Publication | Open Access
Mapping forest canopy height globally with spaceborne lidar
1.3K
Citations
33
References
2011
Year
RadarEarth ObservationEngineeringForest BiometricsGlas DataForestryGeographyRemote SensingCanopy MicrometeorologyForest MeteorologyTerrestrial SensingSpaceborne Light DetectionSpaceborne LidarEarth Observation DataForest InventoryEarth ScienceCanopy HeightDeforestation
Spaceborne lidar enables global mapping of forest vertical structure, but its sparse GLAS coverage limits accuracy. The study produces a wall‑to‑wall global canopy‑height map at 1‑km resolution using 2005 GLAS data from ICESat. Global canopy height (RH100) was modeled from forest type, tree cover, elevation, and climatology, then validated against 66 FLUXNET sites and compared to a recent canopy‑height map. The model shows higher error in closed broadleaved forests (e.g., Amazon), with RMSE 6.1 m (R² = 0.5) or 4.4 m (R² = 0.7) excluding outliers; it is generally taller and more correlated with FLUXNET, revealing a latitudinal gradient and disturbance patterns.
[1] Data from spaceborne light detection and ranging (lidar) opens the possibility to map forest vertical structure globally. We present a wall-to-wall, global map of canopy height at 1-km spatial resolution, using 2005 data from the Geoscience Laser Altimeter System (GLAS) aboard ICESat (Ice, Cloud, and land Elevation Satellite). A challenge in the use of GLAS data for global vegetation studies is the sparse coverage of lidar shots (mean = 121 data points/degree2 for the L3C campaign). However, GLAS-derived canopy height (RH100) values were highly correlated with other, more spatially dense, ancillary variables available globally, which allowed us to model global RH100 from forest type, tree cover, elevation, and climatology maps. The difference between the model predicted RH100 and footprint level lidar-derived RH100 values showed that error increased in closed broadleaved forests such as the Amazon, underscoring the challenges in mapping tall (>40 m) canopies. The resulting map was validated with field measurements from 66 FLUXNET sites. The modeled RH100 versus in situ canopy height error (RMSE = 6.1 m, R2 = 0.5; or, RMSE = 4.4 m, R2 = 0.7 without 7 outliers) is conservative as it also includes measurement uncertainty and sub pixel variability within the 1-km pixels. Our results were compared against a recently published canopy height map. We found our values to be in general taller and more strongly correlated with FLUXNET data. Our map reveals a global latitudinal gradient in canopy height, increasing towards the equator, as well as coarse forest disturbance patterns.
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