Maintaining water availability and electric energy production are the major concerns for the future in countries which are extremely dependent on their water resources like Brazil. The objective of this study was to assess the impacts of climate change on streamflow and therefore on hydropower potential of the Grande river basin headwater region, Southeast Brazil. For this purpose, the SWAT model was used to simulate the hydrological behaviour of the headwaters under the Representative Concentration Pathways 4.5 and 8.5 scenarios, obtained from the Regional Climate Models Eta‐HadGEM‐ES and Eta‐MIROC5 between the years 2007 and 2099. Through power duration curves we estimated the hypothetical average annual energy production at three hydropower plants installed in cascade in the region, being, from upstream to downstream, Camargos, Itutinga and Funil. These plants account for a potential of 277 MW. SWAT was able to simulate the streamflow of the Grande river basin headwaters and, therefore, to reproduce the observed monthly streamflow from the baseline period (1961–2005) reasonably well for all three hydropower plants. In general, the results indicated a significant streamflow reduction and therefore reductions in runoff during all the simulated periods and all radiative forcing analysed, when compared to the baseline period. Thus, these results led to reductions in hydropower potential and hence decreases of the annual energy production varying from 6.1 to 58.6% throughout the 21st Century.

Este trabalho objetivou estimar e mapear a erosividade média (EI30) mensal e anual, analisar a distribuição espacial da precipitação, durante o período chuvoso, e identificar zonas similares quanto a EI30 no Estado de Minas Gerais. Foram levantadas séries históricas de precipitação diária de 248 estações climatológicas para estimativa do coeficiente de chuva de Fournier (Rc). Baseado na relação EI30 x Rc, verificada em algumas localidades do Estado, o índice EI30 mensal foi estimado para as 248 estações. A geoestatística foi aplicada no mapeamento dos dados. O Estado de Minas Gerais pôde ser dividido em três zonas, com erosividade anual variando de 5.000 a 12.000 MJ mm ha-1 ano-1 : erosividade média-alta, nas regiões central, nordeste e parte da Zona da Mata; alta, no Triângulo Mineiro (extremo da região), e parte do nordeste e sul do Estado; e muito alta, na maior parte do Triângulo Mineiro, Alto Paranaíba, noroeste e leste. A erosividade não apresentou relação com a latitude e longitude e foi influenciada por efeitos orográficos e características climáticas de cada região.

Brazilian Cerrado biome is the largest and richest tropical savanna in the world. In order to understand the effects of climate changes on the hydrology of the Cerrado basins, this paper investigates the hydrological impacts of climate change throughout the 21st century under different emissions scenarios on the streamflow and on the droughts in the Sono, Manuel Alves da Natividade and Palma basins, located in the Brazilian Cerrado. For this purpose, the SWAT hydrological model driven by the downscaling of the HadGEM2‐ES and MIROC5 global climate models associated with RCP4.5 and RCP8.5 scenarios were used in three time slices (2011–2040, 2041–2070 and 2071–2099). The Standardized Precipitation Index (SPI) and the Standardized Streamflow Index (SSFI) were used to characterize droughts. In general, the results showed that the duration, intensity and frequency of the meteorological and hydrological droughts are expected to increase during the future periods. However, the hydrological droughts are projected to be larger than the meteorological droughts. Reductions in the streamflow are indicated in all future time slices and under both RCPs, especially, during dry periods, which may cause negative impacts in the ecological functions of the Cerrado biome, risk for reduction of the recharge of aquifers and risk for the electric energy production in northern Brazil.