“…Key features of flow in complex terrain include thermo-topographic flows arising from differential heating (Rucker et al, 2008;Rotach and Zardi, 2007) and lee-side vortices that develop parallel to mountain ridges (Grubišić et al, 2008). Regions with complex topography and land cover heterogeneity also tend to experience more frequent and stronger wind gusts (herein defined as coherent shortterm wind speed maxima) (Letson et al, 2018;Earl et al, 2017;Sheridan, 2011;Hasager et al, 2003) due in part to F. Letson et al: Characterizing wind gusts Wind gusts represent an important source of structural engineering loads for tall buildings, towers, bridges, and wind turbines (Solari, 1987;IEC, 2005;Cheynet et al, 2016), and are known to be of larger magnitude in complex terrain due in part to the factors listed above (Tieleman, 1992;Verheij et al, 1992). A number of numerical wind flow models have been developed for application at high spatial resolution over complex terrain, but model evaluation has been severely constrained by the lack of suitable observational data (Butler et al, 2015;Bechmann et al, 2011;Berg et al, 2011;Suomi and Vihma, 2018).…”