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Improved vegetation greenness increases summer atmospheric water vapor over Northern China

机译:改善的植被绿色度增加了中国北方夏季的大气水汽

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Northern China is an environmentally vulnerable region with a severe water shortage. Several ecological restoration projects since the 1980s have greatly increased vegetation greenness. This study aims to assess the impacts of the changes in vegetation greenness from 1982 to 2008 on the atmospheric precipitable water (PW) over northern China during the summer seasons (June, July, and August) using reanalysis PW and satellite vegetation index data. Several statistical methods, such as linear regression (piecewise, stepwise), the Empirical Orthogonal Function, Pearson's correlation, have been used to explore the variations in and the coupling between vegetation greenness and PW. The influences of three major atmospheric circulations (the East Asian summer monsoon, the South Asian summer monsoon, and the Westerly circulation) have also been considered and excluded. The results show that summer vegetation greenness within the semi-arid western part of northern China, including the Tibetan Plateau, is closely linked to summer PW after excluding the influences of atmospheric circulations and that vegetation accounts for as much as 30% of the total PW variance. Vegetation greenness in the central and western water-limited regions of northern China has significant (>90% confidence level) positive impacts on summer PW. After investigating the relationships among evapotranspiration (ET), PW, and precipitation, it was concluded that strengthened ET driven by increased vegetation greenness makes a major contribution to increased PW. Different from the earlier hypothesis in the literature "only intact contiguous cover of natural forest having extensive borders with larger water bodies is able to keep land moisten up to an optimal for life level everywhere on land," this study found that interior forest covered regions with adequate water supply can also provide an ET benefit of PW for other regions. This study demonstrates the implications of large-scale ecological restoration projects on the hydrological cycle in arid/semi-arid regions. Key Points Vegetation is very important to the moisture cycle in water-limited region ET controlled by terrestrial vegetation is a main reason
机译:中国北方是一个严重缺水的环境脆弱地区。自1980年代以来的几个生态修复项目大大提高了植被的绿色度。这项研究的目的是使用再分析PW和卫星植被指数数据,评估1982年至2008年植被绿色度变化对夏季(六月,七月和八月)中国北方大气可降水量(PW)的影响。几种统计方法,例如线性回归(逐段,逐步),经验正交函数,皮尔森相关性,已被用于探索植被绿色度和PW之间的变化及其耦合。还考虑并排除了三个主要大气环流(东亚夏季风,南亚夏季风和西风)的影响。结果表明,在不包括大气环流影响的情况下,中国北部半干旱西部地区(包括青藏高原)的夏季植被绿色度与夏季PW密切相关,植被占总PW的30%方差。中国北方中部和西部缺水地区的植被绿色度对夏季PW具有显着的积极影响(置信度> 90%)。在调查了蒸散量(ET),PW和降水之间的关系后,得出的结论是,植被绿度增加推动的ET增强对PW的增加做出了重要贡献。与文献中较早的假设不同,“只有完整的连续森林覆盖率较高的天然水体与广阔的水体接壤,才能使土地保持湿润,达到陆地上所有地方的最佳生活水平,”这项研究发现,内部森林覆盖了充足的水供应还可以为其他地区的PW提供ET好处。这项研究表明了大型生态修复项目对干旱/半干旱地区水文循环的影响。要点植被对水分限制区域的水分循环非常重要,该限制是由陆地植被控制的

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