鄱阳湖洪泛系统淹没动态时空异质性特征及驱动机制
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作者单位:

1.西南大学地理科学学院;2.中国科学南京地理与湖泊研究所

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P343.3

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Spatiotemporal heterogeneity and driving mechanism of inundation dynamics in the floodplain system of Poyang Lake
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1.School of Geographical Sciences, Southwest University;2.Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences

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    摘要:

    摘 要:因鄱阳湖主湖区与毗邻碟形湖区之间存在季节性动态的连通条件,导致了主湖区和碟形湖区水体淹没状况的非一致性,这种差异造就了两者不同的生境特点。基于ESTARFM(Enhanced Spatial and Temporal Adaptive reflection fusion model)模型,通过重构2000-2020年鄱阳湖区连续的高时空分辨率水体淹没数据,分析了鄱阳湖洪泛系统淹没动态的时空变化特征及其驱动因素。研究发现,近20年来鄱阳湖洪泛系统主湖区与碟形湖区水体淹没面积多年平均值分别为1239 km2和407 km2。受湖泊淹水自然过程和人为干扰的影响,碟形湖的淹水动态在涨水期(3月)和退水期(10月)与主湖区存在明显差异。在空间上,鄱阳湖的淹没频率总体上呈“北高南低”的分布格局,主湖区和碟形湖区水体淹没频率分别为58%和36%。研究时段内,鄱阳湖洪泛系统水体淹没面积与淹没频率整体上呈减小趋势,但碟形湖区内二者均呈微弱的上升趋势。近年来,鄱阳湖流域入湖流量的增加是导致碟形湖区水体淹没面积和淹没频率呈现增加趋势的主要原因,而主湖区水体淹没面积和淹没频率的下降主要归因于长江中上游来水减少、三峡工程运行引起的长江中下游河床降低、以及鄱阳湖区大规模采砂活动引起的入江水道下切侵蚀等综合作用造成的湖泊泄流能力的增大。研究结果对于深化湖泊洪泛系统水文复杂性的认识、促进洪泛湿地系统的管理实践具有重要的科学意义。

    Abstract:

    Abstract:Due to the seasonal changes of hydrologic connectivity between the main lake and the seasonal lakes of Poyang Lake, the inconsistent characteristics of inundation conditions in both are remarkably obvious, leading to their different habitat. Based on the reconstructed high spatial-temporal resolution inundation dataset of the Poyang Lake from 2000 to 2020 by adopting the ESTARFM model (Enhanced Spatial and Temporal Adaptive reflection fusion model), this study explored the spatio-temporal variation and the driving factors of inundation dynamics in the Poyang Lake-floodplain system. The results show that the mean value of the inundation area in the main lake and the seasonal lakes are 1232 km2 and 392 km2 respectively. The inundation of seasonal lakes in the floodplain area varies significantly in March and October due to the natural process of lake inundation and anthropogenic disturbance. Generally, the spatial distribution of inundation frequency of Poyang Lake decreases from north to south with the inundation frequency in the regions of the main lake and seasonal lakes are of 58% and 36%, and the mean value of 49%. During the study period, the inundation area and inundation frequency of the entire Poyang Lake-floodplain system showed a decreasing trend, while a slight increasing trend was observed for both of the variables in the seasonal lake region. The inundation dynamics in the Poyang Lake-floodplain system is mainly controlled by changes of the catchment inflow, the stage of Yangtze River and the topography of the lake basin. In recent years, the increase of catchment inflow is the main reason for the increasing trend of the inundation area and inundation frequency in the seasonal lake region. However, the decrease of inundation area and inundation frequency in the main lake area is mainly attributed to the increase of the lake outflow capacity caused by the compounding factors of decreasing streamflow from the upper-middle Yangtze River, the riverbed lowering in the middle-lower Yangtze River due to Three Gorges project operation, and the down-cutting of outflow water channel due to large-scale sand mining activities in the lake. The research results have important scientific significance for deepening the understanding of hydrological complexity of lake-floodplain system and promoting the management practice of floodplain wetland system.

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  • 收稿日期:2022-01-05
  • 最后修改日期:2022-01-05
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  • 在线发布日期: 2023-09-01
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