量子光谱成像技术及其在对地观测中的应用前景

综述了量子光谱成像技术的发展概况,简述了量子光谱成像原理的理论,详细介绍了纠缠双光子源的鬼成像,亚波长干涉以及热光的无透镜成像和热光的非定域双缝干涉实验及其原理。最后对量子光谱成像技术在未来的军用和民用对地观测的应用方面做出了展望。     

矢量观测确定卫星姿态的预测粒子滤波算法

在矢量观测的基础上,针对单独的星敏感器定姿,提出了一种将粒子滤波(PF)和预测滤波相结合的姿态确定算法,通过设计粒子初始化,结合重要性采样、重采样和规则化等手段,成功地将姿态四元数作为状态粒子进行更新和传递,避免了状态方程的线性化和协方差矩阵的计算;利用预测滤波算法估计模型误差和姿态角速度,在保证滤波精度的同时,有效降低了粒子滤波器的维数.实验在某对地观测通用小卫星平台上进行,选取卫星自由飞行状态和飞轮控制对地稳定模式,分别对滤波器进行了仿真,实验结果验证了该算法对本质非线性、非高斯的卫星姿态估计问题具有快速的收敛性能和良好的稳定精度.该方法还为粒子滤波器的设计和无角速度敏感器测量的飞行器姿态确定提供了借鉴.     

Remote sensing using GNSS signals: Current status and future directions

The refracted, reflected and scattered signals of global navigation satellite systems (GNSS) have been successfully used to remotely sense the Earth’s surface and atmosphere. It has demonstrated its potential to sense the atmosphere and ionosphere, ocean, land surfaces (including soil moisture) and the cryosphere. These new measurements, although in need of refinement and further validation in many cases, can be used to complement existing techniques and sensors, e.g., radiosonde, ionosonde, radar altimetry and synthetic aperture radar (SAR). This paper presents the current status and new developments of remote sensing using GNSS signals as well as its future directions and applications. Some notable emerging applications include monitoring sea ice, dangerous sea states, ocean eddy and storm surges. With the further improvement of the next generation multi-frequency GNSS systems and receivers and new space-based instruments utilizing GNSS reflections and refractions, new scientific applications of GNSS are expected in various environment remote sensing fields in the near future.     

Inter-satellite links for satellite autonomous integrity monitoring

A new integrity monitoring mechanisms to be implemented on-board on a GNSS taking advantage of inter-satellite links has been introduced. This is based on accurate range and Doppler measurements not affected neither by atmospheric delays nor ground local degradation (multipath and interference). By a linear combination of the Inter-Satellite Links Observables, appropriate observables for both satellite orbits and clock monitoring are obtained and by the proposed algorithms it is possible to reduce the time-to-alarm and the probability of undetected satellite anomalies.     

Earth-Based Visible and Near-IR Imaging of Mercury

New planned orbiter missions to Mercury have prompted renewed efforts to investigate the surface of Mercury via ground-based remote sensing. While the highest resolution instrumentation optical telescopes (e.g., HST) cannot be used at angular distances close to the Sun, advanced ground-based astronomical techniques and modern analytical and software can be used to obtain the resolved images of the poorly known or unknown part of Mercury. Our observations of the planet presented here were carried out in many observatories at morning and evening elongation of the planet. Stacking the acquired images of the hemisphere of Mercury, which was not observed by the Mariner 10 mission (1974–1975), is presented. Huge features found there change radically the existing hypothesis that the “continental” character of a surface may be attributed to the whole planet. We present the observational method, the data analysis approach, the resulting images and obtained properties of the Mercury’s surface.     

天/地基多平台空间目标光电观测时效性分析

针对如何部署光学探测设备才能更好实现对空间目标的高精度高频度监视问题,考虑光照条件、相对关系及探测性能,构建了天/地基空间目标探测与成像仿真模型;按照轨道特征选取了94颗LEO（Low Earth Orbit,低地球轨道）卫星、63颗GEO（Geosynchronous Earth Orbit,地球同步轨道）卫星和18颗大椭圆轨道卫星,选用春夏秋冬典型季节的特定时间长度,仿真分析了国内地基、南北极科考站、LEO卫星、准GEO卫星等多平台光电手段的位置探测和成像观测能力;比对分析地基平台纬度和季节、天基平台轨道高度和倾角对探测能力的影响得出：南北极科考站相比于国内站点可提高重点季节的探测时效性,98°倾角LEO平台对低轨目标成像时效性方面更具优势,等.在此基础上,提出了我国空间目标光电观测设备天地一体的布局构想.     

考虑姿轨耦合的航天器高精度实时导航定轨方法

针对近地轨道航天器及其全球导航卫星系统(GNSS)测量数据驱动的实时导航定轨方法,使用轨道动力学原理解析了由GNSS天线安装位置与航天器质心偏差造成的定轨误差。基于航天器在轨的刚体运动特性和对地姿态特征,提出针对安装关系对应的相对速度修正项。使用姿轨耦合的分析方法,明确了基于航天器质心轨道积分和天线测量点位速修正的GNSS测量信息模拟。结合扩展卡尔曼滤波(EKF)形式的实时导航算法,分析了安装关系造成的定轨系统误差。围绕半长轴确定误差的长期变化规律,仿真证明了GNSS测量数据的位速修正在高精度实时导航定轨过程中的必要性。     

空间站和GNSS共视的差别及精度对比分析

为了对比空间站和导航卫星共视的性能差异,深入分析影响共视性能的主要误差源特征,推进共视技术进一步发展,以对共视时间比对基本原理的分析为基础,从系统设计和关键误差源影响两个方面对比分析空间站和导航卫星共视的差异。理论研究结果表明,不同于导航卫星共视,轨道误差是影响空间站共视精度进一步提升的主要因素;此外,空间站共视还需考虑地球引力时延等精细误差的影响。最后,设计并实施了仿真实验和实测实验,通过实验数据进一步对比两者的性能差异。实验结果表明空间站和导航卫星共视各有利弊,虽然空间站共视的服务区域和连续性逊于导航卫星共视,但可以实现的共视精度至少比导航卫星高一个数量级。     

靶场GNSS增强、监测与评估系统建设构想

针对靶场GNSS（全球导航卫星系统）增强、监测与评估的测量精度和可靠性保障、异常分析和电磁环境监测等复杂技术需求,明确了靶场GNSS增强、监测与评估的概念,分析了各类方法的特点,确定了以大范围基准站网为主干,采用广域差分增强和地面完好性通道监测满足提高测量精度和可靠性主要需求,采用车载信号监测和干扰监测一体化系统满足不同区域间发的异常分析和电磁环境监测需求的技术路线.设计了系统体系架构,重点分析了系统实时工作模式和数据处理流程,为系统建设提供了有益的参考.     

Present-day crustal movement of the Chinese mainland based on Global Navigation Satellite System data from 1998 to 2018

A total of more than 260 continuous stations and 2000 campaign stations from the Crustal Movement Observation Network of China (CMONOC) project, covering the Chinese mainland and its surrounding areas during the period of 1998–2018, are processed using the Bernese Global Navigation Satellite System (GNSS) software via a state-of-the-art method. We obtain the coordinate time series of all the stations given in the reference frame ITRF2014, estimate the coseismic deformation, and remove outliers. Lastly, we present the latest, most complete, and most accurate contemporary horizontal velocity field with respect to the stable Eurasian plate, irrespective of the postseismic deformations. This study shows that the signal of tectonic movement in Western China is stronger than that in Eastern China particularly in the Tibetan Plateau, with a rate of 18–32?mm/a. Moreover, the signal decays sharply from south to north. However, North China and South China move coherently to the ESE direction mostly at a rate of 4–10?mm/a and have not experienced any abrupt velocity gradients in their interiors. Meanwhile, Northeast China has the lowest velocity of only 2–4?mm/a in addition to the coastal areas that have slightly larger velocities. The densified and continuous observation of GNSS stations are of great significance to the study of the present-day crustal movement and tectonic deformation characteristics of the Chinese mainland. This would help to provide better constraints on the kinematics and dynamics of the region.