“…And the streaming flow produced in the boundary layer attached to a vibrating free boundary is of interest in water wave theory (Phillips, 1977;Liu and Davis, 1977;Craik, 1982Craik, , 1985Iskandarani and Liu, 1991 and references therein) and has been shown to play a role in the instability of the ocean to Langmuir circulations (Leibovich, 1983). These flows have also been studied in connection with capillary waves (Mollot et al, 1993) and in conjunction with thermal eflects (Nicolás and Vega, 1996;Nicolás et al, 1997Nicolás et al, , 1998Lyubimov et al, 1997), intending to control thermocapillary convection (Anilkumar et al, 1993), which is undesirable in materials processing in microgravity (Kuhlmann, 1999). Most of these works dealt with the two-dimensional (2D) case and used the 2D formulae derived by Schlichting (1968) and Longuet-Higgins (1953) for the boundary conditions at the edge of the boundary layers when solving the mean flow equations in the bulk.…”