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Large-scale Simulations of Surface Water and Groundwater with a Coupled Hydrologic Model

机译:具有耦合水文模型的地面水和地下水的大规模模拟

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Research on Predictions in Ungauged Basins (PUB) is a fundamental problem and challenge in hydrology. Coupled atmospheric-hydrologic model can provide a promising tool for us on the hydrologic predictions in ungauged or less gauged basins. A newly coupled atmospheric-hydrologic model system is used to simulate the ten-year (1984 - 1993) water balance in the gauged and hypo-thetically ungauged Mississippi River (MR) basin in term of precipitation. Simulated river discharges and groundwater tables at different sub-basins are compared at daily and monthly time scales. The river discharges simulated with site precipitation data are consistent with the observed, while the results simulated without site precipitation data can also capture the general trend of flood hydrograph. The spatial patterns of variables simulated with the two cases are both reasonable. Research indicates that the coupled model system has the capability for hydrologic simulations as well for flood forecasting and water resources assessment on PUB at a certain extent.
机译:未凝固盆地(PUB)预测的研究是水文中的根本问题和挑战。耦合的大气 - 水文模型可以为我们提供一个有前途的工具,用于我们在未吞噬或更少的测量盆地中的水文预测上。一种新耦合的大气 - 水文模型系统用于模拟衡量和QUOGO - 昆士不贵的密西西比河(MR)盆地的10年(1984年至1993)水平衡期限。在日常和每月时间尺度比较不同子盆地的模拟河流排放和地下水表。用现场降水数据模拟的河流排放与观察到的趋势符合,而在没有现场降水数据的情况下模拟的结果也可以捕获洪水水文的总趋势。用两种情况模拟的变量的空间模式是合理的。研究表明,耦合模型系统在一定程度上对PUB的洪水预测和水资源评估具有水文模拟的能力。

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