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Shifts in river-floodplain relationship reveal the impacts of river regulation: A case study of Dongting Lake in China

机译:河洪水关系的转变揭示了河流监管的影响 - 以中国洞庭湖为例

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Better understanding of the dynamics of hydrological connectivity between river and floodplain is essential for the ecological integrity of river systems. In this study, we proposed a regime-switch modelling (RSM) framework, which integrates change point analysis with dynamic linear regression, to detect and date change points in linear regression, and to quantify the relative importance of natural variations and anthropogenic disturbances. The approach was applied to the long-term hydrological time series to investigate the evolution of river-floodplain relation in Dongting Lake in the last five decades, during which the Yangtze River system experienced unprecedented anthropogenic manipulations. Our results suggested that 1) there were five distinct regimes during which the influence of inflows and local climate on lake water level changed significantly. The detected change points were well corresponding to the major events occurred upon the Yangtze; 2) although the importance of inflows from the Yangtze was greater than that of the tributaries flows over the five regimes, the relative contribution gradually decreased from regime 1 to regime 5. The weakening of hydrological forcing from the Yangtze was mainly attributed to the reduction in channel capacity resulting from sedimentation in the outfalls and water level dropping caused by river bed scour in the mainstream; 3) the effects of local climate was much smaller than these of inflows; and 4) since the operation of The Three Gorges Dam in 2006, the river-floodplain relationship entered a new equilibrium in that all investigated variables changed synchronously in terms of direction and magnitude. The results from this study reveal the mechanisms underlying the alternated inundation regime in Dongting Lake. The identified change points, some of which have not been previously reported, will allow a reappraisal of the current dam and reservoir operation strategies not only for flood/drought risk management but also
机译:河漫滩之间的水文连接的动态更好的理解是河流系统的生态完整性至关重要。在这项研究中,我们提出了一个政权开关模型(RSM)框架,变点分析与动态线性回归整合,线性回归检测和日期变化点,并量化自然变化和人为干扰的相对重要性。该方法适用于长期水文时间序列进行调查,在过去的五十年,在此期间,长江水系经历了前所未有的人为操纵洞庭湖河漫滩关系的演变。我们的研究结果表明,1)有五个在此期间,流入和当地气候的湖泊水位的影响显著改变不同的制度。检测到的变化点进行了很好的对应关系在长江发生的重大事件; 2)虽然从扬子流入的重要性大于支流流过五个制度,相对贡献逐渐从政权1下降到政权5的水文从扬子迫使弱化主要是由于在还原从排水口和水位沉淀所得的信道容量由滴在主流河床冲刷引起的; 3)当地气候的影响比这些流入的要小得多; 4)由于三峡大坝在2006年的工作时,河漫滩关系在所有调查的变量在方向和幅度方面同步改变进入了一个新的平衡。从这项研究结果表明洞庭湖交替淹没政权背后的机制。该标识的变化点,其中有一些先前未曾报道过,将允许不仅为洪水/干旱风险管理也是当前大坝和水库经营战略进行了重新评估

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