某涡喷发动机中介机匣振动模态分析

用多点激振单点拾振的脉冲激励试验模态测试方法，对某涡喷发动机中介机匣的振动特性进行了模态分析，对比了模型机中介机匣与改型机中介机匣的振动模态，试验结果表明模型机中介机匣在结构设计方面存在薄弱环节，其结果为某涡喷发动机结构设计、振动故障分析提供了依据。     

A comprehensive study on middle atmospheric thermal structure over a tropic and sub-tropic stations

The general characteristics of middle atmospheric thermal structure have been studied by making use of the Rayleigh lidar data collected over the period of about four years (1998–2001). Here, the data has been used from two different stations in the Indian sub-continent in tropics (Gadanki; 13.5°N, 79.2°E) and in sub-tropics (Mt. Abu; 24.5°N, 72.7°E). The observed monthly mean temperature profiles are compared with different model atmospheres (CIRA-86 and MSISE-90). We observed, the mean temperature profiles have closer agreement with MSISE-90 than CIRA-86. The temperature profiles measured by lidar and HALOE satellite overpass nearby lidar site are generally in agreement with each other. The systematic and statistical errors in deriving temperature are found to be uniform for both the stations, as 1 K at 50 km, 3 K at 60 km and 10 K at 70 km. The special features of mesospheric temperature inversion (MTI) and double stratopause structure (DBS) are also addressed for both the stations.     

我国地区20—80km高空大气温度特征

利用Nimbus-7卫星1979-1981年的平流层和中间层大气温度探测(SAMS)数据,首次较全面地分析了我国上空20-80km高度大气温度的分布特征,并与COSPAR国际参考大气CIRA-1986进行了比较.结果指出,我国上空大气温度分布与COSPAR国际参考大气CIRA-1986的缔向平均温度分布存在一定差别,可供航空航天工作者参考.     

双层卫星网络中MEO与LEO卫星连接度分析

分析了在星座结构参数确定的条件下，中轨道／低轨道(MEO／LEO)双层卫星网络弱连接模型中层间连接度参数的选取。给出了连接度的理论分析和仿真结果，证明了在MEO／LEO双层卫星网络中，MEO卫星不应与其视距范围内的所有LEO卫星建立星间链路连接，而须根据MEO和LEO卫星间仰角等参数作出合理选择。     

雷达寻的技术在远程精确制导导弹中的应用

论述了远程精确制导导弹末段雷达寻的装置的制约因素．分析了末段可机动最小距离、探测域、电磁静默、杂波和目标识别等的影响。在比较时域一维、频域一维、时频二维和合成孔径雷达(SAR)等高分辨处理的基础上．提出了高分辨探测的主要技术途径。最后给出了一个主被动复合寻的系统和SAR探测装置的工作模式。     

A simple model for the interhemispheric coupling of the middle atmosphere circulation

The interhemispheric coupling of the middle atmosphere general circulation is characterized by a global anomaly pattern of the zonal-mean temperature. This pattern reflects an anomalous stratospheric and mesospheric residual circulation, in which a weaker (stronger) stratospheric winter circulation is linked to an upward (downward) shift of its upper mesospheric branch reaching from the summer to the winter pole. This phenomenon is robust in observational data and several middle atmosphere general circulation models. In the present study, the recently proposed mechanism of the interhemispheric coupling is unequivocally proven within the framework of a zonally symmetric model that excludes any additional effects due to resolved waves and non-zonally propagating gravity waves. Two simulations are conducted that differ in the strength of the polar vortex. A weaker polar vortex results in a downward shift of the winter mesospheric gravity wave drag. This leads to changes also in the summer upper mesosphere via a feedback solely between gravity wave breaking and the zonal-mean state. The accompanying temperature anomaly reproduces the pattern of the interhemispheric coupling.     

基于改进伪谱反馈控制的远程变轨闭环制导

利用最优反馈控制和轨迹快速重构技术,设计一种有限推力空间远程变轨自适应闭环制导方法。首先给出了最优反馈控制的求解原理和必要条件。将空间变轨动力学模型特点和伪谱法相结合,设计基于状态量缩减的计算效率改进策略以提高轨迹优化的实时性。基于改进伪谱法进行逐次轨迹快速重构,利用开环最优解形成闭环反馈,从而保证制导指令的实时更新,并通过引入控制逻辑改进制导算法。远程交会仿真表明,该闭环制导方法在保证任务指标具有一定最优性的同时,可以有效抑制多种参数不确定性和外界干扰的影响,具有较高的制导精度、自适应性和鲁棒性。     

利用Aura卫星资料计算全球中层大气背景风场

利用2005年第二代地球观测卫星系统(EOS)的Aura卫星上MLS观测的压强、温度、密度等数据,推算出全球中层大气的平均背景风场,分析了中层大气风场随时间和高度变化的特点.与武汉流星雷达及澳大利亚Adelaide台站观测的比较结果显示,用Aura数据推算出来的风场与实际观测比较符合.与HWM-93模式的比较显示,Aura风场随时间和空间变化的总体趋势与HWM-93基本吻合.特别是在80km以下的高度范围内Aura数据与HWM-93数据符合得比较好;在80 km以上的高度,Aura所算得的风值与HWM-93风值的差别逐渐增大,Aura风值普遍比HWM-93的要大.     

Advances in the Researches in Middle and Upper Atmosphere in 2006-2008

This paper summarizes the research results obtained by Chinese scientists and/or through international collaborations in 2006-2008. Specifically, this paper focus on the research fields in the middle and upper atmosphere, including developments in facilities and instruments, and the advancements in scientific issues.     

Semi-empirical model of middle atmosphere wind from the ground to the lower thermosphere

During recent years, special attention has been paid to understanding the background circulation of the middle atmosphere. Particularly in the mesosphere/lower thermosphere (MLT) region, this has involved including data from a range of new radar measurements. It has also involved the comparison of existing empirical middle atmosphere wind models, such as CIRA-86 and HWM-93 to the new data. This has led to the construction of empirical models of MLT winds such as the Global Empirical Wind Model (GEWM). Further investigations are aimed at the construction of new empirical and semi-empirical wind models of the entire middle atmosphere including these new experimental results. The results of a new wind climatology (0–100 km) are presented here, based upon the GEWM, a reanalysis of stratospheric data, and a numerical model which is used to fill the gap between data from the stratospheric and MLT regions.