Parana River morphodynamics in the context of climate change
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 con...
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2013
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| LEADER | 12734caa a22010577a 4500 | ||
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| 001 | PAPER-12964 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518204311.0 | ||
| 008 | 190411s2013 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-84896692274 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Guerrero, M. | |
| 245 | 1 | 0 | |a Parana River morphodynamics in the context of climate change |
| 260 | |c 2013 | ||
| 270 | 1 | 0 | |m Nones, M.; Research Center for Constructions - Fluid Dynamics Unit, University of Bologna, via del Lazzaretto 15/5, 40121, Bologna, Italy; email: michael.nones@unibo.it |
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a Amsler, M.L., Drago, E.C., Paira, A.R., Fluvial sediments: main channel and floodplain interrelationship (2007) The Middle Paranà River: Limnology of a subtropical Wetland, pp. 123-142. , In: Iriondo M.H., Paggi J.C., Parma M.J., editors Berlin, Heidelberg, Berlin, Heidelberg,: Springler-Verlag | ||
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| 504 | |a Fasolato, G., Validity of uniform flow hypothesis in one-dimensional morphodynamic models (2011) Journal of Hydraulic Engineering, ASCE, 37 (2), pp. 183-195 | ||
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| 504 | |a Guerrero, M., Lamberti, A., Bed-roughness investigation for a 2-D model calibration: the San Martìn case study at Lower Paranà (2013) International Journal of Sediment Research, special issue Sediment loads and processes in large rivers | ||
| 504 | |a Guerrero, M., Szupiany, R.N., Amsler, M., Comparison of acoustic backscattering techniques for suspended sediments investigations (2011) Flow Measurements and Instrumentation, 22 (5), pp. 392-401 | ||
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| 504 | |a Guerrero, M., Di Federico, V., Lamberti, A., Calibration of a 2-D morphodynamic model using water-sediment flux maps derived from an ADCP recording (2013) Journal of Hydroinformatics, 15 (3), pp. 813-828 | ||
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| 504 | |a Nones, M., (2011) Aspects of riverine hydro-morpho-biodynamics at watershed scale, , http://paduaresearch.cab.unipd.it/4468, [online]. Thesis (PhD). University of Padua, Italy. Available from: [Accessed 15 January 2013] | ||
| 504 | |a Nones, M., Guerrero, M., Gaeta, M.G., Analysis of the 1-D morphological evolution of the Paranà River (2012) Submitted to Journal of Hydraulic Engineering | ||
| 504 | |a Olesen, K.W., Bed topography in shallow river bends. Delft: Faculty of Civil Engineering (1987); Saurral, R., The hydrologic cycle of the La Plata Basin in the WCRP-CMIP3 multimodel dataset (2010) Journal of Hydrometeorology, 11 (5), pp. 1083-1102 | ||
| 504 | |a Saurral, R., Montroull, N., Camilloni, I., (2013) Development of statistically unbiased 21st century hydrology scenarios over La Plata Basin, , International Journal of River Basin Management, special issue Impact Assessment of Climate Change on La Plata Basin Water Resources | ||
| 504 | |a Su, F., Lettenmaier, D., Estimation of surface water budget of La Plata Basin (2009) Journal of Hydrometeorology, 10 (4), pp. 981-998 | ||
| 504 | |a Talmon, A.M., (1992) Bed topography of river bends with suspended sediment transport, , Thesis (PhD). Delft Univ. of Technology, The Netherlands | ||
| 504 | |a Williams, R.D., Monitoring braided river change using terrestrial laser scanning and optical bathymetric mapping (2011) Geomorphological mapping: Methods and applications, pp. 507-532. , In: Smith M., Paron P., Griffiths J., editors Amsterdam, Amsterdam,: Elsevier, [Accessed 15 January 2013] | ||
| 520 | 3 | |a 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 variable infiltration capacity hydrological model simulates the flow discharge time series that are applied to an own-developed 1D morphodynamic model. The 1D model simulates future rate of sediment transport and corresponding bed-level changes at watershed scale and provides the boundary conditions for a 2D 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. 1D 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. © 2013 © 2013 International Association for Hydro-Environment Engineering and Research. |l eng | |
| 536 | |a Detalles de la financiación: Universidad de Buenos Aires | ||
| 536 | |a Detalles de la financiación: Centre National de la Recherche Scientifique | ||
| 536 | |a Detalles de la financiación: 212492 | ||
| 536 | |a Detalles de la financiación: Seventh Framework Programme | ||
| 536 | |a Detalles de la financiación: RAMIRO SAURRAL, Centro de Investigaciones del Mar y la Atmósfera (CIMA/CONICET-UBA), UMI IFAECI/ CNRS and Departamento de Ciencias de la Atmósfera y los Océanos (FCEN-UBA), Buenos Aires, Argentina; Universidad de Buenos Aires, Buenos Aires, Argentina | ||
| 536 | |a Detalles de la financiación: NATALIA MONTROULL, Centro de Investigaciones del Mar y la Atmósfera (CIMA/CONICET-UBA), UMI IFAECI/CNRS and Departamento de Ciencias de la Atmósfera y los Océanos (FCEN-UBA), Buenos Aires, Argentina | ||
| 536 | |a Detalles de la financiación: This research has received funding from the European Community’s Seventh Framework Programme (FP7/2007–2013) under Grant Agreement No. 212492 (CLARIS-LPB. A Europe-South America Network for Climate Change Assessment and Impact Studies in La Plata Basin). | ||
| 593 | |a Hydraulic Laboratory, University of Bologna, Bologna, Italy | ||
| 593 | |a Research Center for Constructions - Fluid Dynamics Unit, University of Bologna, via del Lazzaretto 15/5, 40121, Bologna, Italy | ||
| 593 | |a Centro de Investigaciones del Mar y la Atmósfera (CIMA/CONICET-UBA), UMI IFAECI/CNRS and Departamento de Ciencias de la Atmósfera y los Océanos (FCEN-UBA), Buenos Aires, Argentina | ||
| 593 | |a Universidad de Buenos Aires, Buenos Aires, Argentina | ||
| 593 | |a Universidad National del Litoral, Santa Fe, Argentina | ||
| 690 | 1 | 0 | |a CLIMATE CHANGE IMPACT |
| 690 | 1 | 0 | |a MORPHODYNAMICS |
| 690 | 1 | 0 | |a PARANA RIVER |
| 690 | 1 | 0 | |a RIVER MORPHOLOGY |
| 690 | 1 | 0 | |a SEDIMENT TRANSPORT |
| 690 | 1 | 0 | |a CLIMATE CHANGE |
| 690 | 1 | 0 | |a CLIMATE MODELING |
| 690 | 1 | 0 | |a FLUVIAL GEOMORPHOLOGY |
| 690 | 1 | 0 | |a HYDROLOGICAL MODELING |
| 690 | 1 | 0 | |a MEANDER |
| 690 | 1 | 0 | |a MORPHODYNAMICS |
| 690 | 1 | 0 | |a NUMERICAL MODEL |
| 690 | 1 | 0 | |a SEDIMENT TRANSPORT |
| 690 | 1 | 0 | |a STREAMFLOW |
| 690 | 1 | 0 | |a LA PLATA BASIN |
| 690 | 1 | 0 | |a PARANA RIVER |
| 700 | 1 | |a Nones, M. | |
| 700 | 1 | |a Saurral, R. | |
| 700 | 1 | |a Montroull, N. | |
| 700 | 1 | |a Szupiany, R.N. | |
| 773 | 0 | |d 2013 |g v. 11 |h pp. 423-437 |k n. 4 |p Int. J. River Basin Manage. |x 15715124 |t International Journal of River Basin Management | |
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| 856 | 4 | 0 | |u https://doi.org/10.1080/15715124.2013.826234 |y DOI |
| 856 | 4 | 0 | |u https://hdl.handle.net/20.500.12110/paper_15715124_v11_n4_p423_Guerrero |y Handle |
| 856 | 4 | 0 | |u https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_15715124_v11_n4_p423_Guerrero |y Registro en la Biblioteca Digital |
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