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重力异常延拓计算积分半径的选择及远区效应
引用本文:欧阳永忠,邓凯亮,黄谟涛,暴景阳,杜强,刘传勇.重力异常延拓计算积分半径的选择及远区效应[J].海洋测绘,2011,31(4):5-7.
作者姓名:欧阳永忠  邓凯亮  黄谟涛  暴景阳  杜强  刘传勇
作者单位:1. 武汉大学测绘学院,湖北武汉430079;海军海洋测绘研究所,天津300061
2. 海军海洋测绘研究所,天津300061;海军大连舰艇学院海洋测绘科学与工程系,辽宁大连116018
3. 海军海洋测绘研究所,天津,300061
4. 海军大连舰艇学院海洋测绘科学与工程系,辽宁大连,116018
5. 92292部队,山东胶南,266405
基金项目:国家863计划项目(2006AA06A202); 国家重大海洋勘测专项(4200301); 海军大连舰艇学院科研发展基金(20090602)
摘    要:基于球谐展开和两分量模型,推导了基于Poisson积分方程的重力异常延拓的远区效应截断误差的函数表达;研究了近区半径、移去重力场阶次、延拓高度与远区效应截断误差之间的相互关系.数值分析表明,当延拓高度为1 000m时,移去360阶的重力场模型,积分半径大于0.5°能保证远区效应截断误差可以忽略;当移去2160阶的重力场...

关 键 词:重力异常延拓  积分半径的选择  远区效应截断误差  Poisson积分方程

The Choice of Integral Radius and Its Far-zone Effects in the Continuation of the Gravity Anomaly
OUYANG Yong-zhong,DENG Kai-liang,HUANG Mo-tao,BAO Jing-yang,DU Qiang,LIU Chuan-yong.The Choice of Integral Radius and Its Far-zone Effects in the Continuation of the Gravity Anomaly[J].Hydrographic Surveying and Charting,2011,31(4):5-7.
Authors:OUYANG Yong-zhong  DENG Kai-liang  HUANG Mo-tao  BAO Jing-yang  DU Qiang  LIU Chuan-yong
Institution:OUYANG Yong-zhong1,2,DENG Kai-liang2,3,HUANG Mo-tao2,BAO Jing-yang3,DU Qiang4,LIU Chuan-yong2 (1.School of Geodesy and Geomatics,Wuhan University,Wuhan,Hubei,430079,2.Naval Institute of Hydrographic Surveying and Charting,Tianjin,300061,3.Department of Hydrography and Cartography,Dalian Naval Academy,Dalian,Liaoning,116018,4.92292 Troops,Jiaonan,Shandong,266405)
Abstract:Based on the spherical harmonic expansion and the two weight model,the function expression of the truncation error of far-zone effects in the continuation of the gravity anomaly based on the Poisson integral equation is derived.With the near-zone radius and the earth gravity field model degrees increasing,the far-zone effects truncation error decreases;with the increase of the continuation height it increases.The numerical analysis indicates that when the continuation height was 1000m and the Earth Gravity ...
Keywords:continuation of the gravity anomaly  the choice of integral radius  far-zone effects  the poisson integral equation  
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