针对无线通信到达时间差(time difference of arrival,TDOA)定位技术位置解算为复杂的非线性方程最优化问题,采用实数编码遗传算法,提出了改进的自适应遗传算法。该算法设计了自适应交叉率和变异率的计算公式,考虑了随着进化代数增加种...针对无线通信到达时间差(time difference of arrival,TDOA)定位技术位置解算为复杂的非线性方程最优化问题,采用实数编码遗传算法,提出了改进的自适应遗传算法。该算法设计了自适应交叉率和变异率的计算公式,考虑了随着进化代数增加种群的整体变化,同时考虑了每代种群不同个体适应度的作用,并引入最优保存策略防止优良个体的破坏,能有效产生新的个体进而摆脱局部最优值的搜索达到全局最优解。仿真结果表明,改进的遗传算法性能稳定,进化收敛速度和TDOA定位估计精度都有较大的提高。展开更多
We used the Earth Gravitational Model （EGM2008） data sets to analyze the regional gravity anoma- lies and to study the underground structures in Cameroon. We first created a high-resolution Free-Air anomaly database...We used the Earth Gravitational Model （EGM2008） data sets to analyze the regional gravity anoma- lies and to study the underground structures in Cameroon. We first created a high-resolution Free-Air anomaly database, then corrected the gravity field of the topographic effect by using ETOPO1 DEM with a resolution of 0.01~ to obtain the Bouguer anomaly, then applied a multi-scale wavelet-analysis technique to separate the gravity-field components into different parts of shallow-to-deep origins, and finally used the logarithmic power spectrum technique to obtain detailed images and corresponding source depths as well as certain lateral inho- mogeneity of structure density. The anomalies of shallow origin show successive elongated gravity ＂highs＂ and ＂lows＂ attributable to subsurface Tertiary and lower Cretaceous undulations. Our results are in good agreement with previous investigations.展开更多
The height changes of tide gauges directly influence sea level observation. For research of sea level variation in large region or globe, the land vertical displacement must be considered. Two sessions of GPS and abso...The height changes of tide gauges directly influence sea level observation. For research of sea level variation in large region or globe, the land vertical displacement must be considered. Two sessions of GPS and absolute gravity observations in 2001 and 2003 are used to determine the horizontal and vertical motion of China coast in ITRF2000 and Eurasia frame. The difference between results of continuous observation and periodic observation is discussed.展开更多
文摘针对无线通信到达时间差(time difference of arrival,TDOA)定位技术位置解算为复杂的非线性方程最优化问题,采用实数编码遗传算法,提出了改进的自适应遗传算法。该算法设计了自适应交叉率和变异率的计算公式,考虑了随着进化代数增加种群的整体变化,同时考虑了每代种群不同个体适应度的作用,并引入最优保存策略防止优良个体的破坏,能有效产生新的个体进而摆脱局部最优值的搜索达到全局最优解。仿真结果表明,改进的遗传算法性能稳定,进化收敛速度和TDOA定位估计精度都有较大的提高。
基金supported by CAS-TWAS under grant FR 3240267248the National Natural Science Foundation of China(41021003)the Research Project of State Key Laboratory of Geodesy and Earth's Dynamics(SKLGED2013-4-1-Z)
文摘We used the Earth Gravitational Model （EGM2008） data sets to analyze the regional gravity anoma- lies and to study the underground structures in Cameroon. We first created a high-resolution Free-Air anomaly database, then corrected the gravity field of the topographic effect by using ETOPO1 DEM with a resolution of 0.01~ to obtain the Bouguer anomaly, then applied a multi-scale wavelet-analysis technique to separate the gravity-field components into different parts of shallow-to-deep origins, and finally used the logarithmic power spectrum technique to obtain detailed images and corresponding source depths as well as certain lateral inho- mogeneity of structure density. The anomalies of shallow origin show successive elongated gravity ＂highs＂ and ＂lows＂ attributable to subsurface Tertiary and lower Cretaceous undulations. Our results are in good agreement with previous investigations.
文摘全球卫星导航系统(GNSS)能够为用户提供定位、导航和授时(PNT)服务,被广泛应用于国防安全保障和国民经济建设中.实时精密单点定位(RT-PPP)是一种高精度卫星导航定位方法,针对信号中断导致的重新初始化时间长的问题,提出一种基于历元间差分伪距和载波相位观测量的周跳修复算法,设计了一种RT-PPP算法,并介绍其实现流程.采用国际GNSS服务(IGS)观测站数据进行周跳修复实验,成功率在99%以上,缩短了重新收敛时间.在楼顶进行推车实验,RT-PPP在水平方向定位精度优于1 cm,高程定位方向精度为2~3 cm.
文摘The height changes of tide gauges directly influence sea level observation. For research of sea level variation in large region or globe, the land vertical displacement must be considered. Two sessions of GPS and absolute gravity observations in 2001 and 2003 are used to determine the horizontal and vertical motion of China coast in ITRF2000 and Eurasia frame. The difference between results of continuous observation and periodic observation is discussed.
