直升机目标的雷达特性分析

为了研究直升机目标的雷达特性,采用了理论分析、统计分析和性能指标体系分析的方法,对直升机与固定翼飞机、不同直升机之间目标的雷达特性进行了对比分析;建立了直升机的雷达特性统计模型,对统计特性结果进行了分析;采用性能指标体系分析的方法对旋翼调制特性进行了分析,得到了直升机目标的雷达特性影响因素和分布规律。其方法和结果可以作为直升机系统、防空武器系统和直升机靶标的设计参考。     

基于惯性系的双轴旋转式惯导系统转位方法

针对双轴旋转式惯导系统中不能自动补偿标度因数误差与地球自转耦合误差的问题,提出了一种改进的转位方法。该方法不增加转轴数目,通过补偿地球自转在转轴平面的投影抑制耦合误差项,计算结果表明该方法适用于激光陀螺惯导系统和光纤陀螺惯导系统。利用改进的转位方法对双轴旋转式惯导系统进行仿真,仿真结果验证了该方法的可行性。研究结果为双轴旋转式惯导系统的工程设计和改进提供了一定的理论支持。     

极端太阳风条件下的磁层顶位形

基于极端太阳风条件下的三维MHD数值模拟数据, 构建了一种极端太阳风条件下的三维非对称磁层顶位形模型. 所提出的模型考虑了行星际南向磁场(IMF) B_z日下点距离侵蚀的饱和效应, 太阳风动压B_d对磁层顶张角影响的饱和效应, 赤道面、昼夜子午面磁层顶的不对称性以及极尖区的内凹结构和内凹中心的移动, 并利用Levenberg-Marquart多参量非线性拟合方法拟合了模型参数. 数值模拟研究表明, 在极端太阳风条件下, 随B_d增大, 磁层顶日下点距离减小, 磁层顶磁尾张角几乎不变; 随南向(IMF)B_z增大, 磁层顶日下点距离略有减小, 磁层顶磁尾张角减小, 极尖区内凹中心向低纬移动. 通过对2010年8月1日太阳风暴事件验证发现, 本文所建立的模型能够描述极端太阳风条件下的三维磁层顶位形.      

太阳风暴及其对人类社会活动的影响

第24个太阳活动周峰年即将到来。太阳风暴由于其给现代人类社会活动带来的巨大灾难,引起了越来越多的关住。文章首先回顾了太阳风暴及其对人类社会活动的影响,然后对历史上1859年卡林顿事件中太阳风暴和近几十年来著名的太阳风暴的强度进行了比较,最后简要介绍了太阳风暴所涉及的科学和技术问题,并且提出了减轻太阳风暴给社会活动带来灾害的对策。     

可重构自适应无线电引信干扰技术研究

根据无线电引信的工作特点,提出了可重构自适应无线电引信干扰技术。设计了自适应无线电引信干扰技术方案,分析了无线电引信信号调制识别技术。对该技术的应用前景进行了展望。     

Comparison of Diurnal,Seasonal and Solar Cycle Variations of High-latitude,Mid-latitude and Low-latitude Ionosphere

Comparison of regular (diurnal, seasonal and solar cycle) variations of high-latitude,mid-latitude and low-latitude ionospheric characteristics has been provided on basis of local empirical models of the peak electron density and the peak height. The local empirical models were derived from the hand-scaled ionogram data recorded by DPS-4 digisondes located at Norilsk (69°N, 88°E), Irkutsk (52°N, 104°E) and Hainan (19°N, 109°E) for a 6-year period from December, 2002 to December, 2008. The technique used to build the local empirical model is described. The primary focus is diurnal-seasonal behavior under low solar activity and its change with increasing solar activity. Both common and specific features of the high-latitude (Norilsk), mid-latitude (Irkutsk) and low-latitude (Hainan) regular variations were revealed using their local empirical models.      

Moderate geomagnetic storms of January 22–25, 2012 and their influences on the wave components in ionosphere and upper stratosphere-mesosphere regions

Moderate geomagnetic storms occurred during January 22–25, 2012 period. The geomagnetic storms are characterized by different indices and parameters. The SYM-H value on January 22 increased abruptly to 67 nT at sudden storm commencement (SSC), followed by a sharp decrease to −87 nT. A second SSC on January 24 followed by a shock on January 25 was also observed. These SSCs before the main storms and the short recovery periods imply the geomagnetic storms are CME  -driven. The sudden jump of solar wind dynamic pressure and IMF _Bz$B_z$ are also consistent with occurrence of CMEs. This is also reflected in the change in total electron content (TEC) during the storm relative to quiet days globally. The response of the ionospheric to geomagnetic storms can also be detected from wave components that account for the majority of TEC variance during the period. The dominant coherent modes of TEC variability are diurnal and semidiurnal signals which account upto 83% and 30% of the total TEC variance over fairly exclusive ionospheric regions respectively. Comparison of TEC anomalies attributed to diurnal (DW1) and semidiurnal (SW2) tides, as well as stationary planetary waves (SPW1) at 12 UTC shows enhancement in the positive anomalies following the storm. Moreover, the impact of the geomagnetic storms are distinctly marked in the daily time series of amplitudes of DW1, SW2 and SPW1. The abrupt changes in amplitudes of DW1 (5 TECU) and SW2 (2 TECU) are observed within 20°S–20°N latitude band and along 20°N respectively while that of SPW1 is about 3 TECU. Coherent oscillation with a period of 2.4 days between interplanetary magnetic field and TEC was detected during the storm. This oscillation is also detected in the amplitudes of DW1 over EIA regions in both hemispheres. Eventhough upward coupling of quasi two day wave (QTDWs) of the same periodicity, known to have caused such oscillation, are detected in both ionosphere and upper stratosphere, this one can likely be attributed to the geomagnetic storm as it happens after the storm commencement. Moreover, further analysis has indicated that QTDWs in the ionosphere are strengthened as a result of coherent oscillation of interplanetary magnetic field with the same frequency as QTDWs. On the otherhand, occurrences of minor SSW and geomagnetic storms in quick succession complicated clear demarcation of attribution of the respective events to variability of QTDWs amplitudes over upper stratosphere.     

宽带卫星通信信号的多维星座图解调方法

高速卫星数据传输需要利用较高调制维度和较多星座点数来实现,一方面导致接收端具有较大实现复杂度,另一方面系统可靠性极易受信道非线性影响。针对以上问题,通过对多维星座图信号的解调性能进行理论分析,得到极大后验概率（MAP）解调误符号率（SER）的理论公式,在保证系统SER性能的基础上,提出了基于星座图相关的检测方法。该方法利用脉冲正交性得到接收星座点,对其进行向量相关运算得到解调数据,有效降低了解调判决过程的复杂度。针对信号经过高功率放大器（HPA）后的非线性失真问题,建立了HPA信道估计模型,利用最小二乘（LS）信道估计方法对原解调星座图进行修正,提出了基于修正星座图的解调方法。仿真结果表明,该方法在降低实现复杂度的同时,有效提高了系统抗HPA信道非线性失真的能力,可实现对宽带高速卫星通信信号的高效准确解调。     

零偏模式下太阳光压对轨迹保持控制影响分析

从某颗在轨卫星地面轨迹漂移“异常”出发,分析了该现象发生的内在机理,建立了零偏模式下（卫星姿态偏航角保持为零）光压摄动力沿迹方向累积效应解析模型,并基于历史观测数据通过轨道改进估计模型参数。最后,利用该卫星2018年真实地面轨迹对新模型预报精度进行验证。结果表明,采用新模型后,卫星地面轨迹漂移预报误差得到明显改善,为该卫星轨迹保持控制策略制定提供了技术支持。     

近月空间带电粒子环境——“嫦娥1号”“嫦娥2号”观测结果

“嫦娥1号”（CE-1）、“嫦娥2号”（CE-2）都安装了1台太阳高能粒子探测器（High-energetic ParticlesDetectors,HPD）和2台太阳风离子探测器（Solar Wind Ion Detectors,SWIDs）,进行了月球轨道200 km和100 km空间环境探测,获得了月球轨道空间高能带电粒子（质子、电子和重离子）能谱随时间的演化特征、等离子体与月球相互作用特征以及太阳风离子速度、密度和温度参量。空间环境探测数据分析结果表明：太阳活动低年、空间环境扰动水平相对较低、月球处于太阳风中时,近月空间带电粒子环境的基本特征与行星际空间相比变化不大。CE-1、CE-2在轨运行期间,发现了多起0.1～2 MeV能量电子急剧增加事件,这些事件发生在月球从太阳风运动到磁尾的所有空间区域,其中20%的事件伴随着卫星周围等离子体离子加速。模拟和统计研究表明：能量电子急剧增加使得绕月卫星和月球表面电位大幅下降导致了离子加速现象的发生;能量电子总流量大于10¹¹ cm^-2时,绕月卫星和月球表面充电电位可达负的上千伏。此外,月表溅射与反射太阳风离子、太阳风“拾起”离子等空间环境事件的发现,揭示了太阳风离子和月球存在复杂的相互作用过程。