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生态学杂志 ›› 2025, Vol. 44 ›› Issue (9): 3036-3043.doi: 10.13292/j.1000-4890.202509.001

• 研究报告 • 上一篇    下一篇

气候的时滞效应和人为活动对黄土高原植被的影响

郭发苗1,彭道黎1*,苏艳芳2,赵娅冰1,王荫1
  

  1. (1北京林业大学森林资源和环境管理国家林草局重点实验室, 北京 100083; 2东北林业大学园林学院, 哈尔滨 150040)
  • 出版日期:2025-09-10 发布日期:2025-09-08

Time-lag effects of climate and the influence of anthropogenic activities on vegetation of the Loess Plateau.

GUO Famiao1, PENG Daoli1*, SU Yanfang2, ZHAO Yabing1, WANG Yin1   

  1. (1Key Laboratory of Forest Resources & Environmental Management of National Forestry and Grassland Administration, Beijing Forestry University, Beijing 100083, China; 2College of Landscape Architecture, Northeast Forestry University, Harbin 150040, China).

  • Online:2025-09-10 Published:2025-09-08

摘要: 分析气候变化和人类活动对植被的影响,对于植被恢复与维护生态平衡有重大意义。而气候变量的时滞效应对植被的影响往往被忽视,这将导致低估气候变化对植被变化的影响。本研究分析了2000—2019年黄土高原植被的时空变化,探究了植被变化对气候变化时滞效应的响应,提出考虑气候时滞效应的修正残差分析法,揭示气候变化和人类活动对植被变化的影响。结果表明:2000—2019年,黄土高原植被NDVI明显增加,年增长率为0.048·10 a-1;从空间上看,黄土高原大部分地区植被NDVI都在增加,其中76.6%的地区显著增加;温度对NDVI的变化有明显的时滞效应,最佳滞后时间为1个月,降水无滞后效应;不同土地利用类型的植被时滞效应相同,但相关性有所差异;气候变化和人类活动对NDVI变化的贡献分别为0.01·10 a-1和0.03·10 a-1,其共同作用是近20年来黄土高原NDVI变化的主要原因,面积占比达到了58.3%,人类活动的单独作用大于气候变化。


关键词: 植被变化, 时滞效应, 残差分析, 黄土高原

Abstract: Understanding the influences of climate change and anthropogenic activities on vegetation is of great significance for restoring vegetation and maintaining ecological balance. The time-lag impact of climate changes on vegetation is usually overlooked, which would underestimate the impacts of climate change on vegetation changes. We analyzed the spatiotemporal variations of vegetation on the Loess Plateau from 2000 to 2019, explored the time-lagged response of vegetation to climate change, proposed a modified residual analysis method considering the climate time-lag effect, and revealed the impacts of climate change and human activities on vegetation. The results showed that the Normalized Difference Vegetation Index (NDVI) of the vegetation on the Loess Plateau increased significantly from 2000 to 2019, with an annual growth rate of 0.048·10 a-1. Spatially, the NDVI of vegetation in most areas of the Loess Plateau was increasing, with the increases in 76.6% of the area being statistically significant. Temperature had an obvious time-lag effect on the changes of NDVI, with the optimal lag time being 1 month, while precipitation had no lag effect. The time-lag effect of vegetation was the same for different land use types, but the correlation varied. The contributions of climate change and human activities to the changes of NDVI were 0.01·10 a-1  and 0.03·10 a-1, respectively. Their combined effect was the main reason for the changes of NDVI on the Loess Plateau in the past nearly 20 years, accounting for 58.3% of the area. The independent effect of human activities is greater than that of climate change.


Key words: vegetation change, time-lag effect, residual analysis, Loess Plateau