摘要
针对采用矩谐分析方法构建地磁基准图的边界震荡问题,提出一种基于二维经验模态分解的区域地磁异常数据边界补偿方法.采用二维经验模态分解方法对区域地磁异常数据进行多尺度分解,对分解所得小尺度本征模态函数分量,利用总体Hilbert变换法进行瞬时频率和瞬时幅值特征提取,通过自采样和特征匹配进行边界补偿;将大尺度分量之和作为趋势项,利用三角函数方法建立模型并计算边界之外的大尺度磁异常值.实验证明,相比当前已有方法,可以更加有效地抑制对区域地磁异常数据进行矩谐分析的边界震荡问题,稳定提高构建地磁基准图的准确性.
A boundary compensation method based on bi-dimensional empirical mode decomposition(BEMD)is proposed in this paper to address the boundary effect in preparation of geomagnetic navigation reference map.The local geomagnetic anomaly data are firstly decomposed into components with different scales with BEMD;then for small scale ones instant amplitude and frequency are computed with total Hilbert transform,and the boundary is compensated with self-sampling and featurematching;whereas for the large scale ones,trigonometric function model is conducted and used to compute the values outside the boundary.After the compensation of local dataset,rectangular harmonic model is used to prepare geomagnetic map.Experimental results indicate that BEMD method could better compress the boundary effect of rectangular harmonic analysis,and improve the mapping precision steadily in comparison with other existing methods.
出处
《地球科学(中国地质大学学报)》
EI
CAS
CSCD
北大核心
2014年第11期1617-1624,共8页
Earth Science-Journal of China University of Geosciences
基金
国家自然科学基金(No.51379049)
中央高校基础科研业务费专项资金资助(No.HEUCFX41302)
关键词
地磁异常场
矩谐模型
二维经验模态分解
总体Hilbert变换
边界补偿
地球物理
geomagnetic anomaly field
rectangular harmonic model
bi-dimensional empirical mode decomposition(BEMD)
total Hilbert transform
boundary compensation
geophysics.