Temporal Evolution of Wave Overtopping of a Hybrid Dune-Dike Structure Under Extreme Storm Conditions

Book Chapter (2026)
Author(s)

Cem Sevindik (TU Delft - Civil Engineering & Geosciences)

Afshar Adeli Soleimandarabi (Universiteit Gent)

Marion Tissier (TU Delft - Civil Engineering & Geosciences)

Bas Hofland (TU Delft - Civil Engineering & Geosciences)

Ad J.H.M. Reniers (TU Delft - Civil Engineering & Geosciences)

Vincent Gruwez (Flanders Hydraulics)

Peter Troch (Universiteit Gent)

Research Group
Environmental Fluid Mechanics
DOI related publication
https://doi.org/10.1007/978-3-032-15477-4_6 Final published version
More Info
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Publication Year
2026
Language
English
Research Group
Environmental Fluid Mechanics
Pages (from-to)
31-36
Publisher
Springer Nature
ISBN (print)
['978-3-032-15476-7', '978-3-032-15479-8']
ISBN (electronic)
978-3-032-15477-4
Event
Coastal Dynamics 2025 (2025-04-07 - 2025-04-11), Aveiro, Portugal
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12
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Abstract

Hybrid dune-dike structures are innovative developments creating coastal defense systems which are more conveniently integrated with the natural environment. In this study, a numerical study was conducted to investigate the temporal evolution of wave overtopping, with the changing profile of the dune under extreme storm conditions with a constant water level, of two types of hybrid dune-dike structures in Katwijk (dike-in-dune type) and Raversijde (dune-in-front-of-dike type). XBeach 1DH was used to firstly calculate bed profiles for different time steps during a 10-h storm duration using the Surfbeat mode and then, in a second step, mean wave overtopping rates were modelled for each calculated bed profile using the Non-hydrostatic mode. According to the simulation results, most of the dune erosion occurs during the first two hours of the storm, and then continues at a slower rate as the sand deposits in front of the dune. Once the hybrid structure is eroding (so for t > 0), the significant wave height at the dike toe and the mean overtopping discharge increase in time for both Katwijk and Raversijde, although it quickly reaches a plateau for Raversijde. The first simulations with the original non-eroded profiles deviate from this trend. The reason for this deviation needs to be further investigated.