Anisotropic multiresolution analysis in 2D: application to long-range correlations in cloud millimeter-radar fields

Taking a wavelet standpoint, we survey on the one hand various approaches to multifractal analysis, as a means of characterizing long-range correlations in data, and on the other hand various ways of statistically measuring anisotropy in 2D fields. In both instances, we present new and related techniques: (1) a simple multifractal analysis methodology based on Discrete Wavelet Transforms (DWTs), and (2) a specific DWT adapted to strongly anisotropic fields sampled on rectangular grids with large aspect ratios. This DWT uses a tensor product of the standard dyadic Haar basis (dividing ratio 2) and a non-standard triadic counterpart (dividing ratio 3) which includes the famous `French to-hat' wavelet. The new DWT is amenable to an anisotropic version of Multi-Resolution Analysis (MRA) in image processing where the natural support of the field is 2n pixels (vertically) by 3n pixels (horizontally), n being the number of levels in the MRA. The complete 2D basis has one scaling function and five wavelets. The new MRA is used in synthesis mode to generate random multifractal fields that mimic quite realistically the structure and distribution of boundary-layer clouds even though only a few parameters are used to control statistically the wavelet coefficients of the liquid water density field.

[1]  Jensen,et al.  Fractal measures and their singularities: The characterization of strange sets. , 1987, Physical review. A, General physics.

[2]  Patrick Flandrin,et al.  Wavelet analysis and synthesis of fractional Brownian motion , 1992, IEEE Trans. Inf. Theory.

[3]  Roberto Benzi,et al.  A random process for the construction of multiaffine fields , 1993 .

[4]  Anthony B. Davis,et al.  Scale Invariance in Liquid Water Distributions in Marine Stratocumulus. Part II: Multifractal Properties and Intermittency Issues , 1997 .

[5]  Anthony B. Davis,et al.  Scale Invariance of Liquid Water Distributions in Marine Stratocumulus. Part I: Spectral Properties and Stationarity Issues , 1996 .

[6]  Emmanuel Bacry,et al.  THE THERMODYNAMICS OF FRACTALS REVISITED WITH WAVELETS , 1995 .

[7]  Robert F. Cahalan,et al.  Bounded cascade models as nonstationary multifractals. , 1994, Physical review. E, Statistical physics, plasmas, fluids, and related interdisciplinary topics.

[8]  D. Schertzer,et al.  Physical modeling and analysis of rain and clouds by anisotropic scaling multiplicative processes , 1987 .

[9]  Stéphane Mallat,et al.  A Theory for Multiresolution Signal Decomposition: The Wavelet Representation , 1989, IEEE Trans. Pattern Anal. Mach. Intell..

[10]  A. Arneodo,et al.  WAVELET BASED MULTIFRACTAL ANALYSIS OF ROUGH SURFACES : APPLICATION TO CLOUD MODELS AND SATELLITE DATA , 1997 .

[11]  C. Meneveau,et al.  Simple multifractal cascade model for fully developed turbulence. , 1987, Physical review letters.

[12]  O. Rioul,et al.  Wavelets and signal processing , 1991, IEEE Signal Processing Magazine.

[13]  Robert F. Cahalan,et al.  The albedo of fractal stratocumulus clouds , 1994 .

[14]  E. Bacry,et al.  Multifractal formalism for fractal signals: The structure-function approach versus the wavelet-transform modulus-maxima method. , 1993, Physical review. E, Statistical physics, plasmas, fluids, and related interdisciplinary topics.

[15]  B. Mandelbrot Intermittent turbulence in self-similar cascades: divergence of high moments and dimension of the carrier , 1974, Journal of Fluid Mechanics.

[16]  E. Bacry,et al.  The Multifractal Formalism Revisited with Wavelets , 1994 .