Parana River morphodynamics in the context of climate change

Autores
Guerrero, Massimo; Nones, Michael; Saurral, Ramiro Ignacio; Montroull, Natalia Blanca; Szupiany, Ricardo Nicolas
Año de publicación
2013
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
This paper presents an analysis of the sediment dynamics that takes place at different scales within the Middle and the Lower Parana River in the La Plata Basin. The aim of this study is to provide a multi-disciplinary and multi-scale approach for the prediction of river future morphology in the context of climate change, the intended use of which is the prognosis of river morphodynamics long-term impact on manmade structures and activities over or near the river. The study is based on three levels of mathematical modelling, with the output of wider-scale models providing the input conditions for more specific ones. Climate models give the input ensemble, i.e., future precipitation and temperature over La Plata Basin. The semi-distributed macroscale VIC hydrological model simulates the flow discharge time series that are applied to an own-developed 1-D morphodynamic model. The 1-D model simulates future rate of sediment transport and corresponding bed level changes at watershed scale and provides the boundary conditions for a 2-D model. Therefore, streamflow divagations at channel scale are simulated by means of the MIKE21C code developed by the Danish Hydraulic Institute. The analysis indicates a rather low sensitivity of the Parana River bed profile, i.e., 1-D morphology, to the increase predicted in flow discharge, whereas the streamflow appreciably divagates. In particular, surpassing an upper bound in the most frequent discharge appears effective in driving the actual bifurcated morphology into a meandering-multithread configuration.
Fil: Guerrero, Massimo. Universidad de Bologna. Hydraulic Laboratory; Italia
Fil: Nones, Michael. Universidad de Bologna. Fluid Dynamics Unit. Research Center for Constructions; Italia
Fil: Saurral, Ramiro Ignacio. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinacion Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera; Argentina
Fil: Montroull, Natalia Blanca. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinacion Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera; Argentina
Fil: Szupiany, Ricardo Nicolas. Universidad Nacional del Litoral. Facultad de Ingeniería y Ciencias Hídricas; Argentina
Materia
Parana River
Climate Change Impact
Sediment Transport
Morphodynamics
River Morphology
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/4468

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spelling Parana River morphodynamics in the context of climate changeGuerrero, MassimoNones, MichaelSaurral, Ramiro IgnacioMontroull, Natalia BlancaSzupiany, Ricardo NicolasParana RiverClimate Change ImpactSediment TransportMorphodynamicsRiver Morphologyhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1This paper presents an analysis of the sediment dynamics that takes place at different scales within the Middle and the Lower Parana River in the La Plata Basin. The aim of this study is to provide a multi-disciplinary and multi-scale approach for the prediction of river future morphology in the context of climate change, the intended use of which is the prognosis of river morphodynamics long-term impact on manmade structures and activities over or near the river. The study is based on three levels of mathematical modelling, with the output of wider-scale models providing the input conditions for more specific ones. Climate models give the input ensemble, i.e., future precipitation and temperature over La Plata Basin. The semi-distributed macroscale VIC hydrological model simulates the flow discharge time series that are applied to an own-developed 1-D morphodynamic model. The 1-D model simulates future rate of sediment transport and corresponding bed level changes at watershed scale and provides the boundary conditions for a 2-D model. Therefore, streamflow divagations at channel scale are simulated by means of the MIKE21C code developed by the Danish Hydraulic Institute. The analysis indicates a rather low sensitivity of the Parana River bed profile, i.e., 1-D morphology, to the increase predicted in flow discharge, whereas the streamflow appreciably divagates. In particular, surpassing an upper bound in the most frequent discharge appears effective in driving the actual bifurcated morphology into a meandering-multithread configuration.Fil: Guerrero, Massimo. Universidad de Bologna. Hydraulic Laboratory; ItaliaFil: Nones, Michael. Universidad de Bologna. Fluid Dynamics Unit. Research Center for Constructions; ItaliaFil: Saurral, Ramiro Ignacio. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinacion Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera; ArgentinaFil: Montroull, Natalia Blanca. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinacion Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera; ArgentinaFil: Szupiany, Ricardo Nicolas. Universidad Nacional del Litoral. Facultad de Ingeniería y Ciencias Hídricas; ArgentinaTaylor & Francis2013-09info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/4468Guerrero, Massimo; Nones, Michael; Saurral, Ramiro Ignacio; Montroull, Natalia Blanca; Szupiany, Ricardo Nicolas; Parana River morphodynamics in the context of climate change; Taylor & Francis; International Journal of River Basin Management; 11; 4; 9-2013; 423-4371571-5124enginfo:eu-repo/semantics/altIdentifier/url/http://www.tandfonline.com/doi/full/10.1080/15715124.2013.826234info:eu-repo/semantics/altIdentifier/doi/DOI:10.1080/15715124.2013.826234info:eu-repo/semantics/altIdentifier/issn/1571-5124info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:19:13Zoai:ri.conicet.gov.ar:11336/4468instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 10:19:13.309CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Parana River morphodynamics in the context of climate change
title Parana River morphodynamics in the context of climate change
spellingShingle Parana River morphodynamics in the context of climate change
Guerrero, Massimo
Parana River
Climate Change Impact
Sediment Transport
Morphodynamics
River Morphology
title_short Parana River morphodynamics in the context of climate change
title_full Parana River morphodynamics in the context of climate change
title_fullStr Parana River morphodynamics in the context of climate change
title_full_unstemmed Parana River morphodynamics in the context of climate change
title_sort Parana River morphodynamics in the context of climate change
dc.creator.none.fl_str_mv Guerrero, Massimo
Nones, Michael
Saurral, Ramiro Ignacio
Montroull, Natalia Blanca
Szupiany, Ricardo Nicolas
author Guerrero, Massimo
author_facet Guerrero, Massimo
Nones, Michael
Saurral, Ramiro Ignacio
Montroull, Natalia Blanca
Szupiany, Ricardo Nicolas
author_role author
author2 Nones, Michael
Saurral, Ramiro Ignacio
Montroull, Natalia Blanca
Szupiany, Ricardo Nicolas
author2_role author
author
author
author
dc.subject.none.fl_str_mv Parana River
Climate Change Impact
Sediment Transport
Morphodynamics
River Morphology
topic Parana River
Climate Change Impact
Sediment Transport
Morphodynamics
River Morphology
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv This paper presents an analysis of the sediment dynamics that takes place at different scales within the Middle and the Lower Parana River in the La Plata Basin. The aim of this study is to provide a multi-disciplinary and multi-scale approach for the prediction of river future morphology in the context of climate change, the intended use of which is the prognosis of river morphodynamics long-term impact on manmade structures and activities over or near the river. The study is based on three levels of mathematical modelling, with the output of wider-scale models providing the input conditions for more specific ones. Climate models give the input ensemble, i.e., future precipitation and temperature over La Plata Basin. The semi-distributed macroscale VIC hydrological model simulates the flow discharge time series that are applied to an own-developed 1-D morphodynamic model. The 1-D model simulates future rate of sediment transport and corresponding bed level changes at watershed scale and provides the boundary conditions for a 2-D model. Therefore, streamflow divagations at channel scale are simulated by means of the MIKE21C code developed by the Danish Hydraulic Institute. The analysis indicates a rather low sensitivity of the Parana River bed profile, i.e., 1-D morphology, to the increase predicted in flow discharge, whereas the streamflow appreciably divagates. In particular, surpassing an upper bound in the most frequent discharge appears effective in driving the actual bifurcated morphology into a meandering-multithread configuration.
Fil: Guerrero, Massimo. Universidad de Bologna. Hydraulic Laboratory; Italia
Fil: Nones, Michael. Universidad de Bologna. Fluid Dynamics Unit. Research Center for Constructions; Italia
Fil: Saurral, Ramiro Ignacio. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinacion Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera; Argentina
Fil: Montroull, Natalia Blanca. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinacion Administrativa Ciudad Universitaria. Centro de Investigaciones del Mar y la Atmósfera; Argentina
Fil: Szupiany, Ricardo Nicolas. Universidad Nacional del Litoral. Facultad de Ingeniería y Ciencias Hídricas; Argentina
description This paper presents an analysis of the sediment dynamics that takes place at different scales within the Middle and the Lower Parana River in the La Plata Basin. The aim of this study is to provide a multi-disciplinary and multi-scale approach for the prediction of river future morphology in the context of climate change, the intended use of which is the prognosis of river morphodynamics long-term impact on manmade structures and activities over or near the river. The study is based on three levels of mathematical modelling, with the output of wider-scale models providing the input conditions for more specific ones. Climate models give the input ensemble, i.e., future precipitation and temperature over La Plata Basin. The semi-distributed macroscale VIC hydrological model simulates the flow discharge time series that are applied to an own-developed 1-D morphodynamic model. The 1-D model simulates future rate of sediment transport and corresponding bed level changes at watershed scale and provides the boundary conditions for a 2-D model. Therefore, streamflow divagations at channel scale are simulated by means of the MIKE21C code developed by the Danish Hydraulic Institute. The analysis indicates a rather low sensitivity of the Parana River bed profile, i.e., 1-D morphology, to the increase predicted in flow discharge, whereas the streamflow appreciably divagates. In particular, surpassing an upper bound in the most frequent discharge appears effective in driving the actual bifurcated morphology into a meandering-multithread configuration.
publishDate 2013
dc.date.none.fl_str_mv 2013-09
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/4468
Guerrero, Massimo; Nones, Michael; Saurral, Ramiro Ignacio; Montroull, Natalia Blanca; Szupiany, Ricardo Nicolas; Parana River morphodynamics in the context of climate change; Taylor & Francis; International Journal of River Basin Management; 11; 4; 9-2013; 423-437
1571-5124
url http://hdl.handle.net/11336/4468
identifier_str_mv Guerrero, Massimo; Nones, Michael; Saurral, Ramiro Ignacio; Montroull, Natalia Blanca; Szupiany, Ricardo Nicolas; Parana River morphodynamics in the context of climate change; Taylor & Francis; International Journal of River Basin Management; 11; 4; 9-2013; 423-437
1571-5124
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/http://www.tandfonline.com/doi/full/10.1080/15715124.2013.826234
info:eu-repo/semantics/altIdentifier/doi/DOI:10.1080/15715124.2013.826234
info:eu-repo/semantics/altIdentifier/issn/1571-5124
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
application/pdf
application/pdf
dc.publisher.none.fl_str_mv Taylor & Francis
publisher.none.fl_str_mv Taylor & Francis
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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