顾及时滞与累积效应的中国植被时空演变及其对气候-人类活动的响应机制OACHSSCD
Spatio-temporal evolution of vegetation in China and its response mechanism to climate-human activities based on time lag and cumulative effects
时滞和累积效应对植被归一化植被指数(NDVI)时空动态的影响至关重要,深入理解其作用机制对于陆地生态系统的管理与可持续发展具有重要意义.基于MODIS NDVI遥感数据和气象数据,利用Theil-Sen趋势分析和Mann-Kendall检验探讨了2001-2020 年间中国植被NDVI的时空变化特征,并进一步通过引入气候因子的时滞与累积效应,结合偏相关分析和改进的残差分析,全面评估气候变化和人类活动对植被动态的综合驱动机制,突出气候因子的时间响应特征及其对植被变化的作用.结果表明:(1)2001-2020 年间,中国植被NDVI整体呈波动上升趋势,空间分布表现为东部高、西部低,东北、华北和中南地区增幅显著,西北及高寒区较低;未来约 13.84%的区域将持续改善,26.15%的区域可能出现退化.(2)NDVI对气温与降水的响应存在显著的时滞与累积效应,气温和降水的最佳时滞分别为0.199 个月和0.201 个月,累积时间分别为1.152 个月和1.483 个月.(3)79.41%的区域NDVI与气温极显著正相关,64.88%与降水极显著正相关,气温的长期影响大于降水.(4)NDVI增长区域中,80.68%由气候变化和人类活动共同驱动,减少区域中,81.60%主要由人类活动单独驱动,表明人类活动在植被变化中的重要作用.
Time lag and cumulative effects are crucial to the spatio-temporal dynamics of vegetation NDVI,and an in-depth understanding of their mechanisms is of great significance for the management and sustainable development of terrestrial ecosystems.Based on MODIS NDVI remote sensing data and meteorological data,this paper used Theil-Sen trend analysis and Mann-Kendall test to explore the temporal and spatial variation characteristics of vegetation NDVI in China from 2001 to 2020.Furthermore,by introducing the time lag and cumulative effect of climate factors,combined with partial correlation analysis and improved residual analysis,the comprehensive driving mechanism of climate change and human activities on vegetation dynamics was comprehensively evaluated,and the time response characteristics of climate factors and their effects on vegetation change were highlighted.The results showed that:(1)From 2001 to 2020,the NDVI of vegetation in China showed a fluctuating upward trend,and the spatial distribution showed that the NDVI in the eastern part was higher than that in the western part,and the NDVI in the northeast,north and south-central regions increased significantly,while the NDVI in the northwest and alpine regions was lower.In the future,about 13.84%of the region will continue to improve,and 26.15%of the region may be degraded.(2)The response of NDVI to temperature and precipitation has significant time lag and cumulative effect.The optimal time lag of temperature and precipitation was 0.199 and 0.201 months,respectively,and the cumulative time was 1.152 and 1.483 months,respectively.(3)79.41%of the regional NDVI was significantly positively correlated with temperature,and 64.88%was significantly positively correlated with precipitation.The long-term impact of temperature was greater than that of precipitation.(4)In the NDVI growth area,80.68%was driven by climate change and human activities,while in the NDVI reduction area,81.60%was mainly driven by human activities alone,indicating that human activities played an important role in vegetation change.
孙语晗;郭兵;孙晓双
山东理工大学建筑工程与空间信息学院,淄博 255000山东理工大学建筑工程与空间信息学院,淄博 255000山东理工大学建筑工程与空间信息学院,淄博 255000
植被归一化植被指数(NDVI)时滞效应累积效应气候变化人类活动残差分析
vegetation NDVItime lag effectcumulative effectclimate changehuman activitiesresidual analysis
《生态学报》 2026 (2)
705-720,16
国家自然科学基金项目(42471329)山东省高等学校"青创团队计划"团队项目(2022KJ224)
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