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Localization of auroral Langmuir turbulence in thin layers

机译:本地化的极光朗缪尔动荡薄层

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The recently discovered coherent echoes in the Poker Flat Incoherent Scatter Radar data with flat ion-line spectrum and simultaneous double-peaked plasma-line spectrum in the lower ionospheric F region are investigated in greater detail. High-range resolution measurements reveal that the turbulence is sometimes manifested as two concurrent layers separated by about 50 km. The turbulence layers appear at regions of zero electron density gradient, supporting the interpretation that propagation effects play an important role in limiting the waves' amplitude. Although Langmuir intensity is limited by propagation effects outside of the layers, it reaches to nonlinear regime inside the layers, giving rise to the observed range and spectral morphologies. Furthermore, the radar measurements of the electrostatic waves appear to be correlated in space and time with natural auroral electromagnetic emissions, supporting the previous theory that "MF-bursts" are produced by linear conversion of Langmuir waves produced by soft electron precipitation (~few hundred electronvolts) on the topside F region. The results presented in this report suggest that the observed Langmuir turbulence and MF-burst are both manifestations of the same process. Key Points Langmuir turbulence and MF-burst are both manifestations of the same process. Convective saturation play a role in saturating the Langmuir intensity.
机译:最近发现的回声扑克平非相干散射雷达数据平的输电线路频谱和同步双峰plasma-line光谱的低电离层F区大调查细节。湍流是有时表现为两个并发层分离约50公里。湍流层出现在地区的零电子密度梯度,支持解释,传播效果发挥重要的限制作用波的振幅。虽然朗缪尔强度是有限的传播效果以外的层,它达到非线性政权内部的层,导致观察到的范围和光谱形态。静电的似乎与自然极光在时间和空间上的相关性电磁排放,支持先前的理论,是由“MF-bursts”朗缪尔的线性转换波产生的软电子降水(~几百electronvolts)上部F。结果表明,提出报告观察到朗缪尔动荡和MF-burst两个的表现相同的过程。朗缪尔动荡和MF-burst都点表现的过程。饱和饱和的朗缪尔扮演一个角色强度。

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