HIGHLIGHTS
SUMMARY
Regional and global-scale effects of climate change on temperature and precipitation can trigger significant changes in river runoff and groundwater level, which are later reflected in the evolution of water resources and social development at a regional level (de Moura et_al, 2020; Xiao et_al, 2021). In the last decades, the scientific research on the impact of climate change on the various hydroclimatic parameters has been multiplied, most of the analysis focusing on the identification of trends in the extreme seasonal and annual values of precipitation, temperature, or rivers` flow (Taye et_al, 2015; Croitoru . . .
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