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The VLF fingerprint of elves: Step-like and long-recovery early VLF perturbations caused by powerful ±CG lightning EM pulses

机译:精灵的VLF指纹:由强大的±CG闪电EM脉冲引起的阶梯状且可长期恢复的早期VLF扰动

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Subionospheric VLF recordings are investigated in relation with intense cloud-to-ground (CG) lightning data. Lightning impacts the lower ionosphere via heating and ionization changes which produce VLF signal perturbations known as early VLF events. Typically, early events recover in about 100 s, but a small subclass does not recover for many minutes, known as long-recovery early events (LORE). In this study, we identify LORE as a distinct category of early VLF events, whose signature may occur either on its own or alongside the short-lived typical early VLF event. Since LORE onsets coincide with powerful lightning strokes of either polarity (±), we infer that they are due to long-lasting ionization changes in the uppermost D region ionosphere caused by electromagnetic pulses emitted by strong ±CG lightning peak currents of typically>250 kA, which are also known to generate elves. The LORE perturbations are detected when the discharge is located within ∼250 km from the great circle path (GCP) of a VLF transmitter-receiver link. The probability of occurrence increases with stroke intensity and approaches unity for discharges with peak currents greater than ∼300 kA. LOREs are nighttime phenomena that occur preferentially, at least in the present regional data set, during winter when strong ±CG discharges are more frequent and intense. The evidence suggests LORE as a distinct signature representing the VLF fingerprint of elves, a fact which, although was predicted by theory, it escaped identification in the long-going VLF research of lightning effects in the lower ionosphere.
机译:研究了亚电离层VLF记录与强烈的云对地(CG)闪电数据的关系。闪电通过加热和电离变化影响较低的电离层,这会产生称为早期VLF事件的VLF信号扰动。通常,早期事件会在大约100 s内恢复,但是小的子类不会在很多分钟内恢复,这称为长时间恢复早期事件(LORE)。在本研究中,我们将LORE识别为早期VLF事件的不同类别,其签名可能单独发生,也可能与短暂的典型VLF事件一起发生。由于LORE发作与任一极性(±)的强雷击都相符,因此我们推断,这是由于最上方D区电离层中的持久电离变化所致,这是由通常大于250 kA的强±CG雷电峰值电流发出的电磁脉冲引起的,也被称为会产生精灵。当放电距离VLF收发器链路的大圆路径(GCP)约250公里以内时,就会检测到LORE扰动。发生的可能性随着冲程强度的增加而增加,并且对于峰值电流大于约300 kA的放电,趋近于1。 LORE是夜间现象,至少在当前的区域数据集中,这种现象优先出现在冬季,当冬季出现大量±CG强烈放电时,这种现象更为频繁和强烈。证据表明,LORE是代表精灵VLF指纹的独特特征,这一事实尽管经过理论预测,但在长期进行的电离层下层雷电影响的VLF研究中却没有得到认同。

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