摘要
利用一个时变电离层理论模式,研究武昌地区(30.5°N,114.4°E)电离层F_1-ledse现象.表明利用当前关于中性气体和太阳辐射的经验模式,观测到的F_1-ledge出现与演化的基本规律将可基于现有电离层理论加以再现.指出较明显的F_1-ledge结构同较低的中性原子-分子含量比有直接关系,并同原子-分子成份的过渡高度、背景温度及其垂直分布形态有一定联系.同F_1-ledge形态相关联的F_1-F_2谷,其出现主要是由于亚稳态氧离子参与光化过程,以及电离气体参与具有一定垂直变化的输运过程.
The F_1 -ledge behaviour in Wuchang(30.5°N,114.4°E) is studied with the help of a time-dependent theoretical ionospheric model.It is shown that the current ionospheric theories are eligible to repfoduce the observed regularity of the F_1-ledge occurrence and evolution within the atmospheric background defined by the up-todate empirical models. And the simulations reveal that a pronounced ledge correlates directly to a lower ratio of neutral atomic oxygen to molecular compositions, and has something to do with the transition height from the prevailing molecular to atomic ions, and with the background temperature and its height gradient. The F_1-F_2 valley, connected to the F_1-ledgd shape,is considered to be Present with the chemical processes that involve reactons of meta -stable oxyen ions ,as well as the dynamic processes that contain a proper vertical variation of ion movements.
出处
《地球物理学报》
SCIE
EI
CSCD
北大核心
1996年第5期601-607,共7页
Chinese Journal of Geophysics
基金
国家自然科学基金
中国科学院留学经费择优支持项目
关键词
电离层
理论模式
F1-ledge
Theoretical ionospheric model,Ionospheric F_1-ledge,Ionospheric F_1-F_2 valley .