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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Storm Time EMICWaves Observed by Swarm and Van Allen Probe Satellites
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Storm Time EMICWaves Observed by Swarm and Van Allen Probe Satellites

机译:Swarm和Van Allen Probe卫星观察的风暴时间Emicwaves

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摘要

The temporal and spatial evolution of electromagnetic ion cyclotron (EMIC) waves during the magnetic storm of 21-29 June 2015 was investigated using high-resolution magnetic field observations from Swarm constellation in the ionosphere and Van Allen Probes in the magnetosphere. Magnetospheric EMIC waves had a maximum occurrence frequency in the afternoon sector and shifted equatorward during the expansion phase and poleward during the recovery phase. However, ionospheric waves in subauroral regions occurred more frequently in the nighttime than during the day and exhibited less obvious latitudinal movements. During the main phase, dayside EMIC waves occurred in both the ionosphere and magnetosphere in response to the dramatic increase in the solar wind dynamic pressure.Waves were absent in the magnetosphere and ionosphere around the minimum SYM-H. During the early recovery phase, He+ band EMIC waves were observed in the ionosphere and magnetosphere. During the late recovery phase, H+ band EMIC waves emerged in response to enhanced earthward convection during substorms in the premidnight sector. The occurrence of EMIC waves in the noon sector was affected by the intensity of substorm activity. Both ionospheric wave frequency and power were higher in the summer hemisphere than in the winter hemisphere.Waves were confined to an MLT interval of less than 5 hr with a duration of less than 186 min from coordinated observations. The results could provide additional insights into the spatial characteristics and propagation features of EMIC waves during storm periods.
机译:使用来自磁层中的电离层和范例探针在磁性层中的群体和范例探针中的高分辨率磁场观测,研究了2015年6月21日至二二○○五年六月六○○五年六月二十一六月磁场期间的电磁离子回旋/(EMIC)波的时间和空间展现。磁气层的EMIC波在午后扇区中具有最大的发生频率,并且在膨胀阶段期间在膨胀阶段和极向上移动逆转。然而,在夜间发生的亚前地区的电离层波比白天比白天更频繁地发生,并且呈现不太明显的纬度运动。在主阶段期间,在电离层和磁性层中发生杜莎内酯,响应于太阳风电感压力的显着增加。在磁性层和电离层中不存在围绕最小Sym-h的电离。在早期回收阶段,在电离层和磁层中观察到HE +带EMIC波。在后期回收阶段,H +带EMIC波的响应于Premidnight扇区中的代甲在重量流对流中出现。中午行业的铸锭波的发生受到物质活性强度的影响。夏季半球的电离层波频率和功率均高于冬季半球.波,从协调观察中持续时间小于186分钟的持续时间超过5小时的MLT间隔。结果可以在风暴期间提供进入EMIC波的空间特征和传播特征的额外见解。

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  • 作者单位

    Department of Space Physics School of Electronic Information Wuhan University Hubei China;

    Department of Space Physics School of Electronic Information Wuhan University Hubei China;

    GFZ German Research Center for Geosciences Potsdam Germany;

    Department of Physics and Space Science Center (EOS) University of New Hampshire Durham NH USA;

    Department of Physics and Space Science Center (EOS) University of New Hampshire Durham NH USA;

    Department of Physics and Space Science Center (EOS) University of New Hampshire Durham NH USA;

    Department of Space Physics School of Electronic Information Wuhan University Hubei China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 空间物理;
  • 关键词

    Storm; Time EMIC Waves; Observed;

    机译:风暴;时间emiC波;观察到;

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