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Attenuation of electromagnetic waves at the frequency ~1.7 kHz in the upper ionosphere observed by the DEMETER satellite in the vicinity of earthquakes

机译:地震附近观察到的凹痕卫星的上电离层频率〜1.7kHz的电磁波衰减

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摘要

>The DEMETER satellite was the first satellite specifically dedicated to the recording of electromagnetic phenomena connected with seismic activity. Almost 6.5 years of measurements provide good opportunities to analyze a unique dataset with global Earth coverage. We present the results of a statistical study of the intensity of very low frequency electromagnetic waves recorded in the upper ionosphere. Robust two-step data processing has been used. The expected unperturbed distribution of the power spectral densities of electromagnetic emissions was calculated first. Then, the power spectral densities measured in the vicinities of earthquakes are compared with the unperturbed distribution and are examined for the presence of uncommon effects related to seismic activity. The statistical significance of the observed effects is evaluated. We confirm the previously reported results of a very small, but statistically significant, decrease in wave intensities a few hours before times of main shocks using this much larger dataset. The wave intensity decrease at a frequency of about 1.7 kHz is observed only during the night and only for shallow earthquakes. This can potentially be explained by increases in the cut-off frequency of the Earth ionosphere waveguide caused by imminent earthquakes.>
机译:<! - @page {大小:21cm 29.7cm;边缘:2cm} p {边缘底:0.21cm} - > > Demeter卫星是专门用于记录与地震活动相关的电磁现象的第一卫星。近60年的测量提供了分析全球地球覆盖范围的独特数据集的良好机会。我们介绍了在上电离层中记录的非常低频电磁波强度的统计研究结果。已经使用了强大的两步数据处理。首先计算电磁排放功率谱密度的预期不受干扰的分布。然后,将在地震附近测量的功率谱密度与未受带的分布进行比较,并检查是否存在与地震活动相关的罕见效果。评估了观察到的效果的统计学意义。我们确认先前报告的结果非常小,但统计上显着,在主要冲击前几个小时使用这款更大的数据集之前几个小时的波浪强度降低。在夜间仅观察到频率约为1.7kHz的波强度降低,仅用于浅地震。这可以通过迫在眉睫的地震引起的地球电离层波导的截止频率的增加来解释。 >

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