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Article

A Robust Framework for Bamboo Forest AGB Estimation by Integrating Geostatistical Prediction and Ensemble Learning

1
Key Laboratory for Forest Resources Conservation and Utilization in the Southwest Mountains of China, Ministry of Education, Kunming 650224, China
2
College of Soil and Water Conservation, Southwest Forestry University, Kunming 650224, China
3
College of Forestry, Southwest Forestry University, Kunming 650224, China
*
Author to whom correspondence should be addressed.
Remote Sens. 2025, 17(15), 2682; https://doi.org/10.3390/rs17152682 (registering DOI)
Submission received: 2 July 2025 / Revised: 30 July 2025 / Accepted: 30 July 2025 / Published: 3 August 2025

Abstract

Accurate above-ground biomass (AGB) quantification is confounded by signal saturation and data fusion challenges, particularly in structurally complex ecosystems like bamboo forests. To address these gaps, this study developed a two-stage framework to map the AGB of Dendrocalamus giganteus in a subtropical mountain environment. This study first employed Empirical Bayesian Kriging Regression Prediction (EBKRP) to spatialize sparse GEDI and ICESat-2 LiDAR metrics using Sentinel-2 and topographic covariates. Subsequently, a stacked ensemble model, integrating four machine learning algorithms, predicted AGB from the full suite of continuous variables. The stacking model achieved high predictive accuracy (R2 = 0.84, RMSE = 11.07 Mg ha−1) and substantially mitigated the common bias of underestimating high AGB, improving the predicted observed regression slope from a base model average of 0.63 to 0.81. Furthermore, SHAP analysis provided mechanistic insights, identifying the canopy photon rate as the dominant predictor and quantifying the ecological thresholds governing AGB distribution. The mean AGB density was 71.8 ± 21.9 Mg ha−1, with its spatial pattern influenced by elevation and human settlements. This research provides a robust framework for synergizing multi-source remote sensing data to improve AGB estimation, offering a refined methodological pathway for large-scale carbon stock assessments.

1. Introduction

Forest ecosystems cover approximately one-third of the Earth’s terrestrial surface and are integral to the global carbon budget [1]. The accurate quantification of Above-ground biomass (AGB) at broad spatial scales is essential for advancing understanding of the global carbon cycle and for formulating effective emission reduction strategies [2]. This information also underpins sustainable forest management and ecological conservation efforts [3]. As a significant and rapidly growing component of subtropical forest ecosystems, bamboo forests play a crucial role in regional carbon sequestration; thus, the accurate inversion of their AGB is vital. However, conventional methods for AGB estimation, which rely on field inventory data and allometric scaling, are constrained by high costs, logistical challenges, and limited applicability in remote or inaccessible regions [4,5].
The application of remote sensing offers a powerful alternative for large-scale AGB mapping. Although optical sensors such as Sentinel-2 can provide spatially contiguous data, their signals are prone to saturation at relatively low levels of above-ground biomass density (AGBD), a phenomenon particularly acute in optical data due to limited canopy penetration. While Synthetic Aperture Radar (SAR) systems offer improved penetration, saturation still occurs, with the point of saturation being dependent on the radar wavelength used [6]. Light Detection and Ranging (LiDAR) technology overcomes this limitation. By directly quantifying vertical forest structure, LiDAR sensors maintain sensitivity in high-biomass forests and are not susceptible to signal saturation [7]. The potential of spaceborne LiDAR is highlighted by missions such as NASA’s Global Ecosystem Dynamics Investigation (GEDI) and the Ice, Cloud, and land Elevation Satellite-2 (ICESat-2). The GEDI mission uses a full-waveform 1064 nm laser to characterize forest structure, while ICESat-2 employs photon-counting technology with its 532 nm laser to acquire high-resolution elevation data globally [8,9].
However, these spaceborne LiDAR missions possess distinct limitations. GEDI’s orbital inclination limits data acquisition to latitudes between ±51.6°, while the ICESat-2 signal can be attenuated in dense canopies [10]. Furthermore, both missions employ a sparse, along-track sampling strategy and thus cannot directly generate spatially contiguous maps. Conversely, while multispectral imagery from sensors like Sentinel-2 and Landsat offers high temporal resolution and rich spectral data [11], it lacks the ability to directly measure the vertical canopy structure that is highly correlated with biomass. Therefore, producing wall-to-wall AGBD maps from LiDAR data necessitates either a spatial interpolation of the sparse samples [12,13] or data fusion with spatially contiguous predictor variables from other remote sensing sources [14,15].
Consequently, data fusion that integrates vertical structure information from LiDAR with spectral data from optical sensors has emerged as a primary strategy for enhancing the accuracy of AGB estimation. Recent studies demonstrate the efficacy of this fusion approach. For instance, Silva et al. (2021) [16] developed empirical AGB models using simulated GEDI and ICESat-2 data in Sonoma County, USA. Elsewhere, Qi et al. (2019) [17] fused GEDI LiDAR samples with Interferometric SAR (InSAR) data to evaluate the potential for regional AGB extrapolation. Innovations in modeling algorithms have also contributed to improved estimation accuracy. Hu et al. (2016) [18] mapped global forest AGB by integrating spaceborne LiDAR with optical imagery, achieving a plot-level validation accuracy with an R2 of 0.56 and an RMSE of 87.53 Mg ha−1, and the multi-source ensemble learning framework proposed by Chen et al. (2022) [19]—which integrated LiDAR with Sentinel-2 multispectral imagery—also yielded robust results. At a regional scale, Duncanson et al. (2020) [20] established a multi-sensor collaborative inversion framework for major forest types across North America, demonstrating a viable pathway for large-scale AGB mapping.
Despite this progress, two critical limitations persist in the current body of research. Methodologically, many fusion techniques rely on simple feature concatenation, which may not fully exploit the complex, non-linear complementarities inherent in multi-source datasets [16]. Stacking generalization, an ensemble learning technique, offers a promising alternative. This approach uses base learners to process individual data sources and a meta learner to optimally combine their outputs, which has been shown to mitigate overfitting and improve AGB retrieval accuracy in topographically complex areas. From an application perspective, the majority of spaceborne LiDAR fusion research has concentrated on arboreal forests, while bamboo ecosystems—a globally significant carbon sink—have been comparatively overlooked.
As a distinct forest type, bamboo presents unique challenges for AGB estimation. The dense, monolayered canopy structure characteristic of bamboo attenuates LiDAR returns and reduces the sensitivity of optical indices by over 40% [21,22], with signals from both sensor types becoming saturated in mature stands [23]. These challenges are amplified in the mountainous bamboo forests of Xinping County, Yunnan, China, which are characterized by rugged terrain (mean slope: 24°). Here, complex topographic effects interact with rapid bamboo phenological cycles (e.g., shooting from March to May; elongation from June to September) to further compound AGB estimation uncertainty. Steep slopes can induce a broadening of the GEDI waveform and an attenuation of ICESat-2 photon density (leading to errors >30%), while topographic shadowing can obscure optical signatures corresponding to key phenological stages [24,25,26]. This confluence of factors makes the accurate AGB estimation of mountainous bamboo forests a pressing scientific challenge.
To address these challenges, this study introduces a multi-source remote sensing framework for AGB estimation based on stacking generalization. The framework employs Level 0 base models to fuse structural parameters from ICESat-2 and GEDI with temporal spectral features from Sentinel-2, thereby capturing the distinct vertical structure and phenological dynamics of bamboo forests. Subsequently, a Level 1 meta model uses ridge regression to optimally weigh and integrate the predictions from the base models. By leveraging the complementary strengths of LiDAR and optical data, this approach provides a robust and generalizable methodology for accurate AGB mapping in mountainous bamboo forests. Furthermore, to move beyond prediction and provide mechanistic insight, this study integrates the SHAP (SHapley Additive exPlanations) framework to interpret the model’s behavior, identifying key drivers and their non-linear effects on AGB. This framework not only establishes a methodological foundation for future multi-source integration studies on carbon stocks but also contributes to the construction of a local-scale Digital Earth to support sustainable forest management.

2. Materials and Methods

2.1. Study Area

The study area encompasses Xinping County, Yuxi City, Yunnan Province (23°38′15″–24°26′05″N, 101°16′30″–102°16′50″E), located at the eastern piedmont of the Ailao Mountain structural belt within the western Yunnan fold system (Figure 1). The region is characterized by deeply incised mid-mountain terrain (elevation range: 373–3119 m; mean: 1485 m) with considerable topographic relief and a surface fragmentation index of 0.68 (defined as the valley network density extracted from the ALOS DEM). Influenced by both the Indian and Pacific Ocean monsoons, the area exhibits a dry, hot valley climate, with a mean annual temperature of 19.5 °C and mean annual precipitation of 838.7 mm.
The county covers 4270.97 km2, with a forest coverage of 64.6%. Dendrocalamus giganteus forests occupy 14,620 ha, representing 5.52% of the total forested area. These bamboo forests are predominantly found on south-facing steep slopes at elevations ranging from 432 to 1964 m. Although areas with slopes ≥25° account for only 40% of the county’s total land area, they contain 45% of its bamboo forests. The bamboo forests exhibit the dense, monolayered canopy structure previously described, with a culm density of 3200–4500 stems ha−1, a mean diameter at breast height of 8–12 cm, and a canopy height of 12–18 m. The region’s complex topography and unique bamboo forest structure provide an ideal natural laboratory for evaluating multi-source remote sensing AGB retrieval models. The results of this study are therefore relevant for resource management and carbon sequestration assessments in the broader Southwest China bamboo industrial belt.

2.2. Data Collection

2.2.1. Field Data Collection and Biomass Estimation

Field data were collected in January 2024, corresponding to the dormant period for bamboo when the leaf area index is most stable. A stratified random sampling design was employed, guided by the 2023 “one map” forest resource management database from the Yunnan Provincial Forestry Survey and Planning Institute. Initially, 80 pure D. giganteus sub-compartments were selected across representative elevation (422–2100 m) and slope (<15°, 15–25°, and >25°) gradients. Following field reconnaissance to exclude sites with recent human disturbance (e.g., harvesting, pest damage) or accessibility constraints, a final set of 52 sample plots was established (Figure 1), satisfying minimum sample size requirements for statistical analysis.
Each sample plot was a circular area of 490.87 m2 (12.5 m radius). The central coordinate of each plot was recorded using a Qianxun StarMatrix SR3 Pro receiver (WGS84 datum), with post-processing differential correction applied to ensure a horizontal positional accuracy of <0.5 m. Within each plot, the diameter at breast height (DBH, 1.3 m) was measured for all standing bamboo culms with a DBH ≥ 5 cm. Measurements were taken twice in perpendicular directions using a diameter tape, and the mean value was recorded. Quality control was performed by re-measuring 10% of the plots, which confirmed a high level of consistency for DBH measurements (Intraclass Correlation Coefficient, ICC = 0.98). The AGB for each individual culm was calculated using the species-specific allometric equation for D. giganteus developed by Fu et al. (2012) [27]. Plot-level AGB was then determined by summing the biomass of all individual culms within the plot and scaling the total to a per-hectare value (Mg ha−1). A summary of the plot-level AGB statistics is provided in Table 1.
M = 0.8903 D 1.5505 R = 0.9885 ,   R M S E = 0.2354   k g
where M is in kg and D is the DBH (cm). Plot-scale AGB was calculated by summing the biomass of all individual culms and then converted to per-hectare values (Mg ha−1).

2.2.2. ICESat-2 Data

This study utilized the ICESat-2 ATL08 Land and Vegetation Height product (Version 6) and the GEDI L2B Canopy Cover and Vertical Profile product (Version 2), both released in 2023 (Table 2). The data acquired between October 2023 and May 2024 were selected to ensure temporal correspondence with the field survey’s phenological window.
The ICESat-2 satellite, launched in 2018, is equipped with the Advanced Topographic Laser Altimeter System (ATLAS) [28,29]. The ATLAS operates using three pairs of laser beams (six beams total) arranged with ~3.3 km spacing between pairs and ~90 m spacing within each pair. Each pair consists of a strong and a weak beam, with the strong beam having approximately four times the energy of the weak beam [30]. The system produces footprints with a diameter of ~17 m and an along-track spacing of ~0.7 m [31]. The fundamental data product, ATL03, provides geolocated photon data, including height, coordinates, and signal classification for each laser pulse. The ATL08 product is a higher-level derivative of ATL03, where photons are algorithmically classified (e.g., noise, ground, canopy) and aggregated into 100 m along-track segments to produce terrain and canopy height statistics [32].
To ensure the reliability of derived land surface parameters, the ATL08 data underwent a systematic quality filtering and preprocessing workflow. Since the ICESat-2 sensor is a Photon Counting LiDAR (PCL) system sensitive to atmospheric and solar background noise, a rigorous denoising procedure is essential [9]. First, the Differential, Regressive, and Gaussian Adaptive Nearest Neighbor (DRAGANN) algorithm was applied to the photon point cloud histograms to identify and filter out noise photons [9,30,33]. Following this primary denoising, segments were further assessed for quality. Segments containing fewer than 50 resulting signal photons were discarded, as this low signal density is insufficient to accurately represent land cover characteristics. Additionally, segments with a mean canopy height exceeding 50 m or below 2 m were excluded as outliers. After this comprehensive quality control process, 19 parameters describing terrain, canopy height metrics, and laser beam characteristics were extracted from the filtered ATL08 segments for subsequent modeling. A complete list of these parameters is provided in Supplementary Table S1.

2.2.3. GEDI Data

The GEDI mission, operating from the International Space Station (ISS) since its launch in 2018, was the first spaceborne LiDAR system developed specifically for forest structure observation [8,34]. Its primary objective is the high-precision mapping of AGB and 3D structure in global temperate and tropical forests (latitudes ±51.6°). Unlike the photon-counting system of ICESat-2, GEDI employs a full-waveform LiDAR instrument that digitizes the complete vertical distribution of intercepted surfaces, enabling a more detailed characterization of the canopy profile [35]. The instrument uses three 1064 nm lasers, which are dithered to produce eight parallel ground tracks. This strategy results in a total swath width of ~4.2 km, with ~600 m spacing between tracks. Each laser produces a ~25 m footprint with an along-track sampling interval of ~60 m [36].
The GEDI data are provided in a hierarchy of products from Level 1 (georeferenced waveforms) to Level 4 (gridded AGB). This study utilized the L2B product, which provides key metrics describing canopy cover, the plant area index, and the vertical foliage profile, all of which are critical for detailed structural analysis [34]. To ensure temporal correspondence with our field survey, the GEDI data acquired between October 2023 and May 2024 were used. The L2B data covering the study area were acquired from NASA’s Earthdata portal (https://search.earthdata.nasa.gov/ (accessed on 29 July 2025)), comprising 46 orbits. To ensure the quality of the GEDI data, a systematic filtering protocol was applied to the L2B footprints to remove low-quality returns resulting from cloud cover, atmospheric scattering, sensor noise, or complex terrain, based on established methods [37,38,39]. The specific quality flags and thresholds used are detailed in Table 3. From an initial dataset of 70,619 footprints acquired over the study area, this filtering process yielded 55,649 high-quality footprints suitable for analysis. A sensitivity analysis confirmed that the selected sensitivity ≥ 0.90 threshold provides the optimal balance between data quality and model performance (see Supplementary Materials, Table S3 and Figure S1). For these footprints, 21 candidate variables were extracted for modeling, including terrain factors, canopy height metrics, and relative height (RH) percentiles (see Supplementary Table S2).

2.2.4. Optical and Topographic Predictor Variables

To enable the spatial extrapolation of the sparse LiDAR measurements, a suite of spatially contiguous predictor variables was generated from Sentinel-2 imagery and a digital elevation model (DEM). The Sentinel-2 mission is particularly well suited for this purpose as its multispectral instrument includes red-edge bands (e.g., B5, B6, B7), which are highly sensitive to vegetation chlorophyll content and canopy structure. Level 2A surface reflectance products from May 2023 to January 2024 with cloud cover ≤5% were acquired via the Google Earth Engine platform. To mitigate the effects of seasonal phenological variation and cloud contamination, a cloud-free median composite was generated using all available images from the peak growing season (June–September 2023). Cloud masking was performed using the QA60 quality assessment band.
Topographic variables (elevation, slope, and aspect) were derived from the ALOS DEM (12.5 m resolution), which was resampled to a 25 m resolution to align with the scale of the GEDI footprints. From the processed Sentinel-2 imagery, nine vegetation indices were calculated, including the Normalized Difference Vegetation Index (NDVI), Enhanced Vegetation Index (EVI), and Soil-Adjusted Vegetation Index (SAVI) (see Table 4 for a complete list). All predictor variables were co-registered and resampled to a common 25 m grid.

2.3. Research Methods

The analytical framework for this study involved a two-stage process to upscale the field-measured plot AGB to a continuous map for the entire study area (Figure 2). The first stage involved the spatial extrapolation of key structural metrics derived from the sparse ICESat-2 and GEDI footprints. This was achieved by modeling the relationship between the LiDAR metrics and the spatially contiguous auxiliary variables to generate continuous 25 m resolution maps of these structural parameters. In the second stage, a two-level stacked ensemble model was developed to estimate AGB. This model used the field-measured plot AGB (Mg ha−1) as the response variable and the full suite of continuous predictor variables (i.e., the extrapolated LiDAR metrics and the original optical and topographic layers) as inputs. The trained model was then applied to this suite of predictor variables to generate the final, wall-to-wall AGB map for the study area.

2.3.1. Spatial Extrapolation of LiDAR Metrics

Empirical Bayesian Kriging Regression Prediction (EBKRP) was the geostatistical spatial prediction method used to generate the spatially continuous layers of LiDAR-derived structural metrics [49]. EBKRP integrates least-squares regression with kriging, and unlike conventional kriging techniques, it accounts for the uncertainty in the estimated semivariogram by simulating many possible semivariograms from the input data, resulting in more accurate predictions.
The EBKRP process was implemented in ArcGIS Pro 2.8. For each selected LiDAR metric (from GEDI and ICESat-2), a separate model was built using the LiDAR metric values at the footprint locations as the dependent variable and the co-located optical and topographic variables as independent predictors. Key parameters for the EBKRP models included an empirical data transformation, a K-Bessel variogram model, a subset size of 100, and 500 simulation iterations. To account for spatial autocorrelation anisotropy induced by the complex terrain, semivariogram ellipses were visualized to optimize the search neighborhood parameters. The performance of each model was evaluated using Leave-One-Out Cross-Validation (LOOCV). This procedure yielded continuous 25 m resolution raster layers for each key LiDAR structural metric, which served as essential predictor variables in the final AGB model. To assess the accuracy of the EBKRP spatial prediction, several statistical metrics were calculated. The defining equations for each evaluation indicator are as follows:
R 2 =   i = 1 n Z ^ ( x i ) Z ¯ ( x i ) 2 i = 1 N Z ( x i ) Z ¯ ( x i ) 2
R M S E = i = 1 n Z ( x i ) Z ^ ( x i ) 2 n
C R P S ( A , F ) = F ( x ) 1 { x y } 2 d x
where Z ^ ( x i ) is the predicted value at location x i , Z ( x i ) is the observed value at location x i , Z ¯ ( x i ) is the mean of the observed values, and n is the total number of samples. For the Continuous Ranked Probability Score (CRPS), F represents the predicted cumulative distribution function (CDF) from the model, while y represents the true observed value. The term 1 x y is an indicator function, which equals 1 if the condition is met and 0 otherwise.

2.3.2. AGB Estimation Using Stacked Ensemble Modeling

Given the complex, non-linear relationships between topographic and vegetation features in the study area, non-parametric machine learning models are particularly suitable for AGB estimation due to their robust fitting capabilities [50,51,52]. This study therefore selected four widely used machine learning algorithms to serve as base learners within a stacked ensemble framework to estimate bamboo forest AGB.
Base Learner Algorithms
The k-Nearest Neighbor (kNN) algorithm operates by identifying the k samples most similar to a target plot based on a distance metric and then imputes the value for the target plot using a prediction rule applied to these neighbors [53]. The algorithm’s flexibility, stemming from the fact that it does not assume an underlying normal distribution, has led to its wide application in forest parameter estimation. The choice of distance metric, the value of k, and the prediction rule significantly influence the results [54]. In this study, we employed Euclidean distance and an inverse-distance weighting method. The value of k was optimized by searching a range from 1 to 50, with the final value selected via cross-validation. The prediction formula is as follows:
y ^ x q = i = 1 k w i · y i i = 1 k w i
where y ^ is the predicted value for the target plot, y i is the observed value of the i -th nearest neighbor, and w i is the weight of the i -th neighbor, calculated as the inverse of the distance w i = 1 / d i .
Support Vector Machines (SVMs) are known to perform well, even when dealing with a limited number of samples. The core principle of an SVM is to map input data into a higher-dimensional feature space using a non-linear kernel function. This allows the model to address non-linear relationships, effectively reducing both model error and complexity [55,56]. We implemented the SVM model using Python (Version 3.8) and its “scikit-learn” library (Version 1.3.2) and compared the performance of three kernel types: Radial Basis Function (RBF), polynomial, and linear. The penalty coefficient (C) and the kernel parameter (gamma) were optimized via grid search (GridSearchCV) to identify the best parameter combination. The regression function is as follows:
f x = i = 1 N α i α i * K x i , x + b
where α i and α i * are the Lagrange multipliers, b is the bias term, and K x i , x is the kernel function.
Random Forest (RF), a classic ensemble learning method, enhances model generalization and stability by constructing a multitude of decision trees and averaging their predictions [57]. The algorithm incorporates two levels of randomness during training—the bootstrapping of data samples and random selection of features at each split—which effectively mitigates the risk of overfitting. RF is also robust to outliers and provides feature importance scores, offering a valuable basis for variable selection. We developed the optimal RF model by tuning key hyperparameters, including the number of trees (n_estimators), maximum tree depth (max_depth), and the minimum number of samples required at a leaf node (min_samples_leaf). Its regression prediction formula is as follows:
f ^ x = 1 K K = 1 K k x
where K is the total number of trees, and k(x) represents the prediction for sample x from the k-th tree.
XGBoost (eExtreme Gradient Boosting) is an advanced ensemble learning algorithm built upon the Gradient Boosting Decision Tree (GBDT) framework. The algorithm iteratively builds a sequence of decision trees, with each new tree trained to correct the residual errors of the one before it [58]. This progressive optimization strategy significantly enhances prediction accuracy. Key advantages of XGBoost include its built-in regularization mechanism, which effectively controls overfitting, and its outstanding computational efficiency, leading to exceptional performance in a wide range of regression tasks. We implemented the model using the xgboost library in Python and systematically optimized its key hyperparameters—including the number of estimators (n_estimators), maximum tree depth (max_depth), and learning rate—via grid search (GridSearchCV). Its prediction model can be represented by the following formula:
y ^ i = k = 1 k f k x i
where y ^ i is the final prediction for sample i , k is the total number of trees, and f k represents the k -th decision tree model.
Stacking Ensemble Method
The stacking algorithm significantly enhances the accuracy of AGB estimation in complex habitats by integrating the predictive strengths of multiple base models [59]. We developed a two-level stacking architecture (Figure 2). Level 0 comprises four base learners: XGBoost, the SVM, the kNN, and RF. Level 1 employs Ridge Regression as a meta learner, which performs a weighted fusion of the base learners’ outputs to produce the final prediction.
To prevent data leakage during the meta-feature generation stage and to robustly leverage the available sample size (N = 52), a Leave-One-Out Cross-Validation (LOOCV) strategy was applied. In this procedure, an iterative process is performed where for each sample, the base models are trained on all other samples and then used to generate a prediction for that single held-out sample. This yielded a complete set of Out-of-Fold (OOF) predictions, which were then assembled to form an n × 4 meta-feature matrix (where n is the total sample size and 4 is the number of base learners). For the meta model training stage, the Level-1 Ridge Regression model was trained using this complete meta-feature matrix as its input and the field-measured AGB as the target variable. This model constrains regression coefficients via L2 regularization to control complexity and enhance generalization.

2.3.3. Model Performance Assessment

Model performance was evaluated using the LOOCV method. To compare predictive capabilities, each base learner was assessed alongside the final stacking model using three quantitative metrics: the coefficient of determination (R2), root mean square error (RMSE), and mean absolute error (MAE). The formulas are as follows:
R 2 =   1 i = 1 n y i     y ^ i 2 i = 1 n y i     y ¯ 2
R M S E = 1 n i = 1 n y i y ^ i 2
M A E = 1 n i = 1 n y i     y ^ i
In these formulas, y i is the observed value for the i -th sample, y ^ i is the predicted value for the i -th sample, y ¯ is the mean of the observed values, and n is the total number of samples.

2.3.4. SHAP-Based Model Interpretability

To move beyond assessing model performance and gain insight into the ecological mechanisms driving AGB distribution, this study employed SHAP, a method for interpreting complex machine learning model outputs [60]. Grounded in cooperative game theory, SHAP assigns a Shapley value to each feature for every prediction. This value quantifies the feature’s marginal contribution to shifting the model’s output from a baseline (the mean prediction across the dataset) to the final predicted value. The SHAP framework operates on the principle of additive feature attribution, wherein the explanation is a linear function of binary variables:
g z = 0 + i = 1 M i z i
where g is the explanation model, z ∈ {0, 1} M is the simplified input representing feature presence or absence, M is the number of input features, and i   R is the Shapley value for feature i .
For this analysis, SHAP was applied to the Random Forest model, selected for its high performance among the tree-based learners and its compatibility with the efficient TreeExplainer algorithm. Two primary SHAP visualizations were generated: (1) the summary plot, which aggregates absolute Shapley values to rank global feature importance, illustrating the direction and distribution of impacts, and (2) dependence plots, which reveal the effect of a single feature on model predictions across all data points, uncovering non-linear relationships and interaction effects. This application of SHAP transformed the model from a predictive “black box” into an interpretable tool, providing a quantitative foundation for the ecological discussion and management recommendations.

3. Results

3.1. Accuracy of Spatially Extrapolated LiDAR Metrics

The spatial extrapolation of 39 structural metrics derived from GEDI and ICESat-2 using the EBKRP method revealed a clear hierarchy in prediction accuracy (Figure 3). The cross-validation results indicated that R2 values ranged from 0.12 to 1.00, while RMSE and CRPS varied substantially depending on the parameter’s scale, units, and intrinsic spatial variability (see Supplementary Materials).
The accuracy of the spatial prediction was stratified by parameter type. The first tier, comprising parameters related to topography and macro-canopy structure, exhibited the highest spatial continuity and thus the highest prediction accuracy. Specifically, elevation (dem_h) and seven related canopy height metrics demonstrated exceptionally strong spatial autocorrelation (R2 ≥ 0.96), as did the signal-to-noise ratio (snr). A second tier of parameters, representing internal canopy structure and laser return energy, yielded moderate accuracies. This group included energy-related variables such as the asr and rx_energy series (R2 = 0.64–0.66) and other structural metrics like n_seg_ph and h_mean_canopy (R2 = 0.52–0.60). Conversely, the third tier of parameters, which describe fine-scale canopy details, discrete photon counts, and surface reflectance properties, showed the lowest prediction accuracies. Variables such as h_min_canopy, n_toc_photons, and the reflectance-related rv and rg series had R2 values concentrated between 0.26 and 0.47. This result reflects the higher local variance and spatial randomness characteristic of these fine-scale metrics.
A spatial correlation analysis was conducted to test the influence of terrain on the prediction errors of these fine-scale parameters. The analysis found a very weak correlation between error and slope (Pearson’s r = 0.099, p < 0.001), indicating that terrain effects are not a primary driver of the prediction error for these parameters (see Supplementary Materials, Figure S2).
These findings indicate that a parameter’s susceptibility to accurate spatial prediction is strongly linked to its inherent spatial structure. Parameters with high spatial continuity (e.g., topography) were predicted with the greatest accuracy, whereas those with high local variability (e.g., photon counts) were predicted with the lowest accuracy. The strong performance of the EBKRP method for variables with distinct spatial patterns underscores its ability to effectively leverage spatially explicit predictor variables, such as terrain, during the spatial prediction process.

3.2. Feature Importance and Selection for AGB Modeling

The relative importance of the 52 predictor variables in the AGB model, as determined by SHAP values, is shown in Figure 4a. The canopy photon rate (photon_rate_can) emerged as the most influential variable (SHAP value = 5.36), followed by elevation (dem_h, SHAP value = 1.86), a ground-related parameter (rg_sg, SHAP value = 1.64), and a reflectance-related parameter (rv_a4, SHAP value = 1.44). The remaining variables, including those describing vertical canopy structure, laser return energy, and waveform geometry, contributed with progressively lower SHAP values.
To identify the optimal number of variables for the final model, a recursive feature elimination (RFE) process was conducted (Figure 4b). Models were iteratively built by adding variables one by one based on their SHAP importance ranking, and the model performance was assessed at each step. This analysis revealed that model accuracy plateaued after 14 features were included.
Based on these results, the top 14 most important features were selected as the optimal set of predictor variables. This approach balances model performance and parsimony by excluding variables that contribute little explanatory power and could introduce noise or increase computational complexity.

3.3. AGB Model Performance

The validation results for the AGB models demonstrate that the stacking ensemble model significantly outperformed all individual base learners across all evaluation metrics (Table 5, Figure 5). The stacking model achieved an R2 of 0.84, an RMSE of 11.07 Mg ha−1, and an MAE of 8.69 Mg ha−1. Furthermore, the regression fit line for the stacking model’s predictions (y = 0.81x + 12.91) showed strong agreement with the 1:1 reference line, indicating high accuracy and low systematic bias across the full range of AGB values.
Among the four base learners, RF yielded the best performance (R2 = 0.72, RMSE = 14.53 Mg ha−1), followed by the SVM (R2 = 0.69, RMSE = 15.32 Mg ha−1) and XGBoost (R2 = 0.68, RMSE = 15.58 Mg ha−1). The kNN model performed the poorest (R2 = 0.60, RMSE = 17.35 Mg ha−1), reflecting its inherent limitations in capturing the complex, non-linear relationships between the multi-source remote sensing features and AGB in this heterogeneous landscape.
A notable pattern observed in the scatterplots of predicted versus observed values was that all base learners exhibited a similar systematic bias (Figure 5a–d). The slopes of their regression lines were considerably less than 1, indicating a tendency to underestimate high AGB values and overestimate low AGB values. This bias is likely attributable to factors including the limited number of field plots in high-biomass stands and the known propensity for LiDAR signal saturation in dense bamboo canopies. The stacking model, through its two-level learning architecture, effectively integrated the predictive strengths of the diverse base learners and, in doing so, substantially corrected for this systematic bias, which enhanced both its overall accuracy and robustness.

3.4. Mapping and Analysis of D. giganteus AGB

The optimized stacking model was applied to the full suite of predictor variables to generate a continuous AGB map for the 14,620 ha of D. giganteus forest within Xinping County (Figure 6). The mean AGB density for the bamboo forests across the study area was predicted to be 71.8 ± 21.9 Mg ha−1 (mean ± standard deviation), with densities ranging from 10.0 to 135.0 Mg ha−1.
The resulting map reveals significant spatial heterogeneity and distinct patterns of geographic clustering. AGB density was systematically higher in the central–western and northern portions of the county (e.g., Jiasa Town, Laochang Township, Shuitang Town) compared to the eastern and southern regions (e.g., Guishan Street, Pingdian Township, Jianxing Township). An analysis of the AGB frequency distribution shows that the majority of the bamboo forest area (57.4%, or 84.46 km2) falls within a medium-to-high AGB range (64.0–93.0 Mg ha−1). Conversely, areas of very high AGB (>93.0 Mg ha−1) and low AGB (<48.0 Mg ha−1) were less common, accounting for 10.7% and 9.9% of the bamboo forest area, respectively. Spatially, the highest AGB values were concentrated in distinct patches, potentially corresponding to areas with optimal site conditions or intensive management, while the lowest AGB values were typically found in more marginal areas.
Overall, the spatial distribution of D. giganteus AGB in Xinping County is not random but appears to be regulated by a combination of environmental gradients and land management practices, the specific drivers of which will be explored in the discussion.

4. Discussion

4.1. Analysis of Spatial Heterogeneity in EBKRP Results

The stratified prediction accuracies exhibited by the various LiDAR-derived parameters following EBKRP spatial prediction reveal the fundamental relationship between a parameter’s intrinsic spatial structure and the model’s underlying geostatistical assumptions. For parameters related to topography and macro-canopy height (e.g., dem_h), the model achieved an almost perfect fit (R2 = 1.00). This aligns with the findings of (Borselli et al. 2008) [61], confirming that terrain-related variables possess high spatial continuity. This high R2 value, however, is likely less an indicator of the model’s independent predictive power and more a reflection of its ability to replicate a spatial pattern that is strongly driven by the covariates. When significant informational overlap exists between the target and predictor variables, the model effectively learns a deterministic spatial pattern. Consequently, while this result validates the efficacy of the method, the risk of overfitting due to covariate collinearity must be considered.
In contrast, parameters describing laser pulse energy (e.g., the rx_energy series) and certain canopy structure metrics (e.g., n_seg_ph) only achieved moderate prediction accuracies (R2 = 0.51–0.73). This outcome reflects the limitations of EBKRP when encountering complex, non-linear spatial structures. As noted by Tian et al. (2021) [62], LiDAR signal interaction with the canopy is governed by a non-linear combination of biophysical factors, resulting in complex spatial patterns that cannot be fully captured by the smooth semivariogram functions inherent to traditional kriging frameworks. Although EBKRP improves upon traditional methods by incorporating a Bayesian strategy and local subsets, it is still fundamentally based on Gaussian process assumptions and is therefore limited in its ability to model highly heterogeneous or complex distributions.
The poor predictive accuracy for variables with the lowest prediction accuracy, such as h_min_canopy and n_toc_photons, stems from a mismatch in spatial scale and a conflict between the data type (i.e., discrete counts) and the model’s fundamental assumption of a continuous Gaussian field. The spatial variation in fine-scale variables like h_min_canopy is controlled by small-scale factors such as understory vegetation and microtopography [63]. This fine-scale variation occurs at a spatial grain much smaller than the resolution of the covariates, preventing the model from capturing it effectively. Furthermore, variables like n_toc_photons represent discrete count data, whereas EBKRP is built on the theoretical framework of a continuous Gaussian random field. As Zhao et al. (2006) [64] emphasized, applying a continuous-field model directly to discrete count data violates the model’s fundamental assumptions and can lead to systematic bias.
In summary, the performance of EBKRP for spatially predicting LiDAR metrics is highly dependent on the metric’s intrinsic spatial structure, its scale relative to the predictor variables, and its data type. While the model excels at processing macro-scale variables with strong spatial continuity, its suitability for applications involving high spatial frequency, strong non-linearity, or data type mismatches requires careful assessment.

4.2. Influence of Algorithm Selection on Bamboo AGB Estimation

The systematic evaluation of multiple machine learning algorithms underscores the critical influence of model choice on AGB estimation accuracy. The superior performance of the stacking model (R2 = 0.84, RMSE = 11.07 Mg ha−1) surpasses that of the individual base learners and is competitive with results from the recent literature that used single models for other bamboo forest types [65,66]. The strength of this approach lies in its two-level architecture: the diverse base learners capture different aspects of the predictor–response relationship, while the meta learner optimally weighs their individual predictions. This process effectively balances the bias–variance trade-off, which markedly mitigated the underestimation of high AGB values (>78 Mg ha−1) observed in the base models and improved the average regression slope from 0.54 to 0.81.
Among the individual algorithms, while RF performed best in terms of R2, its low regression slope (0.53) also highlighted its limitations. This underestimation is likely related to LiDAR signal saturation, a known issue in dense canopies such as the D. giganteus forests in our study area [67,68,69]. Although XGBoost and the SVM yielded similar R2 values, the lower MAE of the SVM model suggests that its principle of structural risk minimization provided greater robustness against outliers in the dataset [36]. In contrast, the poor performance of the kNN model, given the limited sample size (n = 52), is likely attributable to the ‘curse of dimensionality’, where the local structure of the high-dimensional feature space becomes sparse [70].
Although the proposed framework of fusing multisource remote sensing data within a stacked ensemble model significantly improved estimation accuracy, some systematic bias was not entirely eliminated. Future work could focus on two key areas. First, incorporating a wider array of ancillary eco-environmental factors (e.g., fine-resolution soil and climate data) may improve model performance in complex terrain and high-biomass areas. Second, while SHAP analysis provided valuable insights into feature importance and model behavior, a further exploration of advanced interpretability techniques could enhance our mechanistic understanding of the relationships between remote sensing variables and biomass distribution, enabling more targeted model optimization.
The proposed framework is also applicable to other bamboo species that present similar remote sensing challenges, such as dense canopies and signal saturation. Our approach, which fuses LiDAR structural data with optical spectral data in a stacking ensemble, is designed to overcome these common issues. While calibration with species-specific allometric equations would be necessary, the framework provides a robust and generalizable pathway for improving AGB estimation across diverse bamboo ecosystems.

4.3. Ecological Interpretation and Management Implications

The spatial distribution of AGB in D. giganteus stands within Xinping County, Yunnan, is governed by a complex interplay of ecological and anthropogenic factors (Figure 6). By integrating model feature importance with SHAP value analysis, this study identified primary AGB drivers and uncovered their non-linear response mechanisms and critical thresholds, providing a data-driven foundation for interpreting its distribution mechanisms.

4.3.1. Ecological Drivers and Non-Linear Mechanisms

Ecologically, the high importance of the LiDAR-derived canopy photon rate (photon_rate_can) reflects the strong relationship between LiDAR-derived metrics and the unique canopy architecture of this bamboo species. As a large sympodial bamboo, D. giganteus has a high LAI (6.8 ± 1.2), where its dense canopy markedly intensifies photon scattering. The SHAP summary plot (Figure 7) quantifies this relationship, showing a consistent positive correlation between photon_rate_can and predicted AGB. This confirms that LiDAR-based canopy return metrics are reliable proxies for AGB.
The SHAP dependence plot for photon_rate_can reveals a clear threshold around 0.92. Below this value, the variable predominantly contributes negatively to AGB predictions; above this threshold, its contribution to the model output shifts to strongly positive, indicating that high canopy reflectance is a salient characteristic of high-biomass stands. The significant positive effect of the vegetation return energy (rv_a4) corroborates this finding. These variables collectively underscore the primary role of canopy structure in regulating AGB.
Topographic factors also significantly influence the ecological regulation of AGB. Both elevation (dem_h) and the height above the best-fit terrain (h_te_best_fit) exhibit high SHAP contributions. GIS overlay analysis shows that approximately 73% of high-AGB areas (>78 Mg ha−1) are concentrated in zones with 800–1300 m elevation, <20° slope, and >1200 mm annual precipitation. This significant spatial variation in precipitation is a result of the region’s orographic effect, with mid-to-high elevation windward slopes receiving substantially more rainfall (>1200 mm) than the county average (838.7 mm). The SHAP dependence plot provides finer-grained detail: AGB accumulation is most pronounced for dem_h values 840 m, and h_te_best_fit positively influences AGB accumulation below 1164.11 m. This indicates that topography indirectly shapes biomass distribution by influencing local microclimates and moisture availability [71,72].

4.3.2. Anthropogenic Influences and Implications for Precision Management

Anthropogenic activities markedly affect AGB patterns. The spatial association between exceptionally high-AGB areas (>93 Mg ha−1) and villages suggests that intensive management, including fertilization and irrigation, enhances biomass accumulation by cultivating healthier canopies and elevating photon_rate_can values. Our model successfully captured this coupled human–natural system; future research could integrate socioeconomic variables, such as management intensity and land-use history, for a more profound mechanistic understanding.
Based on these driving mechanisms and SHAP-derived thresholds, this study proposes differentiated management strategies. First, high-potential stands meeting critical thresholds (e.g., photon_rate_can > 0.92 and h_te_best_fit < 1164.11 m) should be delineated as priority carbon sink conservation zones, where long-term carbon stock stability is ensured through strict harvesting intensity controls (e.g., annual felling rate < 10%). Second, for stands with medium-to-low productivity, the primary management objective is to enhance canopy vigor to surpass the 0.92 photon_rate_can threshold. Specific measures include density regulation (>3200 culms/ha) and soil amendment (adjusting pH to 5.5–6.5) to synergistically boost stand productivity. Last, harvesting strategies should be adaptively tailored to stand conditions. Strip thinning is advised for high-AGB zones to preserve stand structure, whereas medium-to-low AGB zones could implement selective cutting with a shorter rotation cycle (6–8 years), leveraging topographic thresholds such as h_te_best_fit < 1164.11 m to optimize resource turnover.
In conclusion, by utilizing the interpretable machine learning framework of SHAP, this study translates complex model outputs into ecologically significant response thresholds, providing a practical framework for advancing the data-driven adaptive management of bamboo forests. LiDAR-derived metrics, exemplified by photon_rate_can, can serve as critical inputs for stand health monitoring and precision interventions, thereby enhancing ecosystem service functions while helping to achieve sustainable forestry objectives.

5. Conclusions

This study successfully developed and validated a multi-stage modeling framework combining EBKRP and stacking. This framework effectively addresses the challenge of the high-accuracy spatial mapping of AGB for the large clumping bamboo species D. giganteus in complex subtropical mountainous environments.
The framework’s core contribution is its use of the EBKRP method to fuse and spatialize discrete structural parameters from GEDI and ICESat-2 with continuous spectral and topographic factors from Sentinel-2, thereby providing high-quality predictor variables for subsequent modeling. Building on this foundation, the developed Stacking model demonstrated excellent predictive performance (R2 = 0.84, RMSE = 11.07 Mg ha−1). Its accuracy was significantly superior to all individual base learners. More critically, it effectively corrected the systematic underestimation in high-biomass regions—a common issue in traditional models—by using a meta learner, which improved the regression slope of the predicted-versus-observed fit line from a base model average of 0.54 to 0.81, while SHAP analysis enhanced model interpretability by quantifying feature contributions and identifying critical ecological thresholds for precision silviculture.
This research demonstrates that the integrated framework provides a robust, high-accuracy technical pathway for the refined assessment of regional-scale bamboo carbon stocks. Furthermore, it offers a methodologically generalizable reference for estimating biomass via remote sensing in other structurally complex forest types. Future research could focus on integrating a wider array of eco-environmental factors to further enhance model accuracy and exploring advanced interpretable AI to deepen the mechanistic understanding of AGB drivers.

Supplementary Materials

The following supporting information can be downloaded at https://www.mdpi.com/article/10.3390/rs17152682/s1: Figure S1: Impact of GEDI sensitivity threshold on AGB estimation model performance; Figure S2: Results of the spatial correlation analysis between terrain slope and the EBKRP model’s prediction error for a representative low-precision parameter (e.g., h_min_canopy); Table S1: Description of ICESat-2 ATL08 parameters used for modeling and analysis; Table S2: Description of GEDI L2B parameters used for modeling and analysis; Table S3: Data retention rates and corresponding AGB model performance for different GEDI sensitivity thresholds.

Author Contributions

Conceptualization, Q.S.; Methodology, L.F. and Q.S.; Software, L.F. and Q.S.; Validation, L.F., Q.S., H.H. and S.M.; Formal Analysis, L.F. and Q.S.; Investigation, L.F., Q.S., H.H., Z.L. (Zhengying Li), S.M., C.Q., R.W., Q.X., X.Z., Y.Z. and H.C.; Resources, Q.S.; Data Curation, Q.S., L.F. and Z.L. (Zhengying Li); Writing—Original Draft Preparation, L.F.; Writing—Review and Editing, L.F., Q.S., C.X., Z.L. (Zeyu Li), H.H., Z.L. (Zhengying Li), S.M., C.Q., R.W., Q.X., X.Z., Y.Z. and H.C.; Visualization, Q.S.; Supervision, Q.S., C.X. and Z.L. (Zeyu Li); Project Administration, L.F. and Q.S.; Funding Acquisition, Q.S. All authors have read and agreed to the published version of the manuscript.

Funding

This work was supported by the National Natural Science Foundation of China under Grant 31860205; the Joint Agricultural Project of Yunnan Province under Grant 202301BD070001-002; and the Forestry Discipline and Key Laboratory Open Fund Project under Grant LXXK-2025D1.

Data Availability Statement

The GEDI and ICESat-2 data used in this study are publicly available through NASA’s Earthdata portal (https://search.earthdata.nasa.gov/ (accessed on 29 July 2025)). The Sentinel-2 imagery was accessed via the Google Earth Engine platform (https://earthengine.google.com/ (accessed on 29 July 2025)), and the ALOS World 3D DEM is available from the Japan Aerospace Exploration Agency at https://www.eorc.jaxa.jp/ALOS/en/dataset/aw3d30/aw3d30_e.htm (accessed on 29 July 2025). The field plot data collected for this research are available from the corresponding author on reasonable request.

Acknowledgments

The authors would like to thank the U.S. National Aeronautics and Space Administration (NASA) for providing the GEDI and ICESat-2 data, the European Space Agency (ESA) for the Sentinel-2 imagery, and the Japan Aerospace Exploration Agency (JAXA) for the ALOS World 3D DEM data. We also acknowledge the Google Earth Engine platform for its powerful data processing capabilities that facilitated this research.

Conflicts of Interest

The authors declare no conflicts of interest.

Abbreviations

The following abbreviations are used in this manuscript:
AGBAbove-Ground Biomass
AGBDAbove-Ground Biomass Density
ATLASAdvanced Topographic Laser Altimeter System
CDFCumulative Distribution Function
CRPSContinuous Ranked Probability Score
DBHDiameter at Breast Height
DEMDigital Elevation Model
DRAGANNDifferential, Regressive, and Gaussian Adaptive Nearest Neighbor
DVI Difference Vegetation Index
EBKRPEmpirical Bayesian Kriging Regression Prediction
ESAEuropean Space Agency
EVIEnhanced Vegetation Index
GBDTGradient Boosting Decision Tree
GDVIGreen Difference Vegetation Index
GEDIGlobal Ecosystem Dynamics Investigation
GNDVIGreen Normalized Difference Vegetation Index
GRVIGreen Ratio Vegetation Index
ICCIntraclass Correlation Coefficient
ICESat-2Ice, Cloud, and land Elevation Satellite-2
InSARInterferometric SAR
ISSInternational Space Station
kNNk-Nearest Neighbor
LAILeaf Area Index
LiDARLight Detection and Ranging
LOOCVLeave-One-Out Cross-Validation
MAEMean Absolute Error
NASANational Aeronautics and Space Administration
NDVINormalized Difference Vegetation Index
NPGINormalized Pigment Chlorophyll Index
OOFOut of Fold
PCLPhoton Counting LiDAR
RBFRadial Basis Function
RFRandom Forest
RFERecursive Feature Elimination
RHRelative Height
RMSERoot Mean Square Error
RRRidge Regression
RVIRatio Vegetation Index
SARSynthetic Aperture Radar
SAVISoil-Adjusted Vegetation Index
SHAPSHapley Additive exPlanations
SVMSupport Vector Machine
XGBoosteXtreme Gradient Boosting

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Figure 1. Location of study area. (a) Yunnan Province within China. (b) Xinping County within Yunnan Province. (c) Distribution of D. giganteus forests and locations of 52 field plots (red dots) within Xinping County.
Figure 1. Location of study area. (a) Yunnan Province within China. (b) Xinping County within Yunnan Province. (c) Distribution of D. giganteus forests and locations of 52 field plots (red dots) within Xinping County.
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Figure 2. Method overview for generating the AGB map of D. giganteus.
Figure 2. Method overview for generating the AGB map of D. giganteus.
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Figure 3. Performance metrics (R2, RMSE, CRPS) for spatial interpolation of GEDI and ICESat-2 derived parameters using EBKRP method.
Figure 3. Performance metrics (R2, RMSE, CRPS) for spatial interpolation of GEDI and ICESat-2 derived parameters using EBKRP method.
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Figure 4. Feature importance results. (a) The importance ranking of explanatory variables based on SHAP values for predicting the AGB of D. giganteus. (b) The relationship between the number of input features and model performance metrics, including the correlation coefficient (R) (red line), RMSE (blue line), and MAE (green line).
Figure 4. Feature importance results. (a) The importance ranking of explanatory variables based on SHAP values for predicting the AGB of D. giganteus. (b) The relationship between the number of input features and model performance metrics, including the correlation coefficient (R) (red line), RMSE (blue line), and MAE (green line).
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Figure 5. Scatterplots of predicted versus observed AGB for D. giganteus in Xinping County from different models: (a) XGBoost; (b) SVM; (c) kNN; (d) RF; and (e) stacking. The dashed line represents the 1:1 reference line, while the solid line is the regression fit line. Model performance is considered better as the slope of the regression equation approaches 1 and the intercept approaches 0.
Figure 5. Scatterplots of predicted versus observed AGB for D. giganteus in Xinping County from different models: (a) XGBoost; (b) SVM; (c) kNN; (d) RF; and (e) stacking. The dashed line represents the 1:1 reference line, while the solid line is the regression fit line. Model performance is considered better as the slope of the regression equation approaches 1 and the intercept approaches 0.
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Figure 6. The spatial distribution map of D. giganteus AGB in the study area (bar charts show the distribution of D. giganteus above-ground biomass across five different density classes within each region, with classes determined using the natural break classification method).
Figure 6. The spatial distribution map of D. giganteus AGB in the study area (bar charts show the distribution of D. giganteus above-ground biomass across five different density classes within each region, with classes determined using the natural break classification method).
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Figure 7. SHAP analysis for the Random Forest model, revealing the key drivers of AGB. The left panel is a SHAP summary plot, which ranks all features by their global importance based on the mean absolute SHAP value (gray bars). The color of each point on the plot represents the feature’s value (from low to high), while its position on the x-axis indicates the impact on the prediction for an individual sample. The right panels are SHAP dependence plots for the top six most important features, detailing the non-linear relationship between each driver and its contribution to the model prediction, with key ecological thresholds indicated by red dotted lines.
Figure 7. SHAP analysis for the Random Forest model, revealing the key drivers of AGB. The left panel is a SHAP summary plot, which ranks all features by their global importance based on the mean absolute SHAP value (gray bars). The color of each point on the plot represents the feature’s value (from low to high), while its position on the x-axis indicates the impact on the prediction for an individual sample. The right panels are SHAP dependence plots for the top six most important features, detailing the non-linear relationship between each driver and its contribution to the model prediction, with key ecological thresholds indicated by red dotted lines.
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Table 1. Statistical summary of AGB in the D. giganteus sample plots.
Table 1. Statistical summary of AGB in the D. giganteus sample plots.
VariableNMinimumMaximumMeanStandard Deviation (SD)
AGB (Mg ha−1)529.96132.0966.8927.59
Table 2. Key parameters of the ICESat-2 and GEDI missions, which represent the state of the art in spaceborne laser altimeters.
Table 2. Key parameters of the ICESat-2 and GEDI missions, which represent the state of the art in spaceborne laser altimeters.
MissonICESat-2GEDI
Full nameIce, Cloud, and land Elevation Satellite-2Global Ecosystem Dynamics Investigation
Launch dateSeptember 15, 2018December 5, 2018
Detector typePhoton countingFull waveform
Wavelength532 nm (green)1064 nm (near IR)
across-track spacing90 m within pairs 3.3 km between pairs600 m
Diameter along-track spacing~0.7 m~60 m
Footprint~12 m~25 m
Track number6 tracks from 1 laser8 tracks from 3 lasers
Orbit inclination and coverage92°; coverage up to 88°N–88°S latitude51.6°; coverage up to 51.6°N–51.6°S latitude
Laser power120 μJ/30 μJ15 mJ/4.5 mJ
Temporal resolution (Revisit time)~91 days (exact repeat orbit)~45 days (non-repeating)
Vertical accuracy~3–5 cm for flat surfaces~1 m (depending on waveform processing and vegetation density)
Table 3. GEDI L2B data quality filtering criteria.
Table 3. GEDI L2B data quality filtering criteria.
ParameteRetention ValueRetention Basis
lon_lowestmode101–103°EDefines the longitudinal extent of the Xinping County study area.
lat_lowestmode23–25°NDefines the latitudinal extent of the Xinping County study area.
algorithmrun_flag1Confirms the successful execution of the L2B algorithm and adequate waveform fidelity.
quality_flag1Indicates good-quality footprint data that meets multiple quality criteria and is located over a vegetated land area.
Sensitivity≥0.90Selects valid returns with high sensitivity (values approaching 1 signify high-quality signals).
degrade_flag0Excludes data flagged due to the degraded performance of the instrument or its pointing/positioning systems.
Table 4. Vegetation indices and terrain variables derived from Sentinel-2 spectral data and the ALOS DEM.
Table 4. Vegetation indices and terrain variables derived from Sentinel-2 spectral data and the ALOS DEM.
Vegetation Indices/Topographic FeaturesFormula/DescriptionCitation
Difference Vegetation Index D V I = N I R R E D [40]
Enhanced Vegetation Index E V I = 2.5 × ( N I R R E D ) 1 + N I R + 6 × R E D 7.5 × B L U E [41]
Green Difference Vegetation Index G D V I = N I R G R E E N [42]
Green Normalized Difference Vegetation Index G N D V I = N I R G R E E N N I R + G R E E N [43]
Green Ratio Vegetation Index G R V I = N I R G R E E N [44]
Normalized Difference Vegetation Index N D V I = N I R R E D N I R + R E D [45]
Normalized Pigment Chlorophyll Index N P C I = R E D G R E E N R E D + G R E E N [46]
Ratio Vegetation Index R V I = N I R R E D [47]
Soil-Adjusted Vegetation Index S A V I = ( 1 + L ) × ( N I R R E D ) N I R + R E D + L [48]
ElevationElevation
SlopeSlope factor extracted by DEM
AspectSlope aspect factor extracted by DEM
RED, GREEN, BLUE, NIR are the reflectance of red band, green band, blue band and near-infrared band.
Table 5. Cross-validation results of model performance for D. giganteus AGB estimation.
Table 5. Cross-validation results of model performance for D. giganteus AGB estimation.
ModelR2RMSE (Mg/ha)MAE (Mg/ha)Regression Fit
Stacking0.8411.078.69 y = 0.81 x + 12.91
Random Forest (RF)0.7214.5310.53 y = 0.53 x + 31.32
Support Vector Machine (SVM)0.6915.329.02 y = 0.59 x + 27.33
XGBoost0.6815.5811.50 y = 0.48 x + 34.48
k-Nearest Neighbor (kNN)0.6017.3514.27 y = 0.55 x + 26.62
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Fu, L.; Shu, Q.; Xia, C.; Li, Z.; He, H.; Li, Z.; Ma, S.; Qin, C.; Wei, R.; Xiang, Q.; et al. A Robust Framework for Bamboo Forest AGB Estimation by Integrating Geostatistical Prediction and Ensemble Learning. Remote Sens. 2025, 17, 2682. https://doi.org/10.3390/rs17152682

AMA Style

Fu L, Shu Q, Xia C, Li Z, He H, Li Z, Ma S, Qin C, Wei R, Xiang Q, et al. A Robust Framework for Bamboo Forest AGB Estimation by Integrating Geostatistical Prediction and Ensemble Learning. Remote Sensing. 2025; 17(15):2682. https://doi.org/10.3390/rs17152682

Chicago/Turabian Style

Fu, Lianjin, Qingtai Shu, Cuifen Xia, Zeyu Li, Hailing He, Zhengying Li, Shaoyang Ma, Chaoguan Qin, Rong Wei, Qin Xiang, and et al. 2025. "A Robust Framework for Bamboo Forest AGB Estimation by Integrating Geostatistical Prediction and Ensemble Learning" Remote Sensing 17, no. 15: 2682. https://doi.org/10.3390/rs17152682

APA Style

Fu, L., Shu, Q., Xia, C., Li, Z., He, H., Li, Z., Ma, S., Qin, C., Wei, R., Xiang, Q., Zhang, X., Zhang, Y., & Cai, H. (2025). A Robust Framework for Bamboo Forest AGB Estimation by Integrating Geostatistical Prediction and Ensemble Learning. Remote Sensing, 17(15), 2682. https://doi.org/10.3390/rs17152682

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