“…Sukhodolov et al, 1998), bedform (Holmes Jr & Garcia, 2008), submerged vegetation (A. N. Sukhodolov & Sukhodolova, 2010) and additional forcing such as tidal currents (Heathershaw, 1979;Sanford & Lien, 1999). In addition, river morphology and man-made hydraulic structures can affect turbulence structures by introducing secondary flows and reshaping vertical turbulent profiles such as at river bends (Constantinescu et al, 2013), near-bank (Kumar Das et al, 2020, wing dikes (Jamieson et al, 2011), river confluences (A. N. Sukhodolov et al, 2017), and chute cutoffs (Qiao et al, 2022;Zinger et al, 2013). Classic turbulent mixing profiles (e.g., parabolic profile of eddy viscosity) are effective and useful in three-dimensional particle tracking models for egg drift (Garcia et al, 2013;Garcia et al, 2015;Heer et al, 2021).…”