GPS软件接收机中载波相位测量的实现

GPS接收机载波相位测量的精度优于码相位测量,但却存在整周模糊度。利用码和载波相位测量的组合可以提高伪距的精度,进而改善接收机的定位性能。研究GPS软件接收机中载波相位测量的实现方法。通过处理实际采集的信号,分析码和载波相位测量组合方法的性能。实验结果表明,通过50 s的平滑,伪距误差可以减小到毫米量级。     

THE APPLICATION OF SATELLITE POSITIONING TECHNOLOGY AND ITS INDUSTRIALIZATION IN CHINA

Satellite positioning technology has been widely used in all kinds of military and civil land, marine, space and aeronautical target positioning tasks, naviga tion activities and accurate surveying measurements since 90 s in the last cen tury due to its advantage in providing all-weather, real-time, three dimensional and high precision positioning information, as well as speed and accurate timing information. By now, it has already formed a new hi-tech industry basically.This paper briefly reviews the development of the global satellite positioning and navigation technologies including the basic information of China's "Plough navigation system", introduces the history of satellite positioning technology and its major application fields as well as the status quo of this being industri alized trade in China, gives an account of the writers' vision for the application and prospect of the satellite positioning technologies in China, and approaches the tactics and stresses of the satellite positioning technology's application and its industrialization future in China.     

时变线性系统的全程滑态变结构控制研究

本文采用分段定常的处理方法研究了一般时变线性系统的滑态变结构控制方案，提出了实时自动分段原则与相应的全程滑态结构控制算法，并通过数字仿真验证了该方案的有效性。     

三维球坐标系下波包非线性传播过程的一种数值求解方法

采用全隐欧拉（FICE）格式，将三维坐标系下的大气基本运动方程作为控制方程，建立起了三维球坐标系下可压大气中的全非线性数值模式；对纬向边界也进行了合理的处理，并对该模式进行了数值检验，计算结果显示出重力波波包在大气中非线性传播的三维图像：波包整体向上传播，波相关扰动速度随高度增加而增长。     

一种新的GPS单频单历元定姿算法研究

将全球卫星定位系统(GPS)单历元的L1波段的载波相位和码相位观测方程进行组合求解整周模糊度的浮点解。基于对浮点解与固定解间关系的分析,提出了一种将低精度浮点解映射到固定解的方法,降低了最小二乘降相关平差(LAMBDA)算法对高精度浮点解的依赖性,避免了多个历元求解高精度浮点解,实现了单频、单历元的整周模糊度估计。实际数据测试结果表明:算法的成功率大于95%,能有效地实时解算动态姿态。     

GNSS接收机中一种新的射频干扰抑制级联方法

为了减少系统复杂度和提高系统实时性,提出了一种新的级联算法。首先,通过三系数滤波器模型对连续波干扰进行建模,从而形成一种非线性卡尔曼自适应滤波器,并利用该滤波器作为预处理器对每路中的窄带干扰进行抑制。随后,将各路滤波器的输出送入空时自适应处理器中进行宽带干扰的抑制。仿真结果表明,在匹配谱干扰环境下,特别是在窄带干扰从卫星信号方向入射时,新算法相对于普通的空时和空频自适应处理表现出了更加优越的性能。     

Global comparison of the model results of GSM TIP with IRI for summer conditions

This paper presents the results of the numerical calculations thermosphere/ionosphere parameters which were executed with using of the Global Self-consistent Model of the Thermosphere, Ionosphere and Protonosphere (GSM TIP)and comparison of these results with empirically-based model IRI-2001. Model GSM TIP was developed in West Department of IZMIRAN and solves self-consistently the time-dependent, 3-D coupled equations of the momentum, energy and continuity for neutral particles (O₂, N₂, O), ions (O⁺, H⁺), molecular ions (M⁺) and electrons and largescale eletric field of the dynamo and magnetospheric origin in the range of height from 80 km to 15 Earth’s radii. The empirically derived IRI model describes the E and F regions of the ionosphere in terms of location, time, solar activity and season. Its output provides a global specification not only of N_e but also on the ion and electron temperatures and the ion composition. These two models represent a unique set of capabilities that reflect major differences in along with a substantial approaches of the first-principles model and global database model for the mapping ionosphere parameters. We focus on global distribution of the N_e, T_i, T_e and TEC for the one moment UT and fixed altitudes: 110 km, h_mF2, 300 km and 1000 km. The calculations were executed with using of GSM TIP and IRI models for August 1999, moderate solar activity and quiet geomagnetic conditions. Results present as the global differences between the IRI and GSM TIP models predictions. The discrepancies between model results are discussed.     

GPS失锁时基于神经网络预测的MEMS-SINS误差反馈校正方法研究

GPS信号失锁时,MEMS-SINS组合GPS导航误差会随着时间迅速积聚而无法导航.提出一种基于RBF神经网络预测的MEMS-SINS误差反馈校正方法,GPS有信号时对神经网络进行训练,GPS信号中断时用训练好的RBF神经网络预测MEMS-SINS的导航误差.地面车载跑车试验,证实了训练后的RBF神经网络能很高精度地逼近MEMS-SINS/GPS组合导航系统输入与输出间的关系,在4个50s以内的GPS人为失锁过程中,该方法导航结果与参考系统比较,平均位置误差为3.8m,平均速度误差为0.6m/s,平均姿态误差为0.5°.     

Quasi-biennial oscillation in GPS VTEC measurements

The quasi-biennial oscillation, QBO, a well known periodicity in the equatorial stratospheric zonal winds, is also found in ionospheric parameters and in solar and geomagnetic activity indices. Many authors speculated about the link between the QBO in solar and geomagnetic activity and the QBO in atmospheric parameters. In this work we analyze the presence of the QBO in the ionosphere using the Vertical Total Electron Content (VTEC) values obtained from Global Navigation Satellite System (GNSS) measurements during the period 1999–2012. In particular, we used IONEX files, i.e. the International GNSS Service (IGS) ionospheric products. IONEX provide VTEC values around the world at 2-h intervals. From these data we compute global and zonal averages of VTEC at different local times at mid and equatorial geomagnetic latitudes. VTEC and Extreme Ultra Violet (EUV) solar flux time series are analyzed using a wavelet multi resolution analysis. In all cases the QBO is detected among other expected periodicities.     

Equatorial Ionospheric Anomaly (EIA) and comparison with IRI model during descending phase of solar activity (2005–2009)

The ionospheric variability at equatorial and low latitude region is known to be extreme as compared to mid latitude region. In this study the ionospheric total electron content (TEC), is derived by analyzing dual frequency Global Positioning System (GPS) data recorded at two stations separated by 325 km near the Indian equatorial anomaly region, Varanasi (Geog latitude 25°, 16^/ N, longitude 82°, 59^/ E, Geomagnetic latitude 16°, 08^/ N) and Kanpur (Geog latitude 26°, 18^/ N, longitude 80°, 12^/ E, Geomagnetic latitude 17°, 18^/ N). Specifically, we studied monthly, seasonal and annual variations as well as solar and geomagnetic effects on the equatorial ionospheric anomaly (EIA) during the descending phase of solar activity from 2005 to 2009. It is found that the maximum TEC (EIA) near equatorial anomaly crest yield their maximum values during the equinox months and their minimum values during the summer. Using monthly averaged peak magnitude of TEC, a clear semi-annual variation is seen with two maxima occurring in both spring and autumn. Results also showed the presence of winter anomaly or seasonal anomaly in the EIA crest throughout the period 2005–2009 only except during the deep solar minimum year 2007–2008. The correlation analysis indicate that the variation of EIA crest is more affected by solar activity compared to geomagnetic activity with maximum dependence on the solar EUV flux, which is attributed to direct link of EUV flux on the formation of ionosphere and main agent of the ionization. The statistical mean occurrence of EIA crest in TEC during the year from 2005 to 2009 is found to around 12:54 LT hour and at 21.12° N geographic latitude. The crest of EIA shifts towards lower latitudes and the rate of shift of the crest latitude during this period is found to be 0.87° N/per year. The comparison between IRI models with observation during this period has been made and comparison is poor with increasing solar activity with maximum difference during the year 2005.