“…Conversely, natural topographic variability could provide the opportunity to reduce the streambed area subjected to high τ* with increasing flows, which in turn ensures a more natural rate of bed entrainment. Strom et al () reported that channel form heterogeneity directs flow such that varying topographic surfaces turn on and off in their control of hydraulics to allow diverse patterns of hydraulic conditions as flow increases (Brown & Pasternack, ; Brown, Pasternack, & Lin, ). This is also consistent with studies recognizing that dynamic channels provide a greater opportunity for more natural rates of bed particle transport, erosion, and deposition (Anim, Vietz, et al, ; Clarke, Bruce‐Burgess, & Wharton, ; Vaughan et al, ; Vietz et al, ).…”