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Calculating global storm activity rate on the basis of Schumann resonance background component

机译:基于舒曼共振本底分量计算全球风暴活动率

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This work presents the results of applying a new method of calculating the global storm activity rate IRS . The permanent analysis of the global storm activity rate IRS may become an important tool for testing Global Electric Circuit (GEC) model. The method uses the background component of the first 7 Schumann resonances (SR). The rate calculations applied based on ELF observations carried out in years 2005-2006 in the observatory station of the Jagiellonian University in the Eastern Carpathians. Diurnal runs of IRS rate were compared with diurnal runs of field intensity E0 Z amplitudes registered at the Earth’s surface in the geophysical observatory IGF PAN in Swider near Warsaw. The days with the high value of the correlation coefficient R between amplitudes of both observed parameters characterizing atmosphere electric activity are shown. The seasonal changes of R, IRS and E0Z are also presented.component is fitted to the formula
机译:这项工作提出了应用一种计算全球风暴活动率IRS的新方法的结果。对全球风暴活动率IRS的永久分析可能会成为测试全球电路(GEC)模型的重要工具。该方法使用前7个舒曼共振(SR)的背景分量。基于2005-2006年在东喀尔巴阡山脉的Jagiellonian大学的天文台进行的ELF观测所应用的费率计算。在华沙附近Swider的地球物理观测台IGF PAN中,将IRS速率的日运行与在地球表面记录的场强E0 Z振幅的日运行进行了比较。示出了具有表征大气电活动的两个观测参数的振幅之间的相关系数R的值较高的日子。还列出了R,IRS和E0Z的季节变化。

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