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The Variability of H Component of Geomagnetic Field at the African Sector

机译:非洲地区地磁场H分量的变异性

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摘要

The investigation of the variability of the Sq(H) in the African sector was carried out using the geomagnetic field measurements of four stations located in the East, West, Central and South Africa. The study shows that the variations of the geomagnetic element were a dusk to dawn phenomenon with a none zero variation observed in the night. The variability of the nighttime Sq(H) is believed to be from sources other than the ionosphere. An enhancement in Sq(H) variations in Addis Ababa station was observed. The observed enhancement in Sq (H) variations in Addis Ababa station was attributed to the influence of Equatorial electro jet [EEJ] current system. Day- to-day variability in Sq(H) was observed in all the stations, these variability from one day to the next was seen to be both in amplitude and in phase, it does not have a definite pattern thus it is random. Equinoctial maximum in Sq(H) was observed for Mbour, Addis Ababa and Bangui stations while December Solstitial maximum was observed for Hermanus station. Latitudinal positions of the stations were found to affect the Sq(H) amplitude.
机译:使用位于东部,西部,中部和南非的四个站点的地磁场测量,对非洲地区Sq(H)的变异性进行了调查。研究表明,地磁元素的变化是黄昏到黎明的现象,而夜间则没有零变化。据信夜间Sq(H)的可变性来自电离层以外的其他来源。观察到亚的斯亚贝巴站的Sq(H)变化有所增强。在亚的斯亚贝巴站观测到的Sq(H)变化的增强归因于赤道电喷[EEJ]电流系统的影响。在所有测站中都观察到了Sq(H)的每日变化,从一天到第二天的这些变化在幅度和相位上都是可见的,没有确定的模式,因此是随机的。在Mbour,亚的斯亚贝巴和班吉站观测到Sq(H)的等值最大值,而在Hermanus站观测到12月的最大值。发现站的纬度位置会影响Sq(H)振幅。

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