Latitudinal Investigation on the Variation of Solar Wind Parameters towards Geomagnetically Induced Currents during 7–8 September 2017 Disturbed Period

Zatul Iffah Abd Latiff, N. M. Anuar, M. H. Jusoh, Siti Amalina Ence Ab Rahim
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引用次数: 6

Abstract

Geomagnetically induced current (GIC) is one of the natural threat driven by solar activity. The geomagnetic disturbances causes high fluctuating current in ionosphere and magnetosphere. As described by Faraday Law of Induction, high variation of magnetic field induces electric field that responsible for driving GIC in our technological system. In this paper, latitudinal investigation is performed to examine the variation of solar wind parameter and geomagnetic indices during the G4 severe geomagnetic storm occurred on 7–8 September 2017. In addition, the resulting time derivative Horizontal Component of geomagnetic field (dH/dt) as indicator of GIC in response to the variation of solar wind parameter is observed. From the study, highest dH/dt value was observed at high latitude region, followed by mid-latitude region while the lowest value dH/dt obtained by low latitude region.
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2017年9月7-8日扰动期太阳风参数对地磁感应电流变化的纬向研究
地磁感应电流(GIC)是太阳活动引起的自然威胁之一。地磁扰动引起电离层和磁层的高波动电流。正如法拉第感应定律所描述的,在我们的技术系统中,磁场的高变化会产生电场,从而驱动GIC。本文对2017年9月7-8日发生的G4强地磁风暴期间太阳风参数和地磁指数的变化进行了纬度调查。此外,还观测了作为GIC指标的地磁场水平分量时间导数(dH/dt)对太阳风参数变化的响应。从研究结果来看,高纬度地区的dH/dt值最高,中纬度地区次之,低纬度地区的dH/dt值最低。
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