Why was the Paraná flood of 2016 weaker than that of 1998?

Although the 2015-16 El Niño was expected to cause a severe Paraná River flood similar to that associated with the 1997?98 El Niño, the Paraná flood of 2016 was considerably weaker than that of 1998. Here we explain this by analyzing Paraná discharge data (1904-2017) to assess the contributions of d...

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Published in:International Journal of Climatology
Main Authors: Antico, Andres, Diaz, Henry
Format: Article in Journal/Newspaper
Language:English
Published: John Wiley & Sons Ltd
Subjects:
Online Access:http://hdl.handle.net/11336/233052
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author Antico, Andres
Diaz, Henry
author_facet Antico, Andres
Diaz, Henry
author_sort Antico, Andres
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
container_issue 1
container_start_page 604
container_title International Journal of Climatology
container_volume 40
description Although the 2015-16 El Niño was expected to cause a severe Paraná River flood similar to that associated with the 1997?98 El Niño, the Paraná flood of 2016 was considerably weaker than that of 1998. Here we explain this by analyzing Paraná discharge data (1904-2017) to assess the contributions of discharge cycles with different frequencies and with different associated climate modes to the formation of the 1998 and 2016 floods. We found that the 2016 flood was relatively weak mainly because the following Paraná discharge cycles contributed less to form the 2016 flood than to form the 1998 flood: (i) a 3-5 year cycle linked to El Niño/Southern Oscillation (ENSO), (ii) a 9 year cycle related to the North Atlantic Oscillation (NAO), and (iii) a 31-85 year cycle associated with the Interdecadal Pacific Oscillation (IPO). This finding suggests that, besides ENSO, two other climate modes (NAO and IPO) may have acted to weaken the 2016 flood. Fil: Antico, Andres. Universidad Nacional del Litoral. Instituto de Humanidades y Ciencias Sociales del Litoral. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Santa Fe. Instituto de Humanidades y Ciencias Sociales del Litoral; Argentina Fil: Diaz, Henry. University of Hawaii at Manoa; Estados Unidos
format Article in Journal/Newspaper
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
geographic Pacific
Argentina
Diaz
geographic_facet Pacific
Argentina
Diaz
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op_doi https://doi.org/10.1002/joc.6204
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http://hdl.handle.net/11336/233052
Antico, Andres; Diaz, Henry; Why was the Paraná flood of 2016 weaker than that of 1998?; John Wiley & Sons Ltd; International Journal of Climatology; 40; 1; 6-2019; 604-609
0899-8418
1097-0088
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/233052 2025-01-16T23:41:52+00:00 Why was the Paraná flood of 2016 weaker than that of 1998? Antico, Andres Diaz, Henry application/pdf http://hdl.handle.net/11336/233052 eng eng John Wiley & Sons Ltd info:eu-repo/semantics/altIdentifier/url/https://rmets.onlinelibrary.wiley.com/doi/10.1002/joc.6204 info:eu-repo/semantics/altIdentifier/doi/10.1002/joc.6204 http://hdl.handle.net/11336/233052 Antico, Andres; Diaz, Henry; Why was the Paraná flood of 2016 weaker than that of 1998?; John Wiley & Sons Ltd; International Journal of Climatology; 40; 1; 6-2019; 604-609 0899-8418 1097-0088 CONICET Digital CONICET info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ SOUTH AMERICA PARANÁ RIVER FLOODS EL NIÑO ENSO NAO IPO 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/joc.6204 2024-04-18T23:41:34Z Although the 2015-16 El Niño was expected to cause a severe Paraná River flood similar to that associated with the 1997?98 El Niño, the Paraná flood of 2016 was considerably weaker than that of 1998. Here we explain this by analyzing Paraná discharge data (1904-2017) to assess the contributions of discharge cycles with different frequencies and with different associated climate modes to the formation of the 1998 and 2016 floods. We found that the 2016 flood was relatively weak mainly because the following Paraná discharge cycles contributed less to form the 2016 flood than to form the 1998 flood: (i) a 3-5 year cycle linked to El Niño/Southern Oscillation (ENSO), (ii) a 9 year cycle related to the North Atlantic Oscillation (NAO), and (iii) a 31-85 year cycle associated with the Interdecadal Pacific Oscillation (IPO). This finding suggests that, besides ENSO, two other climate modes (NAO and IPO) may have acted to weaken the 2016 flood. Fil: Antico, Andres. Universidad Nacional del Litoral. Instituto de Humanidades y Ciencias Sociales del Litoral. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Santa Fe. Instituto de Humanidades y Ciencias Sociales del Litoral; Argentina Fil: Diaz, Henry. University of Hawaii at Manoa; 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) International Journal of Climatology 40 1 604 609
spellingShingle SOUTH AMERICA
PARANÁ RIVER
FLOODS
EL NIÑO
ENSO
NAO
IPO
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Antico, Andres
Diaz, Henry
Why was the Paraná flood of 2016 weaker than that of 1998?
title Why was the Paraná flood of 2016 weaker than that of 1998?
title_full Why was the Paraná flood of 2016 weaker than that of 1998?
title_fullStr Why was the Paraná flood of 2016 weaker than that of 1998?
title_full_unstemmed Why was the Paraná flood of 2016 weaker than that of 1998?
title_short Why was the Paraná flood of 2016 weaker than that of 1998?
title_sort why was the paraná flood of 2016 weaker than that of 1998?
topic SOUTH AMERICA
PARANÁ RIVER
FLOODS
EL NIÑO
ENSO
NAO
IPO
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet SOUTH AMERICA
PARANÁ RIVER
FLOODS
EL NIÑO
ENSO
NAO
IPO
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/233052