九仙山自然雷击负地闪脉冲中长程传播观测

Observations on Medium-to-long Distance Propagation of Pulses from Natural Negative Cloud-to-ground Strokes at the Jiuxian Mountain

  • 摘要: 以2024年4月4日中国气象局雷电野外科学试验基地——福建九仙山自然闪电观测试验基地的雷击高塔事件为研究对象, 基于混合长基线天电阵列同步观测的31次回击闪电低频/甚低频电磁波信号, 分析200~800 km传播范围内电磁波脉冲幅值衰减特征。采用等距离闪电事件对比法标定各探测子站的相对场地增益, 结合不同传播距离的电磁波脉冲幅值校正结果, 拟合得到负地闪回击的传播衰减曲线。结果表明:负地闪回击电磁波脉冲幅值随传播距离呈显著幂函数衰减关系, 衰减指数为1.10~1.20, 31次负地闪回击的平均衰减指数为1.16, 且所有拟合优度均在0.98以上。在闪电放电强度反演中采用平均衰减指数(1.16)进行传播衰减校正, 可有效降低因忽略传播效应导致的系统性误差, 显著提升反演精度与结果可靠性, 并为理解自然闪电电磁脉冲的中长距离(200~800 km)传播机制提供关键实测数据支撑。

     

    Abstract: Attenuation characteristics of lightning electromagnetic waves during propagation are critical physical processes that affect the performance and accuracy of lightning detection systems. To improve the precision of lightning current inversion and enhance the reliability of lightning detection networks, the attenuation behavior of such pulses over medium-to-long propagation distances needs to be systematically characterized and quantitatively described. The study focuses on natural lightning events recorded on 4 April 2024, at the Jiuxian Mountain Observation Base in Fujian, China. Utilizng Hybrid Lightning Sferic Array, analysis is conducted on 31 negative cloud-to-ground return strokes observed synchronously over distances ranging from 200 km to 800 km, with particular emphasis on the amplitude attenuation characteristics of their low-frequency/very low-frequency (LF/VLF) electromagnetic pulses. To ensure the reliability of analysis, the equal-distance lightning event comparison method is employed to calibrate the relative station gains of seven selected observation sub-stations. This approach effectively eliminates instrumental biases, ensuring that the observed amplitude differences primarily reflect genuine propagation path effects. Based on the calibrated amplitudes, statistical fitting is performed to derive the propagation attenuation curves for these return strokes. Results indicate a significant power-law attenuation relationship between the amplitude of return stroke electromagnetic pulses and the propagation distance. The attenuation exponent for individual return strokes ranges from 1.10 to 1.20, with an average value of 1.16 for all 31 events. The goodness-of-fit for all curves exceeds 0.98, confirming the high reliability of this relationship. Furthermore, a detailed analysis is conducted on underestimation ratios in current inversion under different assumptions regarding the attenuation exponent. Results show that, even after distance-based attenuation correction, uncertainties in the attenuation exponent introduce additional errors into the inversion outcomes. Specifically, the underestimation of current varies systematically with both propagation distance and the chosen attenuation exponent, underscoring the importance of accurately characterizing attenuation characteristics for reliable estimation of lightning intensity. These findings hold significant implications for operational lightning detection networks, as inappropriate attenuation correction may lead to systematic biases in reported lightning peak currents. This investigation provides crucial observations for understanding the propagation mechanisms of lightning electromagnetic pulses in 200-800 km range. Results suggest that applying the average attenuation exponent of 1.16 for propagation correction can effectively reduce systematic errors induced by neglecting ground conductivity effects. This approach significantly enhances the accuracy and reliability of lightning discharge intensity inversion and offers valuable references for the calibration and data interpretation of operational lightning location networks.

     

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