Solar cycle evolution of ULF wave power in solar wind and on ground

被引:9
作者
Hynonen, Reko [1 ]
Tanskanen, Eija I. [1 ,2 ]
Francia, Patrizia [3 ]
机构
[1] Aalto Univ Technol, Dept Elect & Nanoengn, Aalto 00076, Finland
[2] Univ Oulu, Sodankyla Geophys Observ, Sodankyla 99600, Finland
[3] Univ Aquila, Dipartimento Sci Fis & Chim, Via Vetoio, I-67100 Laquila, Italy
基金
芬兰科学院;
关键词
ULF waves; Solar cycle; Space climate; Geomagnetic pulsations; Pc5; waves; HIGH-SPEED STREAMS; AURORAL OVAL; GEOMAGNETIC FLUCTUATIONS; MAGNETIC-FIELD; POLAR-CAP; PULSATIONS; MAGNETOSPHERE; TEMPERATURE; ANTARCTICA; DEPENDENCE;
D O I
10.1051/swsc/2020046
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The solar cycle evolution of the ultra-low frequency (ULF) power was studied in solar wind and on ground. We aim finding out how the ULF power in interplanetary and on ground magnetic field evolves over the solar cycle 23 (SC23) and how well do they follow each other in monthly time scales. The hourly power of the ULF waves was computed in the Pc5 frequency range 2-7 mHz for years 1998-2008. The highest wave power in SC23 is found to occur in late 2003 and the lowest at the solar minimum. Ground ULF power follows the IMF power and solar wind speed, particularly well during declining phase. The ULF power in winter exceeds the ULF power in other seasons during the declining phase of SC23, while equinoxes dominate in the ascending phase and the solar maximum. The ground ULF power was found to rise with magnetic latitude from 54 degrees to 73 degrees, after which Pc5 power decreases towards the polar cap. The Pc5 power in the auroral zone is larger in the nightside than the dayside due to substorm activity implying that magnetotail processes are an important contributor to the nightside ULF power.
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页数:11
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