Abstract

Wave overtopping is an important design criterion for coastal structures such as dikes, breakwaters and promenades. Hence, the prediction of the expected wave overtopping discharge is an important research topic. Existing prediction tools consist of empirical overtopping formulae, machine learning techniques like neural networks, and numerical models. In this paper, an innovative machine learning method—gradient boosting decision trees—is applied to the prediction of mean wave overtopping discharges. This new machine learning model is trained using the CLASH wave overtopping database. Optimizations to its performance are realized by using feature engineering and hyperparameter tuning. The model is shown to outperform an existing neural network model by reducing the error on the prediction of the CLASH database by a factor of 2.8. The model predictions follow physically realistic trends for variations of important features, and behave regularly in regions of the input parameter space with little or no data coverage.

Highlights

  • Wave overtopping is traditionally an important criterion in the design of coastal structures.Overtopping waves can lead to flooding of the hinterland at coastal dikes, undesirable wave transmission at breakwaters or the risk of physical harm at promenades

  • A series of empirical overtopping formulae have been developed of which a selection is mentioned in the EurOtop manual and its predecessors [1,2,3]. These formulae provide a relatively quick and easy means to obtain a first indication of the expected mean wave overtopping discharge, q

  • They are derived based on data from physical model tests, collected in the CLASH database [4]

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Summary

Introduction

Wave overtopping is traditionally an important criterion in the design of coastal structures.Overtopping waves can lead to flooding of the hinterland at coastal dikes, undesirable wave transmission at breakwaters or the risk of physical harm at promenades. A series of empirical overtopping formulae have been developed of which a selection is mentioned in the EurOtop manual and its predecessors [1,2,3]. These formulae provide a relatively quick and easy means to obtain a first indication of the expected mean wave overtopping discharge, q. They are derived based on data from physical model tests, collected in the CLASH database [4]. Recent efforts have extended this neural network application to predict wave transmission and reflection [6]

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