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May 14, 2026Scientific Reports0 citationsOpen Access

Assessing the influence of environmental gradients on grassland aboveground biomass density estimation using GEDI and multi-source remote sensing

ELErzheng Liang

Key Points

  • This study aims to evaluate how environmental gradients affect the estimation of aboveground biomass density in grasslands using remote sensing methods.
  • Utilized GEDI L4A footprint-level AGBD as the response variable.
  • Integrated multi-source data from Sentinel-2, Sentinel-1, GLO-30 topography, and TerraClimate.
  • Developed a LASSO-screened, LightGBM-based model for robust AGBD retrieval.
  • Overall accuracy achieved an R^2 of 0.445, with RMSE at 54.62 Mg/ha and MAE at 27.90 Mg/ha.
  • Model performed best at elevations of 2000–2500 m (R^2=0.543) and slope gradients of 0–10° (R^2=0.529).
  • Higher performance noted in areas with <300 mm annual precipitation (R^2=0.476) and mean annual temperatures of 0–5°C (R^2=0.523).

Abstract

Abstract Grassland aboveground biomass density (AGBD) is a key indicator for assessing grassland carbon sinks and ecosystem functioning. With the rapid expansion of satellite observations, remote sensing has been widely applied to estimate grassland AGBD. AGBD is highly sensitive to environmental gradients such as precipitation, temperature, and topography; however, this contextual dependence remains insufficiently assessed in remote-sensing estimates. Focusing on grasslands in China’s Ili River Basin, this study uses GEDI L4A footprint-level AGBD as the response variable and integrates multi-source predictors from Sentinel-2 optical data, Sentinel-1 SAR, GLO-30 topography, and TerraClimate. A LASSO-screened, LightGBM-based model for AGBD retrieval was developed, and its robustness and feature mechanisms were evaluated across elevation, slope, precipitation, and temperature gradients. Results show an overall accuracy of R²=0. 445, RMSE = 54. 62 Mg/ha, and MAE = 27. 90 Mg/ha. Along topographic gradients, the model fits best at elevations of 2000–2500 m (R²=0. 543) and on slopes of 0–10 ^ (R²=0. 529) ; along climatic gradients, performance is higher where annual precipitation <300 mm (R²=0. 476) and is optimal at mean annual temperatures of 0–5 ^ C (R²=0. 523). SHAP interpretations indicate that optical reflectance and textures dominate in low-elevation, gentle-slope areas; where terrain is complex or precipitation is higher, the importance of optical textures and radar features increases; above 3000 m, the contribution of optical features declines markedly while texture/topography/radar contributions rise. This study provides a basis for context-aware AGBD mapping in the Ili River Basin and similar regions.

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Cite This Study

Erzheng Liang (2026) studied this question.

synapsesocial.com/papers/6a05684ea550a87e60a20b56https://doi.org/10.1038/s41598-026-51887-z
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