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首页> 外文期刊>Annals Of Geophysics >Wavelet analysis of the LF radio signals collected by the European VLF/LF network from July 2009 to April 2011
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Wavelet analysis of the LF radio signals collected by the European VLF/LF network from July 2009 to April 2011

机译:2009年7月至2011年4月欧洲VLF / LF网络收集的LF无线电信号的小波分析

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In 2008, a radio receiver that works in very low frequency (VLF; 20-60 kHz) and LF (150-300 kHz) bands was developed by an Italian factory. The receiver can monitor 10 frequencies distributed in these bands, with the measurement for each of them of the electric field intensity. Since 2009, to date, six of these radio receivers have been installed throughout Europe to establish a ‘European VLF/LF Network’. At present, two of these are into operation in Italy, and the remaining four are located in Greece, Turkey, Portugal and Romania. For the present study, the LF radio data collected over about two years were analysed. At first, the day-time data and the night-time data were separated for each radio signal. Taking into account that the LF signals are characterized by ground-wave and sky-wave propagation modes, the day-time data are related to the ground wave and the night-time data to the sky wave. In this framework, the effects of solar activity and storm activity were defined in the different trends. Then, the earthquakes with M ≥5.0 that occurred over the same period were selected, as those located in a 300-km radius around each receiver/transmitter and within the 5th Fresnel zone related to each transmitter-receiver path. Where possible, the wavelet analysis was applied on the time series of the radio signal intensity, and some anomalies related to previous earthquakes were revealed. Except for some doubt in one case, success appears to have been obtained in all of the cases related to the 300 km circles in for the ground waves and the sky waves. For the Fresnel cases, success in two cases and one failure were seen in analysing the sky waves. The failure occurred in?August/September, and might be related to the disturbed conditions of the ionosphere in summer. ?
机译:2008年,一家意大利工厂开发了一种工作在极低频(VLF; 20-60 kHz)和LF(150-300 kHz)频段的无线电接收机。接收器可以监视分布在这些频带中的10个频率,并测量每个电场强度。自2009年以来,迄今为止,在欧洲已安装了其中的六个无线电接收器,以建立“欧洲VLF / LF网络”。目前,其中两个在意大利投入运营,其余四个分别在希腊,土耳其,葡萄牙和罗马尼亚。对于本研究,分析了大约两年内收集的低频无线电数据。首先,将每个无线电信号的白天数据和夜间数据分开。考虑到低频信号的特征在于地波和天波的传播方式,因此白天数据与地波有关,而夜间数据与天波有关。在此框架中,以不同的趋势定义了太阳活动和风暴活动的影响。然后,选择同一时期发生的M≥5.0地震,作为位于每个接收器/发射器周围300公里半径内以及与每个发射器-接收器路径有关的第5菲涅耳区域内的地震。在可能的情况下,将小波分析应用于无线电信号强度的时间序列,并揭示了与先前地震有关的一些异常现象。除非有一个疑问,在与地面波和天波相距300 km的所有情况下,似乎都取得了成功。对于菲涅尔案例,通过分析天波,可以看到有两例成功,有一例失败。该故障发生在8月/ 9月,可能与夏季电离层的扰动有关。 ?

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