快速爬升的奇异摄动中制导律设计

为满足实际作战的要求,基于最优控制理论和奇异摄动方法,提出了一种可保证中远程空地导弹快速爬升到最优高度的中制导律.它由变系数最优爬升控制,最小能量巡航控制和最小能量下滑控制组成.为了减小爬升段控制对下滑段的影响,提出了一种新的控制逻辑.最后针对某型空地导弹进行了仿真.结果表明,该中制导律较好地满足了中远程空地导弹在中制导段的要求.本文的研究结果具有较好地工程参考价值.     

并行加工系统一类排序问题的最优解

讨论了将多个零件分派给并行加工系统加工的排序问题.假设同一零件分配给不同的设备,其加工时间不同,分析了使所有零件的总花费时间(加工时间与等待时间之和)最小的排序方法.首先建立了该类问题的数学模型,然后将其转化为指派问题,通过匈牙利算法可以得到最优解.所得算法的时间复杂性是多项式界的.最后给出了一个数值例子说明求解过程.     

闭环FOG的自诊断及在RSDIMU中的应用

首先阐述了闭环干涉型光纤陀螺(I-FOG)中回路的特点,揭示了它的自诊断能力.由此给出了一种具有自诊断能力的闭环干涉型光纤陀螺并将它应用于一种容错捷联惯性测量单元(RSDIMU)中,针对该单元,设计了一种容错算法.该算法除了利用陀螺的输出外,还引入了它的自诊断信息,从而实现了仪表级的信息冗余,使这种RSDIMU的容错能力由原来的故障运行(FO)-故障运行(FO)-故障安全(FS)上升到FO-FO-FO-FO-FS.用Markov可靠性估计模型对该系统的估计表明,其可靠性也有了很大的提高.      

可见光红外自旋扫描辐射计数据处理方法

原始云图数据缓冲处理方法是ＦＹ－２号静止气象卫星ＣＤＡＳ原始云图处理分系统研制的关键问题直接关系到产生的展宽云图的精度和质量。     

基于卫星加速度数据反演的热层大气密度与NRLMSISE-00模式结果的比较研究

利用CHAMP/STAR加速度数据反演的热层大气密度与NRLMSISE-00模式反演的热层大气密度进行比较, 结果表明, 热层大气密度在春秋季期间高于冬夏季, 并且太阳活动高年比低年更加显著; 日照面和阴影区大气密度的比值在低纬地区由太阳活动高年的4下降到太阳活动低年的2左右, 中纬地区大约由3变化到1.5, 高纬地区变化较小; NRLMSISE-00模式能够较好地模拟热层大气密度的变化趋势, 但是磁暴期间模式精度较差. 统计结果表明, 模式整体比反演结果偏高, 2002-2008年相对偏差分别为16.512%, 20.004%, 18.915%, 18.245%, 25.161%, 33.261%和41.980%; NRLMSISE-00模式在高纬地区的相对偏差为27.337%, 高于中低纬地区的24.047%; 模式在中等太阳活动水平相对偏差较为稳定, 基本在15%左右.     

含钟差修正的脉冲星和太阳观测组合导航

为提高深空探测器巡航段的导航定位精度和钟差修正能力,提出一种利用X射线脉冲星和太阳观测信息的组合导航方法.利用脉冲星导航的脉冲到达时间测量值,同时利用太阳敏感器、分光计分别测量太阳视线矢量和探测器相对于太阳的径向速度,并将星载时钟钟差增广为状态变量,构建组合导航系统,利用基于扩展卡尔曼滤波的UD(Upper triangular matrix-Diagonal matrix)分解信息融合算法进行状态估计.仿真结果表明,该方法能有效解决因钟差漂移引起的导航滤波发散问题,同脉冲星导航相比,该方法提高了定位精度和钟差修正能力.     

基于多目标的消磁绕组优化调整方法

针对目前舰船消磁绕组优化调整方法中只考虑舰艇磁场信号幅值而较少考虑磁场梯度信号幅值的不足,提出同时以磁场幅值和磁场梯度幅值削减为目标的优化调整方法.为此,首先以线圈等效电流值为优化对象,磁场和梯度峰值为优化目标,建立了消磁绕组优化调整的多目标数学模型;随后采用多目标微粒群算法求解得到了该优化问题的Pareto解集;最后通过一个计算实例验证了方法的有效性.实例结果表明该方法能够同时处理磁场和磁场梯度幅值,并能给出多种不同等效电流组合以供选择使用.     

Noise analysis of continuous GPS coordinate time series for CMONOC

The Crustal Movement Observation Network of China (CMONOC) is one of the major scientific infrastructures, mainly using Global Positioning System (GPS) measurements, to monitor crustal deformation in the Chinese mainland. In this paper, decade-long coordinate time series of 26 continuous GPS sites of CMONOC are analyzed for their noise content using maximum likelihood estimation (MLE). We study the noise properties of continuous GPS time series of CMONOC for the unfiltered, filtered solutions and also the common mode signals in terms of power law plus white noise model. In the spatial filtering, we remove for every time series a common mode error that was estimated from a modified stacking of position residuals from other sites within ∼1000 km of the selected site. We find that the common mode signal in our network has a combination of spatially correlated flicker noise and a common white noise with large spatial extent. We demonstrate that for the unfiltered solutions of CMONOC continuous GPS sites the main colored noise is a flicker process, with a mean spectral index of ∼1. For the filtered solutions, the main colored noise is a general power law process, indicating that a major number of the filtered regional solutions have a combination of noise sources or local effects. The velocity uncertainties from CMONOC continuous GPS coordinate time series may be underestimated by factors of 8–16 if a pure white noise model is assumed. In addition, using a white plus flicker noise model, the median values of velocity errors for the unfiltered solutions are 0.16 (north), 0.17 (east) and 0.58 (vertical) mm/yr, and the median values for the filtered solutions are 0.09 (north), 0.10 (east) and 0.40 (vertical) mm/yr.     

A nonlinear background removal method for seismo-ionospheric anomaly analysis under a complex solar activity scenario: A case study of the M9.0 Tohoku earthquake

A precise determination of ionospheric total electron content (TEC) anomaly variations that are likely associated with large earthquakes as observed by global positioning system (GPS) requires the elimination of the ionospheric effect from irregular solar electromagnetic radiation. In particular, revealing the seismo-ionospheric anomalies when earthquakes occurred during periods of high solar activity is of utmost importance. To overcome this constraint, a multiresolution time series processing technique based on wavelet transform applicable to global ionosphere map (GIM) TEC data was used to remove the nonlinear effect from solar radiation for the earthquake that struck Tohoku, Japan, on 11 March, 2011. As a result, it was found that the extracted TEC have a good correlation with the measured solar extreme ultraviolet flux in 26–34 nm (EUV_26–34) and the 10.7 cm solar radio flux (F_10.7). After removing the influence of solar radiation origin in GIM TEC, the analysis results show that the TEC around the forthcoming epicenter and its conjugate were significantly enhanced in the afternoon period of 8 March 2011, 3 days before the earthquake. The spatial distributions of the TEC anomalous and extreme enhancements indicate that the earthquake preparation process had brought with a TEC anomaly area of size approximately 1650 and 5700 km in the latitudinal and longitudinal directions, respectively.     

中层大气受迫Rossby波包的非线性相互作用：Ⅱ.数值计算

本文对中层大气受迫Ｒｏｓｓｂｙ波包的非线性三波相互作用问题作了进一步的数值分析，结果表明，三个波包随时间演化达到的平衡态与文献［１］的理论结果完全一致，而且仅当系统中只有中等波长波包不受外源强迫时，系统运动有可能出现两个稳定平衡态，在一定外源强度范围内，平衡态会产生尖点突变，平衡态随外源的变化有滞后分岔的特征，系统运动最终达到的平衡态不仅与外源强度的变化方式有关，而且依赖于初始状态。