Analysis of hydroclimatic variability and trends using a novel empirical mode decomposition: Application to the Paraná River Basin

The current understanding of hydroclimatic processes is largely based on time series analysis of observations such as river discharge. Although records of these variables are often nonlinear and nonstationary, they have been commonly analyzed by classical methods designed for linear and/or stationar...

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Published in:Journal of Geophysical Research: Atmospheres
Main Authors: Antico, Andres, Schlotthauer, Gaston, Torres, Maria Eugenia
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union
Subjects:
Online Access:http://hdl.handle.net/11336/85993
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author Antico, Andres
Schlotthauer, Gaston
Torres, Maria Eugenia
author_facet Antico, Andres
Schlotthauer, Gaston
Torres, Maria Eugenia
author_sort Antico, Andres
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
container_issue 3
container_start_page 1218
container_title Journal of Geophysical Research: Atmospheres
container_volume 119
description The current understanding of hydroclimatic processes is largely based on time series analysis of observations such as river discharge. Although records of these variables are often nonlinear and nonstationary, they have been commonly analyzed by classical methods designed for linear and/or stationary data. This study investigates the possibility of analyzing hydroclimatic time series using a novel data-driven method named Complete Ensemble Empirical Mode Decomposition with Adaptive Noise (CEEMDAN), which is suitable for nonlinear and nonstationary signals. CEEMDAN is here applied to a monthly mean discharge record (1904–2010) of the Paraná River (South America). The results obtained in this way are interpreted by comparing them with CEEMDAN decompositions of other records such as climate index time series. It is found that Paraná flow modes consist of (i) annual and intraannual oscillations reflecting the rainfall seasonality of different Paraná Basin sectors, and (ii) interannual to interdecadal changes linked to climate cycles like El Niño/Southern Oscillation, the North Atlantic Oscillation, and the Interdecadal Pacific Oscillation. A nonlinear trend of Paraná discharge is found and reveals a monotonic increase that could be attributed to global warming and anthropogenic land-cover changes. The spectral separation of modes obtained using CEEMDAN is cleaner than that achieved by the Ensemble Empirical Mode Decomposition technique. This makes it easier to interpret CEEMDAN results. Hence, CEEMDAN is proposed as a powerful method for extracting physically meaningful information from hydroclimatic data. Fil: Antico, Andres. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional del Litoral. Facultad de Ingeniería y Ciencias Hídricas; Argentina Fil: Schlotthauer, Gaston. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Entre Ríos. Facultad de Ingeniería; Argentina Fil: Torres, Maria Eugenia. Consejo Nacional de Investigaciones ...
format Article in Journal/Newspaper
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
geographic Pacific
Argentina
Gaston
Entre Ríos
geographic_facet Pacific
Argentina
Gaston
Entre Ríos
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language English
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op_doi https://doi.org/10.1002/2013JD020420
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http://hdl.handle.net/11336/85993
Antico, Andres; Schlotthauer, Gaston; Torres, Maria Eugenia; Analysis of hydroclimatic variability and trends using a novel empirical mode decomposition: Application to the Paraná River Basin; American Geophysical Union; Journal of Geophysical Research; 119; 3; 2-2014; 1218-1233
2169-8996
CONICET Digital
CONICET
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/85993 2025-01-16T23:45:04+00:00 Analysis of hydroclimatic variability and trends using a novel empirical mode decomposition: Application to the Paraná River Basin Antico, Andres Schlotthauer, Gaston Torres, Maria Eugenia application/pdf http://hdl.handle.net/11336/85993 eng eng American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1002/2013JD020420 info:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2013JD020420 http://hdl.handle.net/11336/85993 Antico, Andres; Schlotthauer, Gaston; Torres, Maria Eugenia; Analysis of hydroclimatic variability and trends using a novel empirical mode decomposition: Application to the Paraná River Basin; American Geophysical Union; Journal of Geophysical Research; 119; 3; 2-2014; 1218-1233 2169-8996 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ Empirical Mode Decomposition Complete EEMD with Adaptive Noise Nonlinear Trends Paraná River Hydroclimatic Variability https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1002/2013JD020420 2023-09-24T19:05:25Z The current understanding of hydroclimatic processes is largely based on time series analysis of observations such as river discharge. Although records of these variables are often nonlinear and nonstationary, they have been commonly analyzed by classical methods designed for linear and/or stationary data. This study investigates the possibility of analyzing hydroclimatic time series using a novel data-driven method named Complete Ensemble Empirical Mode Decomposition with Adaptive Noise (CEEMDAN), which is suitable for nonlinear and nonstationary signals. CEEMDAN is here applied to a monthly mean discharge record (1904–2010) of the Paraná River (South America). The results obtained in this way are interpreted by comparing them with CEEMDAN decompositions of other records such as climate index time series. It is found that Paraná flow modes consist of (i) annual and intraannual oscillations reflecting the rainfall seasonality of different Paraná Basin sectors, and (ii) interannual to interdecadal changes linked to climate cycles like El Niño/Southern Oscillation, the North Atlantic Oscillation, and the Interdecadal Pacific Oscillation. A nonlinear trend of Paraná discharge is found and reveals a monotonic increase that could be attributed to global warming and anthropogenic land-cover changes. The spectral separation of modes obtained using CEEMDAN is cleaner than that achieved by the Ensemble Empirical Mode Decomposition technique. This makes it easier to interpret CEEMDAN results. Hence, CEEMDAN is proposed as a powerful method for extracting physically meaningful information from hydroclimatic data. Fil: Antico, Andres. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional del Litoral. Facultad de Ingeniería y Ciencias Hídricas; Argentina Fil: Schlotthauer, Gaston. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Entre Ríos. Facultad de Ingeniería; Argentina Fil: Torres, Maria Eugenia. Consejo Nacional de Investigaciones ... Article in Journal/Newspaper North Atlantic North Atlantic oscillation CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Pacific Argentina Gaston ENVELOPE(65.783,65.783,-70.417,-70.417) Entre Ríos ENVELOPE(-66.333,-66.333,-66.433,-66.433) Journal of Geophysical Research: Atmospheres 119 3 1218 1233
spellingShingle Empirical Mode Decomposition
Complete EEMD with Adaptive Noise
Nonlinear Trends
Paraná River
Hydroclimatic Variability
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Antico, Andres
Schlotthauer, Gaston
Torres, Maria Eugenia
Analysis of hydroclimatic variability and trends using a novel empirical mode decomposition: Application to the Paraná River Basin
title Analysis of hydroclimatic variability and trends using a novel empirical mode decomposition: Application to the Paraná River Basin
title_full Analysis of hydroclimatic variability and trends using a novel empirical mode decomposition: Application to the Paraná River Basin
title_fullStr Analysis of hydroclimatic variability and trends using a novel empirical mode decomposition: Application to the Paraná River Basin
title_full_unstemmed Analysis of hydroclimatic variability and trends using a novel empirical mode decomposition: Application to the Paraná River Basin
title_short Analysis of hydroclimatic variability and trends using a novel empirical mode decomposition: Application to the Paraná River Basin
title_sort analysis of hydroclimatic variability and trends using a novel empirical mode decomposition: application to the paraná river basin
topic Empirical Mode Decomposition
Complete EEMD with Adaptive Noise
Nonlinear Trends
Paraná River
Hydroclimatic Variability
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet Empirical Mode Decomposition
Complete EEMD with Adaptive Noise
Nonlinear Trends
Paraná River
Hydroclimatic Variability
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/85993