ENSO and Paraná flow variability: Long-term changes in their connectivity
The Paraná River of South America is one of the largest rivers in the world. Although the connection between Paraná streamflow and El Niño–Southern Oscillation (ENSO) has been studied before, little is known about the long-term (interdecadal) changes of this connectivity. Here we reveal these change...
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/11336/203755 |
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author | Antico, Andres Vuille, Mathias |
author_facet | Antico, Andres Vuille, Mathias |
author_sort | Antico, Andres |
collection | CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) |
container_issue | 14 |
container_start_page | 7269 |
container_title | International Journal of Climatology |
container_volume | 42 |
description | The Paraná River of South America is one of the largest rivers in the world. Although the connection between Paraná streamflow and El Niño–Southern Oscillation (ENSO) has been studied before, little is known about the long-term (interdecadal) changes of this connectivity. Here we reveal these changes by analysing long instrumental records of Paraná flow, ENSO indices and other climate variables. We find that flow and ENSO were connected in 1876–1940 and 1983–2016, but disconnected in 1941–1982. Flow variability was more related to central Pacific ENSO fluctuations in 1876–1940 but more linked with eastern Pacific ones in 1983–2016, probably because the ENSO–Paraná basin teleconnection was different in the two periods. ENSO-related Pacific climate anomalies exhibited their smallest amplitudes during the disconnection period 1941–1982, suggesting that the ENSO–flow link vanishes when ENSO is weak. We also find that the ENSO–flow disconnection coincided with the coldest phase of the Interdecadal Pacific Oscillation (IPO) in the study period. Thus, the IPO may be modulating the ENSO–flow connectivity. Interestingly, during the disconnection years (1941–1982), flow was related to climate variability observed in sectors of the southern South Atlantic and tropical North Atlantic oceans. This and the other empirical results presented here provide new insights into the Paraná response to ENSO and thus provide valuable information for future mechanistic studies on this response. 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: Vuille, Mathias. State University Of New York. University At Albany.; Estados Unidos |
format | Article in Journal/Newspaper |
genre | North Atlantic |
genre_facet | North Atlantic |
geographic | Argentina Pacific |
geographic_facet | Argentina Pacific |
id | ftconicet:oai:ri.conicet.gov.ar:11336/203755 |
institution | Open Polar |
language | English |
op_collection_id | ftconicet |
op_container_end_page | 7279 |
op_doi | https://doi.org/10.1002/joc.7643 |
op_relation | info:eu-repo/semantics/altIdentifier/doi/10.1002/joc.7643 http://hdl.handle.net/11336/203755 Antico, Andres; Vuille, Mathias; ENSO and Paraná flow variability: Long-term changes in their connectivity; John Wiley & Sons Ltd; International Journal of Climatology; 42; 14; 4-2022; 7269-7279 0899-8418 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:11336/203755 2025-01-16T23:43:33+00:00 ENSO and Paraná flow variability: Long-term changes in their connectivity Antico, Andres Vuille, Mathias application/pdf http://hdl.handle.net/11336/203755 eng eng John Wiley & Sons Ltd info:eu-repo/semantics/altIdentifier/doi/10.1002/joc.7643 http://hdl.handle.net/11336/203755 Antico, Andres; Vuille, Mathias; ENSO and Paraná flow variability: Long-term changes in their connectivity; John Wiley & Sons Ltd; International Journal of Climatology; 42; 14; 4-2022; 7269-7279 0899-8418 CONICET Digital CONICET info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ ENSO IPO PARANÁ RIVER SOUTH AMERICA STREAMFLOW 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.7643 2023-09-24T18:43:47Z The Paraná River of South America is one of the largest rivers in the world. Although the connection between Paraná streamflow and El Niño–Southern Oscillation (ENSO) has been studied before, little is known about the long-term (interdecadal) changes of this connectivity. Here we reveal these changes by analysing long instrumental records of Paraná flow, ENSO indices and other climate variables. We find that flow and ENSO were connected in 1876–1940 and 1983–2016, but disconnected in 1941–1982. Flow variability was more related to central Pacific ENSO fluctuations in 1876–1940 but more linked with eastern Pacific ones in 1983–2016, probably because the ENSO–Paraná basin teleconnection was different in the two periods. ENSO-related Pacific climate anomalies exhibited their smallest amplitudes during the disconnection period 1941–1982, suggesting that the ENSO–flow link vanishes when ENSO is weak. We also find that the ENSO–flow disconnection coincided with the coldest phase of the Interdecadal Pacific Oscillation (IPO) in the study period. Thus, the IPO may be modulating the ENSO–flow connectivity. Interestingly, during the disconnection years (1941–1982), flow was related to climate variability observed in sectors of the southern South Atlantic and tropical North Atlantic oceans. This and the other empirical results presented here provide new insights into the Paraná response to ENSO and thus provide valuable information for future mechanistic studies on this response. 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: Vuille, Mathias. State University Of New York. University At Albany.; Estados Unidos Article in Journal/Newspaper North Atlantic CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Argentina Pacific International Journal of Climatology 42 14 7269 7279 |
spellingShingle | ENSO IPO PARANÁ RIVER SOUTH AMERICA STREAMFLOW https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 Antico, Andres Vuille, Mathias ENSO and Paraná flow variability: Long-term changes in their connectivity |
title | ENSO and Paraná flow variability: Long-term changes in their connectivity |
title_full | ENSO and Paraná flow variability: Long-term changes in their connectivity |
title_fullStr | ENSO and Paraná flow variability: Long-term changes in their connectivity |
title_full_unstemmed | ENSO and Paraná flow variability: Long-term changes in their connectivity |
title_short | ENSO and Paraná flow variability: Long-term changes in their connectivity |
title_sort | enso and paraná flow variability: long-term changes in their connectivity |
topic | ENSO IPO PARANÁ RIVER SOUTH AMERICA STREAMFLOW https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
topic_facet | ENSO IPO PARANÁ RIVER SOUTH AMERICA STREAMFLOW https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
url | http://hdl.handle.net/11336/203755 |