时变加权LQT设计方法理论推导及应用

利用矩阵运算公式和极值原理,对时变加权性能指标下的线性二次型跟踪器(LQT)迭代方程进行了理论推导。以F-16飞机为例,利用飞行控制经验构建俯仰速率控制系统线性框图。在MATLAB/Simulink环境下,针对两种时变加权性能指标和一种定常加权性能指标,利用多变量优化算法完成了一个状态点的控制律参数设计,并进行了时域和频域对比分析,初步验证了时变加权LQT设计方法的工程可行性和有效性。     

空空作战飞机敏感性分析研究

为分析战斗机作战能力的敏感性，通过建立战斗机作战能力的指标体系，综合使用幂指数法和模糊参 差分析法对战斗机作战能力进行评估。采用基于方差的全局敏感性分析方法sobol 指数法分析战斗机作战能力 的敏感性，得到选取的输入变量的重要度排序和变量间的交互效应，将结果与熵值法结果进行对比，比较分析 sobol 指数法作敏感性分析的优势。     

Investigation of Satellite Trace (ST) and Multi-reflected Echo (MRE) ionogram signatures and its possible correlation to nighttime spread F development from Cyprus over the solar mini-max (2009–2016)

Multi-reflected echoes (MREs) and satellite traces (STs) are referred in literature as ionogram signatures of Travelling Ionospheric Disturbances (TIDs) which is a phenomenon that apparently drives spread F development mainly at nighttime mid-latitude ionosphere. A long-term statistical study has been undertaken to investigate the morphological aspect of these signatures over the lower midlatitude European station of Nicosia, Cyprus (35.19°N, 33.38°E geographic; magnetic dip. 29.38°N) by inspecting all ionograms recorded by the DPS-4D digisonde in the interval 2009–2016. The results underline the systematic manifestation of these TID signatures over Cyprus with a possible (although not quite clear) solar activity dependence and a distinctive seasonal and diurnal occurrence rate with a seasonal peak of STs during summer and of MREs during January to April. Based on the experimental results of the present study, the seasonal occurrence rate of MREs and STs is found to increase by 75% and 56% during high solar activity periods. Satellite traces are well known ionogram signatures of TIDs and mostly correlated to the nighttime spread F formation. The occurrence of mid-latitude spread Fs over European longitude sector normally increases during summer. The occurrences of TIDs are also prominent at this interval of the year over nighttime mid-latitude ionosphere. The presence of MREs as an ionogram signature of TIDs over mid-latitude ionosphere is unique in nature.     

Black-hole transients: From QPOs to relativistic jets

Due to the impressive amount of new data provided by the RXTE satellite in the past decade, our knowledge of the phenomenology of accretion onto black holes has increased considerably. In particular, it has been possible to schematize the outburst evolution of transient systems on the basis of their spectral and timing properties, and link them to the ejection of relativistic jets as observed in the radio. Here, I present this scheme, concentrating on the properties of the quasi-periodic oscillations observed in the light curves and on the link with jet ejection.     

Solar Influences on Dynamical Coupling Between the Stratosphere and Troposphere

We use a simplified atmospheric general circulation model (AGCM) to investigate the response of the lower atmosphere to thermal perturbations in the lower stratosphere. The results show that generic heating of the lower stratosphere tends to weaken the sub-tropical jets and the tropospheric mean meridional circulations. The positions of the jets, and the extent of the Hadley cells, respond to the distribution of the stratospheric heating, with low latitude heating displacing them poleward, and uniform heating displacing them equatorward. The patterns of response to the low latitude heating are similar to those found to be associated with solar variability in previous observational data analysis, and to the effects of varying solar UV radiation in sophisticated AGCMs. In order to investigate the chain of causality involved in converting the stratospheric thermal forcing to a tropospheric climate signal we conduct an experiment which uses an ensemble of model spin-ups to analyse the time development of the response to an applied stratospheric perturbation. We find that the initial effect of the change in static stability at the tropopause is to reduce the eddy momentum flux convergence in this region. This is followed by a vertical transfer of the momentum forcing anomaly by an anomalous mean circulation to the surface, where it is partly balanced by surface stress anomalies. The unbalanced part drives the evolution of the vertically integrated zonal flow. We conclude that solar heating of the stratosphere may produce changes in the circulation of the troposphere even without any direct forcing below the tropopause. We suggest that the impact of the stratospheric changes on wave propagation is key to the mechanisms involved.     

基于综合指标的最优冗余陀螺配置确定方法

陀螺是航天器控制系统中的关键姿态敏感器,其主要采取冗余措施进行配置。针对航天器控制系统设计中如何进行陀螺冗余配置的问题,提出了一种确定最优冗余陀螺配置的方法,该方法综合考虑了系统的可靠性、精度、成本代价等综合指标。首先,以工程中普遍采用的陀螺斜置式为对象,系统性给出了陀螺斜置式的安装结构,并以测量误差最小为目标确定出确定安装数目下的最优陀螺冗余安装结构。其次,结合实际工程经验对陀螺冗余配置的综合性能指标进行详细系统的分析。然后,利用优化评价方法以综合指标为基础对不同安装数目下的陀螺冗余安装结构进行综合评价,确定出陀螺冗余配置的最优安装数目,即最优冗余陀螺配置。最后,利用该方法对实际工程中的斜置式陀螺冗余配置进行分析和计算。结果表明,当陀螺的安装数目为7时为最优冗余配置,该结论对实际工程具有理论指导作用。     

飞机燃油箱惰化中氧体积分数控制指标分析

对油箱惰化的氧体积分数控制指标,即极限氧体积分数,测定标准、理论与实验研究成果进行了较为系统地梳理与总结,并基于前人研究成果提出:①采用N2惰化时,对于RP-3燃油,其地面状态下,可采用12%作为油箱氧体积分数控制指标。②对于民机,飞行包线内燃油箱氧体积分数控制指标可为从海平面到3 048 m高度,油箱内气相空间极限氧体积分数不超过12%,3 048～12 192 m高度,不超过从12%线性增加到145%;对于军机,可以考虑在民机标准上增加20%安全裕度,即从地面的9%线性增加至12 192 m的12%。③目前国内军机惰化系统研制中,规定在整个飞行包线内控制燃油箱气相空间氧体积分数不超过9%的要求值得商榷,它将直接带来因过度防护而产生的代偿损失过大等问题。     

S形进气道流路造型方法及其对性能影响的研究

根据S形进气道的几何边界条件,提出了一种基于多项式的中心线及面积分布率曲线的流路造型方法。选择不同的拐点位置,采用该方法构造了9条具有代表性的中心线及面积分布率方程。组合不同的中心线和面积分布率曲线建立了相应的S形进气道的几何造型,并采用三维N-S方程进行求解,得到了总压恢复系数和DC60等性能指标。分析计算结果表明,中心线对S形进气道总压恢复和出口动压起着主要影响,随着中心线方程拐点位置后移,S形进气道总压恢复系数和出口动压呈明显增加趋势;中心线和面积分布率组合共同影响着DC60指标,当中心线拐点过于靠近进气道进口而面积分布率曲线拐点靠近进气道出口时,进气道下游的涡将会发展到出口,从而大幅度影响DC60指标。     

军用运输机运输效能指标

给出了运输任务类型和运输效能定义,从效果与耗费两方面着手建立了运输效能指标体系,将运输效能归纳为安全性、质量或体积、距离、准确性、时间、场地、人员、设备及费用等9种因素,在确立各个因素运输效能单项指标的基础上提出了一种运输效能综合指标,以四种典型运输任务为例,建立了常用的运输效能指标。     

Rainfall retrieval over Indian land and oceanic regions from SSM/I microwave data

Present study focuses on the estimation of rainfall over Indian land and oceanic regions from the Special Sensor Microwave/Imager (SSM/I) on the Defense Meteorological Satellite Program (DMSP) F-13. Based on the measurements at 19.35, 22.235 and 85.5 GHz channels of SSM/I Satellite, scattering index (SI) has been developed for the Indian land and oceanic regions separately. These scattering indices were co-located against rainfall from Precipitation Radar (PR) onboard Tropical Rainfall Measuring Mission (TRMM) to develop a new regional relationship between the SI and the rain rate for the Indian land and oceanic regions. A non-linear fit between the rain rate and the SI is established for rain measurement. In order to have confidence in our method, we have also estimated rainfall using the global rainfall and scattering index relationship developed by Ferraro and Marks [Ferraro, R.R., Marks, G.F. The development of SSM/I rain rate retrieval algorithms using ground based radar measurements. J. Atmos. Ocean. Technol. 12, 755–770, 1995]. The validation with the rain-gauge shows that the present scheme is able to retrieve rainfall with better accuracy than that of Ferraro and Marks (1995). Further intercomparison with TRMM-2A12 and validation with rain-gauges rainfall showed that the present algorithm is able to retrieve the rainfall with reasonably good accuracy.