行星际磁场北向时极区电离层日侧对流爆发与高纬重连的关系研究

电离层对流 磁重联 极光 行星际磁场 SuperDARN
胡红桥 2006-01 项目
【英文摘要】Using polar ionospheric convection data observed by SuperDARN, multi-wavelength auroral data at Chinese Zhongshan Station in Antarctica and conjugated Huanghe Station in the Arctic, particle precipitation and field data with DMSP, Cluster/DS satellites, we have studied dayside ionospheric convection and its connection with dayside magnetospheric dynamics (such as high latitude reconnection and FTEs), dayside ionospheric flow bursts and their related features of particle precipitation, the characteristics of the particle precipitation and the radar spectral width in the dayside sunward flow regions, the temporal and special characters of the high latitude reconnection closely related to sunward flow in the cusp, and have given a scheme to illustrate the linkage between the dayside ionopsheric flow burst and the high latitude reconnection when IMF strongly northward. This project found some clues for us to understand the dynamics of the solar wind-magnetospheric-ionospheric coupling.
【中文摘要】利用SuperDARN 雷达的极区电离层对流观测,结合南极中山站和北极黄河站的极光观测、DMSP 卫星的粒子沉降观测以及Cluster和双星的本地探测,研究了行星际磁场北向时高纬重联和通量传输事件的极区电离层对流特征、日侧极区电离层对流与日侧磁层动力学过程的关系、日侧电离层爆发性对流结构及其相关的粒子沉降特征、日侧极光粒子沉降和雷达频谱特征,给出了日侧电离层爆发性对流结构与高纬重联过程间关系的物理解释?将有助于进一步理解太阳风-磁层-电离层耦合过程。