First Evidence of Peat Domes in the Congo Basin using LiDAR from a Fixed-Wing Drone

The world’s most extensive tropical peatlands occur in the Cuvette Centrale depression in the Congo Basin, which stores 30.6 petagrams of carbon (95% CI, 6.3–46.8). Improving our understanding of the genesis, development and functioning of these under-studied peatlands requires knowledge of their to...

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Main Authors: Ian J. Davenport, Iain McNicol, Edward T. A. Mitchard, Greta Dargie, Ifo Suspense, Brice Milongo, Yannick E. Bocko, Donna Hawthorne, Ian Lawson, Andy J. Baird, Susan Page, Simon L. Lewis
Format: Article
Language:English
Published: MDPI AG 2020-07-01
Series:Remote Sensing
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Online Access:https://www.mdpi.com/2072-4292/12/14/2196
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author Ian J. Davenport
Iain McNicol
Edward T. A. Mitchard
Greta Dargie
Ifo Suspense
Brice Milongo
Yannick E. Bocko
Donna Hawthorne
Ian Lawson
Andy J. Baird
Susan Page
Simon L. Lewis
author_facet Ian J. Davenport
Iain McNicol
Edward T. A. Mitchard
Greta Dargie
Ifo Suspense
Brice Milongo
Yannick E. Bocko
Donna Hawthorne
Ian Lawson
Andy J. Baird
Susan Page
Simon L. Lewis
author_sort Ian J. Davenport
collection DOAJ
description The world’s most extensive tropical peatlands occur in the Cuvette Centrale depression in the Congo Basin, which stores 30.6 petagrams of carbon (95% CI, 6.3–46.8). Improving our understanding of the genesis, development and functioning of these under-studied peatlands requires knowledge of their topography and, in particular, whether the peat surface is domed, as this implies a rain-fed system. Here we use a laser altimeter mounted on an unmanned airborne vehicle (UAV) to measure peat surface elevation along two transects at the edges of a peatland, in the northern Republic of Congo, to centimetre accuracy and compare the results with an analysis of nearby satellite LiDAR data (ICESat and ICESat-2). The LiDAR elevations on both transects show an upward slope from the peatland edge, suggesting a surface elevation peak of around 1.8 m over ~20 km. While modest, this domed shape is consistent with the peatland being rainfed. In-situ peat depth measurements and our LiDAR results indicate that this peatland likely formed at least 10,000 years BP in a large shallow basin ~40 km wide and ~3 m deep.
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spelling doaj.art-f3c9e5be76ac4d4b89f8c37c065ea8582023-11-20T06:17:58ZengMDPI AGRemote Sensing2072-42922020-07-011214219610.3390/rs12142196First Evidence of Peat Domes in the Congo Basin using LiDAR from a Fixed-Wing DroneIan J. Davenport0Iain McNicol1Edward T. A. Mitchard2Greta Dargie3Ifo Suspense4Brice Milongo5Yannick E. Bocko6Donna Hawthorne7Ian Lawson8Andy J. Baird9Susan Page10Simon L. Lewis11School of GeoSciences, University of Edinburgh, Edinburgh EH9 3FF, UKSchool of GeoSciences, University of Edinburgh, Edinburgh EH9 3FF, UKSchool of GeoSciences, University of Edinburgh, Edinburgh EH9 3FF, UKSchool of Geography, University of Leeds, Leeds LS2 9JT, UKÉcole Normale Supérieure, Université Marien Ngouabi, Brazzaville 99324, Republic of the CongoÉcole Normale Supérieure, Université Marien Ngouabi, Brazzaville 99324, Republic of the CongoFaculté des Sciences et Techniques, Université Marien NGOUABI, Brazzaville 99324, Republic of the CongoSchool of Geography and Sustainable Development, University of St Andrews, Scotland KY16 9AJ, UKDepartment of Geography and Sustainable Development, University of St Andrews, St Andrews KY16 9AL, UKSchool of Geography, University of Leeds, Leeds LS2 9JT, UKSchool of Geography, Geology and the Environment, University of Leicester, Leicester LE1 7RH, UKSchool of Geography, University of Leeds, Leeds LS2 9JT, UKThe world’s most extensive tropical peatlands occur in the Cuvette Centrale depression in the Congo Basin, which stores 30.6 petagrams of carbon (95% CI, 6.3–46.8). Improving our understanding of the genesis, development and functioning of these under-studied peatlands requires knowledge of their topography and, in particular, whether the peat surface is domed, as this implies a rain-fed system. Here we use a laser altimeter mounted on an unmanned airborne vehicle (UAV) to measure peat surface elevation along two transects at the edges of a peatland, in the northern Republic of Congo, to centimetre accuracy and compare the results with an analysis of nearby satellite LiDAR data (ICESat and ICESat-2). The LiDAR elevations on both transects show an upward slope from the peatland edge, suggesting a surface elevation peak of around 1.8 m over ~20 km. While modest, this domed shape is consistent with the peatland being rainfed. In-situ peat depth measurements and our LiDAR results indicate that this peatland likely formed at least 10,000 years BP in a large shallow basin ~40 km wide and ~3 m deep.https://www.mdpi.com/2072-4292/12/14/2196peatLiDARdomecarbonICESatICESat-2
spellingShingle Ian J. Davenport
Iain McNicol
Edward T. A. Mitchard
Greta Dargie
Ifo Suspense
Brice Milongo
Yannick E. Bocko
Donna Hawthorne
Ian Lawson
Andy J. Baird
Susan Page
Simon L. Lewis
First Evidence of Peat Domes in the Congo Basin using LiDAR from a Fixed-Wing Drone
Remote Sensing
peat
LiDAR
dome
carbon
ICESat
ICESat-2
title First Evidence of Peat Domes in the Congo Basin using LiDAR from a Fixed-Wing Drone
title_full First Evidence of Peat Domes in the Congo Basin using LiDAR from a Fixed-Wing Drone
title_fullStr First Evidence of Peat Domes in the Congo Basin using LiDAR from a Fixed-Wing Drone
title_full_unstemmed First Evidence of Peat Domes in the Congo Basin using LiDAR from a Fixed-Wing Drone
title_short First Evidence of Peat Domes in the Congo Basin using LiDAR from a Fixed-Wing Drone
title_sort first evidence of peat domes in the congo basin using lidar from a fixed wing drone
topic peat
LiDAR
dome
carbon
ICESat
ICESat-2
url https://www.mdpi.com/2072-4292/12/14/2196
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