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Modal analysis of annual runoff volume and sediment load in the Yangtze river-lake system for the period 1956-2013

机译:1956 - 2013年长江 - 湖泊系统年径流体积和沉积物的模态分析

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This study focuses on detecting trends in annual runoff volume and sediment load in the Yangtze river-lake system. Times series of annual runoff volume and sediment load at 19 hydrological gauging stations for the period 1956-2013 were collected. Based on the Mann-Kendall test at the 1% significance level, annual sediment loads in the Yangtze River, the Dongting Lake and the Poyang Lake were detected with significantly descending trends. The power spectrum estimation indicated predominant oscillations with periods of 8 and 20 years are embedded in the runoff volume series, probably related to the El Nino Southern Oscillation (2-7 years) and Pacific Decadal Oscillation (20-30 years). Based on dominant components (capturing more than roughly 90% total energy) extracted by the proper orthogonal decomposition method, total change ratios of runoff volume and sediment load during the last 58 years were evaluated. For sediment load, the mean CRT value in the Yangtze River is about -65%, and those in the Dongting Lake and the Poyang Lake are -92.2% and -87.9% respectively. Particularly, the CRT value of the sediment load in the channel inflow of the Dongting Lake is even -99.7%. The Three Gorges Dam has intercepted a large amount of sediment load and decreased the sediment load downstream.
机译:本研究重点介绍长江 - 湖泊系统年径流量和沉积物的检测趋势。收集了1956 - 2013年1956 - 2013年1956-2013期间的1956-2013水文测量站的年径流量和沉积物载荷的时间。基于Mann-Kendall测试在1%的重要性水平,长江,洞庭湖和鄱阳湖的年沉积物负荷,具有显着下降的趋势。功率谱估计表明径流量系列中嵌入了8和20年的主要振荡,可能与El Nino Southern振荡(2-7岁)和太平洋截止振荡(20-30岁)有关。基于所主体成分(捕获大约90%的总能量)通过适当的正交分解方法提取,评估了在过去58年期间径流量和沉积物负荷的总变化比率。对于沉积物负荷,长江中的平均CRT值约为-65%,洞庭湖和鄱阳湖分别为-92.2%和-87.9%。特别是,洞庭湖通道流入中沉积物负荷的CRT值甚至为-99.7%。三峡坝已经截获了大量的沉积物负荷并降低了下游的沉积物负荷。

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