磁扰和磁静期间海南扩展F起始时间出现率研究

利用2002年2月至2007年12月(第23太阳活动周的下降段)近6年的海南DPS-4型电离层测高仪探测数据, 对磁扰和磁静夜晚期间扩展F起始时间出现率进行统计研究. 结合海南电离层观测站所观测到的扩展F类型, 将扩展F区分为频率型、区域型、混合型和强区域型, 分别进行统计分析. 结果表明, 无论磁扰还是磁静夜晚, 混合型扩展F起始时间总出现率最高, 最为活跃, 其次为频率型和强区域型扩展F, 最不活跃的是区域型扩展F; 无论在磁扰还是在磁静夜晚条件下, 混合扩展F起始时间主要围绕在午夜前后, 且磁静时更多地起始于午夜前, 而磁扰时则倾向于延至午夜后, 频率型扩展F在午夜后较高, 而强区域型扩展F则在午夜前较高. 在本次太阳活动下降阶段, 强区域型与区域型扩展F的起始时间出现率逐年与太阳活动呈现一定的相关性. 所得结果有助于分析不同类型扩展F在形态和机制方面的差异.     

大功率无线电波对高电离层的加热

根据动量方程、能量方程和电子的连续性方程,在偶极扩散的假设下,建立了地面入射的大功率无线电波加热高电离层的理论模型.作为应用,对以上方程组数值求解,计算了高电离层（150-400 km）电子温度和电子密度随时间的变化.计算结果表明,对于一定参数的发射机,一定的吸收模型,电离层电子温度和密度均有明显的变化.我们发现,应用本文选取的加热参数,在电波反射点附近,电子温度有10％-25％的增加,电子密度有1％-2％左右的减少.电子温度达到稳态的时间要快于电子密度达到稳态的时间.最后,用本文的结果解释了电离层加热实验中的一些观测现象.     

大功率高频无线电波对赤道E区双流不稳定性的影响--PIC静电粒子模拟研究

地面入射的大功率高频无线电波（泵波）和电离层等离子体之间的参数相互作用,能够引起静电波的激发,在一定条件下,产生不稳定性.本文用PIC静电粒子模拟方法,研究泵波与赤道电离层E区等离子体的相互作用.研究结果表明,泵波能够控制双流不稳定性的发生,在不同条件下,泵波对双流不稳定性起着稳定与不稳作用,模拟结果定性地与理论研究结果相符合,这为我们对不规则体产生的地面人工控制提供了依据.     

高频电波在背景备向异性和不均匀的随机起伏电离层中的传播

运用波动理论,讨论背景为各向异性、不均匀的随机起伏电离层中高频电波的传播和散射问题,给出了电离层不均匀体散射引起的反射回波波场的起伏,并在垂测条件下计算了接收波场的相位与振幅起伏的谱分布。     

The topside sounder database – Data screening and systematic biases

The ionospheric topside sounder measurement database developed at the US National Space Science Data Center (NSSDC) is a valuable source of information when investigating the composition and complex dynamics of the upper ionosphere. The database is increasingly used by many scientists around the world for both research and development of empirical models. However, there is always a danger of indiscriminately using the data without properly assessing the data quality and applicability for a given purpose. This paper is concerned with the issue of data screening and pre-processing of the Alouette/ISIS topside sounder database. An overview of the original database availability and formatting is given and the use of solar and geomagnetic indices is discussed. Data screening procedures, concerning detection and handling of erroneous profiles, are also presented. Special attention is drawn to the systematic biases observed in the database and the possibilities for their removal.     

一种基于人工扰动电离层的通信对抗技术研究

研究了扰动后的电离层对不同波段的电磁波传播的影响,并探讨了该项技术在通信对抗上的具体应用。结果表明:受扰电离层可以引导VLF波进行"哨声模式"传播,进而实现对潜通信;可以使得HF波传播轨迹发生偏转、逃逸、聚焦和散焦,进而实现短波干扰;可以降低卫星通信频率,进而利用新波段实现卫星保密通信,同时还能产生透镜效应,对实现卫星通信的VHF电波产生额外增益,增强通信效果。     

Regular features of the polar ionosphere characteristics from Digisonde measurements over Norilsk

Regular features of the polar ionosphere have been studied using its local empirical model of the electron density distribution in the bottomside ionosphere. The local empirical model was derived from the hand-scaled ionogram data recorded by DPS-4 Digisonde at Norilsk, Russia (69.4N, 88.1E; 60N GLAT, 166E GLON) for a 6-year period from December, 2002 to December, 2008. The paper describes the technique used to build the local empirical model and discusses its diurnal, seasonal, and solar activity specifications in comparison with the standard IRI-2007 climatological model for the same period of time, long-term observations from the European Incoherent Scatter UHF radar (1988–1999), and the high-latitude ionosondes data. Primary focus of the paper is behavior of the three F2 layer parameters: the F2 peak density (NmF2), the peak height (hmF2) and the bottomside thickness (B0). Special emphasis of the paper is the analysis of the winter anomaly manifestation at Norilsk and the peculiar diurnal–seasonal behavior of hmF2 under low solar activity, named as a “polar day effect”.