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首页> 外文期刊>Annales Geophysicae >Low-frequency ionospheric sounding with Narrow Bipolar Event lightning radio emissions: regular variabilities and solar-X-ray responses
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Low-frequency ionospheric sounding with Narrow Bipolar Event lightning radio emissions: regular variabilities and solar-X-ray responses

机译:具有窄双极事件闪电无线电发射的低频电离层测深:规则变化和太阳X射线响应

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摘要

We present refinements of a method of ionospheric D-region sounding thatmakes opportunistic use of powerful (109–1011 W) broadbandlightning radio emissions in the low-frequency (LF; 30–300 kHz) band. Suchemissions are from "Narrow Bipolar Event" (NBE) lightning, and they arecharacterized by a narrow (10-μs), simple emission waveform. Thesepulses can be used to perform time-delay reflectometry (or "sounding") ofthe D-region underside, at an effective LF radiated power exceeding byorders-of-magnitude that from man-made sounders. We use this opportunisticsounder to retrieve instantaneous LF ionospheric-reflection height whenevera suitable lightning radio pulse from a located NBE is recorded. We show howto correct for three sources of "regular" variability, namely solar zenithangle, radio-propagation range, and radio-propagation azimuth. The residualmedian magnitude of the noise in reflection height, after applying theregression corrections for the three regular variabilities, is on the orderof 1 km. This noise level allows us to retrieve theD-region-reflector-height variation with solar X-ray flux density forintensity levels at and above an M-1 flare. The instantaneous time responseis limited by the occurrence rate of NBEs, and the noise level in the heightdetermination is typically in the range ±1 km.
机译:我们提出了一种电离层D区域探测方法的改进方法,该方法可以机会性地使用低频(LF; 10; 10; 9 –10 11 W)宽带雷电无线电发射。 30–300 kHz)频段。搜索来自“窄双极事件”(NBE)闪电,其特征是窄(10μs),简单的发射波形。这些脉冲可用于以有效的LF辐射功率执行超过D级区域底面的时延反射法(或“测声”),其有效的LF辐射功率超过了人造发声器的数量级。每当记录到来自定位的NBE的合适的雷电无线电脉冲时,我们就利用这种机会来检索瞬时LF电离层反射高度。我们展示了如何校正“常规”变异性的三个来源,即太阳天顶角,无线电传播范围和无线电传播方位角。在对三个规则变量进行回归校正后,反射高度上的噪声的残留中值约为1 km。此噪声级别使我们能够检索M-1耀斑及其以上强度级别的D区域反射器高度随太阳X射线通量密度的变化。瞬时时间响应受NBE发生率的限制,并且高度测定中的噪声水平通常在±1 km范围内。

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