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Ionospheric Anomalies Observed by GPS-TEC Prior to the 3rd of July 2013 Uganda’s Earthquake

机译:GPS-TEC在2013年7月第3次地震前观测到的电离层异常

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Recently ionospheric variability remains one of the most intensive studies in the area of ionospheric physics. Despite the massive improved knowledge of its dynamics, the ability to use this data to provide early, as well as valid warning of upcoming earthquakes (seismo-ionospheric coupling) is still controversial. However, anomalous behaviours of TEC in the ionosphere before the occurrence of earthquakes have received several attentions by scientists. In this paper, GPS-TEC variations of 31 days (15 days before and 15 days after the occurrence of Uganda’s earthquake of July 3 ~( rd ) 2013) were examined to see if there was any seismo-ionospheric coupling. Any correlation between the identified TEC anomalies and the earthquake in question was examined. It was discovered that, there was the presence of an anomaly that occurred on the 8 ~( th ) day of the data. And then there was another set of consistent rise in the TEC values that started 4 days before the day of the earthquake and continued till the day of the earthquake. A change of situation was however noticed after the occurrence of the earthquake. The combination of all these led to the conclusions that the anomaly in the TEC is an ionospheric signature for the earthquake.
机译:最近,电离层的可变性仍然是电离层物理学领域最密集的研究之一。尽管人们对其动力学有了更深入的了解,但使用该数据提供早期地震以及对即将发生的地震(地震-电离层耦合)的有效预警的能力仍存在争议。然而,地震发生前电离层中TEC的异常行为受到了科学家的关注。本文研究了31天(2013年7月3日乌干达地震发生前15天和地震发生后15天)的GPS-TEC变化,以查看是否存在地震电离层耦合。检查已识别的TEC异常与所讨论的地震之间的任何相关性。发现在数据的第8天有异常发生。然后,TEC值又发生了一组持续的上升,从地震发生前的4天开始一直持续到地震发生为止。但是,地震发生后,情况发生了变化。所有这些结合在一起得出结论:TEC中的异常是地震的电离层标志。

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