Contributions of different time scales to extreme Paraná floods

The present study provides the first complete examination of how different time scales contributed to generate the four largest observed floods of the Paraná River (1905, 1983, 1992 and 1998). This inspection is based on the results from a previous study where an empirical method was used to decompo...

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Published in:Climate Dynamics
Main Authors: Antico, Andres, Torres, Maria Eugenia, Diaz, Henry F.
Format: Article in Journal/Newspaper
Language:English
Published: Springer
Subjects:
Online Access:http://hdl.handle.net/11336/45961
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author Antico, Andres
Torres, Maria Eugenia
Diaz, Henry F.
author_facet Antico, Andres
Torres, Maria Eugenia
Diaz, Henry F.
author_sort Antico, Andres
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
container_issue 11-12
container_start_page 3785
container_title Climate Dynamics
container_volume 46
description The present study provides the first complete examination of how different time scales contributed to generate the four largest observed floods of the Paraná River (1905, 1983, 1992 and 1998). This inspection is based on the results from a previous study where an empirical method was used to decompose a 1904-2010 Paraná flow record (monthly means) into several physically meaningful oscillations with distinctive time scales or periods (few months to decades), and a secular increasing trend. We show that all the oscillations largely contributed to the four extreme floods, except an 18-year cycle that did not contribute to the 1992 flood. Sporadic intense constructive interferences between interannual-to-interdecadal (3-85 years) cycles determined (i) the favorable conditions for extreme-flood occurrence, and (ii) notable differences among floods. Indeed, in 1983, the largest flood ever recorded resulted mainly from an exceptionally strong constructive interference between cycles of 3-5, 9, 18 and 31-85 years, which are related to El Niño events, the North Atlantic Oscillation, the South Atlantic Convergence Zone, and the Pacific Ocean, respectively. Contributions of the 31-85-year cycle to the two biggest floods (1983 and 1992) are larger than the contributions of the secular upward trend, suggesting the importance of this slow oscillation in flood formation processes. The implications of our results for understanding and predicting Paraná floods are discussed. Fil: Antico, Andres. Universidad Nacional del Litoral. Facultad de Ingeniería y Ciencias Hídricas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Santa Fe; Argentina Fil: Torres, Maria Eugenia. Universidad Nacional de Entre Ríos. Facultad de Ingeniería; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Santa Fe; Argentina Fil: Diaz, Henry F. State University of Colorado Boulder; Estados Unidos
format Article in Journal/Newspaper
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
geographic Pacific
Argentina
Diaz
Entre Ríos
geographic_facet Pacific
Argentina
Diaz
Entre Ríos
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/45961 2025-01-16T23:45:11+00:00 Contributions of different time scales to extreme Paraná floods Antico, Andres Torres, Maria Eugenia Diaz, Henry F. application/pdf http://hdl.handle.net/11336/45961 eng eng Springer info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-015-2804-x info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/article/10.1007%2Fs00382-015-2804-x http://hdl.handle.net/11336/45961 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ Parana River Extreme Floods Empirical Time-Scale Decomposition Climate Oscillations 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/10.1007/s00382-015-2804-x 2024-10-04T09:34:03Z The present study provides the first complete examination of how different time scales contributed to generate the four largest observed floods of the Paraná River (1905, 1983, 1992 and 1998). This inspection is based on the results from a previous study where an empirical method was used to decompose a 1904-2010 Paraná flow record (monthly means) into several physically meaningful oscillations with distinctive time scales or periods (few months to decades), and a secular increasing trend. We show that all the oscillations largely contributed to the four extreme floods, except an 18-year cycle that did not contribute to the 1992 flood. Sporadic intense constructive interferences between interannual-to-interdecadal (3-85 years) cycles determined (i) the favorable conditions for extreme-flood occurrence, and (ii) notable differences among floods. Indeed, in 1983, the largest flood ever recorded resulted mainly from an exceptionally strong constructive interference between cycles of 3-5, 9, 18 and 31-85 years, which are related to El Niño events, the North Atlantic Oscillation, the South Atlantic Convergence Zone, and the Pacific Ocean, respectively. Contributions of the 31-85-year cycle to the two biggest floods (1983 and 1992) are larger than the contributions of the secular upward trend, suggesting the importance of this slow oscillation in flood formation processes. The implications of our results for understanding and predicting Paraná floods are discussed. Fil: Antico, Andres. Universidad Nacional del Litoral. Facultad de Ingeniería y Ciencias Hídricas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Santa Fe; Argentina Fil: Torres, Maria Eugenia. Universidad Nacional de Entre Ríos. Facultad de Ingeniería; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Santa Fe; Argentina Fil: Diaz, Henry F. State University of Colorado Boulder; Estados Unidos Article in Journal/Newspaper North Atlantic North Atlantic oscillation CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Pacific Argentina Diaz ENVELOPE(-60.667,-60.667,-63.783,-63.783) Entre Ríos ENVELOPE(-66.333,-66.333,-66.433,-66.433) Climate Dynamics 46 11-12 3785 3792
spellingShingle Parana River
Extreme Floods
Empirical Time-Scale Decomposition
Climate Oscillations
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Antico, Andres
Torres, Maria Eugenia
Diaz, Henry F.
Contributions of different time scales to extreme Paraná floods
title Contributions of different time scales to extreme Paraná floods
title_full Contributions of different time scales to extreme Paraná floods
title_fullStr Contributions of different time scales to extreme Paraná floods
title_full_unstemmed Contributions of different time scales to extreme Paraná floods
title_short Contributions of different time scales to extreme Paraná floods
title_sort contributions of different time scales to extreme paraná floods
topic Parana River
Extreme Floods
Empirical Time-Scale Decomposition
Climate Oscillations
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet Parana River
Extreme Floods
Empirical Time-Scale Decomposition
Climate Oscillations
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/45961