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EurOCEAN 2000 - Vlaams Instituut voor de Zee

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available for plane and barred beaches. A theoretical study has been ma<strong>de</strong> on the generation of<br />

long waves from wave groups and the non-linear effect of long waves on short waves.<br />

The effects of wave reflection on surf zone dynamics have been studied by experimental and<br />

theoretical investigations.<br />

Boussinesq wave mo<strong>de</strong>ls for surf zone conditions have been verified against published data,<br />

including wave generated currents. Efficient 2DH mo<strong>de</strong>ls <strong>de</strong>scribing the vorticity generated by<br />

bores have been <strong>de</strong>veloped.<br />

Sediment transport in surf beat and long waves has been studied by numerical mo<strong>de</strong>ls verified<br />

against published data, and by analysis of hydrodynamic data from flume experiments to<br />

<strong>de</strong>termine zones of convergence and divergence. The theoretical study inclu<strong>de</strong>s the effect of<br />

bound long waves outsi<strong>de</strong> the breaker zone, surf zone wave mo<strong>de</strong>ls that resolve the low<br />

frequency motion but averages out the short waves, and by phase resolving wave mo<strong>de</strong>ls.<br />

The propagation of edge waves has been mo<strong>de</strong>lled for a plane beach with a shelf and a seawall<br />

to explain the formation of rhythmic morphology at a location in Spain. Work has continued<br />

with mo<strong>de</strong>lling of edge waves along a permeable barrier and resonance of a harbour un<strong>de</strong>r<br />

edge wave forcing.<br />

Project 2: Vertical structure of motion and associated sediment transport,<br />

and morphological mo<strong>de</strong>lling of coastal profiles<br />

The goal of the project is to study 3-D structures of wave-generated motions in the surf zone<br />

with focus on the large-scale vortices generated by plunging breakers, the turbulence<br />

generated by breaking and broken waves and the velocity distribution in wave-driven currents,<br />

and also to investigate morphological mo<strong>de</strong>lling of coastal profiles. Project 2 consists of two<br />

topics: (1) Vertical structure of wave- and breaker-induced motion and the associated sediment<br />

transport (Topics 1.2a - d); and (2) morphological mo<strong>de</strong>lling of the surf zone without structures<br />

(Topic 2.1a).<br />

Topic 1.2a. Description of a plunging breaker. The work has been concentrated on two<br />

aspects: (1) DHI/ISVA has been <strong>de</strong>veloping a mo<strong>de</strong>l for plunging breakers and to study the<br />

turbulent flow structures initiated by plunging breakers. (2) UEDIN in cooperation with ISVA<br />

has been doing PIV experiments of plunging breakers. The Volume of Fluid (VOF) method has<br />

been implemented in the general non-orthogonal Navier-Stokes solver in the DHI/ISVA work.<br />

Mo<strong>de</strong>l results have been compared to PIV measurements performed by UEDIN un<strong>de</strong>r waves<br />

breaking on a 1:13.5 slope. The k- mo<strong>de</strong>l has been used to mo<strong>de</strong>l the turbulence, and applied<br />

to simulate periodic breaking waves. All PIV experiments have been completed at two<br />

laboratories, at UEDIN and at ISVA. Different dynamics of selected breaker types have been<br />

found. The comparison of the mo<strong>de</strong>l results to measurements will be completed by the end of<br />

the project period.<br />

Topic 1.2b. Wave- boundary-layer investigation un<strong>de</strong>r breaking waves. An experimental<br />

study (ISVA) is being un<strong>de</strong>rtaken to study the interaction between turbulence generated by<br />

wave breaking, and the turbulence generated in an oscillatory boundary layer. The experiments<br />

are carried out in an oscillating water tunnel, and the wave-breaking generated turbulence is<br />

simulated by placing a grid in the upper part of the tunnel. The externally generated turbulence<br />

affects the transition to turbulence in the bed boundary layer, the phase difference between the<br />

free stream velocity and the bed shear stress and the wave friction factor. In another study at<br />

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