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OA
Impacts of climate changes and human activities on net primary productivity of vegetation in the Huang-Huai-Hai Plain
[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.
[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.
张静;李状;杨俊泉;刘宏伟;李婷;王威
中国地质调查局天津地质调查中心(华北地质科技创新中心),天津 300170||天津市海岸带地质过程与环境安全重点实验室,天津 300170||中国地质调查局雄安城市地质研究中心,天津 300170中国地质调查局天津地质调查中心(华北地质科技创新中心),天津 300170||天津市海岸带地质过程与环境安全重点实验室,天津 300170||中国地质调查局雄安城市地质研究中心,天津 300170中国地质调查局天津地质调查中心(华北地质科技创新中心),天津 300170||天津市海岸带地质过程与环境安全重点实验室,天津 300170||中国地质调查局雄安城市地质研究中心,天津 300170中国地质调查局天津地质调查中心(华北地质科技创新中心),天津 300170||天津市海岸带地质过程与环境安全重点实验室,天津 300170||中国地质调查局雄安城市地质研究中心,天津 300170中国地质调查局天津地质调查中心(华北地质科技创新中心),天津 300170||天津市海岸带地质过程与环境安全重点实验室,天津 300170||中国地质调查局雄安城市地质研究中心,天津 300170中国地质调查局天津地质调查中心(华北地质科技创新中心),天津 300170||天津市海岸带地质过程与环境安全重点实验室,天津 300170||中国地质调查局雄安城市地质研究中心,天津 300170
天文与地球科学
净初级生产力时空变化规律气候变化人类活动黄淮海平原
net primary productivityspatio-temporal change lawclimate changehuman activitiesHuang-Huai-Hai Plain
《地质通报》 2026 (2)
320-336,17
国家自然科学基金地质联合基金项目《北方农牧交错带生态退化的地质-生态-水文耦合机制与生态承载力阈值识别》(批准号:U2244230)和中国地质调查局项目《浑善达克沙地草地生态区自然生态调查》(编号:DD202607101906)、《华北地区自然资源与国土空间遥感监测》(编号:DD202607202804)、《京津冀协同发展区国土空间规划实施监测评价》(编号:DD202607203002)、《晋东-冀西太行山区易灾地质结构调查》(编号:DD202606101102) Supported by the National Natural Science Foundation of China Joint Fund Project(No.U2244230),and the Project of China Geological Survey(Nos.DD202607101906,DD202607202804,DD202607203002,DD202606101102)
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