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Analysis of observations backing up the existence of VLF and ionospheric TEC anomalies before the Mw6.1 earthquake in Greece, January 26, 2014

机译:2014年1月26日希腊Mw6.1地震前支持VLF和电离层TEC异常存在的观测结果分析

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摘要

The present work integrates ground-based ionosphere measurements using very-low-frequency radio transmissions with satellite measurements of the total electron content to draw common conclusions about the possible impact that the Mw6.1 earthquake that took place in Greece on January 26, 2014, had on the ionosphere.\ud\udVery-low-frequency radio signals reveal the existence of an ∼4-day anomaly in the wavelet spectra of the signals received inside the earthquake preparation zone and a significant increase in the normalized variance of the signals prior to the earthquake (approximately 1 day before).\ud\udThrough total electron content analysis, it was possible to identify a clear anomaly from 15:00 until 20:00 UT on the day before the earthquake that appears again on the day of the earthquake between 07:00 UT and 08:00 UT. The anomalous values reach TEC∗Sigma ∼4.36 and 3.11, respectively. Their spatial and temporal distributions give grounds to assume a possible link with the earthquake preparation. The geomagnetic, solar and weather conditions during the considered period are presented and taken into account.\ud\udThis work is an initial and original step towards a multi-parameter approach to the problem of the possible earthquake-related effects on the ionosphere joining observations made from both ground stations and satellites. A well-founded knowledge of these phenomena is clearly necessary before dealing with their application to earthquake prediction purposes.
机译:目前的工作将使用超低频无线电传输的地面电离层测量与总电子含量的卫星测量相结合,以得出关于2014年1月26日在希腊发生的Mw6.1地震可能产生的影响的共同结论, \ ud \ ud非常低频率的无线电信号揭示了地震准备区内接收到的信号的子波频谱中存在约4天的异常,并且信号的归一化方差显着增加。 \ ud \ ud通过总电子含量分析,有可能识别出地震发生前一天的15:00到20:00 UT之间的明显异常,并在该天再次出现。 UT 07:00至UT 08:00之间发生地震。异常值分别达到TEC * Sigma〜4.36和3.11。它们的时空分布为与地震准备工作可能建立联系提供了基础。介绍并考虑了所考虑时期内的地磁,太阳和天气状况。\ ud \ ud这项工作是朝着多参数方法进行的初步和原始步骤,以解决可能对电离层结合观测产生地震相关影响的问题由地面站和卫星组成。在将这些现象应用于地震预测目的之前,显然有必要充分了解这些现象。

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