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磁暴期间中纬度电离层剖面结构变化的数值模拟
引用本文:张奇伟,郭兼善.磁暴期间中纬度电离层剖面结构变化的数值模拟[J].空间科学学报,1994,14(1):39-47.
作者姓名:张奇伟  郭兼善
作者单位:中国科学院空间科学与应用研究中心
摘    要:利用电离层理论模型模拟了磁暴期间热层大气温度、成分、中性风和电场扰动对电离层电子密度剖面结构,特别是峰值密度和峰值高度变化的影响,结果表明,热层大气温度变化所引起光化反应系数的改变对电离层剖面结构影响不大;热层大气成分特别是N2/O的变化能有效地引起密度剖面变化,N2增加足以使峰值密度产生所观测到的负相暴;由中性风和电场引起等离子体漂移是峰值高度hmF2变化的主要原因,但对电子密度的影响不足以抵消

关 键 词:电离层暴  电子密度剖面  数值模拟

MODEL STUDY OF MID-LATITUDE IONOSPHERIC DENSITY PROFILE VARIATION DURING GEOMAGNETIC STORMS
Zhang Qi-wei, Guo Jian-shan, Zhang Gong-liang.MODEL STUDY OF MID-LATITUDE IONOSPHERIC DENSITY PROFILE VARIATION DURING GEOMAGNETIC STORMS[J].Chinese Journal of Space Science,1994,14(1):39-47.
Authors:Zhang Qi-wei  Guo Jian-shan  Zhang Gong-liang
Abstract:A theoretical ionospheric model is developed in order to study the variation of ionospheric density profile during geomagnetic storms, considering the disturbances of thermospheric temperature, composition, wind and electric field. The results show that the increase of N2/O is the most efficient way to decrease the electron density as well as the peak density NmF2, but the up and down movement of peak height (hmF2) is mainly caused by neutral wind or electric field disturbance. The temperature change has little effect on the profile variation. It is possible to distinguish these different physical processes using f0F2 and hmF2 parameters in practical measurement.
Keywords:Ionospheric storm  Electron density profile  Ionospheric model  
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