基于机器学习模型的东北地区湖冰物候变化特征及驱动因子分析
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中国科学院东北地理与农业生态研究所

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中国科学院重大资助项目,国家自然科学基金项目(面上项目,重点项目,重大项目),国家重点基础研究发展计划(973计划)


A machine-learning model for identifying characteristics and driving factors of lake ice phenology changes in Northeast China*
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Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences

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The Major Program of the Chinese Academy of Sciences, The National Natural Science Foundation of China (General Program, Key Program, Major Research Plan),The National Basic Research Program of China (973 Program)

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    摘要:

    东北地区是我国中高纬度湖泊分布区和气候敏感区,其特有的季节性湖冰物候变化对湖泊生态系统产生重要影响。然而,东北地区缺少长时间序列湖冰物候数据,难以识别湖冰物候变化特征。为此,本研究基于XGBoost-SHAP机器学习模型,构建了1981-2023年东北地区重要湖泊(呼伦湖、连环湖、查干湖、兴凯湖和卧龙湖)的湖冰物候数据集,量化解析了湖冰物候变化特征及其驱动因子。研究结果表明:(1) 基于XGBoost的湖冰物候预测模型精度较高,其中结冰日预测的决定系数(R2)达到0.97,平均绝对百分比误差为0.5%;融冰日预测的决定系数(R2)为0.97,平均绝对百分比误差为1.9%。(2)湖冰物候呈现“结冰日期推迟、融冰日期提前、冰封期缩短” 特征及趋势,位于高纬度地区的呼伦湖湖冰物候变化明显,结冰日延后0.18d/a,融冰日提前0.37d/a,冰封期缩短0.55d/a;而纬度相对较低的卧龙湖变化相对缓和,结冰日延后0.13d/a,融冰日提前0.20d/a,冰封期缩短0.33d/a。(3)湖冰物候变化的关键驱动因子是气温,其对结冰日和融冰日的贡献度分别达到40.5%和31.2%。研究结果有助于理解全球气候变化背景下寒区湖泊湖冰物候响应机制,可为湖泊水环境保护和水生态治理提供科学支撑。

    Abstract:

    Northeast China is a mid- to high-latitude region with significant lake distribution and high sensitivity to climate change. Its unique seasonal lake ice phenology changes have a substantial impact on the lake ecosystem. However, there is a lack of long-term lake ice phenology data in Northeast China, making it difficult to identify the characteristics of lake ice phenology changes. To this end, this study employed the XGBoost-SHAP machine learning model to construct a lake ice phenology dataset for key lakes in Northeast China (Hulun, Lianhuan, Chagan, Xingkai, and Wolong Lakes) from 1981 to 2023, and conducted a quantitative analysis of the characteristics of lake ice phenology changes and their driving factors. The results show that (1) the XGBoost-based lake ice phenology prediction model achieves high accuracy. Specifically, the coefficient of determination (R2) for predicting freeze-up data is 0.97, with an average absolute percentage error of 0.5%. For predicting break-up data, the R2 value is also 0.97, but the average absolute percentage error is slightly higher at 1.9%. (2) Lake ice phenology exhibits the characteristics and trends of delayed freeze-up data, advanced break-up data, and shortened ice cover duration. At high-latitude Hulun Lake, freeze-up is delayed by 0.18 d/a, break-up advances by 0.37 d/a, and ice cover duration is shortened by 0.55 d/a. In contrast, at the relatively lower-latitude Wolong Lake, freeze-up is delayed by 0.13 d/a, break-up advances by 0.20 d/a, and ice cover duration is reduced by 0.33 d/a. (3) The primary driver of lake ice phenology changes is air temperature, contributing 40.5% and 31.2% to freeze-up and break-up data, respectively. The study"s findings enhance our understanding of the response mechanisms of lake ice phenology in cold regions to global climate change and provide scientific support for lake water environment protection and water ecology management.

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历史
  • 收稿日期:2025-07-01
  • 最后修改日期:2026-04-11
  • 录用日期:2025-10-09
  • 在线发布日期: 2025-11-26
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