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Hydrological response to urbanization at different spatio-temporal scales simulated by coupling of CLUE-S and the SWAT model in the Yangtze River Delta region

机译:结合CLUE-S和SWAT模型对长三角地区不同时空尺度下城市化的水文响应

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The Main objective of the study is to understand and quantify the hydrological responses of land use and land cover changes. The Yangtze River Delta is one of the most developed regions in China with the rapid development of urbanization which serves as an excellent case study site for understanding the hydrological response to urbanization and land use change. The Xitiaoxi River basin, one of the main upstream rivers to the Taihu Lake in the Yangtze River Delta, was selected to perform the study. The urban area in the basin increased from 37.8km~2 in 1985 to 105km~2 in 2008. SWAT model, which makes direct use of land cover and land use data in simulating streamflow, provides as a useful tool for performing such studies and is therefore used in this study. The results showed that (1) the expansion of urban areas had a slight influence on the simulated annual streamflow and evapotranspiration (ET) as far as the whole catchment is concerned; (2) surface runoff and baseflow were found more sensitive to urbanization, which had increased by 11.3% and declined by 11.2%, respectively; (3) changes in streamflow, evapotranspiration and surface runoff were more pronounced during the wet season (from May to August), while baseflow and lateral flow had a slight seasonal variation; (4) the model simulated peak discharge increased 1.6-4.3% and flood volume increased 0.7-2.3% for the selected storm rainfall events at the entire basin level, and the change rate was larger for smaller flood events than for larger events; (5) spatially, changes of hydrological fluxes were more remarkable in the suburban basin which had a relative larger increase in urbanization than in rural sub-basins; and (6) analysis of future scenarios showed the impacts of urbanization on hydrological fluxes would be more obvious with growth in impervious areas from 15% to 30%. In conclusion, the urbanization would have a slight impact on annual water yield, but a remarkable impact was found on surface runoff, peak discharge and flood volume especially in suburban basins in the study area. The study suggested that more attention must be paid for flood mitigation and water resources management in planning future urban development in the region.
机译:研究的主要目的是了解和量化土地利用和土地覆盖变化的水文响应。长江三角洲是中国城市化快速发展的最发达地区之一,是了解城市化和土地利用变化的水文响应的绝佳案例研究基地。西iao溪流域是长江三角洲太湖的主要上游河流之一,因此进行了此项研究。流域的市区面积从1985年的37.8km〜2增加到2008年的105km〜2。SWAT模型直接利用了土地覆盖和土地利用数据来模拟水流,为进行此类研究提供了有用的工具,因此在本研究中使用。结果表明:(1)就整个集水区而言,城市面积的扩大对模拟的年流量和蒸散量(ET)的影响较小; (2)地表径流和基流对城市化比较敏感,分别增长了11.3%和下降了11.2%; (3)在雨季(5月至8月),水流,蒸散量和地表径流的变化更为明显,而底流和侧流则有轻微的季节性变化。 (4)在整个流域范围内,选定暴雨事件的模型模拟峰值流量增加了1.6-4.3%,洪水量增加了0.7-2.3%,较小洪水事件的变化率大于较大洪水事件的变化率。 (5)在空间上,郊区流域的水文通量变化更为明显,城市化的增长幅度大于农村次流域; (6)对未来情景的分析表明,城市化对水文通量的影响将在不透水地区从15%增长到30%时更加明显。总之,城市化对年产量有轻微影响,但对地表径流,高峰流量和洪水量有显着影响,特别是在研究区域的郊区。研究表明,在规划该地区未来的城市发展时,必须更加重视防洪和水资源管理。

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