The Differences in the Origination and Properties of the Near-Earth Solar Wind between Solar Cycles 23 and 24

被引:0
|
作者
Shi, Xinzheng [1 ]
Fu, Hui [1 ]
Huang, Zhenghua [1 ]
Yan, Limei [2 ]
Ma, Chi [1 ]
Huangfu, Chenxi [1 ]
Song, Hongqiang [1 ]
Xia, Lidong [1 ]
机构
[1] Shandong Univ, Inst Space Sci, Shandong Key Lab Opt Astron & Solar Terr Environm, Weihai 264209, Shandong, Peoples R China
[2] Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Beijing 100029, Peoples R China
来源
ASTROPHYSICAL JOURNAL | 2024年 / 972卷 / 01期
基金
中国国家自然科学基金;
关键词
CORONAL MASS EJECTIONS; IN-SITU PROPERTIES; OPEN MAGNETIC-FLUX; HELIUM ABUNDANCE; ELECTRON-TEMPERATURE; CHARGE STATES; FLOW SPEEDS; INTERPLANETARY; FIELD; EVOLUTION;
D O I
10.3847/1538-4357/ad5be1
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The dependence of the sources and properties of the near-Earth solar wind on solar cycle activity is an important issue in solar and space physics. We use the improved "two-step" mapping procedure that takes into account the initial acceleration processes to trace the near-Earth solar winds back to their source regions from 1999-2020, covering solar cycles (SCs) 23 and 24. Then, the solar wind is categorized into coronal hole (CH), active region (AR), and quiet Sun (QS) solar wind based on the source region type. We find that the proportions of CH and AR (QS) wind during SC 23 are higher (lower) than those during SC 24. During solar maximum and declining phases, the magnetic field strength, speed, helium abundance (A He), and charge states of all three types of solar wind during SC 23 are generally higher than those during SC 24. During solar minimum, these parameters of solar wind are generally lower during SC 23 than those during SC 24. There is a significant decrease in the charge states of all three types of solar wind during the solar minimum of SC 23. The present statistical results demonstrate that the sources and properties of the solar wind are both influenced by solar cycle amplitude. The temperatures of AR, QS, and CH regions exhibit significant differences at low altitudes, whereas they are almost uniform at high altitudes.
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页数:16
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