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Advances in Inner Magnetosphere Passive and Active Wave Research

机译:磁层内部被动和主动波研究的进展

摘要

This review identifies a number of the principal research advancements that have occurred over the last five years in the study of electromagnetic (EM) waves in the Earth's inner magnetosphere. The observations used in this study are from the plasma wave instruments and radio sounders on Cluster, IMAGE, Geotail, Wind, Polar, Interball, and others. The data from passive plasma wave instruments have led to a number of advances such as: determining the origin and importance of whistler mode waves in the plasmasphere, discovery of the source of kilometric continuum radiation, mapping AKR source regions with "pinpoint" accuracy, and correlating the AKR source location with dipole tilt angle. Active magnetospheric wave experiments have shown that long range ducted and direct echoes can be used to obtain the density distribution of electrons in the polar cap and along plasmaspheric field lines, providing key information on plasmaspheric filling rates and polar cap outflows.
机译:这篇综述指出了过去五年来在地球内部磁层中电磁(EM)波研究中发生的许多主要研究进展。本研究中使用的观测值来自等离子波仪器和Cluster,IMAGE,Geotail,Wind,Polar,Interball等上的无线电测深仪。来自无源等离子体波仪器的数据带来了许多进步,例如:确定等离子层中惠斯勒模式波的起源和重要性,发现连续公里辐射源,以“精确”精度绘制AKR源区域,以及将AKR源位置与偶极子倾斜角相关联。活跃的磁层波实验表明,可以使用长距离的管道和直接回波来获得极帽中以及沿等离子层磁力线的电子密度分布,从而提供有关等离子层填充率和极帽流出的关键信息。

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