Wave-driven circulation patterns in the lee of groynes |
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| Authors: | Charitha Pattiaratchi Dale Olsson Yasha Hetzel Ryan Lowe |
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| Affiliation: | 1. School of Geography, Environment and Earth Sciences, Victoria University, PO Box 600, Wellington 6140, New Zealand;2. Institut des Sciences de la Terre (ISTO), Centre National de la Recherche Scientifique (CNRS), l''Université d''Orléans, 1a rue de la Férollerie, Orléans Cedex 2, 45071, France;3. Institute of Geosciences, University of Mainz, Mainz, Germany;4. Lancaster Environment Centre, Lancaster University, UK;1. University of Liverpool, Department of Geography and Planning, 74 Bedford St S., Liverpool, UK;2. Liverpool John Moores University, Department of Civil Engineering, Peter Jost Enterprise Centre, Byrom Street, Liverpool L3 3AF, UK;3. U.S. Geological Survey, Woods Hole Coastal and Marine Science Center, MA 02543, USA;4. Cambridge Coastal Research Unit (CCRU), Department of Geography, University of Cambridge, Downing Place, Cambridge CB2 3EN, United Kingdom;5. Ecosystem Management Research Group, University of Antwerp, Universiteitsplein 1, 2610 Wilrijk, Belgium |
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| Abstract: | Surf zone drifters and a current meter were used to study the nearshore circulation patterns in the lee of groynes at Cottesloe Beach and City Beach in Western Australia. The circulation patterns revealed that a persistent re-circulation cell was present in the lee of the groyne which was driven by changes in wave set-up resulting from lower wave heights in the lee of the groyne. The re-circulation consisted of a longshore current directed towards the groyne which was deflected offshore due to groyne resulting in a rip current along the groyne face. The offshore-flowing rip current and the incoming waves converged at the offshore extent of this circulation cell, with the deflection of the rip current parallel to the shoreline and then completing the recirculation through an onshore component. The Eulerian measurements revealed that 55% of the currents on the lee side of the groyne were directed offshore and that these currents had a maximum speed of 2 m s?1. Spectral analysis of the wave heights and the currents revealed several corresponding peaks in the measured spectral densities with timescales between 12 s and 50 min. Numerical simulations of an idealised beach with a shore-normal groyne were conducted using a circulation model driven by waves, and confirmed the formation of a persistent eddy in the lee of the groyne. Sensitivity studies indicated that the incident wave angle, wave period, and especially the wave height controlled the circulation. The eddy vorticity, a measure of an eddy's strength, increased roughly proportional to an increase in the incident wave energy flux. |
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