Abstract

The ability to monitor the evolution of the coastal zone over time is an important factor in coastal knowledge, development, planning, risk mitigation, and overall coastal zone management. While traditional bathymetry surveys using echo-sounding techniques are expensive and time consuming, remote sensing tools have recently emerged as reliable and inexpensive data sources that can be used to estimate bathymetry using depth inversion models. Deep learning is a growing field of artificial intelligence that allows for the automatic construction of models from data and has been successfully used for various Earth observation and model inversion applications. In this work, we make use of publicly available Sentinel-2 satellite imagery and multiple bathymetry surveys to train a deep learning-based bathymetry estimation model. We explore for the first time two complementary approaches, based on color information but also wave kinematics, as inputs to the deep learning model. This offers the possibility to derive bathymetry not only in clear waters as previously done with deep learning models but also at common turbid coastal zones. We show competitive results with a state-of-the-art physical inversion method for satellite-derived bathymetry, Satellite to Shores (S2Shores), demonstrating a promising direction for worldwide applicability of deep learning models to inverse bathymetry from satellite imagery and a novel use of deep learning models in Earth observation.

Highlights

  • Coastal areas are under a constant multitude of pressures resulting from different natural forces

  • The metrics used to evaluate the predictions of each of the models are the root mean squared error (RMSE), the Pearson correlation coefficient (r), the concordance correlation coefficient (CCC) [48], and the slope of the predictions compared to the target depths

  • We propose two different variants of Deep Single-Point Estimation of Bathymetry (DSPEB) based on wave kinematics (W-DSPEB) and color (C-DSPEB; Section 2.3) and we compare them to a state-of-the-art physics-based SDB

Read more

Summary

Introduction

Coastal areas are under a constant multitude of pressures resulting from different natural forces. Traditional in situ bathymetric measurements using echo-sounding or Light Detection and Ranging (LiDAR) are time-consuming and expensive [3] and are preconditioned on a number of environmental factors such as the navigability of the site to be surveyed [4], in addition to a multitude of logistical constraints [5,6]. Remote sensing tools have recently become an important tool to collect different types of data that allows the monitoring of coastal areas [7,8]. These tools differ in their temporal frequency and spatial coverage.

Objectives
Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call