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EDITORIAL
Remote sensing and the UN Ocean Decade: high
expectations, big opportunities
Vincent Lecours
1
, Mathias Disney
2
, Kate He
3
, Nathalie Pettorelli
4
, J. Marcus Rowcliffe
4
,
Temuulen Sankey
5
& Kylie Scales
6
1
School of Forest, Fisheries, & Geomatics Sciences, University of Florida, 7922 NW 71st St., Gainesville Florida, 32653, USA
2
Department of Geography, University College London, Gower Street, London WC1E 6BT, UK
3
Department of Biological Sciences, Murray State University, Murray Kentucky, 42071, USA
4
Zoological Society of London, Institute of Zoology, Regent’s Park, London NW1 4RY, UK
5
School of Informatics, Computing, and Cyber Systems, Northern Arizona University, Flagstaff Arizona, 86011, USA
6
Global-Change Ecology Research Group, University of the Sunshine Coast, Maroochydore Queensland 4556, Australia
doi: 10.1002/rse2.241
This year officially marks the beginning of the United
Nations Decade of Ocean Science for Sustainable Devel-
opment (2021–2030)—the Ocean Decade. A primary
objective of this coordination framework is to support
scientific research and technological developments that
can contribute to the conservation and sustainable man-
agement of the world’s oceans. One of the seven Decade
Outcomes is to secure healthy and resilient oceans where
marine biodiversity is mapped and protected; however,
fulfilling this goal will require data, knowledge, and tech-
nology. The use of remote sensing is now established in
marine research and management and is crucial in devel-
oping our understanding of ocean patterns and processes
at multiple spatial and temporal scales (e.g., Jawak et al.,
2015). As such, remote sensing technology is expected to
play a critical role in achieving the vision set by the
Ocean Decade.
In the last 20 years, technological developments in
remote sensing have boosted our ability to monitor the
distribution and status of previously understudied ecosys-
tems, from tidal flats and mangroves (Goldberg et al.,
2020; Murray et al., 2019) to continental shelves (Pygas
et al., 2020) and the deep sea (Lim et al., 2021). These
developments have also enabled the mapping of marine
physical and biogenic habitats and ecosystems at spatial
resolutions never achieved before. For example, Lyons
et al. (2020) recently demonstrated how coral reef habitats
ranging from individual reefs (~200 km
2
) to entire barrier
reef systems (200 000 km
2
) could be mapped across vast
ocean extents (>6 000 000 km
2
) using global multiscale
earth observations, generating high-resolution maps that
can be used to support ecosystem risk assessments and to
inform management. Deeper seafloor habitats can now be
mapped and imaged at a centimeter scale using autono-
mous underwater vehicles and sensors like synthetic aper-
ture sonars (e.g., Thorsnes et al., 2019). Maps produced
by such efforts are invaluable communication tools; they
have become key for data integration and synthesis to
inform decision-making in a variety of contexts (Guisan
et al., 2013; Harris & Baker, 2020). These mapping exer-
cises can also be used to predict the distribution of spe-
cies, communities, or ecosystems based on their
associations with the physical and chemical characteristics
of the environment and can support seascape ecology
studies that relate spatial patterns with ecological pro-
cesses (Pittman, 2018).
Passive sensors mounted on unoccupied aerial vehicles
(UAVs) and satellites are commonly used to map and
monitor characteristics and components of the marine
environment, such as sea surface temperature, salinity,
marine mammal distribution, primary productivity, and
harmful algal blooms (Pettorelli, 2019). Satellite radar
altimeters have also long been used to study the oceans
and derive coarse-scale digital bathymetric models (e.g.,
Dixon et al., 1983). The information compiled by differ-
ent sensors can then be integrated to delineate broad
marine biogeographic units such as ecoregions (e.g., Sayre
et al., 2017; Spalding et al., 2007). At finer scales, UAV-
mounted lidar sensors have enabled increased above-
ground biomass monitoring in coastal systems such as
mangroves (e.g., Qiu et al., 2019), while bathymetric lidar
systems have boosted data collection efforts in submerged
coastal areas, where it is often too dangerous and resource
intensive to collect acoustic data and challenging for radar
altimeters to differentiate land from water (Sandwell
et al., 2002).
While active underwater cameras mounted on remotely
operated vehicles or towed or dropped platforms have
been extensively used to collect species and seafloor data
and create photomosaics of the seafloor (e.g., Jones, 2009;
Sward et al., 2021), optical remote sensing is usually lim-
ited to shallow and optically clear waters. This means
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267
that, in most situations, acoustic remote sensing repre-
sents the most effective source of data for ecologists inter-
ested in marine biodiversity. Acoustic remote sensing can
be passive (i.e., using hydrophones to capture sounds in
the environment) or active (i.e., using sonars that pro-
duce directional sound and listen for returns); both have
their place in support of marine ecology and conserva-
tion. For example, multibeam echosounders enable the
production of high-resolution digital bathymetric models,
from which different terrain attributes (e.g., slope, rugos-
ity) known to be direct or indirect surrogates of species
distributions can be derived (Lecours et al., 2015,2016;
McArthur et al., 2010). Multibeam backscatter data and
sidescan sonar imagery can also provide information
about the distribution of sediment and seafloor habitat
characteristics important to many species. Most often
used in fisheries, singlebeam echosounders can provide
critical information about what lives in the water column,
while passive acoustic remote sensing can contribute spe-
cies occurrence and distribution data and inform abun-
dance and behavioral research (Stowell & Sueur, 2020).
There is no doubt that the UN Ocean Decade will pro-
vide exciting opportunities for the field of remote sensing
and its applications to marine and coastal environments.
Active acoustic remote sensing technologies have histori-
cally been associated with military uses and the field of
hydrography rather than with the remote sensing commu-
nity of practice; this has slowed the integration of data
processing and analysis methods that have proven effec-
tive in the study of terrestrial environments. This gap
offers new research opportunities that remain unexplored
in marine environments. For example, because raw multi-
beam echosounder data are displayed as point clouds that
share many characteristics with lidar point clouds,
Table 1. A meta-analysis of original research articles published in Remote Sensing in Ecology and Conservation highlights an increase in coastal
and marine studies and a strong reliance on optical remote sensing and, to a lesser extent, passive acoustics.
References Topics Remote sensing approaches
Weishampel et al. (2016) Mapping of sea turtle nesting patterns in
Florida
Satellite-based visible and infrared sensors
Asner et al. (2017) Coral reef mapping Satellite multispectral imagery
Lecours et al. (2017) Assessment of artifacts in marine habitat
maps and species distribution models
Multibeam echosounder bathymetric and backscatter
data
Di Iorio et al. (2018)Posidonia oceanica meadows monitoring Hydrophones (passive acoustic monitoring)
Ettritch et al. (2018) Coastal sand dunes monitoring Archived satellite data and aerial photography
Nahirnick et al. (2019) Seagrass habitat mapping UAV imagery
Rahman et al. (2019) Mangrove forests mapping Satellite multispectral imagery and radar data
Wedding et al. (2019) Predictions of coral fish assemblages Satellite multispectral imagery and topo-bathymetric lidar data
LaRue et al. (2020) Coastal habitat mapping of Weddell seal Satellite multispectral imagery
Bolin et al. (2020) Entanglement of humpback whales in
coastal environments
Satellite-derived sea surface temperature
Roca and Van Opzeeland (2020) Characterization of underwater acoustic
biodiversity
Acoustic recorders (passive acoustic monitoring)
Schroeder et al. (2020) Nearshore kelp beds monitoring Satellite multispectral imagery
Cubaynes et al. (2020) Measuring whale skin spectral reflectance Spectroradiometer
Ridge et al. (2020) Intertidal oyster reefs mapping UAV imagery
Lyons et al. (2020) Coral reef mapping Satellite multispectral imagery, airborne hyperspectral sensor,
satellite-derived bathymetry, bathymetric data compilations
Soto et al. (2021) Estimating animal density in three
dimensions
Theoretical passive acoustic detectors and cameras
Ellis et al. (2021) Marine habitat mapping UAV imagery
Aldous et al. (2021) Coastal wetland mapping Satellite multispectral imagery and radar data, UAS imagery
Fretwell and Trathan (2021) Coastal emperor penguins colony
mapping
Satellite multispectral imagery
Ventura et al. (2021) Characterization of underwater worm
colonies
Underwater multispectral sensor
Poursanidis et al. (2021) Marine habitat mapping Satellite multispectral imagery, satellite-derived bathymetry,
underwater camera
Sward et al. (2021) Producing density estimates for the long
spined urchin
Stereo video from a remotely operated vehicle, archived
multibeam bathymetric data
Articles are listed chronologically.
268 ª2021 The Authors. Remote Sensing in Ecology and Conservation published by John Wiley & Sons Ltd on behalf of Zoological Society of London.
Editorial V. Lecours
acoustic data processing workflows might benefit from
algorithms developed for processing lidar data. The oppo-
site is also true; the commonly used CUBE (Combined
Uncertainty and Bathymetry Estimator) algorithm for the
generation of digital bathymetric models and the com-
bined storage of bathymetry and uncertainty layers within
a single BAG (Bathymetric Attributed Grid) file format
may benefit other types of remotely sensed data like lidar-
derived digital surface and terrain models. Data fusion
techniques offer opportunities for the production of
seamless digital surface models spanning the terrestrial
and marine environments that combine both optical and
acoustic remotely sensed data (e.g., Linklater et al., 2018).
New developments in image processing tools, analytical
methods like object-based image analysis, and artificial
intelligence have the potential to enhance marine ecology
and seascape ecology research (Pittman et al., 2021). New
ways to study the marine environment, such as multi-
beam water column data (e.g., Schimel et al., 2020), mul-
tispectral acoustic systems (e.g., Brown et al., 2019), and
satellite-derived bathymetry (Ashphaq et al., 2021), high-
light the need for more research into how remote sensing
can contribute to the understanding and conservation of
the world’s oceans.
The issues targeted by the Ocean Decade, such as cli-
mate change and unsustainable exploitation of marine
resources, are global and, as such, will require collabora-
tive efforts and data from around the world. However,
both ocean science and remote sensing capacities are
unevenly distributed. Mapping marine ecosystems and
biodiversity in places or through organizations that can-
not count on well-funded initiatives must rely on existing,
publicly available datasets such as the GEBCO (General
Bathymetric Chart of the Oceans) global bathymetric
dataset, archived satellite imagery, or marine biodiversity
datasets like those compiled on OBIS (Ocean Biodiversity
Information System). This highlights the need for open-
source multidisciplinary data in both remote sensing and
the marine sciences that can be spatially integrated accu-
rately; it also highlights the need for a common platform
where information gathered by these communities can be
shared and scientific agendas synchronized. Since its
inception, the editorial board of Remote Sensing in Ecology
and Conservation has welcomed contributions to coastal
and marine ecology and conservation that rely on remote
sensing (Pettorelli et al., 2015). In 2017, the editorial
board made it a goal to increase their engagement with
communities working in marine systems and acoustic
remote sensing (Pettorelli et al., 2017). The number of
published “original research” articles on coastal or marine
environments has steadily increased every year since 2016,
reaching 21% of all contributions in 2020 (Table 1).
However, the use of active acoustic remote sensing is still
underrepresented, with only one article published since
the launch of our journal. With efforts like the Seabed
2030 Project, which aims to map the world’s seafloor by
2030 and relies heavily on acoustic remote sensing tech-
nologies (Mayer et al., 2018), we expect the availability of
seafloor data to increase and, with them, the opportuni-
ties to better understand the ecology of our seas and
oceans. We thus want to reiterate our commitment to
marine remote sensing developments and applications
and hope that the increased opportunities will be reflected
in the submissions to come.
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V. Lecours Editorial
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