Multifractality of Brazilian rivers

•We use the Multifractal Detrended Fluctuation Analysis to study water levels.•We model 16 Brazilian hydrological stations situated in 12 rivers.•We obtain the generalized Hurst exponents for water level time series.•All the analyzed series demonstrate multifractality and nonstationary behavior.•We...

Full description

Saved in:
Bibliographic Details
Published in:Journal of hydrology (Amsterdam) Vol. 495; pp. 208 - 215
Main Authors: Rego, C.R.C., Frota, H.O., Gusmão, M.S.
Format: Journal Article
Language:English
Published: Kidlington Elsevier B.V 12-07-2013
Elsevier
Subjects:
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:•We use the Multifractal Detrended Fluctuation Analysis to study water levels.•We model 16 Brazilian hydrological stations situated in 12 rivers.•We obtain the generalized Hurst exponents for water level time series.•All the analyzed series demonstrate multifractality and nonstationary behavior.•We use the multiplicative cascade model equation to fit the spectra of the exponents. We use the Multifractal Detrended Fluctuation Analysis (MF-DFA) to study the complex water fluctuations of some of the principal Brazilian rivers. We obtain the generalized Hurst exponents for the series of water level of 16 hydrological stations, situated in cities of different climatic zones in Brazil. From this analysis, we can state that all the series analyzed demonstrate multifractality and nonstationary behavior. This paper shows that it is possible to treat the Brazilian river water levels from the multifractal perspective and thereby to have a better understanding of the complex behavior of the scaling laws present within these series.
Bibliography:ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0022-1694
1879-2707
DOI:10.1016/j.jhydrol.2013.04.046