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- Publisher Website: 10.3390/f13101686
- Scopus: eid_2-s2.0-85140729475
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Article: Evaluation of NASA’s GEDI Lidar Observations for Estimating Biomass in Temperate and Tropical Forests
Title | Evaluation of NASA’s GEDI Lidar Observations for Estimating Biomass in Temperate and Tropical Forests |
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Authors | |
Keywords | aboveground biomass airborne lidar carbon forest structure GEDI ground elevation |
Issue Date | 2022 |
Citation | Forests, 2022, v. 13, n. 10, article no. 1686 How to Cite? |
Abstract | Accurate estimation of forest aboveground biomass (AGB) is vital for informing ecosystem and carbon management. The Global Ecosystem Dynamics Investigation (GEDI) instrument—a new-generation spaceborne lidar system from NASA—provides the first global coverage of high-resolution 3D altimetry data aimed specifically for mapping Earth’s forests, but its performance is yet to be tested for large parts of the world. Here, our goal is to evaluate the accuracies of GEDI in measuring terrain, forest vertical structures, and AGB in reference to independent airborne lidar data over temperate and tropical forests in North America. We compared GEDI-derived elevations and canopy heights (e.g., relative height percentiles such as RH50 and RH100) with those from the Shuttle Radar Topography Mission (SRTM) or from two airborne lidar systems: the Laser Vegetation Imaging Sensor (LVIS) and Goddard’s Lidar, Hyperspectral and Thermal system (G-LiHT). We also estimated GEDI’s geolocation errors by matching GEDI waveforms and G-LiHT pseudo-waveforms. We assessed the predictive power of GEDI metrics in estimating AGB using Random Forests regression. Results showed that GEDI-derived ground elevations correlated strongly those from LVIS, G-LiHT, and LVIS (R2 > 0.91), but with nonnegligible RMSEs of 5.7 m (G-LiHT), 3.1 m (LVIS), and 10.9 m (SRTM). GEDI canopy heights had poorer correlation with LVIS (e.g., R2 = 0.44 for RH100) than with G-LiHT (e.g., R2 = 0.60 for RH100). The estimated horizontal geolocation errors of GEDI footprints averaged 6.5 meters, comparable to the nominal accuracy of 9 m. Correction for the locational errors improved the correlation of GEDI vs G-LiHT canopy heights significantly, on average by 53% (e.g., R2 from 0.57 to 0.82 for RH50). GEDI canopy metrics were useful for predicting AGB (R2 = 0.82 and RMSE = 19.1 Mg/Ha), with the maximum canopy height RH100 being the most useful predictor. Our results highlight the importance of accommodating or correcting for GEDI geolocation errors for estimating forest characteristics and provide empirical evidence on the utility of GEDI for monitoring global biomass dynamics from space. |
Persistent Identifier | http://hdl.handle.net/10722/329885 |
ISI Accession Number ID |
DC Field | Value | Language |
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dc.contributor.author | Sun, Mei | - |
dc.contributor.author | Cui, Lei | - |
dc.contributor.author | Park, Jongmin | - |
dc.contributor.author | García, Mariano | - |
dc.contributor.author | Zhou, Yuyu | - |
dc.contributor.author | Silva, Carlos Alberto | - |
dc.contributor.author | He, Long | - |
dc.contributor.author | Zhang, Hu | - |
dc.contributor.author | Zhao, Kaiguang | - |
dc.date.accessioned | 2023-08-09T03:36:03Z | - |
dc.date.available | 2023-08-09T03:36:03Z | - |
dc.date.issued | 2022 | - |
dc.identifier.citation | Forests, 2022, v. 13, n. 10, article no. 1686 | - |
dc.identifier.uri | http://hdl.handle.net/10722/329885 | - |
dc.description.abstract | Accurate estimation of forest aboveground biomass (AGB) is vital for informing ecosystem and carbon management. The Global Ecosystem Dynamics Investigation (GEDI) instrument—a new-generation spaceborne lidar system from NASA—provides the first global coverage of high-resolution 3D altimetry data aimed specifically for mapping Earth’s forests, but its performance is yet to be tested for large parts of the world. Here, our goal is to evaluate the accuracies of GEDI in measuring terrain, forest vertical structures, and AGB in reference to independent airborne lidar data over temperate and tropical forests in North America. We compared GEDI-derived elevations and canopy heights (e.g., relative height percentiles such as RH50 and RH100) with those from the Shuttle Radar Topography Mission (SRTM) or from two airborne lidar systems: the Laser Vegetation Imaging Sensor (LVIS) and Goddard’s Lidar, Hyperspectral and Thermal system (G-LiHT). We also estimated GEDI’s geolocation errors by matching GEDI waveforms and G-LiHT pseudo-waveforms. We assessed the predictive power of GEDI metrics in estimating AGB using Random Forests regression. Results showed that GEDI-derived ground elevations correlated strongly those from LVIS, G-LiHT, and LVIS (R2 > 0.91), but with nonnegligible RMSEs of 5.7 m (G-LiHT), 3.1 m (LVIS), and 10.9 m (SRTM). GEDI canopy heights had poorer correlation with LVIS (e.g., R2 = 0.44 for RH100) than with G-LiHT (e.g., R2 = 0.60 for RH100). The estimated horizontal geolocation errors of GEDI footprints averaged 6.5 meters, comparable to the nominal accuracy of 9 m. Correction for the locational errors improved the correlation of GEDI vs G-LiHT canopy heights significantly, on average by 53% (e.g., R2 from 0.57 to 0.82 for RH50). GEDI canopy metrics were useful for predicting AGB (R2 = 0.82 and RMSE = 19.1 Mg/Ha), with the maximum canopy height RH100 being the most useful predictor. Our results highlight the importance of accommodating or correcting for GEDI geolocation errors for estimating forest characteristics and provide empirical evidence on the utility of GEDI for monitoring global biomass dynamics from space. | - |
dc.language | eng | - |
dc.relation.ispartof | Forests | - |
dc.subject | aboveground biomass | - |
dc.subject | airborne lidar | - |
dc.subject | carbon | - |
dc.subject | forest structure | - |
dc.subject | GEDI | - |
dc.subject | ground elevation | - |
dc.title | Evaluation of NASA’s GEDI Lidar Observations for Estimating Biomass in Temperate and Tropical Forests | - |
dc.type | Article | - |
dc.description.nature | link_to_subscribed_fulltext | - |
dc.identifier.doi | 10.3390/f13101686 | - |
dc.identifier.scopus | eid_2-s2.0-85140729475 | - |
dc.identifier.volume | 13 | - |
dc.identifier.issue | 10 | - |
dc.identifier.spage | article no. 1686 | - |
dc.identifier.epage | article no. 1686 | - |
dc.identifier.eissn | 1999-4907 | - |
dc.identifier.isi | WOS:000873016700001 | - |