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首页> 外文期刊>Journal of Hydrology >Examining the influence of river-lake interaction on the drought and water resources in the Poyang Lake basin
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Examining the influence of river-lake interaction on the drought and water resources in the Poyang Lake basin

机译:考察of阳湖流域相互作用对干旱和水资源的影响

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摘要

In recent years, the Poyang Lake basin is in a prolonged drought which has placed immense pressure on the water resources utilization. In this paper, we explore the spatial and temporal distributions of extreme droughts in the Poyang Lake basin by using the methods of SPI (Standardized Precipitation Index) and EOF (Empirical Orthogonal Function) for the period of 1956-2009, which are influenced by regional precipitation anomalies and river-lake interaction due to water impounding of the Three Gorges Dam (TGD). The results show that: (I) the Poyang Lake basin experienced six extreme droughts during the past 60 years, which lead to decreases in streamflow from five tributary rivers down to the Poyang Lake. The droughts in the 1960s and the 2000s were the most serious ones. However, there was an increasing trend of streamflow in the upper and middle Yangtze in the 1960s, and a decreasing trend appeared in the 2000s. The decline of streamflow in the upper Yangtze reaches has lowered the water level of lower Yangtze River which has-caused more outflow from the Poyang Lake to the Yangtze River; (2) the operation of the Three Gorges Dam (TGD) has altered the seasonal pattern of flow regimes in the Poyang Lake and significantly reduced the water level in the lower Yangtze River during the TGD impounding period from late September to early November; and (3) the conjunction of extreme droughts in the Poyang lake and the upper Yangtze reaches coincided with the impounding of the TGD is the main cause of the low water level in the Poyang Lake. Although the impact of the recent droughts in the Poyang Lake and upper Yangtze reaches has played a crucial role in the low water level of Poyang lake, more attention should be paid to its sensitivity to the influence of the large dam-induced changes in the interaction between river and lake, particularly during impounding periods. (C) 2015 Elsevier B.V. All rights reserved.
机译:近年来,the阳湖流域长期干旱,给水资源利用带来了巨大压力。本文利用SPI(标准降水指数)和EOF(经验正交函数)方法,探讨了受区域性影响的Po阳湖流域极端干旱的时空分布。三峡大坝(TGD)的蓄水导致降水异常和河湖相互作用。结果表明:(I)在过去的60年中,the阳湖流域经历了6次极端干旱,导致从5条支流河到to阳湖的流量减少。 1960年代和2000年代的干旱是最严重的干旱。但是,1960年代长江中上游的水流量呈上升趋势,而2000年代则呈下降趋势。长江上游水流的下降使长江下游的水位降低,导致from阳湖向长江的出水量增加。 (2)三峡大坝(TGD)的运行改变了September阳湖在9月下旬至11月初的TGD蓄水期间的水流变化的季节性模式,并大大降低了长江下游的水位; (3)yang阳湖与长江上游的极端干旱相结合并伴有TGD的蓄积是is阳湖水位偏低的主要原因。尽管最近the阳湖和长江上游干旱的影响在of阳湖低水位中发挥了关键作用,但应更多地注意其对大坝诱发的相互作用变化影响的敏感性。在河流和湖泊之间,特别是在蓄水期间。 (C)2015 Elsevier B.V.保留所有权利。

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