“…These have been shown to interact in a non-linear way in the near-bottom region Simons, 1982, 1983;Soulsby et al, 1993), leading to a wave-current boundary layer with altered logarithmic velocity profiles and Reynolds shear stresses. The mechanics of WCI have been investigated extensively by analytical approaches (Lundgren, 1972;Grant and Madsen, 1979;Myrhaug, 1982;Fredsøe, 1984;Christoffersen and Jonsson, 1985;Myrhaug and Slaattelid, 1989;You et al, 1991You et al, , 1992You, 1994aYou, , 1994bMalarkey and Davies, 1998;Umeyama, 2005;2009;Yuan and Madsen, 2015), laboratory experiments (Bakker and van Doorn, 1978;Van Doorn, 1981; Simons, 1982, 1983;Arnskov et al, 1993;Klopman, 1994;Simons et al, 1992Simons et al, , 1994Simons et al, , 2000Lodahl et al, 1998;Fredsøe et al, 1999;Simons and MacIver, 2001;Umeyama, 2005Umeyama, , 2009Umeyama, , 2011Carstensen et al, 2010;Madsen, 2014, 2015) and numerical methods (Davies et al, 1988;Holmedal et al, 2003;Teles et al, 2012Teles et al, , 2013Zhang et al, 2014;Zhang et al, 2017). Coherent vortical structures are the dominant feature in unidirectional turbulent boundary layers, and play crucial roles in carrying turbulent energy and contributing to Re...…”