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IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING 1
Deep Learning for Predicting Significant Wave
Height From Synthetic Aperture Radar
Brandon Quach , Yannik Glaser , Justin Edward Stopa , Alexis Aurélien Mouche , and Peter Sadowski
Abstract— The Sentinel-1 satellites equipped with synthetic
aperture radars (SARs) provide near-global coverage of the
world’s oceans every six days. We curate a data set of collocations
between SAR and altimeter satellites and investigate the use of
deep learning to predict significant wave height from SAR. While
previous models for predicting geophysical quantities from SAR
rely heavily on feature-engineering, our approach learns directly
from low-level image cross-spectra. Training on collocations from
2015 to 2017, we demonstrate on test data from 2018 that deep
learning reduces the state-of-the-art root mean squared error
by 50%, from 0.6 to 0.3 m when compared to altimeter data.
Furthermore, we isolate the contributions of different features to
the model performance.
Index Terms— CWAVE, deep learning, machine learning,
neural networks, Sentinel-1, significant wave height, synthetic
aperture radar (SAR).
I. I NTRODUCTION
S
YNTHETIC aperture radar (SAR) enables us to measure
submesoscale phenomena with unprecedented coverage,
resolution, and frequency. By measuring the backscatter from
the ocean surface, SAR captures information about ocean
swells and sea surface roughness at high spatial resolutions
( <10 m) [1], from which many oceanic, atmospheric, and
biologic phenomena can be identified [2]. The two Sentinel-
1 satellites of the European Space Agency (ESA) take regular
SAR measurements of the ocean surface, together covering the
entire globe every six days [3], and have already accumulated
more than 600 TB of level-1 (L1) wave mode data. However,
in order to take full advantage of this technology and the tor-
rent of data being produced, new methods are needed to extract
useful information from the high-dimensional measurements.
Sea state information extracted from SAR has been instru-
mental in understanding swell decay [1], [4], [5], improving
swell propagation in numerical models [6], and predicting
swell amplitudes and arrivals times by assimilation into numer-
ical models [7]. SAR can also be used to estimate extreme
Manuscript received February 14, 2020; revised May 22, 2020; accepted
June 8, 2020. (Corresponding author: Justin Edward Stopa.)
Brandon Quach is with the Computing and Mathematical Sciences Depart-
ment, California Institute of Technology, Pasadena, CA 91125-0002 USA, and
also with the Information and Computer Sciences Department, University of
Hawai’i at M¯ anoa, Honolulu, HI 96822 USA.
Yannik Glaser and Peter Sadowski are with Information and Computer
Sciences Department, University of Hawai’i at M¯ anoa, Honolulu, HI 96822
USA.
Justin Edward Stopa is with Ocean Engineering Department, University of
Hawai’i at M¯ anoa, Honolulu, HI 96822 USA (e-mail: stopa@hawaii.edu).
Alexis Aurélien Mouche is with the Univ. Brest, CNRS, IRD, IFRE-
MER, Laboratoire d’Océanographie Physique et Spatiale (LOPS), IUEM,
29280 Brest, France.
Color versions of one or more of the figures in this article are available
online at http://ieeexplore.ieee.org.
Digital Object Identifier 10.1109/TGRS.2020.3003839
sea states in extra-tropical and tropical cyclones [8]–[10].
A geophysical quantity of particular interest is the significant
wave height, H
s
, defined as the mean of the top third of a
wave height distribution, and estimating H
s
from SAR has
immediate practical uses in alerting ships to dangerously large
waves. Traditional “inverse” algorithms for inferring H
s
from
SAR are slow and perform poorly in windy conditions typical
of most storms [11], [12] because of the complex nonlinear
mechanism involved in the image synthesis when observing
moving scenes. As a result, several recent studies have focused
on data-driven statistical models [8]–[10], [13].
Previous data-driven approaches for predicting H
s
from
SAR used small data sets of buoy observations as targets
for training ( <5000 examples) [14]–[16], or numerical mod-
els of global wave generation such as WAVEWATCH3 [8],
[10], [13], [17]. The current state-of-the-art method uses a
neural network trained on the latter, and predicts H
s
with
0.6-m root mean squared error (RMSE) [10]. However, the
WAVEWATCH3 targets are only an estimate of H
s
and are
known to be unreliable in high sea states [18]–[20].
Furthermore, the neural network in [10] relies on a
reduced representation of the modulation cross-spectra: a set
of 22 engineered features known as CWAVE [13]. Such
dimensionality-reduction methods can be very useful, but
often come at the cost of discarding relevant information.
We hypothesize that the SAR image modulation spectra con-
tains additional information about H
s
that is lost by the
CWAVE dimensionality-reduction step. We propose to learn
the relevant intermediate data representations using deep learn-
ing with artificial neural networks, similar to what has been
done in other fields from computer vision [21] to high-energy
physics [22]–[24].
In this work, we address both limitations of current data-
driven H
s
prediction models. First, we curate a data set
containing direct observations of ocean wave heights by iden-
tifying 750,000 collocations of SAR and altimeter satellites.
Second, we train a statistical model to extract information
directly from low-level SAR image spectra using deep learn-
ing. Finally, we analyze the importance of the different inputs
to this model, and its performance in different settings.
II. DATA AND METHODS
A. Sensors, Collocations and Preprocessing
Our first contribution is a data set of historical measure-
ments from two types of polar-orbiting satellites: Sentinel-1
SAR satellites and altimeter satellites. Because the satel-
lites are in different orbits, their paths intersect, providing
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