Abstract
The double boundary-layer theory ofStuart (1963, 1966) andRiley (1965, 1967) is employed to investigate the mass transport velocity due to two-dimensional standing waves in a homogeneous fluid. The double boundary-layer structure occurs only at the bottom, and the existence of jet-like motions is predicted, due to the nature of the mean flows in the bottom boundary layers. A vector equation governing mean motions in the secondary layer is derived for threedimensional wave motions.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
