Wave growth limit in shallow water: Analytical study of wave growth curves and SWAN source terms

Verkenning golfbelasting op kribben

Inzicht in extreme golfcondities: Stormmetingen en SWAN berekeningen

Hydrodynamic and Morphodynamic Validation of Cross-shore Profile Model (CROSMOR) based on Large Scale Flume Tests (LIP-TESTS)

The CROSMOR-model (Van Rijn, 1997, 1998), representing wave propagation, refraction, shoaling, breaking, associated sand transport and morphology in cross-shore direction based on a probabilistic approach, has been applied to simulate the hydrodynamics and the nearshore bar behaviour for three experiments in the large-scale Delta flume o f Delft...

Effects of a self-scaling cut-off frequency on wave growth in SWAN

Validation of wave propagation on curvilinear grids in SWAN

Extreme wave conditions along the coast of the Netherlands: Wave propagation models for the coast between Cadzand and Hoek van Holland

Yearly-averaged sand transport at the -20 and -8 NAP depth contours of the Jarkus profiles 14, 40, 76 and 103

Extreme wave conditions along the coast of the Netherlands: Wave propagation models for the coast between Hoek van Holland and Rottumeroog

Wave Propagation in Shallow Water

The propagation of waves from offshore to onshore is a difficult problem due to the mathematical complexities of the governing equations and the degree of uncertainty of the bathymetry over which the waves must travel. In this lecture, the various methods of transforming offshore wave trains to shallow water are discussed. First, single wave...

Europoortkering: Seiches-berekeningen in het kader van de tracé-nota Europoortkering

Verification of numerical wave propagation models with laboratory measurements: HISWA verification in the directional wave basin

Verification of numerical wave propagation models with field measurements: CREDIZ verification Haringvliet

On the parabolic equation method for water wave propagation

A parabolic approximation to the reduced wave equation is investigated for the propagation of periodic surface waves in shoaling water. The approximation is derived from splitting the wave field into transmitted and reflected components. In the case of an area with straight and parallel bottom contourlines, the asymptotic form of the solution...