Author(s): P. M. Lloyd; P. K. Stansby; D. Chen; J. Yin; Y. Chen; R. A. Falconer
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Keywords: No Keywords
Abstract: Oscillatory flows around a headland of conical form have been investigated experimentally in the UKCRF. The structure of the eddy shedding is shown to be dependent on the Keulegan-Carpenter number and is shown to be rather complex at higher values, e.g. 15, with prominent vortex pairing. Comparisons are made with a numerical model of the depth-averaged shallow-water equations.
Year: 1997