Remote sensing of shallow waters – a 50 year retrospective and future directions

Technical advancements have widened the limits of remote sensing in mapping shallow water benthic habitats and bathymetry over the last decades. On the other hand, the needs of shallow water remote sensing have pushed instrument development. In this manuscript we provide 50-year retrospective of the...

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Published in:Remote Sensing of Environment
Main Authors: Kutser, Tiit, Hedley, John, Giardino, Claudia, Roelfsema, Chris, Brando, Vittorio E.
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2020
Subjects:
Online Access:https://espace.library.uq.edu.au/view/UQ:fe24aeb
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spelling ftunivqespace:oai:espace.library.uq.edu.au:UQ:fe24aeb 2023-05-15T15:08:20+02:00 Remote sensing of shallow waters – a 50 year retrospective and future directions Kutser, Tiit Hedley, John Giardino, Claudia Roelfsema, Chris Brando, Vittorio E. 2020-04-01 https://espace.library.uq.edu.au/view/UQ:fe24aeb eng eng Elsevier doi:10.1016/j.rse.2019.111619 issn:0034-4257 issn:1879-0704 orcid:0000-0003-0182-1356 PRG302 776348 Computers in Earth Sciences Soil Science Geology 1111 Soil Science 1903 Computers in Earth Sciences 1907 Geology Journal Article 2020 ftunivqespace https://doi.org/10.1016/j.rse.2019.111619 2020-12-08T08:03:07Z Technical advancements have widened the limits of remote sensing in mapping shallow water benthic habitats and bathymetry over the last decades. On the other hand, the needs of shallow water remote sensing have pushed instrument development. In this manuscript we provide 50-year retrospective of the developments in the field in terms of both instrumentation and methods. We also show that spectral features characteristic of the main benthic groups in shallow water are consistent from the tropics to sub-arctic regions and from salty to freshwaters. The fundamental limiting factor in both benthic mapping and bathymetry is absorption of light by water molecules. However, spectral absorption by water molecules is the key to bathymetry derivation. Variable backscattering by particles and absorption by dissolved organic matter is a confounding factor for all objectives. The combination of using the spectral and textural characteristics of bottom features and our knowledge about these features have now resulted in the ability to map habitats over large coastal systems. This manuscript has shown that optically shallow water remote sensing has reached levels where the satellite derived bathymetry and habitat maps are accepted by different end users (including the International Maritime Organisation) and are routinely used in ecological studies, monitoring and management of coastal environments. Article in Journal/Newspaper Arctic The University of Queensland: UQ eSpace Arctic Remote Sensing of Environment 240 111619
institution Open Polar
collection The University of Queensland: UQ eSpace
op_collection_id ftunivqespace
language English
topic Computers in Earth Sciences
Soil Science
Geology
1111 Soil Science
1903 Computers in Earth Sciences
1907 Geology
spellingShingle Computers in Earth Sciences
Soil Science
Geology
1111 Soil Science
1903 Computers in Earth Sciences
1907 Geology
Kutser, Tiit
Hedley, John
Giardino, Claudia
Roelfsema, Chris
Brando, Vittorio E.
Remote sensing of shallow waters – a 50 year retrospective and future directions
topic_facet Computers in Earth Sciences
Soil Science
Geology
1111 Soil Science
1903 Computers in Earth Sciences
1907 Geology
description Technical advancements have widened the limits of remote sensing in mapping shallow water benthic habitats and bathymetry over the last decades. On the other hand, the needs of shallow water remote sensing have pushed instrument development. In this manuscript we provide 50-year retrospective of the developments in the field in terms of both instrumentation and methods. We also show that spectral features characteristic of the main benthic groups in shallow water are consistent from the tropics to sub-arctic regions and from salty to freshwaters. The fundamental limiting factor in both benthic mapping and bathymetry is absorption of light by water molecules. However, spectral absorption by water molecules is the key to bathymetry derivation. Variable backscattering by particles and absorption by dissolved organic matter is a confounding factor for all objectives. The combination of using the spectral and textural characteristics of bottom features and our knowledge about these features have now resulted in the ability to map habitats over large coastal systems. This manuscript has shown that optically shallow water remote sensing has reached levels where the satellite derived bathymetry and habitat maps are accepted by different end users (including the International Maritime Organisation) and are routinely used in ecological studies, monitoring and management of coastal environments.
format Article in Journal/Newspaper
author Kutser, Tiit
Hedley, John
Giardino, Claudia
Roelfsema, Chris
Brando, Vittorio E.
author_facet Kutser, Tiit
Hedley, John
Giardino, Claudia
Roelfsema, Chris
Brando, Vittorio E.
author_sort Kutser, Tiit
title Remote sensing of shallow waters – a 50 year retrospective and future directions
title_short Remote sensing of shallow waters – a 50 year retrospective and future directions
title_full Remote sensing of shallow waters – a 50 year retrospective and future directions
title_fullStr Remote sensing of shallow waters – a 50 year retrospective and future directions
title_full_unstemmed Remote sensing of shallow waters – a 50 year retrospective and future directions
title_sort remote sensing of shallow waters – a 50 year retrospective and future directions
publisher Elsevier
publishDate 2020
url https://espace.library.uq.edu.au/view/UQ:fe24aeb
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_relation doi:10.1016/j.rse.2019.111619
issn:0034-4257
issn:1879-0704
orcid:0000-0003-0182-1356
PRG302
776348
op_doi https://doi.org/10.1016/j.rse.2019.111619
container_title Remote Sensing of Environment
container_volume 240
container_start_page 111619
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