Geomagnetic Secular Variation at the Indian Observatories

S. Bhardwaj, G. Rangarajan
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引用次数: 9

Abstract

Annual mean values of geomagnetic field components D, H and Z for all days and quiet days at six observatories are analysed to investigate the secular variations and geomagnetic jerks in the Indian region. Secular trends show a region of demarkation between equatorial and low latitude stations. The residual D, H and Z curves, obtained by removing polynomial fits, do not show any parallelism with the Il-year sunspot cycle. However, the D residual has a periodicity of 2 solar cycles, whereas H and Z residuals indicate a quasi-periodicity of 3 solar cycles at Alibag. For the period 1958 to 1990, D and Z residuals show a periodicity of nearly 2 solar cycles, while H shows out-of-phase variations with the sunspot cycle for all the six stations. The secular jerk around 1969-70, noted at many observatories over the globe, is not seen in D but is noted in the H and Z components at some of the six Indian stations. A comparison between the observed annual means and IGRF models indicates very low secular variation anomaly in the Indian region.
印度天文台地磁的长期变化
本文分析了印度地区6个观测站在全日和无活动日的地磁分量D、H和Z的年平均值,探讨了该地区的长期变化和地磁跳变。长期趋势显示赤道站和低纬度站之间有分界线。通过去除多项式拟合得到的残差D、H和Z曲线不显示与太阳黑子周期的任何平行性。然而,D残差具有2个太阳周期的周期性,而H和Z残差表明在Alibag具有3个太阳周期的准周期性。在1958 ~ 1990年期间,D和Z残差表现出近2个太阳周期的周期性,而H与黑子周期均表现出非相位变化。1969-70年前后的长期波动,在全球许多观测站都有记录,但在D中没有看到,但在印度六个观测站中的一些观测站的H和Z分量中有记录。将观测到的年平均值与IGRF模式的比较表明,印度地区的长期变化异常非常低。
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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