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基于集成机器学习的祁连山草地全球变暖潜力预测
摘要点击 468  全文点击 15  投稿时间:2025-07-17  修订日期:2025-10-15
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中文关键词  祁连山草地生态系统  全球变暖潜力(GWP)  放牧强度  集成机器学习  气候情景
英文关键词  Qilian Mountain grassland ecosystem  global warming potential(GWP)  grazing intensity  ensemble machine learning  climate scenario
DOI  10.13227/j.hjkx.202507231
作者单位E-mail
王涵颖 甘肃农业大学理学院, 兰州 730070 494296748@qq.com 
张美玲 甘肃农业大学理学院, 兰州 730070
甘肃农业大学数量生物学研究中心, 兰州 730070 
zhangml@gsau.edu.cn 
巩彦君 甘肃农业大学理学院, 兰州 730070  
蔡佳坊 甘肃农业大学理学院, 兰州 730070  
中文摘要
      祁连山草地生态系统作为重要碳储存区,其全球变暖潜力(GWP)预测对气候适应性管理至关重要. 基于1980~2024年多源数据,融合XGBoost、LightGBM、CatBoost和随机森林,构建集成的机器学习模型,预测2025~2060年在不同气候情景下的GWP动态. 结果表明:①集成机器学习模型性能最优,决定系数(R2)为0.938,均方根误差(RMSE)显著低于单一模型,能够有效刻画草地生态系统复杂的非线性关系;②土壤黏粒与粉粒含量及放牧强度是影响GWP的关键驱动因子,其中放牧强度对GWP的影响存在阈值效应;③未来情景预测显示,在SSP5-8.5情景下,GWP呈持续上升趋势,年际波动性增强,高放牧区域风险显著提升,2060年超过42 g·(m2·a)-1,而SSP1-2.6低排放情景下则保持平稳. 空间格局上,GWP呈“东南高和西北低”分布,在高排放情景下东南部高值区呈扩展态势. 研究结果可为典型高原草地全球变暖风险识别、生态系统管理分区与低碳路径制定提供理论依据与技术支持.
英文摘要
      The Qilian Mountain grassland ecosystem serves as an important carbon reservoir, and accurate prediction of its global warming potential (GWP) is essential for climate-adaptive management. Based on multi-source data from 1980 to 2024, an ensemble machine learning model integrating XGBoost, LightGBM, CatBoost, and RF was developed to predict GWP dynamics under different climate scenarios during 2025-2060. The results indicate that: ① The ensemble machine learning model achieved the best performance, with a coefficient of determination (R2) of 0.938 and a root mean square error (RMSE) significantly lower than those of individual models, effectively capturing the complex nonlinear relationships of the grassland ecosystem. ② Soil clay and silt contents, together with grazing intensity, were identified as the key driving factors of GWP, among which grazing intensity exhibited a threshold effect. ③ Future scenario simulations suggest that under the SSP5-8.5 high-emission pathway, GWP shows a continuous upward trend with intensified interannual fluctuations, and the risk in high-grazing areas increases substantially, exceeding 42 g·(m2·a)-1 by 2060, while under the SSP1-2.6 low-emission pathway, GWP remains relatively stable. In terms of spatial patterns, GWP demonstrates a “higher in the southeast and lower in the northwest” distribution, with the southeastern high-value areas expanding further under high-emission scenarios. These findings provide theoretical support and technical guidance for global warming risk assessment, ecosystem management zoning, and low-carbon pathway development in typical alpine grasslands.

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