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Satellite image-based investigation of the seasonal variations in the hydrological connectivity of a large floodplain (Poyang Lake, China)

机译:基于卫星图像的大型洪泛区水文连接季节变化调查(鄱阳湖,中国)

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Hydrological processes of floodplains in large river-lake systems are subjected to strong flood pulses from catchment flows and lake inundations. Hydrological connectivity (HC) is one of the important characteristics of floodplains that can be used to provide evidence of mass and energy transport that influences the health of ecosystems and the biological productivity of floodplain water bodies. This study used geostatistical methods in combination with remote sensing data (2000-2015) to investigate the hydrological connectivity in a complex river-lake floodplain (Nanji Wetland National Natural Reserve) of the Poyang Lake floodplain, which is naturally connected to the middle Yangtze River. The geomorphic characteristics of the study area were characterized by the connection of surface water bodies including rivers, wetlands, sub-lakes and main lake. Results of this research indicated the apparent seasonal shifts of the dominant hydrological factors that affect the spatial-temporal changes of HC. In particular, we find that the main lake stage plays a dominant role in determining the hydrological connectivity during the lake's flooding and receding periods. We also find the existence of a threshold that causes an abrupt change of HC, i.e., if the main lake stage is below this threshold, the whole system becomes weakly hydrologically-connected. This threshold is related to the local topography, but has ecological implications for the entire floodplain system. The outcomes of this research provide an improved understanding of the hydrological behaviour of the catchment-floodplain-lake system. Considering the encountering of consistent drought of the lakes in the middle Yangtze River, this work may help clarify the intensity of the drought impacts on the ecologically important floodplains, and also assist in optimizing the interactions between the lake and the Yangtze River.
机译:大型河湖系统中洪泛区的水文过程受到集水流量和湖淹没的强大洪水脉冲。水文连通性(HC)是可用于提供影响生态系统健康和洪泛区水体的生物生产率的质量和能源运输证据之一的重要特征之一。本研究采用地统计方法与遥感数据(2000-2015)结合使用,探讨了鄱阳湖泛洪普兰的复杂河湖洪泛区(南报湿地国家自然保护区)中的水文连通性,这自然连接到长江中部。研究区的地貌特征是通过地表水体的连接,包括河流,湿地,湖泊和主要湖泊。该研究的结果表明了影响HC的空间变化的主要水文因子的表观季节性转变。特别是,我们发现主湖阶段在确定湖水洪水和后退期间的水文连接方面发挥着主导作用。我们还发现存在导致HC的突然变化的阈值,即,如果主湖阶段低于该阈值,则整个系统变得薄弱地连接。该阈值与本地地形有关,但对整个洪泛体系具有生态影响。该研究的结果提供了改善对集水区 - 泛湖湖系统的水文行为的理解。考虑到中江中湖的一致干旱,这项工作可能有助于澄清干旱影响对生态重要洪水平均值的强度,并有助于优化湖泊与长江之间的相互作用。

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