Abstract

Waveform broadening effects of large-footprint lidar caused by terrain slopes are still a great challenge limiting the estimation accuracy of forest aboveground biomass (AGB) over mountainous areas. Slope-adaptive metrics of waveforms were proposed in our previous studies. However, its validation was limited by the unavailability of enough reference data. This study made full validation of slope-adaptive metrics using data acquired by the Global Ecosystem Dynamics Investigation (GEDI) mission, meanwhile exploring GEDI waveforms on estimations of forest AGB. Three types of waveform metrics were employed, including slope-adaptive metrics (RHT), typical height metrics relative to ground peaks (RH), and waveform parameters (WP). In addition to terrain slopes, two other factors were also explored including the geolocation issue and signal start and ending points of waveforms. Results showed that footprint geolocations in the first version GEDI data products were shifted to the left forward of nominal geolocations with a distance of about 24 m~30 m and were substantially corrected in the second version; the fourth and fifth groups of signal start and ending points of waveforms had worse performance than the rest of the four groups because they used the maximum and minimum signal thresholds, respectively. Taking airborne laser scanner (ALS) data as reference, the root mean square error (RMSE) of terrain slopes extracted from the digital elevation model of the shuttle radar topography mission (SRTM DEM) was about 3°. The coefficients of determination ( R 2 ) of estimation models of forest AGB based on RH metrics were improved from 0.48 to 0.68 with RMSE decreased from 19.7 Mg/ha to 15.4 Mg/ha by the second version geolocations. The RHT and WP metrics gave the best and the worst estimation accuracy, respectively. RHT further improved R 2 to 0.77 and decreased RMSE to 13.0 Mg/ha using terrain slopes extracted from SRTM DEM with a resolution of 1 arc second. R 2 of estimation models based on RHT was finally improved to 0.8 with RMSE decreased to 11.7 Mg/ha using exact terrain slopes from ALS data. This study demonstrated the great potential of slope-adaptive metrics of GEDI waveforms on estimations of forest aboveground biomass over mountainous areas.

Highlights

  • Accurate accounting of forest carbon storage in vegetation is essential for global carbon budgets

  • In order to make full validation of slopeadaptive metrics using data acquired by the Global Ecosystem Dynamics Investigation (GEDI) mission, exploring GEDI waveforms on estimations of forest AGB, this study reports the assessment of slopeadaptive metrics of waveforms using GEDI data for estimations of forest aboveground biomass over mountainous areas

  • Three types of waveform metrics are employed in the model development, including slope-adaptive metrics (i.e., RHT), relative height metrics defined by referencing to the lowest mode of waveform (i.e., RH), and waveform parameters (i.e., WP)

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Summary

Introduction

Accurate accounting of forest carbon storage in vegetation is essential for global carbon budgets. According to the results of global carbon budgets, the imbalance item for the last decade is 0.4 GtCyr-1, which is about 26.6% of carbon emissions from land-use change [1]. The role of remote sensing in the accounting of global carbon budgets has been widely recognized, and several regional remotely sensed estimations/maps have been released [2,3,4,5]. Huge inconsistency among them was reported using multiple reference datasets [6]. These estimations still are not based on the measurement of variables determining the forest carbon storage but only a kind of combination of landcover types and representative carbon values [7]. Measurements provided by spaceborne lidar are employed, these wall-to-wall maps were mostly produced relying on multispectral reflectance and/or radar backscattering coefficients

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