空气离子密度异常与地震和相关的电离层前兆扰动的可能关系:从临界性角度的分析

M. Hayakawa, S. Potirakis, Y. Saito
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引用次数: 2

摘要

对2013年2月10日至2016年4月30日(3年多)在仙台观测到的空气离子密度进行了自然时间临界分析。然后发现空气离子在某些特定时期表现出临界状态,作为岩石圈震前破裂过程的标志。因此,很可能得出这样的结论:这种临界性分析使我们能够将离子密度的临界性与EQ作为一般趋势联系起来。在一个特定地点检测到的空气离子表明,这些离子可能是发生在距离离子观测站200公里半径范围内的EQ(大于5.0级)的前兆。然而,根据与相应的VLF/LF亚电离层传播数据的比较,我们不能说这些空气离子与VLF/LF所看到的较低电离层扰动有一定的关系,因为离子的时间尺度是中期的,而VLF/LF扰动是短期的,这使得两者之间的关联非常困难。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Possible relation of air ion density anomalies with earthquakes and the associated precursory ionospheric perturbations: An analysis in terms of criticality
The air ion density observed at Sendai during a period of 10/02/2013 to 30/04/2016 (more than 3 years) has been analyzed in terms of natural time critical analysis. It is then found that the air ions exhibit criticalities at some specific time periods, as a signature of pre-earthquake (EQ) fracturing process in the lithosphere. So it is likely to conclude that this criticality analysis enables us to associate the criticality in ion density to an EQ as a general tendency. The detection of air ions at a particular place suggests that those ions may be a precursor to an EQ (magnitude greater than 5.0) occurring within a radius of 200 km from the ion observatory. However, based on a comparison with the corresponding VLF/LF sub-ionospheric propagation data, we cannot say anything about a certain relationship of those air ions with the lower ionospheric perturbation as seen by VLF/LF, because the temporal scale of ions is medium-termed, but VLF/LF perturbation is short-termed, which makes it extremely difficult to correlate between the two.
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