首页 | 本学科首页   官方微博 | 高级检索  
     

离散重力数据等值线生成算法
引用本文:李振海,田辉. 离散重力数据等值线生成算法[J]. 地理空间信息, 2010, 8(2): 70-72
作者姓名:李振海  田辉
作者单位:1. 武汉大学测绘学院,湖北,武汉,430079
2. 河北理工大学交通与测绘学院,河北,唐山,063009
基金项目:武汉大学地球空间环境与大地测量教育部重点实验室开放基金资助项目 
摘    要:网格化是等值线图生成算法中的主要步骤,使用Shepard曲面拟合法、加权趋势面拟合法及普通克里金算法对重力异常数据网格化,从计算速度、网格化后数据连续性、网格化结果精度、网格化运算时间等方面对三种方法比较分析,普通克里金法拥有较好计算精度和图形连续性,但是计算时间最长,Shepard法计算精度不错、时间短,只是生成图形连续性差,趋势面法计算时间长、结果精度低,不是一种很适用的方法。

关 键 词:Shepard曲面拟合  趋势面拟合  普通克里金法  等值线  网格化  重力异常

Algorithm for Drawing Discrete Gravity Data's Contour Chart
LI Zhenhai,TIAN Hui. Algorithm for Drawing Discrete Gravity Data's Contour Chart[J]. Geospatial Information, 2010, 8(2): 70-72
Authors:LI Zhenhai  TIAN Hui
Affiliation:1. School of Geodesy and Geomatics, Wuhan University, Wuhan 430079, China; 2. College of Traffic and Survey, Hebei Polytechnic University, Tangshan 063009, China )
Abstract:Gridding was one important step in drawing contour chart. Gravity anomaly data were interpolated for gridding by using Shepard surface fitting method, Weight trend surface fitting method and Ordinary Kriging method, then this paper compared and analyzed the gridding results through three ways: continuity of gridded surface, the accuracy of results and the calculating speed : Ordinary Kriging method had the best interpolation precision and the nice continuity of gridded results, but calculating speed was slow; The Shepard method own good precision, and calculating speed was fast, however, the continuity is not very well; The trend surface fitting method was not a suitable method for its slow speed and low precision.
Keywords:Shepard surface fitting  weight trend surface fitting  ordinary Kriging method  contour  gridding  gravity anomaly
本文献已被 CNKI 维普 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号