气候变化和人类活动对黄淮海平原植被净初级生产力的影响

    Impacts of climate changes and human activities on net primary productivity of vegetation in the Huang−Huai−Hai Plain

    • 摘要:
      研究目的 揭示2001—2022年黄淮海平原植被净初级生产力(NPP)的时空变化规律,量化气候变化与人类活动对NPP变化的相对贡献,并深入剖析其内在驱动机制,以期为区域生态管理、植被恢复及碳汇能力提升提供科学依据。
      研究方法 基于MODIS NPP数据、气象观测数据、土地利用等多源数据,综合运用趋势分析、偏相关分析、多元回归残差分析等方法,解析NPP时空动态及其对气候因子的响应;进一步采用增强回归树(BRT)模型,评估气候变化(气温、降水)与人类活动(土地利用程度、人口密度等)多因子对NPP变化的相对重要性及偏依赖关系。
      研究结果 2001—2022年,黄淮海平原植被NPP总体呈显著增长趋势(增速为5.19 gC·m−2·a−1),空间上表现为南高北低格局。NPP与降水呈显著正相关,降水是影响NPP的主要气候因子。植被NPP变化以气候变化和人类活动共同驱动为主,二者贡献率分别为41.81%和39.24%。BRT模型结果显示,降水、土地利用程度和人口密度是影响2020年NPP空间分异的关键因子。
      结论 黄淮海平原植被NPP变化是自然因素与人为干预共同作用的结果,降水资源的合理调控与土地利用结构的优化是维持和提升区域生态系统生产力的关键路径。本研究为理解植被动态的驱动机制及区域生态安全策略制定提供了定量支持。

       

      Abstract:
      Objective  This study aims to reveal the spatio−temporal variation patterns of the net primary productivity (NPP) of vegetation in the Huang−Huai−Hai Plain from 2001 to 2022, quantify the relative contributions of climate change and human activities to the changes in NPP, and deeply analyze its internal driving mechanisms, with the expectation of providing a scientific basis for regional ecological management, vegetation restoration, and the improvement of carbon sink capacity.
      Methods  Based on multi−source data such as MODIS NPP data, meteorological observation data and land use, methods such as trend analysis, partial correlation analysis and multiple regression residual analysis were comprehensively applied to analyze the spatio−temporal dynamics of NPP and its response to climatic factors; Further, the enhanced regression tree (BRT) model was adopted to evaluate the relative importance and partial dependence of multiple factors such as climate change (temperature, precipitation) and human activities (land use degree, population density, etc.) on the changes in NPP.
      Results  From 2001 to 2022, the NPP of vegetation in the Huang−Huai−Hai Plain generally showed a significant growth trend (with a growth rate of 5.19 gC·m−2·a−1), and spatially presented a pattern of being higher in the south and lower in the north. NPP is significantly positively correlated with precipitation, and precipitation is the main climatic factor affecting NPP. The changes in vegetation NPP are mainly driven by both climate change and human activities, with their contribution rates being 41.81% and 39.24% respectively. The results of the BRT model show that precipitation, land use degree and population density are the key factors influencing the spatial differentiation of NPP in 2020.
      Conclusions  The changes in vegetation NPP in the Huang−Huai−Hai Plain are the result of the combined effect of natural factors and human intervention. The rational regulation of precipitation resources and the optimization of land use structure are the key paths to maintain and enhance the productivity of the regional ecosystem. This study provides quantitative support for understanding the driving mechanism of vegetation dynamics and formulating regional ecological security strategies.

       

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