| IMF北向时太阳风粒子向磁层输运的试验粒子模拟研究 |
| |
| 引用本文： | 赵明现. IMF北向时太阳风粒子向磁层输运的试验粒子模拟研究[J]. 空间科学学报, 2022, 42(6): 1068-1078. doi: 10.11728/cjss2022.06.210721078 |
| |
| 作者姓名： | 赵明现 |
| |
| 作者单位： | 中国气象局空间天气重点开放实验室/国家卫星气象中心(国家空间天气监测预警中心) 北京 100081;;许健民气象卫星创新中心 北京 100081 |
| |
| 基金项目： | 国家自然科学基金项目资助（42274217，41774195） |
| |
| 摘 要： | 以ACE卫星实时观测数据驱动的全球磁流体模拟为背景场，选取2003年10月22－24日行星际磁场（IMF）持续北向的事件，使用试验粒子方法，对太阳风粒子向磁层输运的过程进行模拟研究，分析北向IMF下太阳风粒子注入磁层过程中粒子在磁层内的空间分布和时间演化特征。IMF北向期间，进入环电流区域的粒子在晨侧区域的密度大于昏侧，且晨侧的粒子分布范围更广。背阳面磁鞘中的太阳风粒子可以通过低纬边界层进入磁层，但很难通过南北侧磁层顶进入磁层。进入磁尾的太阳风粒子聚集形成冷而密的等离子体片（CDPS），模拟中CDPS的空间分布和密度大小与观测数据符合。在IMF长时间北向期间，磁尾的粒子数量呈现随时间增长的趋势，并存在约20 min的小幅度准周期变化和约5~6 h的较大幅度的准周期变化。
|
| 关 键 词： | 太阳风 北向行星际磁场 磁层 试验粒子模拟 |
| 收稿时间： | 2021-07-18 |
| 修稿时间： | 2022-03-15 |
Test Particle Simulation of Solar Wind Transport into the Magnetosphere during Northward IMF |
| |
| ZHAO Mingxian. Test Particle Simulation of Solar Wind Transport into the Magnetosphere during Northward IMF (in Chinese). Chinese Journal of Space Science, 2022, 42(6): 1068-1078 doi: 10.11728/cjss2022.06.210721078 |
| |
| Authors: | ZHAO Mingxian |
| |
| Affiliation: | Key Laboratory of Space Weather, National Satellite Meteorological Center (National Center for Space Weather), China Meteorological Administration, Beijing 100081;;Innovation Center for FengYun Meteorological Satellite (FYSIC), Beijing 100081 |
| |
| Abstract: | Using test particle method, with the background fields obtained from a global Magnetohydrodynamics (MHD) simulation driven by the ACE satellite observation data, the transport process of solar wind particles into the Earth’s magnetosphere was simulated during a long-term northward Interplanetary Magnetic Field (IMF) event on 22－24 October 2003. The particle density distribution in the magnetosphere and the time evolution characteristics of the particles were analyzed and discussed. During the northward IMF, the particle density in the dawn-side ring current region is higher than that on the dusk side, and the radial range on the dawn side is wider. The magnetosheath particles on the tail side can transport into magnetosphere through the low-latitude boundary layer, but they are difficult to enter into magnetosphere through the north and south magnetopause. The solar wind particles transported into the nightside magnetosphere gather to form a Cold Dense Plasma Sheet (CDPS). The spatial scale and particle density of the CDPS obtained from the simulation are consistent with observations. During the long-term northward IMF period, the total number of particles in the magnetotail showed a trend of increasing over time. At the same time, there exists a weak quasi-periodic variation with a period of about 20 min and a strong quasi-periodic variation with a period of about 5～6 h. |
| |
| Keywords: | Solar wind Northward IMF Magnetosphere Test particle simulation |
|
| 点击此处可从《空间科学学报》浏览原始摘要信息 |
|
点击此处可从《空间科学学报》下载免费的PDF全文 |
