Abstract
The characteristics of the streaming are presented by considering the closure scheme based on one equation model in the turbulent boundary layer, where the Stokes' second order irrotational velocity profile is adopted at the upper boundary as the boundary condition along with the Batchelor's condition for the streaming. The calculated profile is compared with the existing analytical results based on zero equation models and the experimental data of van Doom (1981).
It is shown that the streaming velocity profiles differ from condition to condition of the relative depth, but the dependence on the roughness is weak.
