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总强度磁异常匹配水下导航方法研究
引用本文:肖胜红,边少锋,黄晓颖. 总强度磁异常匹配水下导航方法研究[J]. 海洋测绘, 2011, 31(2): 17-20
作者姓名:肖胜红  边少锋  黄晓颖
作者单位:1. 海军工程大学导航工程系,湖北武汉,430033
2. 海军工程大学导航工程系,湖北武汉430033;中国科学院测量与地球物理研究所,湖北武汉430077
基金项目:国家杰出青年科学基金,国家自然科学基金
摘    要:匹配算法是水下潜器匹配导航的核心技术,提出一种利用测量磁场与世界地磁模型(world magnet model,WMM)计算磁场之差作为匹配特征量的水下匹配导航新模式.首先引入快速傅里叶级数拟合技术建立区域的磁场模型,然后将测量地磁异常与惯导指示地磁异常之差表示成连续的解析形式,结合惯导力学编排方程建立的12维状态模型...

关 键 词:匹配导航  磁场异常  傅里叶级数  区域磁场模型  扩展卡尔曼滤波

Research on the Matching Method of Underwater Geomagnetic Navigation
XIAO Sheng-hong,BIAN Shao-feng,HUANG Xiao-ying. Research on the Matching Method of Underwater Geomagnetic Navigation[J]. Hydrographic Surveying and Charting, 2011, 31(2): 17-20
Authors:XIAO Sheng-hong  BIAN Shao-feng  HUANG Xiao-ying
Affiliation:1.Department of Navigation,Naval University of Engineering,Wuhan,Hubei,430033;2.Institute of Geodesy and Geophysics,Chinese Academy of Sciences,Wuhan,Hubei,430077)
Abstract:As the matching algorithms have been used as the major technology for correcting the errors of underwater INS,a new pattern of underwater matching navigation is introduced in this paper which is based on the matching characteristics derived from the difference between measured magnetic intensity and WMM calculated magnetic intensity.Firstly,the fast Fourier series is introduced to model the local geomagnetic anomaly field,and by which the difference between measured geomagnetic anomaly and the INS indicated geomagnetic anomaly is expressed as continual analytical format.Finally,the optimum estimate position error of INS is given with the extended Kalman filter based on the 12 dimension state model of INS error equation.Simulation is done on 3′×3′ geomagnetic anomaly database,and the results show that the mean square error of regional geomagnetic model is less than 0.2283nT,and in the 16 hours' simulation time,the mean location error in longitude and latitude is 1.3897 and 1.4679 nautical mile respectively.
Keywords:matching navigation  geomagnetic anomaly  Fourier series  regional geomagnetic field  extended Kalman filter
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