摘要
利用北京、乌鲁木齐、武汉GPS观测数据计算的垂直总电子含量,分析了发生于2000年4月6-8日磁暴期间观测区域的电离层状态.结果表明,在4月7日北京时间0200-0700之间,在中、低纬地区出现了较弱的电离层负相暴,与前一日相比,最大TEC之差在-8TECU左右;在北京时间0700之后,在较高纬度地区开始出现强烈的电离层负相暴,并且该负相暴随着时间逐渐增强;但在北京时间0700-0900之间,在低纬地区出现了电离层正相暴.在一定时间内较高纬度地区的负相暴逐渐增强并向南移动而低纬地区的正相暴经历了增强到减弱的过程.
One large coronal mass ejection (CME) occurred in the Sun at 1642UT, Apr. 4, 2000. At about 1600 UT, Apr, 6, the high speed solar wind was detected by ACE satellite, the speed of which increased suddenly from 380 km/s up to 600 km/s. Then a southwards interplanetary magnetic field that lasts for 7 hours was observed. The solar wind push magnetosphere, and a large magnetic storm happened near the earth. At 0000 UT, Apr. 7, 2000, the Kp index reaches 8 and lasts for 6 hours. The minimum Dst index is -318 nT. During the magnetic storm, an ionospheric storm was also happened over the region of China shown by the observations of the ionosondes. Combining the temporal ionospheric TEC curves and the curves of the corresponding sub-ionospheric point derived from GPS measurements observed at Beijing, Wulumuqi, and Wuhan GPS stations, the morphology of ionospheric TEC over the region of 30°N-45°N and 85°E-120°E during the magnetic storm occurred on April 6-8, 2000 is studied. The results showed that, a weak negative storm over this region happened between 0200 BT and 0700 BT on April 7, 2000. Compared with the TEC on April 6, the largest value of TEC change is -8TECU. After 0800 BT, a strong ionospheric negative storm appeared over higher latitude region and became stronger and stronger with time. Meanwhile, an ionospheric positive storm developed over lower latitude region between 0700 BT and 0900 BT. During this period, the negative storm over higher latitude became gradually stronger, and moved southwards. Nevertheless the positive storm over lower latitude experienced an enhancing and declining process.
出处
《空间科学学报》
CAS
CSCD
北大核心
2002年第3期212-219,共8页
Chinese Journal of Space Science
基金
国家自然科学基金资助项目(40134020
49990455)
