The scale invariant generator technique for quantifying anisotropic scale invariance

被引:34
|
作者
Lewis, GM
Lovejoy, S
Schertzer, D
Pecknold, S
机构
[1] McGill Univ, Dept Phys, Montreal, PQ H3A 2T8, Canada
[2] Univ Paris 06, LMD CNRS, F-75252 Paris 05, France
关键词
anisotropy; scale invariance; analysis technique; texture; multifractal;
D O I
10.1016/S0098-3004(99)00061-8
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
Scale invariance is rapidly becoming a new paradigm for geophysics. However, little attention has been paid to the anisotropy that is invariably present in geophysical fields in the form of differential stratification and rotation, texture and morphology. In order to account for scaling anisotriopy, the formalism of generalized scale invariance (GSI) was developed. Until now there has existed only a single fairly ad hoc GSI analysis technique valid for studying differential rotation. In this paper, we use a two-dimensional representation of the linear approximation to generalized scale invariance, to obtain a much improved technique for quantifying anisotropic scale invariance called the scale invariant generator technique (SIG). The accuracy of the technique is tested using anisotropic multifractal simulations and error estimates are provided for the geophysically relevant range of parameters. It is found that the technique yields reasonable estimates for simulations with a diversity of anisotropic and statistical characteristics. The scale invariant generator technique can profitably be applied to the scale invariant study of vertical/horizontal and space/time cross-sections of geophysical fields as well as to the study of the texture/morphology of fields. (C) 1999 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:963 / 978
页数:16
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