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Statistical Study on Variations of the Ionospheric Ion Density Observed by DEMETER and Related to Seismic Activities

机译:侦测观察到的电离层离子密度的变化和地震活动相关的统计研究

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In this paper, we present the result of a statistical study performed on the ionospheric ion density variations above areas of seismic activity. The ion density was observed by the low altitude satellite DEMETER between 2004 and 2010. In the statistical analysis a superposed epoch method is used where the observed ionospheric ion density close to the epicenters both in space and in time is compared to background values recorded at the same location and in the same conditions. Data associated with aftershocks have been carefully removed from the database to prevent spurious effects on the statistics. It is shown that, during nighttime, anomalous ionospheric perturbations related to earthquakes with magnitudes larger than 5 are evidenced. At the time of these perturbations the background ion fluctuation departs from a normal distribution. They occur up to 200 km from the epicenters and mainly 5 days before the earthquakes. As expected, an ion density perturbation occurring just after the earthquakes and close to the epicenters is also evidenced.
机译:在本文中,我们介绍了对高于地震活动区域的电离层离子密度变化进行的统计研究的结果。由2004和2010之间的低空卫星侦探观察到离子密度。在统计分析中,使用叠加的时期方法,其中观察到靠近空间和时间内的震中的电离层离子密度与记录的背景值进行比较相同的位置和在相同的条件下。与余震相关的数据已被仔细从数据库中删除,以防止对统计数据的虚假影响。结果表明,在夜间期间,可以证明与大于5的大于5的地震有关的异常电离层扰动。在这些扰动的时候,背景离子波动从正态分布中脱离。它们距离震中最多可达200​​公里,主要在地震前5天。如预期的那样,刚刚发生在地震后并接近震中后发生的离子密度扰动也是如此。

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