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...
Published in: | International Journal of Climatology |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
John Wiley & Sons Ltd
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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 |
id | ftconicet:oai:ri.conicet.gov.ar:11336/233052 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-60.667,-60.667,-63.783,-63.783) |
op_collection_id | ftconicet |
op_container_end_page | 609 |
op_doi | https://doi.org/10.1002/joc.6204 |
op_relation | 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 |
op_rights | info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
publisher | John Wiley & Sons Ltd |
record_format | openpolar |
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 |