Davenport, IJ; McNicol, I; Mitchard, ET; Dargie, G; Suspense, I; Milongo, B; Bocko, YE; ... Lewis, SL; + view all Davenport, IJ; McNicol, I; Mitchard, ET; Dargie, G; Suspense, I; Milongo, B; Bocko, YE; Hawthorne, D; Lawson, I; Baird, AJ; Page, S; Lewis, SL; - view fewer (2020) First evidence of peat domes in the congo basin using LiDAR from a fixed-wing drone. Remote Sensing , 12 (14) , Article 2196. 10.3390/rs12142196.

Preview

Text remotesensing-12-02196-v3.pdf - Published Version Download (4MB) | Preview

Abstract

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.

Download activity - last month

Export as JSONXMLCSV

Download activity - last 12 months

Export as XMLJSONCSV

Downloads by country - last 12 months

Export as XMLJSONCSV

Archive Staff Only

View Item