Mapping tropical forest biomass with radar and spaceborne LiDAR in Lopé National Park, Gabon: overcoming problems of high biomass and persistent cloud
Spatially-explicit maps of aboveground biomass are essential for calculating the losses and gains in forest carbon at a regional to national level. The production of such maps across wide areas will become increasingly necessary as international efforts to protect primary forests, such as the REDD+...
Main Authors: | , , , , , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2012-01-01
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Series: | Biogeosciences |
Online Access: | http://www.biogeosciences.net/9/179/2012/bg-9-179-2012.pdf |
Summary: | Spatially-explicit maps of aboveground biomass are essential for calculating
the losses and gains in forest carbon at a regional to national level. The
production of such maps across wide areas will become increasingly necessary
as international efforts to protect primary forests, such as the REDD+
(Reducing Emissions from Deforestation and forest Degradation) mechanism,
come into effect, alongside their use for management and research more
generally. However, mapping biomass over high-biomass tropical forest is
challenging as (1) direct regressions with optical and radar data saturate,
(2) much of the tropics is persistently cloud-covered, reducing the
availability of optical data, (3) many regions include steep topography,
making the use of radar data complex, (5) while LiDAR data does not suffer
from saturation, expensive aircraft-derived data are necessary for complete
coverage.
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We present a solution to the problems, using a combination of
terrain-corrected L-band radar data (ALOS PALSAR), spaceborne LiDAR data
(ICESat GLAS) and ground-based data. We map Gabon's Lopé National Park
(5000 km<sup>2</sup>) because it includes a range of vegetation types from savanna
to closed-canopy tropical forest, is topographically complex, has no recent
contiguous cloud-free high-resolution optical data, and the dense forest is
above the saturation point for radar. Our 100 m resolution biomass map is
derived from fusing spaceborne LiDAR (7142 ICESat GLAS footprints), 96
ground-based plots (average size 0.8 ha) and an unsupervised classification
of terrain-corrected ALOS PALSAR radar data, from which we derive the
aboveground biomass stocks of the park to be 78 Tg C (173 Mg C ha<sup>−1</sup>).
This value is consistent with our field data average of 181 Mg C ha<sup>−1</sup>,
from the field plots measured in 2009 covering a total of 78 ha, and which
are independent as they were not used for the GLAS-biomass estimation. We
estimate an uncertainty of ±25% on our carbon stock value for the
park. This error term includes uncertainties resulting from the use of a
generic tropical allometric equation, the use of GLAS data to estimate
Lorey's height, and the necessity of separating the landscape into distinct
classes.
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As there is currently no spaceborne LiDAR satellite in operation (GLAS data
is available for 2003–2009 only), this methodology is not suitable for
change-detection. This research underlines the need for new satellite LiDAR
data to provide the potential for biomass-change estimates, although this
need will not be met before 2015. |
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ISSN: | 1726-4170 1726-4189 |