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首页> 外文期刊>Journal of Environmental Management >Evaluating the cumulative and time-lag effects of drought on grassland vegetation: A case study in the Chinese Loess Plateau
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Evaluating the cumulative and time-lag effects of drought on grassland vegetation: A case study in the Chinese Loess Plateau

机译:干旱对草地植被的累积效应和时滞效应评估-以黄土高原地区为例

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摘要

The increased frequency of drought events in recent years is known to be responsible for significantly altering plant biodiversity in many of Earth's ecosystems, though the specifics of vegetation-drought interactions, especially the cumulative and time-lag responses, remains unclear. This study aimed to quantitatively investigate how grassland vegetation over the Chinese Loess Plateau (CLP) reacts to drought, specifically the observed cumulative and time-lag effects which are caused, using a combination of the Normalized Difference Vegetation Index (NDVI) and a multiple time-scale drought index (Standardized Precipitation and Evapotranspiration Index, SPEI). Our results revealed that while drought conditions have widespread cumulative impacts on grass growth in the CLP, the time lag effect of drought covered about half of the total area of the CLP. The cumulative effect of drought on grass was found to take place over various time scales, ranging from 5 to 10 months, while the time lag effect occurred within 2-3 months. The different response time of vegetation growth to the cumulative effect of drought in the CLP was found to be highly related to different water conditions. The accumulated months and mean r_(max-cum) both had a significant negative correlation with the mean annual SPEI (R~2 = 0.90, P < 0.001; R~2 = 0.70, P < 0.001, respectively). The lagged months and mean r_(max-lag) were also found to be negatively correlated with the mean annual SPEI (R~2 = 0.547, P < 0.05; R~2 = 0.785, P < 0.01, respectively).
机译:众所周知,近年来干旱事件的频率增加是导致地球许多生态系统中植物生物多样性发生重大变化的原因,尽管尚不清楚植被与干旱相互作用的具体情况,尤其是累积响应和时滞响应。这项研究旨在定量地研究黄土高原(CLP)的草地植被对干旱的反应,特别是使用归一化植被指数(NDVI)和多次干旱相结合的观测到的累积和时滞效应。尺度干旱指数(标准降水和蒸散指数,SPEI)。我们的结果表明,尽管干旱条件对中电的草生长具有广泛的累积影响,但干旱的时滞效应却覆盖了中电总面积的一半。发现干旱对草的累积影响发生在5到10个月的不同时间范围内,而时滞影响发生在2-3个月内。在中电,不同的植被生长对干旱累积效应的响应时间被发现与不同的水分条件高度相关。累积月份和平均r_(max-cum)均与年均SPEI呈显着负相关(R〜2 = 0.90,P <0.001; R〜2 = 0.70,P <0.001)。还发现滞后月份和平均r_(max-lag)与年平均SPEI呈负相关(R〜2 = 0.547,P <0.05; R〜2 = 0.785,P <0.01)。

著录项

  • 来源
    《Journal of Environmental Management》 |2020年第may1期|110214.1-110214.8|共8页
  • 作者单位

    College of Mining and Geomatics Hebei University of Engineering Handan 056038 China State Key Laboratory of Resources and Environmental Information Systems Institute of Geographical Sciences and Natural Resources Research Chinese Academy of Sciences Beijing 100101 China;

    Department of Plant and Environmental Sciences New Mexico State University Las Cruces 88003 NM USA;

    College of Mining and Geomatics Hebei University of Engineering Handan 056038 China;

    State Key Laboratory of Resources and Environmental Information Systems Institute of Geographical Sciences and Natural Resources Research Chinese Academy of Sciences Beijing 100101 China;

  • 收录信息 美国《科学引文索引》(SCI);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Cumulative effect; Time-lag effect; Drought; Grassland NDVI3g; SPEI; Chinese loess plateau;

    机译:累积效果;时滞效应;干旱;草原NDVI3g;SPEI;黄土高原;

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