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Watershed Modeling of Surface Water-Groundwater Interaction under ProjectedClimate Change and Water Management in theHaihe River Basin, China

机译:海河流域预估气候变化与水管理下地表水-地下水相互作用的分水岭模型

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The Haihe River Basin (HRB), located in northern China with a drainage area of 318,200 km2, is one of the most developed regions in China. With rapid population growth and economic development, the combined problems of water shortage and groundwater over-pumping significantly constrain the sustainable development in this area. In order to strengthen the unified management of groundwater and surface water, we developed hydrologic modeling of surface water and groundwater interaction by coupling SWAT (for surface water simulation) and MODFLOW (for groundwater simulation). The newly developed modeling framework reasonably captured the spatiotemporal variability of the hydrological processes of the surface water and groundwater in the study area. The modeling results showed a good agreement with the measurements of surface water and groundwater during 1996-2006. Results of model evaluation indicated that the developed model could be a promising tool in watershed management planning under the context of global climate change and the “South-North Water Transfer Project”. In the HRB, climate change has significant effects on surface hydrology as indicated by the predicted increases on actual evapotranspiration and precipitation during 2041-2050 relative to those during 1991-2000. Changes of groundwater storage were mainly contributed by water diversion which would reduce the requirement of water pumping from groundwater especially for domestic and industrial uses. By the middle of the 21st century, increased water supply by projected precipitation and water diversion would result in annual increases of 3.9~9.9 billion m3 for river discharge and 1.7~2.9 billion m3 for groundwater storage as annual averages.
机译:海河流域(HRB)位于中国北部,流域面积为318,200 km2,是中国最发达的地区之一。随着人口的快速增长和经济的发展,水资源短缺和地下水超采的综合问题大大制约了该地区的可持续发展。为了加强地下水和地表水的统一管理,我们通过结合SWAT(用于地表水模拟)和MODFLOW(用于地下水模拟)开发了地表水和地下水相互作用的水文模型。新开发的建模框架合理地捕获了研究区域地表水和地下水的水文过程的时空变化。模拟结果与1996-2006年的地表水和地下水测量结果吻合良好。模型评估的结果表明,在全球气候变化和“南北调水工程”的背景下,开发的模型可能是流域管理规划中有希望的工具。在HRB中,气候变化对地表水文学有重大影响,正如2041-2050年期间相对于1991-2000年期间实际蒸散量和降水量的预测增加所表明的。地下水储量的变化主要是通过调水来实现的,这将减少从地下水中抽水的需求,特别是用于家庭和工业用途。到21世纪中叶,由于预计的降水量和引水量而增加的供水量将导致每年平均增加3.9〜99亿立方米的河流排放量和1.7〜29亿立方米的地下水存储量。

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