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

机译:水文耦合模型对地表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:疏ga盆地(PUB)的预测研究是水文学中的一个基本问题和挑战。耦合的大气水文模型可以为我们提供一个有前途的工具,用于我们对未开挖或较少测量盆地的水文预测。一个新耦合的大气水文模型系统被用来模拟十年(1984-1993)的降水量,该降水量是在假设的和无假设的密西西比河(MR)流域中进行的。在每日和每月的时间尺度上比较不同子流域的模拟河流流量和地下水位。用现场降水数据模拟的河流流量与实测值一致,而没有现场降水数据的模拟结果也可以反映洪水水位的总体趋势。用这两种情况模拟的变量的空间格局都是合理的。研究表明,耦合模型系统在一定程度上具有水文模拟的能力,也具有一定的洪水预报和水资源评估能力。

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