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Criticality Analysis of the Lower Ionosphere Perturbations Prior to the 2016 Kumamoto (Japan) Earthquakes as Based on VLF Electromagnetic Wave Propagation Data Observed at Multiple Stations

机译:基于在多个站点观测到的VLF电磁波传播数据,对2016年熊本(日本)地震之前的下部电离层扰动进行临界分析

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The perturbations of the ionosphere which are observed prior to significant earthquakes (EQs) have long been investigated and could be considered promising for short-term EQ prediction. One way to monitor ionospheric perturbations is by studying VLF/LF electromagnetic wave propagation through the lower ionosphere between specific transmitters and receivers. For this purpose, a network of eight receivers has been deployed throughout Japan which receive subionospheric signals from different transmitters located both in the same and other countries. In this study we analyze, in terms of the recently proposed natural time analysis, the data recorded by the above-mentioned network prior to the catastrophic 2016 Kumamoto fault-type EQs, which were as huge as the former 1995 Kobe EQ. These EQs occurred within a two-day period (14 April: M W = 6.2 and M W = 6.0 , 15 April: M W = 7.0 ) at shallow depths (~10 km), while their epicenters were adjacent. Our results show that lower ionospheric perturbations present critical dynamics from two weeks up to two days before the main shock occurrence. The results are compared to those by the conventional nighttime fluctuation method obtained for the same dataset and exhibit consistency. Finally, the temporal evolutions of criticality in ionospheric parameters and those in the lithosphere as seen from the ULF electromagnetic emissions are discussed in the context of the lithosphere-atmosphere-ionosphere coupling.
机译:在大地震(EQs)之前观测到的电离层扰动已被长期研究,可以被认为对短期EQ预测很有希望。监视电离层扰动的一种方法是研究VLF / LF电磁波在特定发射器和接收器之间通过较低电离层的传播。为此目的,已经在整个日本部署了由八个接收器组成的网络,该网络从位于同一国家和其他国家的不同发射器接收亚电离层信号。在这项研究中,我们根据最近提出的自然时间分析来分析上述网络在灾难性的2016年熊本断层型EQ之前记录的数据,该数据与1995年的神户EQ一样大。这些情商发生在两天的时间内(4月14日:M W = 6.2和M W = 6.0,4月15日:M W = 7.0),深度较浅(〜10 km),而震中是相邻的。我们的结果表明,较低的电离层扰动呈现出从主震发生前两周到两天的关键动态。将结果与通过相同数据集获得的常规夜间波动方法进行比较,并显示出一致性。最后,在岩石圈-大气-电离层耦合的背景下,讨论了从超低频电磁辐射观察到的电离层参数和岩石圈中的临界时间变化。

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