On the Imminent Regional Seismic Activity Forecasting Using INTERMAGNET and Sun-Moon Tide Code Data

S. Mavrodiev, L. Pekevski, Giorgi Kikuashvili, E. Botev, P. Getsov, G. Mardirossian, G. Sotirov, D. Teodossiev
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引用次数: 3

Abstract

In this paper we present an approach for forecasting the imminent regional seismic activity by using geomagnetic data and Earth tide data. The time periods of seismic activity are the time periods around the Sun-Moon extreme of the diurnal average value of the tide vector module. For analyzing the geomagnetic data behaviour we use diurnal standard deviation of geomagnetic vector components F (North, East, Down) for calculating the time variance GeomagSignal. The Sun storm influence is avoided by using data for daily A-indexes (published by NOAA). The precursor signal for forecasting the incoming regional seismic activity is a simple function of the present and previous day GeomagSignal and A-indexes values. The reliability of the geomagnetic “when, regional” precursor is demonstrated by using statistical analysis of day difference between the times of “predicted” and occurred earthquakes. The base of the analysis is a natural hypothesis that the “predicted” earthquake is the one whose surface energy density in the monitoring point is bigger than the energy densities of all occurred earthquakes in the same period and region. The reliability of the approach was tested using the INTERMAGNET stations data located in Bulgaria, Panagurishte, PAG (Jan 1, 2008-Jan 29, 2014), Romania, Surlari, SUA (Jan 1, 2008-Jan 27, 2014), Italy, L’Aquila, AQU (Jan 1, 2008-May 30, 2013) in the time of EU IRSES BlackSeaHazNet (2011-2014) project. The steps of program for solving the “when, where and how” earthquake prediction problem are shortly described.
利用磁体间和日月潮码资料预报区域即将发生的地震活动
本文提出了一种利用地磁资料和潮汐资料预报区域地震活动的方法。地震活动的时间周期是潮汐矢量模块日平均值的日月极值附近的时间周期。为了分析地磁数据行为,我们使用地磁矢量分量F(北、东、下)的日标准差来计算时间方差GeomagSignal。使用每日a指数数据(由NOAA公布)避免了太阳风暴的影响。预报即将到来的区域地震活动的前兆信号是当日和前一天的GeomagSignal和a指数值的简单函数。通过对“预报”地震与发生地震的日差进行统计分析,证明了地磁“何时、区域”前兆的可靠性。分析的基础是一个自然假设,即“预测”的地震是监测点的表面能量密度大于同一时期和同一地区所有发生地震的能量密度。在欧盟IRSES BlackSeaHazNet(2011-2014)项目期间,使用INTERMAGNET站点数据测试了该方法的可靠性,这些站点位于保加利亚、PAG的Panagurishte(2008年1月1日至2014年1月29日)、罗马尼亚、SUA的Surlari(2008年1月1日至2014年1月27日)、意大利、aquila、aquu(2008年1月1日至2013年5月30日)。简要介绍了解决“何时、何地、如何”地震预报问题的程序步骤。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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