基于网络的GPS时钟信号发布系统

从空管的实际应用出发,本次研究尝试以TCP Server/Client的模式进行GPS时钟信号的网络发布,通过这种方式实现多套系统灵活的时钟信号引接。     

一种基于元路径拥塞模式挖掘的移动对象位置预测方法

路网上移动对象位置预测是许多位置相关服务的基础。目前移动对象位置预测方法没有充分考虑到轨迹数据中所蕴含的道路拥塞信息,而路网上的道路拥塞状态对移动对象的位置更新会产生巨大影响。提出基于元路径拥塞模式挖掘的方法(Meta-congestion-pattern mining,MCPM)。在离线挖掘阶段,从历史轨迹的频繁路径(元路径)的紧集中挖掘当地的拥塞模式,并对运动模式进行建模,其中采用基于k均值的聚类算法解决数据稀疏性问题。在线预测阶段根据挖掘的拥塞模式和运动模式依概率进行预测。最后通过理论分析和实验验证得出了算法的有效性,与相同条件下的精度预测(WhereNext,WN)方法相比,平均预测准确性提高了近20%,预测时间平均缩短了近50%。     

A regional tropospheric model for airborne GPS applications

A regional tropospheric model can be constructed using surveys from GPS ground networks. Using this model the tropospheric delays of a kinematic station within the region can be interpolated. However, such a model is generally not suitable for an airborne platform high above the ground networks. In this paper, a method of constructing a regional tropospheric model for airborne GPS applications is described. First, the kinematic station in the air is projected onto the ground. Then the tropospheric delays at projected point are interpolated from those of the ground networks. Finally, the tropospheric delays at projected point are extended upward to the airborne platform using pressure and temperature gradients and humidity exponential function. For validation of this method, the data of airborne campaign carried out by BKG in cooperation with GFZ and BGR 2008 in the northern Alps are used. The results show that GPS kinematic positioning precision in height component can be improved using this method.     

The geomagnetic solar flare effect identified by SIIG as an indicator of a solar flare observed by GOES satellites

This paper studies the efficiency of geomagnetic solar flare effects (gsfe) in X solar flare detection; so during the period 1999–2007 a comparison between solar flare (sf) observed by satellites of the Geostationary Operational Environmental Satellite (GOES) programme and gsfe published by the Service International des Indices Geomagnetiques (SIIG) is made.     

基于计算机视觉/GPS/MG姿态测量的盲人行走组合导航方法研究

电子导盲辅助装置(ETA)是解决盲人出行困难的重要手段,而导航是ETA的关键技术.现有的ETA主要用GPS来定位定向,但在城市环境中经常存在GPS信号遮挡导致导航信息丢失的问题.针对该问题,利用视觉导航短时间内定位精度高,输出连续的优点以及 MG(Magnetic Gravity)姿态测量可补偿姿态积累误差的优点,提出一种基于视觉、GPS和MG姿态测量的盲人行走组合导航算法.该方法构建系统误差模型并以Kalman滤波为框架.仿真和实验结果表明,提出的组合导航算法准确度优于单独的导航算法,满足盲人户外安全出行导航的需求.     

一种射频仿真时统子系统的技术设计

针对射频仿真系统中的时间同步问题,设计基于FPGA、DSP和GPS的时间统一系统。从工程实施的角度出发,详细阐述时统的硬件设计,介绍IRIG-B码的解码原理和各采样频率信号输出的过程。试验证明：该时统克服了常规时统设备的不足,性能更稳定,可靠性更高,更易于调试。     

应用GPS载波确定载体姿态

本文简述了利用GPS载波相位技术进行载体姿态确定的原理，比较了目前已有的多种整周模糊度求解算法，选用最小二乘法进行了载体定姿实践，减少了备选整周模糊度的组合数，并采用多种约束信息来剔除不正确的模糊度组合，结合实验，指出了载体姿态变化和整周模糊度搜索速度的关系，提出了一种模糊度确定的辅助方法，并给出了应用算例。     

用加权几何精度因子选星的GPS抗多径定位方法

在ＧＰＳ（Ｇｌｏｂａｌ ｐｏｓｉｔｉｏｎｉｎｇ ｓｙｓｔｅｍ）中普遍用几何精度因子（Ｇｅｏｍｅｔｒｉｃ ｄｉｌｕｔｉｏｎ ｏｆ ｐｒｅｃｉｓｉｏｎ，ＧＤＯＰ）来选星，但对近距差分ＧＰＳ，多径干扰已变成了主要误差源，传统的ＧＤＯＰ值选星不是最佳的。为减小多径误差，文中提出了一种新的加权ＧＤＯＰ值选星方法。在仿真验证过程中，分析了多径的几何传播机理，并考虑了抗多径天线的抑制效应。仿真结果表明，用加权Ｇ     

运用GPS空中校正飞机无线电罗差误差分析

针对某些特种飞机无线电罗差无法沿用传统校正方法在地面进行校正的状况 ,首次提出了运用 GPS接收机在空中校正飞机无线电罗差的方法。本文对影响该校正方法校正精度的各项误差因素进行了分析。     

Vertical motions in Thailand after the 2004 Sumatra–Andaman Earthquake from GPS observations and its geophysical modelling

Following previous findings from ongoing GPS research in Thailand since 2004 we continue to exploit the GPS technique to monitor and model land motions induced by the Sumatra–Andaman Earthquake. Our latest results show that up to the end of 2010, Thailand has been co-seismically displaced and is subsequently undergoing a post-seismic horizontal deformation with total displacements (co-seismic plus post-seismic) ranging from 10.5 to 74.7 cm. We observed the largest horizontal displacements in the southern part of Thailand and moderate and small displacements in the central and northern parts. In addition to horizontal displacements throughout Thailand, continuous GPS measurements show that large parts of Thailand are subsiding at rates up to 1 cm/yr. It is the first time that such vertical post-seismic deformations at large distances (650–1500 km away from the Earthquake’s epicentre) have been recorded. We have investigated the physical processes leading to the observed subsidence. While after-slip on the subduction interface induces negligible or even slightly positive vertical motions, relaxation in the asthenosphere is associated with a sizable subsidence. Predictions from a 3D finite element model feature an asthenosphere with an effective viscosity of the order of 3 * 10¹⁸ Pas, fit the horizontal post-seismic data and the observed subsidence well. This model is then used to predict the subsidence over the whole seismic cycle. The subsidence should go on with a diminishing rate through the next two decades and its final magnitude should not exceed 10 cm in the Bangkok area.