Effects of solar flares and coronal mass ejections on Earth's horizontal magnetic field and solar wind parameters during the minimum solar cycle 24

被引:6
|
作者
Zafar, S. N. A. Syed [1 ]
Umar, R. [1 ]
Sabri, N. H. [2 ]
Jusoh, M. H. [3 ]
Dagang, A. N. [4 ]
Yoshikawa, A. [5 ]
机构
[1] Univ Sultan Zainal Abidin, East Coast Environm Res Inst, Terengganu 21300, Malaysia
[2] Univ Malaysia Terengganu, Fac Sci & Marine Environm, Adv Nano Mat ANoMa Res Grp, Terengganu 21030, Malaysia
[3] Univ Teknol Mara, Fac Elect Engn, Appl Electromagnet Res AERG, Shah Alam 40450, Selangor, Malaysia
[4] Univ Malaysia Terengganu, Fac Ocean Engn Technol & Informat, Terengganu 21030, Malaysia
[5] Kyushu Univ, Int Ctr Space Weather Sci & Educ ICSWSE, Fukuoka, Japan
关键词
magnetic fields; Sun: activity; Sun: coronal mass ejections (CMEs); Sun: flares; solar wind;
D O I
10.1093/mnras/stab1161
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Previous studies have reported that coronal mass ejections (CMEs) and solar flares lead to the development of huge storms and high-speed streams. Our aim in this paper is to investigate the response of the geomagnetic index SYM/H to the solar wind parameters, such as solar wind speed V, dynamic pressure P, input energy IE and the interplanetary magnetic field (IMF) B-z component, associated with solar flares and CME events. The response of the ground geomagnetic field (H-component) to the solar wind parameters and the IMF B-z component at three low-latitude stations has also been analysed. Our findings show that the delay of the solar wind changes in the Earth's magnetosphere in response to the weak geomagnetic storm (SYM/H=-30 nT) at the beginning of 2014 December 21. A weak storm of SYM/H=-30 nT in the middle of 2014 November 5 is suggested by a low magnetic reconnection process in the magnetosphere. In addition, the strong southward IMF B-z component and high solar wind changes in the magnetosphere system, which were a result of the X2.0 solar flare event and the CMEs on 2014 October 27, responded to the moderate storm (SYM/H = -60 nT) at the beginning of 2014 October 28. This dynamic physical process in the magnetosphere caused by solar wind variation is seen to excite the Earth's H-component through ultra low frequency at the ground-based magnetometers at the BCL (Vietnam), TIR (India) and SCN (Indonesia) stations during the geomagnetic storm. This study relates to seismic investigations and geomagnetic-induced current on the ground.
引用
收藏
页码:3812 / 3822
页数:11
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