“…These works use data provided by global atmospheric reanalysis (e.g., Cannon et al, 2015;González-Aparicio et al, 2017;Gruber et al, 2022), mesoscale numerical weather prediction (NWP) models (Murcia Leon et al, 2021;Koivisto et al, 2021), or both (Jourdier, 2020;Murcia et al, 2022). Because mesoscale NWP models cannot represent the effects of the most detailed microscale processes, extra information, such as the effect of the terrain in the wind speed distribution, can be added by combining (i.e., adjusting) mesoscale with microscale data (e.g., Staffell and Pfenninger, 2016;Ruiz et al, 2019;Murcia et al, 2022). Due to their relatively low temporal resolution (usually available from 30 min to 1 h resolution) and intrinsic numerical smoothing, data from mesoscale models cannot include minute-to second-scale variability, and even hourly variability may be too low compared to measurements (Koivisto et al, 2020).…”