Abstract:Climate change has resulted in an increase in drought in most global land areas, mainly due to a decrease in regional precipitation (P) or an increase in potential evapotranspiration (PET) induced by climate warming. However, knowledge on the contributions of P and PET to long-term changes in global drought duration and intensity is still limited. In this study, we quantitatively analysed the respective contributions of P and PET to long-term drought duration and intensity on a global scale, using standardized… Show more
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