磁暴对赤道地区L波段电离层闪烁的影响研究

利用赤道地区Vamimo站闪烁数据, 选取两次典型大磁暴时段重点分析, 对比磁暴发生前、发生时以及发生后连续几天电离层幅度闪烁强度和发生率的变化, 引入瑞利elax-elax泰勒不稳定性(Rayleigh-Taylor, R-T不稳定性)线性增长率γ₀, 对磁暴影响闪烁的机制进行初步探讨. 结果表明, 磁暴可能触发闪烁发生, 也可能抑制闪烁发生, 这既与观测季节有关, 也与磁暴不同发展阶段的地方时有关. 触发发生于闪烁少发季节磁暴主相所在的午夜至黎明时段, 可能是磁层穿透电离层的东向电场所致; 抑制发生于闪烁多发季节磁暴恢复相所在的午夜前时段, 可能是西向电场作用的结果. 磁暴发生时的电场变化可能是抑制或触发闪烁的主导因素, 但仍需进一步分析研究.      

Response of Hainan GPS ionospheric scintillations to the different strong magnetic storm conditions

Using the GPS ionospheric scintillation data at Hainan station (19.5°N, 109.1°E) in the eastern Asia equatorial regions and relevant ionospheric and geomagnetic data from July 2003 to June 2005, we investigate the response of L-band ionospheric scintillation activity over this region to different strong magnetic storm conditions (Dst < −100 nT) during the descending phase of the solar cycle. These strong storms and corresponding scintillations mainly took place in winter and summer seasons. When the main phase developed rapidly and reached the maximum near 20–21 LT (LT = UT + 8) after sunset, scintillations might occur in the following recovery phase. When the main phase maximum occurred shortly after midnight near 01–02 LT, following the strong scintillations in the pre-midnight main phase, scintillations might also occur in the post-midnight recovery phase. When the main phase maximum took place after 03 LT to the early morning hours no any scintillation could be observed in the latter of the night. Moreover, when the main phase maximum occurred during the daytime hours, scintillations could also hardly be observed in the following nighttime recovery phase, which might last until the end of recovery phase. Occasionally, scintillations also took place in the initial phase of the storm. During those scintillations associated with the nighttime magnetic storms, the height of F layer base (h’F) was evidently increased. However, the increase of F layer base height does not always cause the occurrence of scintillations, which indicates the complex interaction of various disturbance processes in ionosphere and thermosphere systems during the storms.     

L波段数字航空通信系统研究

随着全球航空运输的发展,空中交通管制与航空公司运控等航空业务对航空通信系统的数据传输速率、频谱利用率、航空通信网容量等性能提出了更高的要求。虽然现阶段基于甚高频的航空通信系统得到了迅速的发展,但仍受限于标准体制、技术壁垒等因素,难以满足持续增长的运行需求。L波段数字航空通信（L-band digital aeronautical communication system,L-DACS）数据链技术作为新一代航空通信系统的预选方案,是有效解决频谱资源饱和难题、满足高速率传输需求的有效途径。本文在总结L-DACS数据链技术发展现状的基础上,阐述了该通信系统现阶段的技术标准,分析了L-DACS发展所面临的挑战,提出了对应的发展建议,为面向航空宽带通信L-DACS的研究提供了参考与借鉴。     

机载L波段电视发射天线

本文讨论了在满足空气动力特性和电性能条件下,L波段分流激励倒L型天线的分析计算和L波段天线尺寸对电性能的影响。给出了机载电视图象传输系统发射天线的设计结果、驻波比和天线方向性图测试曲线,以及在现役轰炸机上飞行试验的传播性能数据。结果表明,用这种型式的发射天线效果是好的。     

多普勒测风激光雷达风廓线探测精度对比分析

在晴空干洁的大气条件下,多普勒测风激光雷达能够以较高的时间、空间分辨率,获得大气三维风场信息。为验证北京遥测技术研究所研制的WINDLE LIDAR型多普勒测风激光雷达探测的准确性,2020年4月~5月,用该雷达在北京市南郊观象台和L波段探空雷达进行同时同址对比观测。2022年6月~7月,用该雷达与北京遥测技术研究所的WINDLE U7相干测风激光雷达进行同时同址对比观测。通过对数据进行相关性分析,得到比对结果如下：1）垂直探测距离大于5 km,最大探测高度可达8.5 km;2）与L波段探空雷达对比,风速和风向数据拟合总相关系数分别为0.990和0.998。总体风速和风向的系统偏差、标准偏差分别为0.114 m/s和3.078°、0.489 m/s和3.969°,二者具有较好的一致性;3）与WINDLE U7雷达对比,风速和风向数据拟合总相关系数分别为0.999和0.999。总体风速和风向的系统偏差和标准偏差分别为0.209 m/s和1.077°、0.255 m/s和1.220°,可以看出该雷达系统的优越性。     

联合压缩感知与干扰白化的脉冲干扰抑制方法

针对L频段数字航空通信系统1(L-DACS1)以内嵌方式部署在航空无线电导航频段而产生的测距仪脉冲干扰(DME)正交频分复用(OFDM)接收机的问题,提出联合压缩感知与残留干扰白化的测距仪脉冲干扰抑制方法.首先接收机通过空子载波信道来观测测距仪脉冲干扰,并利用测距仪脉冲干扰在时域的稀疏特性,基于l1范数最小化约束的凸优化方法重构测距仪脉冲干扰;然后将重构的脉冲干扰转换到频域进行干扰消除;最后,接收机通过信号解交织器与逆正交变换器将残留的脉冲干扰转换为高斯白噪声,避免了残留干扰信号造成的突发性解调错误.仿真研究表明:联合干扰抑制方法可有效消除测距仪脉冲信号干扰,显著提高L-DACS1系统链路传输的可靠性.      

Comments on the percentage of occurrence methodology used in “a study of L band scintillations during the initial phase of rising solar activity at an Indian low latitude station” by H J Tanna,S P Karia and K N Pathak

Following Tanna et al. (2013), we computed the percentage of occurrence of S₄ index for the period of 2012–2015 using the data of the dual frequency GPS receiver at the Tripura University, Agartala station (23.76°N, 91.26°E) situated at the northern crest of the equatorial ionization anomaly (EIA) region of the Indian Subcontinent. We have observed discrepancy in the results contradicting the actual scintillation occurrence. The distinctly noticeable discrepancy is that the maximum occurrence month is shifted to April 2013 instead of March 2014. The problem arises due to the denominator term used in the percentage of occurrence ratio i.e. the total number of days of observed scintillation activity during the complete period under consideration. But the conventional percentage of occurrence methodology uses the number of days of observation (the total number of days for which data is available) during each month in the denominator. It correctly assigns the maximum occurrence to March 2014 instead of April 2013 and the obtained monthly statistics follow the solar activity during this period.     

GPS scintillation and TEC depletion near the northern crest of equatorial anomaly over South China

This study presents a statistical analysis of GPS L-band scintillation with data observed from July 2008 to March 2012 at the northern crest of equatorial anomaly stations in Guangzhou and Shenzhen of South China. The variations of the scintillation with local time, season, solar activity and duration of scintillation patches were investigated. The relationship between the scintillation and TEC depletion was also reported. Our results revealed that GPS scintillation occurred from 19:30 LT (pre-midnight) to 03:00 LT (post-midnight). During quiet solar activity years, the scintillation was only observed in pre-midnight hours of equinox months and patches durations were mostly less than 60 min. During high solar activity years, more scintillation occurred in the pre-midnight hours of equinox and winter months; and GPS scintillation started to occur in the post-midnight hours of summer and winter. The duration of scintillation patches extended to 180 min in high solar activity years. Solar activity had a larger effect to strong scintillations (S₄ > 0.6) than to weak scintillations (0.6 ? S₄ > 0.2). Strong scintillations were accompanied by TEC depletion especially in equinox months. We also discussed the relationship between TEC depletion and plasma bubble.     

面向L 波段导航监视功能的波形兼容管理技术研究

随着射频综合技术的发展，各射频功能之间的耦合性越来越高，对其兼容管理的需求越来越大。本 文基于某型综合射频系统项目，针对L 波段通用波形的兼容管理开展了技术论证和研究。结果表明，该射频兼 容管理措施可以有效保证L 波段导航监视功能波形正常工作。