数字通信信号漂移测量方法研究

在通信系统中,数字信号的传输漂移是衡量数据传输质量的一项重要指标,因此对数字信号漂移量的准确测量是非常重要的。介绍了数字通信信号漂移的定义、测量原理和目前国内外测量数字通信信号漂移指标的主要方法,示波器法和专用漂移测量仪表法适用于测量准确度要求不高的工程测量,而时间间隔测量法和频偏测量法适用于建立测量标准。最后简介了北京无线电计量测试研究所建立的数字通信信号漂移测量仪检定装置。     

船用时统设备NTP网络授时服务的实现

为了满足船用入网设备多样化的用时需求,并保证船舶系统内部时间的一致性和准确性,在满足船用时间统一系统特点的基础上,设计了一种具有NTP网络授时功能的船用时统设备,增强了船用时统设备的通用性.时统设备作为船舶系统的NTP 1级授时服务器,基于NTP向用时用户同步时间.根据实际使用环境,给出了NTP网络授时最简方案,并对N...     

基于实时解空间的三维声源定位

提出了一种基于实时解空间库的快速三维声源定位算法。该算法使用来自四个声传感器 ,一个风速传感器和一个风向传感器的信号能够准确快速地计算出声源的位置。     

基于光纤双环网的高精度时频同步技术研究

本文介绍了一种基于光纤双环网的时频同步技术设计方法，针对时频设备协同使用时如何获得高精度同步指标这一问题提出了一种设计思路。以系统时间源使用北斗/GPS/GLONASS，本系统同步精度优于5E-13，频率稳定度优于5E-13@1d；以UTC(BIRMM)输出的TOD+1PPS做系统时间源，本系统同步精度优于4E-13，频率稳定度优于6E-14@1d。本方案提出的方法原理简单，系统可根据使用情况进行裁剪，相比卫星双向等手段成本低廉，适合在时频同步领域推广。     

本地标准时间频率的产生与保持

近年来，地方协调时UTC(BIRM)守时能力稳步提升，截至目前，UTC(BIRM)与UTC的相对频率偏差优于3E-14，时间偏差优于20ns。本文概括介绍了守时系统的组成，本地频率驾驭与主备同步技术，以及TA(BIRM)算法研究等。     

Land use/land cover classification using time series Landsat 8 images in a heavily urbanized area

It is of great significance to timely, accurately, and effectively monitor land use/cover in city regions for the reasonable development and utilization of urban land resources. The remotely sensed dynamic monitoring of Land use/land cover (LULC) in rapidly developing city regions has increasingly depended on remote-sensing data at high temporal and spatial resolutions. However, due to the influence of revisiting periods and weather, it is difficult to acquire enough time-series images with high quality at both high temporal and spatial resolution from the same sensor. In this paper we used the temporal-spatial fusion model ESTARFM (Enhanced Spatial and Temporal Adaptive Reflectance Fusion Model) to blend Landsat8 and MODIS data and obtain time-series Landsat8 images. Then, land cover information is extracted using an object-based classification method. In this study, the proposed method is validated by a case study of the Changsha City. The results show that the overall accuracy and Kappa coefficient were 94.38% and 0.88, respectively, and the user/producer accuracies of vegetation types were all over 85%. Our approach provides an accurate and efficient technical method for the effective extraction of land use/cover information in the highly heterogeneous regions.     

原子时系统主备钟同步技术研究

主钟系统作为原子时系统的重要组成部分，其运行状态直接关系到整个原子时系统的性能。为了提高系统的可靠性，建立备份主钟系统尤为必要。本文围绕原子时系统中的主备钟同步技术开展相关研究，建立了主备钟同步系统。通过分析原子钟性能，建立钟差模型；并根据钟差模型对备份主钟的频率进行驾驭调整，实现主备钟之间的时间频率一致性。通过调整，原子时系统的主备钟时差可实时保持在1ns以内，频率偏差实时保持在10E-15量级，为原子时系统的主备无缝切换奠定良好基础。     

嫦娥五号探测器多舱段间接力式校时及误差控制方法

为优化嫦娥五号探测器操控,达到通过给任意具备测控链路的舱段校时即可实现多舱段组合体时间同步的目标,提出了一种接力式校时及误差控制方法。该方法通过相邻舱段间接力式时间传递实现舱段间时间自流动。设计了基于飞行模式的时间基准设备检索方法,通过统一的检索配置表使各设备能够根据飞行模式识别上级时间基准设备,实现了各舱段的自主校时。设计了总线控制器(Bus controller,BC)与远置单元(Remote terminal,RT)间的分布式时间传递误差控制方法,BC端修正时间信息发送时产生的误差,RT端控制时间信息接收时引入的误差,保证了整器时统精度。研究方法实现了多舱段复杂航天器的器内自组织时统,已在嫦娥五号探测器上得到应用并取得预期效果,可为后续航天器软件设计提供参考。     

Time series modeling and analysis of trends of daily averaged ionospheric total electron content

A 10.7 cm solar radio flux F10.7, geomagnetic planetary equivalent amplitude (Ap index), and period variations were considered in this paper to construct a linear model for daily averaged ionospheric total electron content (TEC). The correlation coefficient of the modeled results and International GNSS Service (IGS) observables was approximately 0.97, which implied that the model could accurately reflect the realistic variation characteristics of the daily averaged TEC. The influences of the different factors on TEC and its characteristics at different latitudes were examined with this model. Results show that solar activity, annual and semiannual cycles are the three most important factors that affect daily averaged TEC. Solar activity is the primary determinant of TEC during periods with high solar activity, whereas periodic factors primarily contribute to TEC during periods with minimum solar activity. The extent of the influences of the different factors on TEC exhibits obvious differences at varying latitudes. The magnitude of the semiannual variation becomes less significant with the increase in latitude. Furthermore, a geomagnetic storm causes an increase in TEC at low latitudes and a decrease at high latitudes.