Identifies wind erosion drivers and assesses ecological risk in alpine drylands, suggesting targeted mitigation strategies.
Wind erosion is a key pathway of land degradation in the alpine drylands of the Qinghai-Tibet Plateau, yet its dominant controls and risk trajectories remain difficult to attribute in a spatially heterogeneous system. Here we integrated the RWEQ with an interpretable machine learning framework (XGBoost coupled with SHAP) to quantify spatiotemporal patterns of potential wind erosion from 1981 to 2020, identify dominant drivers, and delineate management-oriented ecological risk zones. The Plateau-wide mean potential wind erosion modulus was 3.03x104 t/km2, with localized hotspots up to 1.08x105 t/km2. Wind erosion showed strong seasonality, with most losses occurring from late winter to spring, and a predominantly declining long-term tendency that was spatially heterogeneous across climate classes. SHAP interpretation ranked erosive wind speed as the leading control (mean(|SHAP|) = 10.28), followed by sand content (5.17) and fractional vegetation cover (4.05), with elevation and soil organic matter as secondary modifiers. Dominant driver mapping attributed 59.69% of the Plateau to wind dominance, 9.96% to sand dominance, and 4.49% to vegetation dominance, while 24.74% was non-erosive. Risk zoning indicated extensive recovery areas (54.01%) and substantial gradually worsening belts (17.73%), with rapid worsening hotspots concentrated in wind driven zones (3.33%). The proposed RWEQ plus XGBoost-SHAP framework provides a transparent basis for prioritizing monitoring and targeted mitigation under climate variability.
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Ouyang et al. (2026) studied this question.
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