4.6 Article

Climate change impact assessment on water resources underRCPscenarios: A case study in Mundau River Basin, Northeastern Brazil

期刊

INTERNATIONAL JOURNAL OF CLIMATOLOGY
卷 41, 期 -, 页码 E1045-E1061

出版社

WILEY
DOI: 10.1002/joc.6751

关键词

bias correction; CMIP5; Eta-HadGEM2; Eta-MIROC5; hydrological simulation; SWAT model

资金

  1. Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [446254/2015-0, 307641/2013-9, 441305/2017-2]
  2. Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior [23038007733/2013-76]
  3. Financiadora de Estudos e Projetos [REHIDRO 1830]
  4. Fundacao de Amparo a Ciencia e Tecnologia do Estado de Pernambuco [IBPG 0231-5.03/14, BCT 0176-5.03/14, APQ 0300-5.03/17, APQ 0913-5.03/15]

向作者/读者索取更多资源

Climate models predict significant decreases in annual precipitation, increases in maximum and minimum temperatures, decreases in surface runoff, decreases in evapotranspiration, increases in potential evapotranspiration, and decreases in annual streamflow for the Mundau River Basin in Brazil under future climate change scenarios.
Global climate predictions and possible environmental impacts have an increasing source of concern in recent years. Analyses of the impacts of climate change scenarios on regional hydrology are required to design effective adaptation strategies for specific river basins. This study focuses on assessment of future climate change impacts on water resources of the Mundau River Basin (MRB), in Brazil, using the Soil Water Assessment Tool (SWAT) and Regional Climate Models (RCMs) Eta-MIROC5 and Eta-HadGEM2, for three time periods under two Representative Concentration Pathways (RCPs). In general, climate models predict that the MRB will experience significant annual precipitation decreases, between 0.4% (1,087.45 mm) and 25.3% (815.59 mm), in both scenarios (RCP 4.5 and RCP 8.5) respectively, when compared to the observed period (2003-2016). Maximum and minimum temperature increases up to 2.3 degrees C and 0.65 degrees C under the RCP 4.5 scenario, and up to 4.3 degrees C and 2.2 degrees C under the RCP 8.5 scenario. SWAT simulations predict substantial surface runoff decreases with a minimum average annual value of 21.3 mm for the RCP 8.5 in medium-term. Additionally, actual evapotranspiration (ET) is predicted to decrease from 780.77 to a minimum of 648.1 mm, although increases in potential evapotranspiration (ET0) are expected. In general, annual streamflow also is expected to decrease, more severely under RCP 8.5 conditions, reaching a drop of approximately 66.7% (15.2 m(3)center dot s(-1)), compared to the observed period (45.5 m(3)center dot s(-1)). Seasonal streamflow is predicted to decrease for both models, in both rainy and dry seasons, except for medium-term of the Eta-HadGEM2. Although there are still some uncertainties associated with climate models, the findings from this study can assist water resource managers in management decisions for appropriate water use, development of public policies that favour sustainability, and adoption of mitigation and prevention practices to ensure water security in the basin.

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