pointed out that the extreme precipitation in the global monsoon regions has shown an increasing trend in the past century, with a significant increasement in the contrast between wet and dry seasons 9 .
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Long-term variability of extreme precipitation with WRF model at a complex terrain River Basin.
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Specifically, R1mm of both observations and simulations show a decreasing trend, with − 1.29 mm·10years −1 and − 3.32 mm·10years −1 , respectively, indicating a strong correlation in the time series (CC of 0.93, KGE of 0.83, PBIAS of −9.70%).
The observed PRCPTOT has a positive trend of 31.83 mm·10years −1 , while the WRF results show a negative trend of −32.46 mm·10years −1 .