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Vegetation Restoration Projects Intensify Intraregional Water Recycling Processes in the Agro-Pastoral Ecotone of Northern China

机译:植被恢复项目加强了中国北方农业牧区的内部水循环过程

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摘要

From 1998 to the present, the Chinese government has implemented numerous large-scale ecological programs to restore ecosystems and improve environmental protection in the agro-pastoral ecotone of northern China (APENC). However, it remains unclear how vegetation restoration modulates intraregional moisture cycles and changes regional water balance. To fill this gap, we first investigated the variation in precipitation (P) from the China Meteorological Forcing Dataset and evapotranspiration (ET) estimated using the Priestley-Taylor Jet Propulsion Laboratory model under two scenarios: dynamic vegetation (DV) and no dynamic vegetation (no-DV). We then used the dynamic recycling model to analyze the changes in precipitation recycling ratio (PRR). Finally, we examined how vegetation restoration modulates intraregional moisture recycling to change the regional water cycle in APENC. Results indicate P increased at an average rate of 4.42 mm yr(-2) from 1995 to 2015. ET with DV exhibited a significant increase at a rate of 1.57, 3.58, 1.53, and 1.84 mm yr(-2) in the four subregions, respectively, compared with no-DV, and the annual mean PRR values were 10.15%, 9.30%, 11.01%, and 12.76% in the four subregions, and significant increasing trends were found in the APENC during 1995-2015. Further analysis of regional moisture recycling shows that vegetation restoration does not increase local P directly, but has an indirect effect by enhancing moisture recycling process to produce more P by increasing PRR. Our findings show that large-scale ecological restoration programs have a positive effect on local moisture cycle and precipitation.
机译:从1998年至今,中国政府在中国北方农牧交错带(APENC)实施了许多大型生态项目,以恢复生态系统和改善环境保护。然而,目前尚不清楚植被恢复如何调节区域内水分循环和改变区域水平衡。为了填补这一空白,我们首先研究了中国气象强迫数据集中的降水量(P)变化,以及在两种情况下使用Priestley-Taylor喷气推进实验室模型估算的蒸散量(ET):动态植被(DV)和无动态植被(no DV)。然后利用动态循环模型分析了降水循环率(PRR)的变化。最后,我们研究了植被恢复如何调节区域内水分循环,从而改变APENC的区域水循环。结果表明,从1995年到2015年,磷的平均增长率为4.42毫米年(-2)。与无DV相比,有DV的ET在四个分区域分别以1.57、3.58、1.53和1.84毫米年(-2)的速度显著增加,四个分区域的年平均PRR值分别为10.15%、9.30%、11.01%和12.76%,在1995-2015年期间,APENC中发现了显著增加的趋势。对区域水分循环的进一步分析表明,植被恢复不会直接增加局部P,而是通过提高PRR,加强水分循环过程,产生更多P的间接效应。我们的研究结果表明,大规模的生态恢复计划对当地的水分循环和降水有积极的影响。

著录项

  • 来源
    《Journal of hydrometeorology》 |2021年第6期|共19页
  • 作者单位

    Lanzhou Univ Coll Earth &

    Environm Sci Key Lab West Chinas Environm Syst Minist Educ Lanzhou Peoples R China;

    Lanzhou Univ Coll Earth &

    Environm Sci Key Lab West Chinas Environm Syst Minist Educ Lanzhou Peoples R China;

    Lanzhou Univ Coll Earth &

    Environm Sci Key Lab West Chinas Environm Syst Minist Educ Lanzhou Peoples R China;

    Lanzhou Univ Coll Earth &

    Environm Sci Key Lab West Chinas Environm Syst Minist Educ Lanzhou Peoples R China;

    Lanzhou Univ Coll Earth &

    Environm Sci Key Lab West Chinas Environm Syst Minist Educ Lanzhou Peoples R China;

    Lanzhou Univ Coll Earth &

    Environm Sci Key Lab West Chinas Environm Syst Minist Educ Lanzhou Peoples R China;

    Lanzhou Univ Coll Earth &

    Environm Sci Key Lab West Chinas Environm Syst Minist Educ Lanzhou Peoples R China;

    Lanzhou Univ Coll Earth &

    Environm Sci Key Lab West Chinas Environm Syst Minist Educ Lanzhou Peoples R China;

    Lanzhou Univ Coll Earth &

    Environm Sci Key Lab West Chinas Environm Syst Minist Educ Lanzhou Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 水文循环与水文气象;
  • 关键词

    Atmosphere-land interaction; Evapotranspiration; Hydrometeorology; Water vapor; Land use;

    机译:None;

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