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Streamflow Decline in the Yellow River along with Socioeconomic Development: Past and Future

机译:黄河中的流出下降以及社会经济发展:过去和未来

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摘要

Human society and ecosystems worldwide are increasinAagly threatened by water shortages. Despite numerous studies of climatic impacts on water availability, little is known about the influences of socioeconomic development on streamflow and water sustainability. Here, we show that the streamflow from the Yellow River to the sea has decreased by more than 80% in total over the last 60 years due to increased water consumption by agricultural, industrial and urban developments (76% of the streamflow decrease, similarly hereinafter), decreased precipitation (13%), reservoir construction (6%) and revegetation (5%). We predict that if the past trends in streamflow will continue, year-round dry-up in the lower Yellow River will commence in the late 2020s or early 2030s, unless effective countermeasures such as water diversion from the Yangtze River are taken. These results suggest that streamflow in semiarid basins is highly vulnerable to human impacts and that streamflow decline would in turn hinder further socioeconomic development and endanger river-sea ecosystems.
机译:世界各地的人类社会和生态系统被水资源短缺增加。尽管对水利的巨大影响有很多研究,但对社会经济发展对流流和水可持续性的影响很少。在这里,我们表明,由于农业,工业和城市发展的水消耗增加,黄河到海上的流向海上的流出量总共减少了80%以上总量(76%的流流程减少,在下文中类似),降水量(13%),水库建设(6%)和再培养(5%)。我们预测,如果流流的过去趋势将继续,在20世纪20年代后期或20世纪30年代初期将在较低黄河中进行全年干涸,除非采取了长江的有效对策等。这些结果表明,半干旱盆地的流流量非常容易受到人类影响的影响,并且流出的流出拒绝妨碍进一步的社会经济发展和危险的河流生态系统。

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