中性风在中低纬Spread-F中的作用  

The Role of Neutral Wind in Spread-F of Low and Mid-latitudes

作　　者：谢红[1] 刘滨莎 萧佐[1] 

机构地区：[1]北京大学地球物理系,北京100871

出　　处：《北京大学学报（自然科学版）》1996年第1期78-88,共11页Acta Scientiarum Naturalium Universitatis Pekinensis

基　　金：国家自然科学基金

摘　　要：讨论了中低纬度电离层F区中有碰撞的Rayleigh-Taylor不稳定性的线性增长率,着重考察背景中性风对增长率的影响,首先建立了适合于描述中低纬地区R-T不稳定性的基本方程,其中包括背景中性风和电场。在此基础上导出了色散关系和不稳定性增长率γ。结果表明,γ随纬度增加而逐渐减小,虽然东西方向和垂直向下的中性风分量有利于不稳定性增长,但在比30度更高的纬度,正常的背景中性风很难使γ为正值,除非存在合适的东西方向电场,亦即电场在中纬度Spread F的形成方面起着重要的作用。文中还根据比较合乎实际的电离层电子密度分布模式估算了线性增长率γ的季节变化。Collisinal Rayleigh-Tailor instability in the ionospheric F region of lowand mid-latitudes is discussed.Emphasis is put on the effects of the backgroundneutral wind to the growth rate of the instability.A set of equations governing theR-T instability in this region is established with electric field and neutral wind in-cluded and the linear growth rate is deduced.The results show that the growth ratedecreases as increasing latitude.For latitudes higher than 30 degree,normal neu-tral wind alone can no longer make the growth rate keeping positive values even un-der most favorable conditions,unless there is an eastward electric field.This indi-cates that the electric field may take an important role in local R-T instability evolu-tion in mid-latitudes.Seasonal variations of the growth rate is also discussed usingcertain electron density profile model.

关 键 词：中纬扩展F 中性风 电离层 R-T不稳定性 SPREAD-F 

分 类 号：P352.5[天文地球—空间物理学]