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Different types of whistler mode chorus in the equatorial source region

机译:赤道震源区的不同类型的啸叫模式合唱

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摘要

The Time History of Events and Macroscale Interactions during Substorms-D spacecraft crossed an active equatorial source region of whistler mode chorus rising tones on 23 October 2008. Rising tones are analyzed in terms of spectral and polarization characteristics, with special emphasis on wave normal angles. The latter exhibit large variations from quasi-parallel to oblique, even within single bursts, but seem to follow a definite pattern, which enables an unambiguous classification into five different groups. Furthermore, we discuss the frequently observed splitting of chorus bursts into a lower and an upper band around one half of the local electron cyclotron frequency. At chorus frequencies close to the gap, we find significantly lowered wave planarities and a tendency of wave normal angles to approach the Gendrin angle.
机译:2008年10月23日,亚暴-D航天器的事件和宏尺度相互作用的时间历史越过了惠斯勒合唱的活跃赤道源区域,上升声调。从频谱和极化特性方面分析了上升声调,特别着重于波法向角。后者即使在单个脉冲串内也表现出从准平行到倾斜的巨大变化,但似乎遵循确定的模式,从而可以将其明确分为五个不同的组。此外,我们讨论了经常观察到的合唱爆发分裂为局部电子回旋加速器频率的一半附近的较低和较高的频带。在接近间隙的合唱频率处,我们发现波平面度显着降低,并且波法向角趋近于Gendrin角的趋势。

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