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Whistler propagation in ionospheric density ducts: Simulations and DEMETER observations

机译:电离层密度管道中的吹口哨传播:模拟和DEMETER观测

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[1] On 16 October 2009, the Detection of Electromagnetic Emissions Transmitted from Earthquake Regions (DEMETER) satellite observed VLF whistler wave activity coincident with an ionospheric heating experiment conducted at HAARP. At the same time, density measurements by DEMETER indicate the presence of multiple field-aligned enhancements. Using an electron MHD model, we show that the distribution of VLF power observed by DEMETER is consistent with the propagation of whistlers from the heating region inside the observed density enhancements. We also discuss other interesting features of this event, including coupling of the lower hybrid and whistler modes, whistler trapping in artificial density ducts, and the interference of whistlers waves from two adjacent ducts.
机译:[1] 2009年10月16日,从地震区发射的电磁辐射(DEMETER)卫星观测到VLF哨声波活动与在HAARP进行的电离层加热实验相吻合。同时,通过DEMETER进行的密度测量表明存在多个场对准的增强。使用电子MHD模型,我们显示DEMETER观察到的VLF功率分布与所观察到的密度增强中来自加热区域的啸叫声传播相一致。我们还将讨论此事件的其他有趣特征,包括较低的混合模式和吹口哨模式的耦合,人工密度管道中的吹口哨陷井以及来自两个相邻管道的吹口哨波的干扰。

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