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Water balance components and climate extremes over Brazil under 1.5 °C and 2.0 °C of global warming scenarios
This work aimed to evaluate changes in water balance components (precipitation, evapotranspiration, and water availability) and precipitation extremes projected under global warming levels (GWLs) of 1.5 °C and 2 °C, in Brazil. An ensemble of eight twenty-first-century projections with the Eta Region...
Autores principales: | , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Springer Berlin Heidelberg
2023
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9932420/ https://www.ncbi.nlm.nih.gov/pubmed/36820201 http://dx.doi.org/10.1007/s10113-023-02042-1 |
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author | da Silva Tavares, Priscila Acosta, Ricardo Nobre, Paulo Resende, Nicole Costa Chou, Sin Chan de Arruda Lyra, André |
author_facet | da Silva Tavares, Priscila Acosta, Ricardo Nobre, Paulo Resende, Nicole Costa Chou, Sin Chan de Arruda Lyra, André |
author_sort | da Silva Tavares, Priscila |
collection | PubMed |
description | This work aimed to evaluate changes in water balance components (precipitation, evapotranspiration, and water availability) and precipitation extremes projected under global warming levels (GWLs) of 1.5 °C and 2 °C, in Brazil. An ensemble of eight twenty-first-century projections with the Eta Regional Climate Model and their driving Global Climate Models (CanESM2, HadGEM2-ES, MIROC5, and BESM) were used. Projections of two Representative Concentration Pathway scenarios, RCP4.5 and RCP8.5, considered intermediate and high concentration, respectively, were used. The results indicate that the RCP8.5 scenario under 2 °C GWL is likely to have a higher impact on the water balance components, amplifying trends in drier conditions and increasing the number of consecutive dry days in some regions of Brazil, particularly in the North and Northeast regions. On the other hand, the projections indicate the opposite sign for the South region, with trends toward wetter conditions and significant increases in extreme rainfall. The 0.5 °C difference between the GWLs contributes to intensifying reductions (increases) from 4 to 7% in water availability, mainly in the North-Northeast (South) regions. The projected changes could have serious consequences, such as increases in the number of drought events in hydrographic regions of the Northeast region of Brazil and increases in flood events in the South of the country. The results here presented can contribute to the formulation of adaptive planning strategies aimed at ensuring Brazil’s water security towards climate change. SUPPLEMENTARY INFORMATION: The online version contains supplementary material available at 10.1007/s10113-023-02042-1. |
format | Online Article Text |
id | pubmed-9932420 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2023 |
publisher | Springer Berlin Heidelberg |
record_format | MEDLINE/PubMed |
spelling | pubmed-99324202023-02-16 Water balance components and climate extremes over Brazil under 1.5 °C and 2.0 °C of global warming scenarios da Silva Tavares, Priscila Acosta, Ricardo Nobre, Paulo Resende, Nicole Costa Chou, Sin Chan de Arruda Lyra, André Reg Environ Change Original Article This work aimed to evaluate changes in water balance components (precipitation, evapotranspiration, and water availability) and precipitation extremes projected under global warming levels (GWLs) of 1.5 °C and 2 °C, in Brazil. An ensemble of eight twenty-first-century projections with the Eta Regional Climate Model and their driving Global Climate Models (CanESM2, HadGEM2-ES, MIROC5, and BESM) were used. Projections of two Representative Concentration Pathway scenarios, RCP4.5 and RCP8.5, considered intermediate and high concentration, respectively, were used. The results indicate that the RCP8.5 scenario under 2 °C GWL is likely to have a higher impact on the water balance components, amplifying trends in drier conditions and increasing the number of consecutive dry days in some regions of Brazil, particularly in the North and Northeast regions. On the other hand, the projections indicate the opposite sign for the South region, with trends toward wetter conditions and significant increases in extreme rainfall. The 0.5 °C difference between the GWLs contributes to intensifying reductions (increases) from 4 to 7% in water availability, mainly in the North-Northeast (South) regions. The projected changes could have serious consequences, such as increases in the number of drought events in hydrographic regions of the Northeast region of Brazil and increases in flood events in the South of the country. The results here presented can contribute to the formulation of adaptive planning strategies aimed at ensuring Brazil’s water security towards climate change. SUPPLEMENTARY INFORMATION: The online version contains supplementary material available at 10.1007/s10113-023-02042-1. Springer Berlin Heidelberg 2023-02-16 2023 /pmc/articles/PMC9932420/ /pubmed/36820201 http://dx.doi.org/10.1007/s10113-023-02042-1 Text en © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023, Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. This article is made available via the PMC Open Access Subset for unrestricted research re-use and secondary analysis in any form or by any means with acknowledgement of the original source. These permissions are granted for the duration of the World Health Organization (WHO) declaration of COVID-19 as a global pandemic. |
spellingShingle | Original Article da Silva Tavares, Priscila Acosta, Ricardo Nobre, Paulo Resende, Nicole Costa Chou, Sin Chan de Arruda Lyra, André Water balance components and climate extremes over Brazil under 1.5 °C and 2.0 °C of global warming scenarios |
title | Water balance components and climate extremes over Brazil under 1.5 °C and 2.0 °C of global warming scenarios |
title_full | Water balance components and climate extremes over Brazil under 1.5 °C and 2.0 °C of global warming scenarios |
title_fullStr | Water balance components and climate extremes over Brazil under 1.5 °C and 2.0 °C of global warming scenarios |
title_full_unstemmed | Water balance components and climate extremes over Brazil under 1.5 °C and 2.0 °C of global warming scenarios |
title_short | Water balance components and climate extremes over Brazil under 1.5 °C and 2.0 °C of global warming scenarios |
title_sort | water balance components and climate extremes over brazil under 1.5 °c and 2.0 °c of global warming scenarios |
topic | Original Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9932420/ https://www.ncbi.nlm.nih.gov/pubmed/36820201 http://dx.doi.org/10.1007/s10113-023-02042-1 |
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