Extreme discharge events in the Paraná River and their climate forcing
The largest discharge anomalies of the Paraná River were examined focusing on the contribution from the sub-basins and on the climate forcing of these events. Major discharge anomalies at Corrientes originated in the central and southern Upper Paraná basin with relatively small contributions from th...
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Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00221694_v278_n1-4_p94_Camilloni http://hdl.handle.net/20.500.12110/paper_00221694_v278_n1-4_p94_Camilloni |
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paper:paper_00221694_v278_n1-4_p94_Camilloni2023-06-08T14:46:52Z Extreme discharge events in the Paraná River and their climate forcing Camilloni, Ines Angela Barros, Vicente Ricardo El Niño Flood Paraná River discharge Climatology Precipitation (meteorology) Rivers Climate forcing Hydrology climate forcing El Nino-Southern Oscillation extreme event flooding river discharge Parana River South America The largest discharge anomalies of the Paraná River were examined focusing on the contribution from the sub-basins and on the climate forcing of these events. Major discharge anomalies at Corrientes originated in the central and southern Upper Paraná basin with relatively small contributions from the Paraguay river and the northern Upper Paraná basin. About two thirds of the major discharge anomalies in Corrientes occurred during El Niño events while none was registered during La Niña events. Major discharge anomalies related to El Niño occurred either in the spring of the year of El Niño onset or in autumn of the following year (autumn (+)) accompanying the precipitation signal of El Niño in eastern subtropical South America. The signal during autumn (+) is the most relevant as five out the six top discharges of the Paraná River at Corrientes occurred in this season. The remaining third of the major discharges not related to El Niño took place during the austral spring or austral summer of neutral periods. In each of these seasons, they share a common sea surface temperature anomaly pattern in the proximity of the South American coasts. © 2003 Elsevier Science B.V. All rights reserved. Fil:Camilloni, I.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Barros, V.R. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2003 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00221694_v278_n1-4_p94_Camilloni http://hdl.handle.net/20.500.12110/paper_00221694_v278_n1-4_p94_Camilloni |
institution |
Universidad de Buenos Aires |
institution_str |
I-28 |
repository_str |
R-134 |
collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
topic |
El Niño Flood Paraná River discharge Climatology Precipitation (meteorology) Rivers Climate forcing Hydrology climate forcing El Nino-Southern Oscillation extreme event flooding river discharge Parana River South America |
spellingShingle |
El Niño Flood Paraná River discharge Climatology Precipitation (meteorology) Rivers Climate forcing Hydrology climate forcing El Nino-Southern Oscillation extreme event flooding river discharge Parana River South America Camilloni, Ines Angela Barros, Vicente Ricardo Extreme discharge events in the Paraná River and their climate forcing |
topic_facet |
El Niño Flood Paraná River discharge Climatology Precipitation (meteorology) Rivers Climate forcing Hydrology climate forcing El Nino-Southern Oscillation extreme event flooding river discharge Parana River South America |
description |
The largest discharge anomalies of the Paraná River were examined focusing on the contribution from the sub-basins and on the climate forcing of these events. Major discharge anomalies at Corrientes originated in the central and southern Upper Paraná basin with relatively small contributions from the Paraguay river and the northern Upper Paraná basin. About two thirds of the major discharge anomalies in Corrientes occurred during El Niño events while none was registered during La Niña events. Major discharge anomalies related to El Niño occurred either in the spring of the year of El Niño onset or in autumn of the following year (autumn (+)) accompanying the precipitation signal of El Niño in eastern subtropical South America. The signal during autumn (+) is the most relevant as five out the six top discharges of the Paraná River at Corrientes occurred in this season. The remaining third of the major discharges not related to El Niño took place during the austral spring or austral summer of neutral periods. In each of these seasons, they share a common sea surface temperature anomaly pattern in the proximity of the South American coasts. © 2003 Elsevier Science B.V. All rights reserved. |
author |
Camilloni, Ines Angela Barros, Vicente Ricardo |
author_facet |
Camilloni, Ines Angela Barros, Vicente Ricardo |
author_sort |
Camilloni, Ines Angela |
title |
Extreme discharge events in the Paraná River and their climate forcing |
title_short |
Extreme discharge events in the Paraná River and their climate forcing |
title_full |
Extreme discharge events in the Paraná River and their climate forcing |
title_fullStr |
Extreme discharge events in the Paraná River and their climate forcing |
title_full_unstemmed |
Extreme discharge events in the Paraná River and their climate forcing |
title_sort |
extreme discharge events in the paraná river and their climate forcing |
publishDate |
2003 |
url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00221694_v278_n1-4_p94_Camilloni http://hdl.handle.net/20.500.12110/paper_00221694_v278_n1-4_p94_Camilloni |
work_keys_str_mv |
AT camilloniinesangela extremedischargeeventsintheparanariverandtheirclimateforcing AT barrosvicentericardo extremedischargeeventsintheparanariverandtheirclimateforcing |
_version_ |
1768541878764961792 |