Author(s): Ivar G. Jonsson Ph.D.; Niels A. Carlsen M.Sc.

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Abstract: The oscillatory flow near the sea bed under a wave motion is always rough turbulent in a coastal zone. This type of an oscillatory boundary layer (or “wave boundary layer”) was therefore chosen as a subject for detailed velocity measurements, from which characteristics such as shear stresses, eddy viscosities, energy loss, and boundary layer thickness were determined.

DOI: https://doi.org/10.1080/00221687609499687

Year: 1976