic latitude of the equatorial plane. The spatial structure of the EMIC wave bursts may have been related to the proton drift paths outside the plasmasphere and influenced by total magnetic field strength variations associated with solar wind pressure enhancements. The EMIC waves were observed in a narrow L shell region from L ≈ 4.55-5.32 between 10 and 11 magnetic local time (MLT) on the outbound halves of the spacecraft orbits and from L ≈ 4.82-5.51 between 13 and 14 MLT on the inbound halves of the spacecraft orbits. However, Pc1 pulsations were observed on the ground over a broad range of local times. The anisotropy of the proton pitch angle distributions was enhanced when the EMIC waves were observed. Although the overall radiation belt response during this storm was dominated by acceleration and transport processes, the EMIC waves produced local pitch angle scattering of 13-15 keV protons and 2.1-2.6 MeV electrons, consistent with calculations of the expected resonant energies.
机译:在2015年12月22日,当探针A和探针B都分开0.57至0.68 RE时,两组VAN艾伦探针观察到两组电磁离子回转(EMIC)波突发。在冠状大量喷射驱动的地磁风暴的回收阶段的活跃时段期间发生EMIC波。两个航天器观察到在1-2分钟的时间延迟内具有相似的空间结构的EMIC波突发。在PLASMASPARE之外发生的EMIC波,在逆峰的ΔL≈1-2之内,在赤道平面的磁纬度的几度内。 EMIC波突发的空间结构可以与浮子外部外部的质子漂移路径有关,并且受到与太阳风压增强相关的总磁场强度变化的影响。在航天器轨道的出站半部的L≈4.4.55-5.32的窄L壳区域中观察到EMIC波,在入学上的13至14mLt之间的L≈4.82-5.51之间航天器轨道的一半。然而,在地面上观察到PC1脉动在广泛的当地时间。当观察到EMIC波时,增强了质子桨距角分布的各向异性。尽管在该风暴期间的整体辐射带响应是通过加速和运输过程的主导,但是EMIC波产生了13-15keV质子和2.1-2.6meV电子的局部俯仰角散射,与预期共振能量的计算一致。

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