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首页> 外文期刊>Annales Geophysicae >ULF wave activity during the 2003 Halloween superstorm: multipoint observations from CHAMP, Cluster and Geotail missions
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ULF wave activity during the 2003 Halloween superstorm: multipoint observations from CHAMP, Cluster and Geotail missions

机译:2003年万圣节超级风暴期间的ULF波活动:来自CHAMP,Cluster和Geotail任务的多点观测

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摘要

We examine data from a topside ionosphere and two magnetospheric missions (CHAMP, Cluster and Geotail) for signatures of ultra low frequency (ULF) waves during the exceptional 2003 Halloween geospace magnetic storm, when Dst reached ~-380 nT. We use a suite of wavelet-based algorithms, which are a subset of a tool that is being developed for the analysis of multi-instrument multi-satellite and ground-based observations to identify ULF waves and investigate their properties. Starting from the region of topside ionosphere, we first present three clear and strong signatures of Pc3 ULF wave activity (frequency 15-100mHz) in CHAMP tracks. We then expand these three time intervals for purposes of comparison between CHAMP, Cluster and Geotail Pc3 observations but also to be able to search for Pc4-5 wave signatures (frequency 1-10 mHz) into Cluster and Geotail measurements in order to have a more complete picture of the ULF wave occurrence during the storm. Due to the fast motion through field lines in a low Earth orbit (LEO) we are able to reliably detect Pc3 (but not Pc4-5) waves from CHAMP. This is the first time, to our knowledge, that ULF wave observations from a topside ionosphere mission are compared to ULF wave observations from magnetospheric missions. Our study provides evidence for the occurrence of a number of prominent ULF wave events in the Pc3 and Pc4-5 bands during the storm and offers a platform to study the wave evolution from high altitudes to LEO. The ULF wave analysis methods presented here can be applied to observations from the upcoming Swarm multi-satellite mission of ESA, which is anticipated to enable joint studies with the Cluster mission.
机译:我们检查了顶空电离层和两个磁层探测任务(CHAMP,Cluster和Geotail)的数据,这些数据是在异常的2003年万圣节万圣节空间磁暴中,当Dst达到〜-380 nT时超低频(ULF)波的特征。我们使用一套基于小波的算法,这是一种工具的子集,该工具正在开发中,用于分析多仪器多卫星和地面观测,以识别ULF波并研究其特性。从顶部电离层区域开始,我们首先呈现CHAMP轨道中Pc3 ULF波活动(频率15-100mHz)的三个清晰而有力的特征。然后,我们扩展这三个时间间隔,以便在CHAMP,簇和Geotail Pc3观测值之间进行比较,还能够搜索簇和Geotail测量中的Pc4-5波特征(频率1-10 mHz),以便获得更多暴风雨期间发生ULF波的完整图片。由于在低地球轨道(LEO)中通过磁力线的快速运动,我们能够可靠地检测到来自CHAMP的Pc3(而非Pc4-5)波。据我们所知,这是第一次将来自顶空电离层飞行任务的ULF波观测与来自磁层飞行任务的ULF波观测进行比较。我们的研究为暴风雨期间Pc3和Pc4-5波段发生了许多重要的ULF波事件提供了证据,并为研究从高海拔到LEO的波演变提供了一个平台。此处介绍的ULF波浪分析方法可以应用于即将到来的欧空局Swarm多卫星任务的观测,该任务有望与星团任务进行联合研究。

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  • 来源
    《Annales Geophysicae》 |2012年第12期|1751-1768|共18页
  • 作者单位

    Institute for Astronomy, Astrophysics, Space Applications and Remote Sensing, National Observatory of Athens, Greece;

    Institute for Astronomy, Astrophysics, Space Applications and Remote Sensing, National Observatory of Athens, Greece;

    RVBXP, Air Force Research Laboratory, Hanscom AFB, MA, USA;

    Institute for Astronomy, Astrophysics, Space Applications and Remote Sensing, National Observatory of Athens, Greece,Section of Astrophysics, Astronomy and Mechanics, Department of Physics, University of Athens, Greece;

    Institute for Astronomy, Astrophysics, Space Applications and Remote Sensing, National Observatory of Athens, Greece,Section of Astrophysics, Astronomy and Mechanics, Department of Physics, University of Athens, Greece;

    European Space Research and Technology Centre, European Space Agency, Noordwijk, The Netherlands;

    Section of Astrophysics, Astronomy and Mechanics, Department of Physics, University of Athens, Greece;

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  • 正文语种 eng
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  • 关键词

    magnetospheric physics (magnetospheric configuration and dynamics; plasma waves and instabilities; storms and substorms);

    机译:磁层物理学(磁层构造和动力学;等离子波和不稳定性;风暴和亚暴);

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