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Comprehensive survey of Pc4 and Pc5 band spectral content in Cluster magnetic field data

机译:团簇磁场数据中Pc4和Pc5谱带含量的综合调查

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摘要

In the first part of this study we present two case studies of pulsations that, with the help of ground-based data, are identified as field line resonances (FLRs). These pulsations occurred at frequencies which belong to a set of frequencies that has been suggested to be preferred in the terrestrial magnetosphere (CMS frequencies). We go on to show that for both events there is a significant signature at the same frequency in the time series of the compressional magnetic field observed by the conjugate Cluster satellites. We interpret these as signatures of the compressional mode driving the FLRs. In the second part we present a statistical study including one year's worth of Cluster magnetic field data. For each orbit between May 2004 and June 2005 we identified a three hour interval during which the satellites were located on closed magnetic field lines. We identified peaks in the spectrum between 1.0 and 15.0 mHz of the compressional, poloidal and toroidal components of the magnetic field. We use this database of spectral peaks observed on closed magnetic field lines to investigate whether peaks occur at a preferred set of frequencies which would be indicative for the Earth's magnetosphere behaving like a cavity/waveguide. We find no consistent preference for all CMS frequencies in our dataset, however we do find a preference for certain higher frequencies suggesting that higher harmonics of the cavity/waveguide are a persistent feature of the inner magnetosphere, and are detected by the Cluster spacecraft. This result could be explained by the polar orbit of the Cluster satellites.
机译:在本研究的第一部分中,我们介绍了两个关于脉动的案例研究,借助地面数据,这些案例被确定为场线共振(FLR)。这些脉动发生在属于一组频率的频率上,该频率已被建议在陆地磁层中是首选的(CMS频率)。我们继续表明,对于这两个事件,在共轭簇状卫星观测到的压缩磁场的时间序列中,在相同频率下都具有显着特征。我们将这些解释为驱动FLR的压缩模式的特征。在第二部分中,我们进行了一项统计研究,其中包括一年的簇磁场数据。对于2004年5月至2005年6月之间的每个轨道,我们确定了三个小时的间隔,在此间隔中,卫星位于封闭的磁力线上。我们确定了在磁场的压缩,极化和环形分量的1.0到15.0 mHz之间的频谱峰值。我们使用在闭合磁场线上观察到的频谱峰值数据库来研究峰值是否出现在一组首选频率上,这些频率将指示地球磁层的行为类似于腔体/波导。我们在数据集中找不到所有CMS频率的一致偏好,但是确实发现了对某些更高频率的偏好,这表明腔体/波导的高次谐波是内部磁层的持久特征,并且被星团航天器检测到。这一结果可以用星团卫星的极轨道来解释。

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  • 年度 2009
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  • 正文语种 {"code":"en","name":"English","id":9}
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