卫星星座整网轨道确定分析与仿真

编队飞行的卫星或卫星星座对轨道确定自主性和精度提出了较高要求。针对这个问题,通过建立星座的轨道动力学模型和星间观测的测量模型,将星座中的星间观测数据和地面观测数据融合起来,将待估的卫星轨道参数和部分动力学参数进行适当的分类,研究卫星星座整网轨道确定的新方法,并在理论上分析了整网定轨方法能提高定轨精度的原因;最后采用自主开发的卫星星座整网轨道确定软件进行了仿真计算。计算表明,该方法能有效地减少对地面站的依赖,并较大幅度提高定轨时卫星绝对位置和相对位置精度。
     

对地观测卫星成像调度的多目标约束修正方法

 约束修正是对地观测卫星成像调度的重要组成部分,负责处理成像调度方案的约束满足与优化,是一类复杂的组合优化问题。为得到优化可行的成像调度方案,提出一种新的约束修正方法。针对约束修正问题构建时间序有向图模型,并将约束修正问题归结为点带约束成本的优化路径搜索问题;在此基础上,提出一种基于标记更新的多目标约束修正算法。实际问题的实验与分析表明：该方法能够在规定的时间内求得问题所有的多目标优化解,有效地解决了卫星成像调度的约束满足与优化问题。     

GEO长寿命卫星热管在轨等温性能分析

热管是GEO长寿命卫星热控设计大量使用的重要传热元件，其在轨等温传热性能是影响卫星安全可靠工作的关键因素。针对中国在轨长期稳定运行的GEO长寿命卫星热管，基于热管在轨温度遥测数据，采用数理统计方法分析热管在轨等温性能随时间的实际变化规律，分析表明：GEO长寿命卫星热管在轨等温性能稳定性良好，等温性受热管自身温度水平影响较大，年周期内呈现季节性变化，全寿命周期内随飞行时间推移呈现性能衰减下降趋势，寿命末期等温性优于1.6℃，并从热管设计、热负荷大小与分布、使用环境等方面进行等温性改进分析及应用建议。     

The USSR and satellite communications : Competition and cooperation

This article examines the USSR's satellite communications provision in the international arena. The author first outlines the Intercosmos programme, collaboration between the USSR and France and India, and maritime satellite communications. He then discusses in detail the INTERSPUTNIK system, and Soviet international coverage and competitiveness in television. In conclusion, the complex interaction and overlap between cooperation and competition in space is explained.     

同时地形高程测量和地面运动目标检测的分布式InSAR最优编队构形

分布式小卫星干涉SAR为了同时获得时间基线(用于地面运动目标检测)和空间基线(用于地形高程测量),采取空间立体编队构形(即非沿航向直线编队),然而这种混合基线的情况会导致地面运动目标与地形杂波存在相位耦合,而且只靠信号处理方法很难分离,这对于检测地面运动目标极为不利。提出几种最优编队构形,在保证获得两种干涉基线的同时,通过对消两对干涉SAR图像来抑制掉固定杂波,从而可以检测地面运动目标,这种方法具有处理简单和性能较好等优点。最后给出了仿真结果。     

挠性双自旋卫星的姿态稳定判据

本文建立了挠性双自旋卫星的姿态稳定性判据。挠性双自旋卫星由半刚性平台、转子以及固连于平台的挠性附件组成,选择由姿态角和模态坐标表示的系统的相对能量函数为Liapunov函数,由此建立的姿态稳定判据由两个部分组成,即忽略附件弹性运动时,半刚性双自旋卫星的姿态稳定条件和附件振动频率所应满足的条件。文中还给出了具体的应用例子。     

一种基于相对位置约束的双星定位方法

全球卫星定位系统(GNSS)需要至少4颗卫星才能提供持续、准确的定位结果。在有障碍物遮挡的城市街道、山谷或者存在压制式干扰的战场环境中,往往会出现可见星数量降低至4颗以下的情况。针对只有2颗可见星的定位问题,提出了通过相对位置变化对绝对位置进行解算的定位模型,证明了该模型的可行性,并研究了该模型的数值计算方法和几何搜索方法。仿真实验和实际跑车试验表明,在只有2颗可见星条件下,该方法的定位精度明显优于传统的INS/GNSS紧组合算法,并且对初始位置的精度不具有依赖性。     

Influence of time variable geopotential models on precise orbits of altimetry satellites,global and regional mean sea level trends

During the last decade a significant progress has been reached in the investigation of the gravity field of the Earth. Besides static, also time variable geopotential models have been recently created. In this paper we investigate the impact of the recent time variable geopotential models on altimetry satellite orbits and such altimetry products based on these orbits, as global and regional mean sea level trends. We show that the modeling of time variable gravity improves the orbit solutions, at least for the GRACE period where time variable gravity is sufficiently accurately observed by this mission. Our analysis includes six geopotential models jointly developed by GFZ German Research Centre for Geosciences and Space Geodesy Research Group (CNES/GRGS) Toulouse: the stationary model EIGEN-GL04S, a stationary version of EIGEN-6S (EIGEN-6S_stat), a corrected version of EIGEN-6S and three enhanced versions of EIGEN-6S called EIGEN-6S2, EIGEN-6S2A and EIGEN-6S2B. By “stationary” we mean “containing periodic parameters such as annual and semi-annual variations, but no secular (drift) terms”. We computed precise orbits for the radar altimetry satellites ERS-1, ERS-2, TOPEX/Poseidon, and Envisat over 20 years between 1991 and 2011. The orbit, single-mission and multi-mission altimetry crossover analyses show that the time variable models EIGEN-6S_corrected, EIGEN-6S2 and its two precursors EIGEN-6S2A/B perform notably better than the stationary models for the GRACE period from 2003 onwards. Thus, using EIGEN-6S2 and EIGEN-6S2A/B we have got 3.6% smaller root mean square fits of satellite laser ranging observations for Envisat, as when using EIGEN-GL04S. However, for the pre-GRACE period 1991–2003, the stationary geopotential models EIGEN-GL04S and EIGEN-6S_stat as well as EIGEN-6S2 having no drift terms for degree 3–50 at this time interval perform superior compared to EIGEN-6S_correct and EIGEN-6S2A/B which contain drifts for this period. We found, that the time variable geopotential models have a low (0.1–0.2 mm/yr) impact on our results for the global mean sea level trend. However, we found strong East/West differences up to 3 mm/yr in the regional mean sea level trends when using orbits of all four satellites based on time variable and stationary geopotential models. We show that these differences are related to the relative drifts of the centers-of-origin between the orbit solutions based on the time variable and stationary geopotential models. From the results of our detailed study, we conclude that the final version of the time variable gravity field model EIGEN-6S2 performs best for the four satellites tested. This model provides the most reliable and mission-consistent sea level estimates for the whole time period from 1992 to 2010. This model is of maximum spherical harmonic degree and order 260 and contains time series for drifts as well as annual and semiannual variations of the spherical harmonic coefficients for degree 2–50.     

Coastal salinity measurement using a Doppler Radiometer

Coastal salinity is characterised by large and variable salinity contrasts on relatively small scales. Measurements of salinity at a resolution compatible with these coastal regions on a regular basis would provide a rich source of information that could be used for a number of applications that have a fundamental bearing on the world’s lifestyle. Doppler radiometry offers an approach to capture such measurements, as it reduces the number of required antennas needed to form an image, compared with an Interferometer type instrument.     

Astrometric positioning and orbit determination of geostationary satellites

In the project titled “Astrometric Positioning of Geostationary Satellite” (PASAGE), carried out by the Real Instituto y Observatorio de la Armada (ROA), optical observation techniques were developed to allow satellites to be located in the geostationary ring with angular accuracies of up to a few tenths of an arcsec. These techniques do not necessarily require the use of large telescopes or especially dark areas, and furthermore, because optical observation is a passive method, they could be directly applicable to the detection and monitoring of passive objects such as space debris in the geostationary ring.