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Climate change impact assessment on water resources under RCP scenarios: A case study in Mundaú River Basin, Northeastern Brazil
Author(s) -
Andrade Carolyne W. L.,
Montenegro Suzana M. G. L.,
Montenegro Abelardo A. A.,
Lima José R. de S.,
Srinivasan Raghavan,
Jones Charles A.
Publication year - 2021
Publication title -
international journal of climatology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.58
H-Index - 166
eISSN - 1097-0088
pISSN - 0899-8418
DOI - 10.1002/joc.6751
Subject(s) - evapotranspiration , environmental science , climate change , soil and water assessment tool , swat model , precipitation , surface runoff , representative concentration pathways , water resources , streamflow , hydrology (agriculture) , climatology , drainage basin , climate model , structural basin , geography , meteorology , ecology , geology , paleontology , cartography , geotechnical engineering , biology
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 Mundaú 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°C and 0.65°C under the RCP 4.5 scenario, and up to 4.3°C and 2.2°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 (ET 0 ) 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 ·s −1 ), compared to the observed period (45.5 m 3 ·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.