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Groundwater Simulation in the Yangtze River Basin with a Coupled Climate-Hydrologic Model

机译:水文模型耦合的长江流域地下水模拟

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The effect of climate change on groundwater as one important research content of IPCC, IUGC, WMO and IAHS is well worth our research. A coupled climate-hydrologic model is developed and used to simulate the interaction of climate and hydrology components over Yangtze River basin. The coupled climate-hydrology model has various schemes handling the transfer of various variables between the coarse grid-climate model and the finer-grid hydrologic model. The hydrologk model system with a grid resolution of 20 km is forced with the global 6-h gridded NCEP/NCAR reanalysis data for simulations. The parameters, boundary conditions, and initial conditions are determined based on spatial, climatic and hydrogeologic multivariate data information (Le., satellites, remote sensing, geological survey). The results show that the simulation captures the spatial patterns of soil moisture, and groundwater depth and recharge. Because of the lack of detailed spatial hydrogeologic parameters to a great extent, discrepancy in simulated values occurs for some variables. The field research and test should be carried out and basin database should be constructed to improve the simulation capacity of the model.
机译:作为IPCC,IGC,WMO和IAHS的重要研究内容之一,气候变化对地下水的影响非常值得我们研究。建立了耦合的水文模型,用于模拟长江流域气候和水文要素之间的相互作用。耦合的气候水文学模型具有处理粗网格气候模型和细网格水文模型之间各种变量转移的各种方案。网格分辨率为20 km的Hydrologk模型系统被强制使用全球6小时网格化NCEP / NCAR再分析数据进行仿真。参数,边界条件和初始条件是根据空间,气候和水文地质多变量数据信息(例如,卫星,遥感,地质勘测)确定的。结果表明,该模拟捕获了土壤水分,地下水深度和补给的空间格局。由于在很大程度上缺乏详细的空间水文地质参数,因此某些变量的模拟值出现了差异。应进行现场研究和试验,并建立流域数据库,以提高模型的仿真能力。

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