某型飞机加装空中受油状态改进电传系统研究

为满足未来战争需要,某型飞机根据空中加油对受油飞机的要求,对该型飞机电传操纵系统进行了加装设计.仿真结果表明,经过重新设计的电传操纵系统,在空中加油状态下,飞机稳定性增加,并且能在规定范围内稳定地改变和保持姿态角,从而跟踪加油机的姿态变化.本文提出了依靠三维大气紊流场的方法,建立了空中加油状态下飞机动力学模型.设计出了加装空中受油后的控制规律,得到了受油状态下的仿真结果,对电传操纵系统加装空中受油技术实现进行了展望.     

在轨航天器地气光环境分析

为得出定量化的遥感观测地气光环境数据,建立了简化的航天器地气光分布计算模型,首先将航天器及其各类运行轨道归纳到统一的照明模式中,地气光的分布主要考察航天器轨道面与地球晨昏面的夹角,然后考察航天器在每轨中的具体相位,以建立照度的几何传递关系;随后考察太阳辐照经地表后,最终到达航天器遥感观测载荷的光照度.计算结果能反映地气光在载荷观测方向2π半球视场内的分布情况,根据分布随空间变化的具体量级,对不同的离轴角进行照度积分,可转化为对观测仪器的地气光抑制能力要求.      

高空长航时无人机高精度自主定位方法

针对传统基于轨道动力学模型及非线性滤波进行间接敏感地平天文导航定位方法在实际应用中的局限性,提出了一种适用于高空长航时无人机自主导航定位的快速间接敏感地平天文解析定位新方法。分析了星光折射视高度天文量测的机理,导出天文三维定位的解析表达式,详细阐述了利用最小二乘微分校正法代替非线性滤波的天文定位方法,通过直接求解非线性量测方程组即可得到飞行器的精确位置信息,并对这种定位方法的定位精度进行了理论分析。该天文定位方法利用了星光折射间接敏感地平精度高的特点,又不需要飞行器动力学模型也不需要任何先验知识,算法简单可靠,计算量小,而定位精度与传统方法相当。最后,通过计算机仿真,验证了这种天文定位方法的有效性。     

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.     

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.      

A numerical model approximating extreme energetic electron events involved in the physical and chemical processes of the middle atmosphere

Relativistic electrons (with energies >150 keV) which originate in the outer radiation belt and detected by the Russian ‘Meteor’ series of satellites have been correlated with the atmospheric total ozone data compiled by almost 90 stations located around the world within the latitude zone 40°–70°N. In more than 60% of the stations examined we have detected a clear decrease of the ozone 3–5 days after the electron flux excess. A numerical model has been applied to approximate this effect based on relativistic electron initiated nitric oxides creation in the upper mesosphere with subsequent atmospheric transport (both vertical and horizontal) towards the upper stratosphere. A first attempt of local and temporal prediction of ozone depletion because of energetic electrons impact in the middle atmosphere has been illustrated.     

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.     

临边昏暗在恒星角直径测量中的影响

讨论了恒星临力昏暗在恒星角直径测量中的影响。研究表明,相对于二项式近似而言,ＵＤ模型和线性模型均对恒星角直径测量有所低估,在线性临力昏暗系数较小时,这种影最大,ＵＤ和一近似与二项式近似的差别最多分别达２５．５％和１２．６％;而在线性系数值趋近于１时,其相互差别随之可以忽略。而新旧线性临边近似之间对于恒星角直径测量的影响似乎并不很大。最后我们认为非线性临边昏暗效应的影响不可忽略。     

固液混合火箭发动机喷焰红外辐射特性分析

为了研究固液混合火箭发动机喷焰在不同飞行状态的红外辐射特性,建立了固液两相状态下喷焰的红外辐射计算模型,获得了喷焰在2~12μm波段的红外辐射.将喷焰的温度、压力、摩尔组分等作为输入条件,米氏散射(Mie)模型计算颗粒相的散射,采用有限体积法(FVM)离散辐射传递方程,利用中分辨率大气辐射传输(MODTRAN)模型计算不同观测距离的大气透过率,编程计算得到不同飞行高度,不同观测方向下喷焰的红外辐射.结果表明喷焰红外辐射亮度与温度分布类似,在2.7~3.0μm和4.2~4.5μm波段范围内的辐射较强,高温粒子在近红外比远红外对总辐射的贡献大,太空与地面观测不同飞行高度的发动机喷焰辐射率因大气衰减的不同而有所差异,可为目标跟踪与发动机设计提供参考.      

Gravity wave propagation studies using the Indian MST radar observations

The Indian MST radar facility at Gadanki (13.5°N, 79.2°E) has been utilised to study the propagation of gravity waves from the troposphere/lower stratosphere to the mesosphere and their interaction with the radar backscattered signal variations. The main objective is to correlate vertically propagating gravity waves derived from the tropospheric velocity fields with the dynamics of mesospheric scattering centres. The tropospheric wind velocities and signal strengths over the entire height range have been subjected to power spectral and wavelet analysis to determine the predominant wave periods/amplitudes and the coupling between the lower atmosphere and mesosphere. Results show that (a) the gravity waves are clearly detectable near tropopause heights, (b) while relatively higher period gravity waves (20–50 min) interact with mesospheric scattering centres, the lower period waves (<20 min) are absorbed in the troposphere itself, (c) the mesospheric scattering layers are affected by gravity waves of complementary periods.