星载GNSS确定GEO卫星轨道的积分滤波方法

采用星载全球导航卫星系统（GNSS）确定地球静止轨道（GEO）,以解决目前应用星载全球定位系统(GPS)时导航卫星可见性差的问题。以风云卫星为例,分析了未来的GNSS相对于GEO卫星的可见性,针对GEO轨道上导航接收机采样间隔较长的问题,综合轨道积分和卡尔曼滤波方法的优点,提出了确定GEO卫星轨道的积分滤波方法。并利用STK软件仿真产生所需数据,用MATLAB对提出的算法编程并进行仿真验证,结果表明,提出的方法性能优越,定轨精度较高。     

月地转移轨道快速设计与特性分析

对采用直接大气再入方式的月地转移轨道,考虑大气再入界面参数和地面落点位置约束,提出了一种基于双二体模型的快速设计方法。该方法分为内外两层迭代循环,内层循环使月心段轨道和地心段轨道在月球影响球边界处连续,并采用Lambert问题与Newton-Raphson法相集合的方法求解满足再入角约束的地心段轨道参数;外层循环通过调整地心段轨道倾角和轨道置入时间使月地转移轨道满足地面落点位置约束。分析表明,存在四种类型的月地转移轨道满足大气再入界面约束,分别为降 降型、降 升型、升 降型和升 升型。在此基础上,对四种类型月地转移轨道的近地点地心距、置入分布点、再入点分布等特性进行了分析。仿真结果验证了所提出方法的有效性。     

GEO卫星广播星历的拟合参数设计

基于第一类无奇点要素的拟合参数和5°倾角旋转法,可以实现GEO发播电文与MEO和IGSO的电文一致性,但是没有完全避免数学奇异性.文章从无奇点要素的选取和主要摄动力的影响分析两方面出发,提出了一套16参数的GEO星历表示法.首先,利用同步要素描述卫星的星下点运动轨迹;其次,摄动参数中顾及了地球引力位田谐项引起的定点漂移.拟合试验表明,2h星历拟合的用户距离误差的均方根优于0.01m.     

基于三频数据的北斗卫星导航系统DCB参数精度评估方法

差分码偏差（Differential Code Biases,DCB）参数作为导航电文中重要的一项,是影响用户PNT服务的主要误差源之一。北斗卫星导航系统（后文简称“北斗系统”）发射三个频点的导航信号,在导航电文中需要发播卫星的2个TGD（Timing Group Delay）参数。文章首先介绍了北斗系统卫星DCB参数最小二乘解算与形式误差评估;其次根据北斗系统三频特点,提出了不同频点组合计算垂直方向电离层电子总含量（VTEC）互差的DCB精度定量评估方法,并与IGS(International GNSS Service)提供的GPS卫星DCB精度进行比较;最后,详细分析了DCB参数精度对用户等效距离误差（UERE）计算和定位计算的影响,分别采用卫星出场标定DCB参数和经过解算DCB参数进行评估。实测数据分析结果表明,北斗系统卫星DCB参数解算形式误差与IGS解算GPS卫星DCB参数形式误差相当,但受卫星类型和解算测站的几何分布限制,北斗系统卫星DCB参数解算不确定度相比IGS略差,估计精度优于0.5ns,不同频率组合计算VTEC互差绝对值均值优于0.6TECU。相比采用卫星出场标定值,采用系统解算DCB参数后,双频用户三维位置误差改善13.80%～47.42%。     

A global weighted mean temperature model based on empirical orthogonal function analysis

A global empirical orthogonal function (EOF) model of the tropospheric weighted mean temperature called GEOFM_Tm was developed using high-precision Global Geodetic Observing System (GGOS) Atmosphere T_m data during the years 2008–2014. Due to the quick convergence of EOF decomposition, it is possible to use the first four EOF series, which consists base functions U_k and associated coefficients P_k, to represent 99.99% of the overall variance of the original data sets and its spatial-temporal variations. Results show that U₁ displays a prominent latitude distribution profile with positive peaks located at low latitude region. U₂ manifests an asymmetric pattern that positive values occurred over 30° in the Northern Hemisphere, and negative values were observed at other regions. U₃ and U₄ displayed significant anomalies in Tibet and North America, respectively. Annual variation is the major component of the first and second associated coefficients P₁ and P₂, whereas P₃ and P₄ mainly reflects both annual and semi-annual variation components. Furthermore, the performance of constructed GEOFM_Tm was validated by comparison with GTm_III and GTm_N with different kinds of data including GGOS Atmosphere T_m data in 2015 and radiosonde data from Integrated Global Radiosonde Archive (IGRA) in 2014. Generally speaking, GEOFM_Tm can achieve the same accuracy and reliability as GTm_III and GTm_N models in a global scale, even has improved in the Antarctic and Greenland regions. The MAE and RMS of GEOFM_Tm tend to be 2.49?K and 3.14?K with respect to GGOS T_m data, respectively; and 3.38?K and 4.23?K with respect to IGRA sounding data, respectively. In addition, those three models have higher precision at low latitude than middle and high latitude regions. The magnitude of T_m remains at the range of 220–300?K, presented a high correlation with geographic latitude. In the Northern Hemisphere, there was a significant enhancement at high latitude region reaching 270?K during summer. GEOFM_Tm is capable to represent the spatiotemporal variations of T_m, with the high accuracy and reliability in a global scale, therefore, will be of great significance to the real-time GNSS water vapor inversion and climate studies.     

On the lunar node resonance of the orbital plane evolution of the Earth’s satellite orbits

This paper aims to investigate the effects of lunar node resonance on the circular medium Earth orbits (MEO). The dynamical model is established in classical Hamiltonian systems with the application of Lie transform to remove the non-resonant terms. Resonant condition, stability and phase structures are studied. The lunar node resonance occurs when the secular changing rates of the orbital node (with respect to the equator) and the lunar node (with respect to the ecliptic) form a simple integer ratio. The resonant conditions are satisfied for both inclined and equatorial orbits. The orbital plane would have long period (with typical timescales of several centuries) fluctuation due to the resonance.     

自助法中若干问题研究及其在命中精度评估中的应用

在小样本的试验评估中,自助法是一种较优的小子样方法。本文在简要阐述自助法的基础上,深入分析了自助法应用中存在的若干问题,如再抽样样本的获取方式、再抽样样本量、各样本数据容量和适用范围,并给出了自助法的实施步骤,最后比较了自助法和落入概率点小样本方法在命中精度评估中的应用效果,指出了自助法的优点。     

轨道分子屏极高真空实验室设计技术研究

给出了一种新型的近地轨道极高真空分子屏实验室设计。作者计算了可变翼分子屏周围大气分子的入射及散射、分子屏材料放气在屏内的分子数流密度。通过调整分子屏的翼角,分子屏内的压力可以达到10-12Pa。计算结果指出:在近地轨道选择合适的分子屏参数,可以在极高真空环境下加工超纯材料。     

相邻两航天器相对运动近似方程的解析解及比动能方程

在地心引力场中,当目标航天器沿近圆轨道作无动力运动时,与目标航天器相邻的受控航天器相对于目标航天器的运动可以近似地用Hill方程描述。文章给出了受控航天器对目标航天器运动的推力加速度随时间线性变化时Hill方程的解析解。并根据Hill方程导出了受控航天器相对目标航天器运动的比动能方程。还讨论了比动能方程在上述两航天器轨道相遇和轨道交会问题中的应用。     

用N2O-C2H2火焰原子吸收光谱法测定不锈钢材料中硅含量

运用N2O-C2H2火焰原子吸收光谱法测定不锈钢材料中的硅含量。介绍硅的最佳测定条件以及线性范围的浓度，在样品测定中对干扰因素进行了综合考虑。实验表明：N2O-C2H2火焰原子吸收光谱法灵敏度高、干扰小、选择性和重现性好，步骤简单、操作容易、分析周期短。测定样品含硅量10μg/mL～60μg/mL(n=6)时，其相对标准偏差均小于1．0％，标准加入回收率均为97．0％～103．0％(n=6)，适用于不锈钢材料中硅含量的测试，达到了实验室分析质量控制的要求。