“…Across these data sets there are ample discrepancies in space and time, highlighting the need for comparative assessments (e.g., Koutsouris et al, 2016;Alijanian et al, 2017Alijanian et al, , 2019Balsamo et al, 2018;Sun et al, 2018;Massari et al, 2020;Brocca et al, 2019;Sharifi et al, 2019;Caroletti et al, 2019;Levizzani and Cattani, 2019;Roca et al, 2019;Fallah et al, 2020;Satgé et al, 2020;Contractor et al, 2020;Xu et al, 2020;Zhou et al, 2020). In particular, indirect evaluation of the data sets through application in hydrological modeling is a valuable alternative in this context as precipitation is translated into variables with more reliable observations, such as runoff, as long as runoff is measured in catchments with near-natural dynamics (Thiemig et al, 2013;Nerini et al, 2015;Beck et al, 2017aBeck et al, , b, 2019aFereidoon et al, 2019;Ehsan Bhuiyan et al, 2019;Mazzoleni et al, 2019;Arheimer et al, 2020;Dembélé et al, 2020). However, while this approach relies on the propagation of precipitation uncertainty into runoff, it is largely underexplored with respect to when and where this propagation pathway is active.…”