An assessment of South American sediment fluxes under climate changes.

Autor: de Oliveira Fagundes H; Hydraulic Research Institute, Federal Univerisity of Rio Grande do Sul (UFRGS), Av. Bento Gonçalves, 9500 Porto Alegre, Rio Grande do Sul, Brazil. Electronic address: h.o.fagundes@hotmail.com., de Paiva RCD; Hydraulic Research Institute, Federal Univerisity of Rio Grande do Sul (UFRGS), Av. Bento Gonçalves, 9500 Porto Alegre, Rio Grande do Sul, Brazil., Brêda JPLF; Institute of Geosciences, University of Brasília (UnB), Campus Universitário Darcy Ribeiro, Brasília, Brazil., Fassoni-Andrade AC; Hydraulic Research Institute, Federal Univerisity of Rio Grande do Sul (UFRGS), Av. Bento Gonçalves, 9500 Porto Alegre, Rio Grande do Sul, Brazil; Institute of Geosciences, University of Brasília (UnB), Campus Universitário Darcy Ribeiro, Brasília, Brazil., Borrelli P; Department of Environmental Sciences, Environmental Geosciences, University of Basel, Basel, Switzerland; Department of Science, Roma Tre University, Rome, Italy., Fan FM; Hydraulic Research Institute, Federal Univerisity of Rio Grande do Sul (UFRGS), Av. Bento Gonçalves, 9500 Porto Alegre, Rio Grande do Sul, Brazil.
Jazyk: angličtina
Zdroj: The Science of the total environment [Sci Total Environ] 2023 Jun 25; Vol. 879, pp. 163056. Date of Electronic Publication: 2023 Mar 27.
DOI: 10.1016/j.scitotenv.2023.163056
Abstrakt: Climate change can affect all levels of society and the planet. Recent studies have shown its effects on sediment fluxes in several locations worldwide, which can impact ecosystems and infrastructure such as reservoirs. In this study, we focused on simulating sediment fluxes using projections of future climate change for South America (SA), a continent with a high sediment transport rate to the oceans. Here, we used four climate change data yielded by the Eta Regional Climate Model: Eta-BESM, Eta-CanESM2, Eta-HadGEM2-ES, and Eta-MIROC5. In addition, it was evaluated the RCP4.5 greenhouse gas emissions scenario from CMIP5, which represents a moderate scenario. Climate change data between 1961 and 1995 (past) and 2021 and 2055 (future) were used to simulate and compare changes that may occur in water and sediment fluxes using the hydrological-hydrodynamic and sediment model MGB-SED AS. The Eta climate projections provided input data to MGB-SED AS model, such as precipitation, air surface temperature, incident solar radiation, relative humidity, wind speed, and atmospheric pressure. Our results showed sediment fluxes are expected to reduce (increase) in north-central (south-central) SA. While a sediment transport (QST) increase >30 % might occur, a 28 % decrease is expected to occur in the water discharge for the main SA basins. The most significant QST reductions were estimated for the Doce (-54 %), Tocantins (-49 %), and Xingu (-34 %) rivers, while the most significant increases were estimated for the Upper Paraná (409 %), Juruá (46 %), and Uruguay (40 %) rivers. We also observed that different climate change signals over large basins can impact the river water composition, which could lead to a new composition of the Amazon basin waters in the future, accompanied by a significant increase in sediment concentration.
Competing Interests: Declaration of competing interest There is no competing interest.
(Copyright © 2023 Elsevier B.V. All rights reserved.)
Databáze: MEDLINE
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