On the Variation of Geomagnetic H-Component during Solar Quiet Days

E. B. Ugwu, C. E. Okeke
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Abstract

The hourly variation of the H-component of the geometric field from two equatorial electrojet stations, Huancayo and Addis Ababa, and one non-equatorial electrojet station, Alibag, were studied to find out the trend of solar quiet variation of H for the year 2008. The dH amplitudes of the electrojet stations showed enhancement in H, while there was no enhancement in the non-electrojet station which was located far away from the dip equator. The day-to-day monthly diurnal variation was, however, observed in all the three stations. Also, at nighttime, the dH amplitudes of all the stations were non-zero which we attributed to non-ionospheric current sources like the magnetosphere since at night there was no solar radiations. For seasonal variations, an Equinoctial maximum, J-Solstitial maximum, and S-Solstitial maximum were observed in the equatorial stations while the non-equatorial station recorded an equinoctial minimum, J-solstitial minimum and D-Solstitial minimum.
太阳平静日地磁h分量的变化
研究了环卡约和亚的斯亚贝巴两个赤道电喷站和阿里巴格一个非赤道电喷站的几何场H分量的逐时变化,找出了2008年太阳H平稳变化的趋势。电喷台站的H值振幅随H值的增加而增加,而远离倾角赤道的非电喷台站的H值振幅则没有增加。然而,在所有三个站点都观察到逐月逐日的变化。此外,在夜间,所有站点的dH振幅都是非零的,我们将其归因于非电离层电流源,如磁层,因为夜间没有太阳辐射。季节变化方面,赤道站观测到分点最大值、j -至点最大值和s -至点最大值,非赤道站观测到分点最小值、j -至点最小值和d -至点最小值。
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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