Multidimensional Models for Methodological Validation in Multifractal Analysis
Mathematical modelling of natural phenomena, Tome 3 (2008) no. 6, pp. 33-47
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Multifractal analysis is known as a useful tool in signal analysis. However, the methods are often used without methodological validation. In this study, we present multidimensional models in order to validate multifractal analysis methods.
Affiliations des auteurs :
R. Lopes 1 ; I. Bhouri 2 ; S. Maouche 3 ; P. Dubois 1 ; M. H. Bedoui 4 ; N. Betrouni 1
@article{10_1051_mmnp:2008080,
author = {R. Lopes and I. Bhouri and S. Maouche and P. Dubois and M. H. Bedoui and N. Betrouni},
title = {Multidimensional {Models} for {Methodological} {Validation} in {Multifractal} {Analysis}},
journal = {Mathematical modelling of natural phenomena},
pages = {33--47},
publisher = {mathdoc},
volume = {3},
number = {6},
year = {2008},
doi = {10.1051/mmnp:2008080},
language = {en},
url = {http://geodesic.mathdoc.fr/articles/10.1051/mmnp:2008080/}
}
TY - JOUR AU - R. Lopes AU - I. Bhouri AU - S. Maouche AU - P. Dubois AU - M. H. Bedoui AU - N. Betrouni TI - Multidimensional Models for Methodological Validation in Multifractal Analysis JO - Mathematical modelling of natural phenomena PY - 2008 SP - 33 EP - 47 VL - 3 IS - 6 PB - mathdoc UR - http://geodesic.mathdoc.fr/articles/10.1051/mmnp:2008080/ DO - 10.1051/mmnp:2008080 LA - en ID - 10_1051_mmnp:2008080 ER -
%0 Journal Article %A R. Lopes %A I. Bhouri %A S. Maouche %A P. Dubois %A M. H. Bedoui %A N. Betrouni %T Multidimensional Models for Methodological Validation in Multifractal Analysis %J Mathematical modelling of natural phenomena %D 2008 %P 33-47 %V 3 %N 6 %I mathdoc %U http://geodesic.mathdoc.fr/articles/10.1051/mmnp:2008080/ %R 10.1051/mmnp:2008080 %G en %F 10_1051_mmnp:2008080
R. Lopes; I. Bhouri; S. Maouche; P. Dubois; M. H. Bedoui; N. Betrouni. Multidimensional Models for Methodological Validation in Multifractal Analysis. Mathematical modelling of natural phenomena, Tome 3 (2008) no. 6, pp. 33-47. doi: 10.1051/mmnp:2008080
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