摘要
用3个经度链上电离层垂测站资料分析磁暴时夜间h'F的同时突增现象提出了电动耦合在夜间出现东向电场从而使F层抬升的物理机制同时也解释了突增现象在午夜后更多,且增幅更强的事实.
The simultaneously sudden enhancements of h' F at nighttime during magneticstorms are analyzed by using ionosonde data from stations distributed nearby 3meridian chains. The related physical mechanism is proposed. Generally, the effects ofthe magnetospheric convection and the driving potential across the polar cap (or theregion 1 field-aligned current) during a magnetic storm will lead to a westwardelectric field, but not an eastward one. On the other hand, the shielding effect of theregion 2 field-aligned current may confine the disturbed field within the auroral oveland weaken its influence in lower latitude area. Since the region 1 field--alignedcurrent is usually stronger than the region 2 current the westward electric field cannot be reversed eastward. The turning of the interplanetary magnetic field (IMF) fromsouthward to northward is equivalent to shutting off the driving potential across thepolar cap. If the region 2 field--aligned current strengthens during an IMF turning, theappearance of an eastward field at nighttime is possible, and the drift E×B effectwill lift the F--region obviously. With this mechanism, it is also easy to be understoodwhy the enhancement occurs more frequently and is more intensive in themidnight--dawn sector.
出处
《地球物理学报》
SCIE
EI
CAS
CSCD
北大核心
1998年第2期156-161,共6页
Chinese Journal of Geophysics
基金
国家自然科学基金!49674245
关键词
磁暴
电离层
F层扰动
h′F变化
电离层
Magnetic storm, Disturbance of the ionospheric F-regions, Variation of h' F