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Magnetospheric ULF wave studies in the frame of Swarm mission: a time-frequency analysis tool for automated detection of pulsations in magnetic and electric field observations

机译:群体任务框架中的磁层超低频波研究:一种时频分析工具,用于自动检测磁场和电场观测中的脉动

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摘要

We combine the advantages of multi-spacecraft and ground-based monitoring of the geospace environment in order to analyze and study magnetospheric ultra low frequency (ULF) waves. In line with this aim, we also develop and deliver relevant analysis tools based on wavelet transforms and tailored to the Swarm mission. In the preparation phase as well as the lifetime of the Swarm mission, the analysis of isolated ULF wave events- especially those detected in the Pc3 frequency range (20-100 mHz) that a topside ionosphere mission efficiently resolves-can help to elucidate the processes that play a crucial role in the generation of waves and their most defining propagation characteristics. Additionally, we offer a useful platform to monitor the wave evolution from the outer boundaries of Earth's magnetosphere through the topside ionosphere down to the surface. Data from a single Low Earth Orbit (LEO) satellite (CHAMP), a multi-satellite LEO mission (ST5) and the ongoing multisatellite magnetospheric mission (Cluster) along with a ground-based magnetic network (CARISMA) are used to demonstrate the potential of our analysis technique in studying wave evolution in detail. A better understanding of the generation and propagation of waves will also allow to geophysically validate some of Swarm's data products, especially those related to the magnetic and electric fields in geospace. With a carefully selected case study focusing on the recovery phase of a moderate magnetic storm (9 April 2006 with a minimum D_(st) value of -82 nT) as a starting point, we clearly demonstrate the capabilities offered by our wavelet analysis tools and highlight the options opened to treat various categories of multipoint multi-instrument measurements (both spaceborne and ground-based) for signatures of ULF wave signals as well as the effects of various other sources.
机译:为了分析和研究磁层超低频(ULF)波,我们将多航天器的优势与对地球空间环境的地面监视相结合。为了实现这一目标,我们还开发并提供了基于小波变换并针对Swarm任务量身定制的相关分析工具。在准备阶段以及Swarm任务的生命周期中,对孤立的ULF波事件(尤其是在顶电离层任务有效解决的Pc3频率范围(20-100 mHz)中检测到的那些事件)的分析有助于阐明这些过程。在波的产生及其最确定的传播特性中起着至关重要的作用。此外,我们提供了一个有用的平台来监视从地球磁层外边界到顶侧电离层再到地表的波的演变。来自单个低地球轨道(LEO)卫星(CHAMP),多卫星LEO任务(ST5)和正在进行的多卫星磁层任务(Cluster)以及地磁网络(CARISMA)的数据被用来证明其潜力详细研究波浪演化的分析技术。更好地了解电波的产生和传播还可以从地理上验证Swarm的某些数据产品,尤其是与地理空间中的磁场和电场有关的数据产品。以精心挑选的案例研究为重点,以中等磁暴的恢复阶段(2006年4月9日,最小D_(st)值为-82 nT)为起点,我们清楚地证明了小波分析工具提供的功能以及突出显示为处理ULF波信号的特征以及各种其他源的影响而处理的各种类型的多点多仪器测量(星载和地面)的选项。

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