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On the Determination of the Codimension Function

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Non-Linear Variability in Geophysics

Abstract

Motivated by the necessity of developing new multifractal analysis techniques to characterize empirical fields by scale invariant (sensor resolution independent) codimension functions, we introduce a new method, PDMS, to directly estimate the codimension of the singularity spectrum c(γ) and we also indicate the theoretical (or practical) limits of this method as well as its consequences for the determination of highest values of c(γ). These properties also have implications for the behaviour of K(h) — related to c(γ) by a Legendre transformation — in particular for large h. The characteristic behaviour of c(γ) and K(h) are illustrated respectively by the estimation of the scaling properties of the probability distribution and of statistical moments of simulated fields, obtained with multiplicative self similar cascade processes.

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© 1991 Kluwer Academic Publishers

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Lavallée, D., Schertzer, D., Lovejoy, S. (1991). On the Determination of the Codimension Function. In: Schertzer, D., Lovejoy, S. (eds) Non-Linear Variability in Geophysics. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-2147-4_7

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  • DOI: https://doi.org/10.1007/978-94-009-2147-4_7

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-94-010-7466-7

  • Online ISBN: 978-94-009-2147-4

  • eBook Packages: Springer Book Archive

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