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Quantitative contributions of climate change and human activities to vegetation changes over multiple time scales on the Loess Plateau

机译:在黄土高原上的多个时间尺度上,气候变化和人类活动的定量贡献在黄土高原上的多个时间尺度变化

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摘要

Vegetation is a crucial component of terrestrial ecosystems, and its changes are driven mainly by a combination of climate change and human activities. This paper aims to reveal the relationship between vegetation and climate change by using the normalized difference vegetation index (NDVI) and standardized precipitation evapo-transpiration index (SPEI), and to find the cause of vegetation change by performing residual analysis on the Loess Plateau during the period from 2000 to 2016. The results showed that the NDVI on the Loess Plateau exhibited an increase of 0.086 per decade, and an increasing trend was observed across 94.86% of the total area. The relationship between the NDVI and SPEI was mainly positive, and the correlation increased as the time scale of the SPEI lengthened, indicating that long-term water availability was the major climate factor affecting vegetation growth. Residual analysis indicated that climate change was responsible for 45.78% of NDVI variation, while human activities were responsible for 54.22%. In areas with degraded vegetation, the relative roles of climate change and human activities were 28.11% and 72.89%. respectively. In addition, the relative role of climate change increased with an increase in the time scales, implying that the long-term NDVI trend was more sensitive to climate change then the short-term trend. The results of this study are expected to enhance our understanding of vegetation changes under climate change and human activities and provide a scientific basis for future ecological restoration in arid regions.
机译:植被是陆地生态系统的关键组成部分,其变化主要由气候变化和人类活动的结合而导致。本文旨在通过使用归一化差异植被指数(NDVI)和标准化降水蒸发指数(SPEI)来揭示植被和气候变化的关系,并通过对黄土高原进行残余分析来找到植被变化的原因2000年至2016年的期限。结果表明,黄土高原上的NDVI展出了0.086每年的0.086,占总面积的94.86%的趋势。 NDVI和SPEI之间的关系主要是阳性的,并且随着Spei的时间标尺而增加,表明长期水可用性是影响植被生长的主要气候因素。残余分析表明,气候变化负责NDVI变异的45.78%,而人类活动则负责54.22%。在植被劣化的地区,气候变化和人类活动的相对角色为28.11%和72.89%。分别。此外,气候变化的相对作用随着时间尺度的增加而增加,暗示长期的NDVI趋势对气候变化更敏感,那么短期趋势。预计本研究的结果将加强我们对气候变化和人类活动下的植被变化的理解,并为干旱地区的未来生态恢复提供科学依据。

著录项

  • 来源
    《The Science of the Total Environment》 |2021年第2期|142419.1-142419.14|共14页
  • 作者单位

    Key Laboratory of Water Cycle and Related Land Surface Processes Institute of Geographic Sciences and Natural Resources Research Chinese Academy of Sciences Beijing 100101 PR China University of Chinese Academy of Sciences Beijing 100049 PR China;

    Key Laboratory of Water Cycle and Related Land Surface Processes Institute of Geographic Sciences and Natural Resources Research Chinese Academy of Sciences Beijing 100101 PR China University of Chinese Academy of Sciences Beijing 100049 PR China;

    University of Chinese Academy of Sciences Beijing 100049 PR China Institute of Soil and Water Conservation Northwest A&F University Yangling 712100 Shaanxi PR China;

    Key Laboratory of Water Cycle and Related Land Surface Processes Institute of Geographic Sciences and Natural Resources Research Chinese Academy of Sciences Beijing 100101 PR China University of Chinese Academy of Sciences Beijing 100049 PR China;

    Key Laboratory of Water Cycle and Related Land Surface Processes Institute of Geographic Sciences and Natural Resources Research Chinese Academy of Sciences Beijing 100101 PR China University of Chinese Academy of Sciences Beijing 100049 PR China;

    Institute of Soil and Water Conservation Northwest A&F University Yangling 712100 Shaanxi PR China Qingdao Engineering Research Center for Rural Environment College of Resources and Environment Qingdao Agricultural University Qingdao 266109 Shandong PR China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Vegetation; Climate change; Human activities; Multiple time scales; Normalized difference vegetation index; Standardized precipitation evapotranspiration index;

    机译:植被;气候变化;人类活动;多次尺度;归一化差异植被指数;标准化降水蒸发指数;
  • 入库时间 2022-08-18 23:02:46

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