2019
DOI: 10.1080/02626667.2019.1612521
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Performance evaluation of AR5-CMIP5 models for the representation of seasonal and multi-annual variability of precipitation in Brazilian hydropower sector basins under RCP8.5 scenario

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Cited by 14 publications
(9 citation statements)
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References 58 publications
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“…For, in most cases, the declivity module is always greater for the RCP 8.5 scenario in comparison to the RCP 4.5 one. These results are similar to the ones obtained by Silveira et al (2014Silveira et al ( , 2016Silveira et al ( , 2019 with CMIP5 data. In the North and Southeast/Midwest sectors, most models and stations indicated a negative trend in the annual naturalized streamflows and NEA in both scenarios.…”
Section: Resultssupporting
confidence: 90%
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“…For, in most cases, the declivity module is always greater for the RCP 8.5 scenario in comparison to the RCP 4.5 one. These results are similar to the ones obtained by Silveira et al (2014Silveira et al ( , 2016Silveira et al ( , 2019 with CMIP5 data. In the North and Southeast/Midwest sectors, most models and stations indicated a negative trend in the annual naturalized streamflows and NEA in both scenarios.…”
Section: Resultssupporting
confidence: 90%
“…In the South sector, however, most models indicated an annual naturalized streamflows and NEA increase (see Figures 5, 6 and 7), with some models and model medians, respectively, presenting magnitudes greater than 5%. The possible increase in naturalized streamflows projections for the South sector had already been demonstrated in previous works using data from the CMIP3 and CMIP5 models, the works of Silveira et al (2014Silveira et al ( , 2016Silveira et al ( , 2019 and Ribeiro Neto et al (2016) are examples. As well as in the period 2010-2039, in the period 2040-2069, the annual NEA and naturalized streamflows average percentage anomalies also indicated a reduction for most NIS models and stations for all sectors and scenarios.…”
Section: Resultsmentioning
confidence: 61%
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“…A disponibilidade de água no Brasil depende em grande parte do clima. O ciclo anual das chuvas e de vazões no país varia entre bacias, e de fato a variabilidade interanual do clima, associada aos fenômenos de El Niño, La Niña, ou à variabilidade na temperatura da superfície do mar (TSM) do Atlântico Tropical e Sul podem gerar anomalias climáticas, que produzem grandes secas, como em 1877, 1983 e 1998 no Nordeste, 2004-2006no Sul do Brasil, 2001no Centro-Oeste e Sudeste, e em 1926, 1983, 1998e 2005na Amazônia (Marengo e Nobre, 2004Marengo et al, 2012;Silva, 2013), assim como projeções de secas futuras (da Costa et al, 2018;Marcos Junior et al, 2018;Silveira et al, 2019;da Silva, 2020).…”
Section: Introductionunclassified