Submodal anomalies in Schumann resonance phenomenon possibly associated with earthquakes

D. Pundhir, Birbal Singh, O. Singh
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Abstract

Schumann resonance (SR) observations have been carried out at a low latitude station Bichpuri, Agra (Geograph. Lat. 27.2 o N, Long. 78 o E), India using a set of 3-component search coil magnetometer and accessories since 01 April, 2010. Here, we analyse the data for a period of one year from 01 January to 31 December, 2013 in search of possible anomalies in SR data associated with earthquakes. We find that unusual submodal amplitude enhancements ≈ 10-15 dB, frequency shifts 1 Hz-4Hz, precursory period 7 days and duration of the anomaly ≈ 6 hours occurred beyond third and fourth SR bands associated with 03 major earthquakes (M > 6.0). The earthquakes occurred in neighbouring countries of China and Pakistan around India in the months of July and September, 2013. We show that the anomalies appeared as a result of constructive interference maxima at the receiver between the direct ELF waves generated from African and South Asian thunderstorm centers and reflected from the disturbances over epicentres of earthquakes.
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舒曼共振现象的次模态异常可能与地震有关
舒曼共振(Schumann resonance, SR)观测是在阿格拉的一个低纬度站进行的。自2010年4月1日起,在印度北纬27.2度,东经78度,使用一套三分量搜索线圈磁强计及附件。在这里,我们分析了2013年1月1日至12月31日的数据,以寻找与地震相关的SR数据中可能存在的异常。研究发现,03次大地震(震级> 6.0)在第3和第4 SR带之外出现异常次模态振幅增强≈10-15 dB,频率移位1 Hz-4Hz,前兆周期7天,异常持续时间≈6小时。2013年7月和9月,地震发生在印度周边的邻国中国和巴基斯坦。我们发现,这些异常的出现是由于非洲和南亚雷暴中心产生的直接极低频波与地震震中扰动反射的极低频波在接收端产生的建设性干涉极大值的结果。
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