研究福布什下降与地磁截止刚度的关系

O. C Nwuzor, O. Okike, A. E Umahi, C. C Nwaevo, C. I Nworie, A. Ojobeagu, A. Chikwendu, C. Ozibo, P. B Otah
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摘要

研究了福布什下降与地磁截止刚度的关系。该研究旨在探讨地磁截止刚度对福布什下降的影响。为了达到这个目的,研究使用了西藏、埃索伊岛、措美布岛、奥卢岛、阿帕提岛和马加丹岛六个中子站的宇宙射线日计数数据。这些数据涵盖了从 2010 年到 2015 年的六年时间。Okike和Umahi(2019b)开发了一种先进的人工方法,通过R.统计软件来选择FDs。 结果发现,宇宙射线变化强度急剧下降,被称为福布什下降(FD)。记录了大量的 FDs。我们将分析结果分为高、低和中等刚度的站点。刚度低的站点记录的 FDs 数量最多,其次是刚度中等的站点,而刚度高的站点记录的 FDs 数量最少。对这些 FD 的大小进行了测定。结果表明,FD 的大小与站点的刚性成反比。还测试了宇宙射线(CR)台站的 FD 幅值之间的相关性。结果表明,低刚度台站的相关性最好,其次是中等刚度台站,而高刚度台站的相关性最小。进一步测试了不同站点的 FD 幅值之间的回归关系。不同站点 FD 之间的回归结果显示,低刚度、高刚度和中等刚度站点的显著性分别为 99.8%、98% 和 97.5%。总之,本研究使用了大量的事件来检验 FDs 的刚度依赖性,并观察到 FDs 与临界刚度成反比关系。因此,在 CR 站测量的 FDs 可用来研究站与站之间刚性的影响。
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Investigating The Dependence Of Forbush Decrease On Geomagnetic Cutoff Rigidity
The dependence of Forbush decreases on geomagnetic cutoff rigidity has been studied. The study aimed to investigate the implications of geomagnetic cutoff rigidity on forbush decrease. To achieve this aim, the data of cosmic ray daily count from six neutron stations of Tibet, Esoi, Tsumeb, Oulu, Apatity, and Magadan were used. These data covered a period of six (6) years from the year 2010 to 2015. An advanced manual method developed by Okike and Umahi (2019b) was used to select the FDs through R. statistical software.  A sharp depression in the intensity of cosmic ray variation known as Forbush decrease (FD) was detected. A large number of FDs were recorded. The results of our analysis was grouped into stations of high, low and middle rigidity. The stations of low rigidity recorded the highest number of FDs followed by stations of middle rigidity while the stations of high rigidity recorded the least number of FDs. The magnitude of these FDs was determined. It was observed that FD magnitudes vary inversely with the station's rigidity. A correlation between the FD magnitudes of the cosmic ray (CR) stations was also tested. It was observed that stations of low rigidity indicated the best correlation followed by the stations of middle rigidity, while the stations of high rigidity indicated the least correlation. A regression was further tested between the FD magnitudes of the different stations. The result of the regression between FDs of different stations was 99.8% , 98% and 97.5% significant for stations low, high and middle rigidity stations respectively. In summary, this study used a large number of events to test the rigidity dependence of FDs, and it was observed that FDs are inversely related to the cutoff rigidity. Thus, FDs measured at the CR stations can be used to examine the effects of rigidity between the stations.    
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