“…Parameters such as the fluid velocity, direction, pressure, and shear stress in secondary airflow are altered by the topography of obstacles (Walker & Nickling, 2002;Wang & Huang, 2017). Secondary airflow differs in energy and direction due to variations in the geometry and alignment of obstacles and the wind regime (e.g., wind velocity, wind direction, and angle of incidence; Escauriaza & Sotiropoulos, 2011;McKenna-Neuman and Bédard, 2015;Meire et al, 2014;McKenna-Neuman et al, 2015;Vinuesa et al, 2015;Bruno et al, 2018;Kindere & Ganapathisubramani, 2018;Sun & Huang, 2018;He et al, 2018). Although the relationships between the geometric parameters of the obstacles, the wind velocity, and the length of flow reattachment and recovery have been reported previously (Clemmensen, 1986;Gillies et al, 2014;Gunatilaka & Mwango, 1987;Hesp, 1981 ;Hesp & Smyth, 2017), questions remain about the sensitivity of these secondary airflow structures to changes in wind velocity, the geometry of the obstacles, and the subsequent shadow dune formation.…”