All models have a substantial dry bias over Greenland when compared to CRU (TRMM/TMPA (3B43) does not include Greenland). Large differences in bias ratios can be observed in the Atacama, where CHELSA, and GPCC are drier than CRU, and WorldClim, CHPclim, TRMM/TMPA (3B43), and ERA-Interim are wetter. Also on the Himalaya plateau large differences are visible, with CHELSA, GPCC, and TRMM (3B43) being drier, and WorldClim and ERA-Interim being wetter.