“…Although there is a lack of general consensus on global drought assessments [8][9][10][11][12], drought indices designed on the basis of the concept of atmospheric supply and demand have shaped our understanding of drought [3,7,[13][14][15]. Thus, within this context, the selfcalibrating Palmer Drought Severity Index (scPDSI), a typical example of such a drought index [12], has been widely used for drought climatology studies at global scales [8,9] and for regional specific studies [15][16][17][18][19], among others [6]. The scPDSI, by design, is a physical-based drought index that incorporates antecedent P, moisture supply, and demand (i.e., potential evaporation (PET)) to account for surface warming effects on wet and dry spells [12].…”