Interpolation with splines in tension: A Green's function approach

被引:112
作者
Wessel, P [1 ]
Bercovici, D [1 ]
机构
[1] Univ Hawaii Manoa, Sch Ocean & Earth Sci & Technol, Dept Geol & Geophys, Honolulu, HI 96822 USA
来源
MATHEMATICAL GEOLOGY | 1998年 / 30卷 / 01期
基金
美国国家科学基金会;
关键词
gridding; interpolation; splines;
D O I
10.1023/A:1021713421882
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Interpolation and gridding of data are procedures in the physical sciences and al-e accomplished typically using an averaging or finite difference scheme on an equidistant grid. Cubic splines are popular because of their smooth appearances; however, these functions can have undesirable oscillations between data points. Adding tension to the spline overcomes this deficiency. Here, we derive a technique for interpolation and gridding in one, two, and three dimensions using Green's functions for splines in tension and examine some of the properties of these functions. For moderate amounts of data, the Green's function technique is superior to conventional finite-difference methods because (1) both data values and directional gradients can be used to constrain the model surface, (2) noise can be suppressed easily by seeking a least-squares fit rather than exact interpolation, and (3) the model can be evaluated at arbitrary locations rather than only on a rectangular grid. We also show that the inclusion of tension greatly improves the stability of the method relative to gridding without tension. Moreover, the one-dimensional situation can be extended easily to handle parametric curve fitting in the plane and in space. Finally, we demonstrate the new method on both synthetic and real data and discuss the merits and drawbacks of the Green's function technique.
引用
收藏
页码:77 / 93
页数:17
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