Abstract

One of the most promising techniques for the analysis of Spatio-Temporal ocean wave fields is stereo vision. Indeed, the reconstruction accuracy and resolution typically outperform other approaches like radars, satellites, etc. However, it is computationally expensive so its application is typically restricted to the analysis of short pre-recorded sequences. What prevents such methodology from being truly real-time is the final 3D surface estimation from a scattered, non-equispaced point cloud. Recently, we studied a novel approach exploiting the temporal dependence of subsequent frames to iteratively update the wave spectrum over time. Albeit substantially faster, the unpredictable convergence time of the optimization involved still prevents its usage as a continuously running remote sensing infrastructure. In this work, we build upon the same idea, but investigating the feasibility of a fully data-driven Machine Learning (ML) approach. We designed a novel Convolutional Neural Network that learns how to produce an accurate surface from the scattered elevation data of three subsequent frames. The key idea is to embed the linear dispersion relation into the model itself to physically relate the sparse points observed at different times. Assuming that the scattered data are uniformly distributed in the spatial domain, this has the same effect of increasing the sample density of each single frame. Experiments demonstrate how the proposed technique, even if trained with purely synthetic data, can produce accurate and physically consistent surfaces at five frames per second on a modern PC.

Highlights

  • Introduction published maps and institutional affilIn the last decade, we witnessed a growing interest in the spatio-temporal characterization of ocean wave fields

  • Our experiments show the ability of the proposed CNN to estimate reliable wave fields at a fraction of time of the WASSfast PU algorithm, and with a more even noise distribution in the directional wave spectrum

  • In order to analyze the quality of the sea surface reconstruction using our approach, we divided the experimental validation into two parts

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Summary

Introduction

We witnessed a growing interest in the spatio-temporal characterization of ocean wave fields. Many complex phenomena are accounted for (and better described) by leveraging the traditional one-point observation systems (like buoy, wave probes, etc.) to its spatial extent. Showed that classical point-based models were unsuitable to predict the likelihood, shape, and height of rogue waves over an area. Filipot et al [4] studied extreme breaking waves and their mechanical loading on heritage offshore lighthouses, Stringari et al [5] developed a probabilistic wave breaking model for wind-generated waves, and Douglas et al [6]. Analyzed wave interactions against rubble mound breakwaters. Acquisition of such data are made with a remote sensing infrastructure comprising different sensors and computational techniques according to the desired scale and resolution. The range of application spans from millimeter wavelength, exploiting iations

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