the frequency of unprecedented extreme occasions (Diffenbaugh et al., 2017 ; Huang et al., 2018 ; Pendergrass et al., 2017 ; Swain et al., 2018 ). Rising temperatures and rising atmospheric evaporation will additional amplify the impact of precipitation variability, doubtlessly rising the period and intensity of drought (Diffenbaugh et al., 2015 ; Overpeck, 2013 ; Trenberth et al., 2013 ). Indeed, the increasing risk of future megadrought could also be pushed primarily by persistent warmth and temperature‐driven aridity, as opposed to decreases in precipitation (Prepare dinner et al., 2015 ). Thus, shifts within the temporal and spatial
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