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首页> 外文期刊>Hydrological Processes >Impact of the spatial variability of daily precipitation on hydrological projections: A comparison of GCM‐ and RCMdriven cases in the Han River basin, Korea
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Impact of the spatial variability of daily precipitation on hydrological projections: A comparison of GCM‐ and RCMdriven cases in the Han River basin, Korea

机译:日降水量的空间变化对水文预测的影响:韩国汉江流域GCM和RCM驱动案例的比较

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摘要

In this study, we investigate the impact of the spatial variability of daily precipitation on hydrological projections based on a comparative assessment of streamflow simulations driven by a global climate model (GCM) and two regional climate models (RCMs). A total of 12 different climate input datasets, that is, the raw and bias-corrected GCM and raw and bias-corrected two RCMs for the reference and future periods, are fed to a semidistributed hydrological model to assess whether the bias correction using quantile mapping and dynamical downscaling using RCMs can improve streamflow simulation in the Han River basin, Korea. A statistical analysis of the daily precipitation demonstrates that the precipitation simulated by the GCM fails to capture the large variability of the observed daily precipitation, in which the spatial autocorrelation decreases sharply within a relatively short distance. However, the spatial variability of precipitation simulated by the two RCMs shows better agreement with the observations. After applying bias correction to the raw GCM and raw RCMs outputs, only a slight change is observed in the spatial variability, whereas an improvement is observed in the precipitation intensity. Intensified precipitation but with the same spatial variability of the raw output from the bias-corrected GCM does not improve the heterogeneous runoff distributions, which in turn regulate unrealistically high peak downstream streamflow. GCM-simulated precipitation with a large bias correction that is necessary to compensate for the poor performance in present climate simulation appears to distort streamflow patterns in the future projection, which leads to misleading projections of climate change impacts on hydrological extremes.
机译:在这项研究中,我们根据全球气候模型(GCM)和两个区域气候模型(RCM)驱动的水流模拟的比较评估,研究了每日降水的空间变异性对水文预测的影响。总共12个不同的气候输入数据集,即参考时期和未来时期的原始和偏差校正的GCM以及原始和偏差校正的两个RCM,被馈送到半分布式水文模型以评估是否使用分位数映射进行偏差校正使用RCM进行动态降尺度可以改善韩国汉江流域的水流模拟。对日降水量的统计分析表明,由GCM模拟的降水未能捕获观测到的日降水量的较大变化,其中空间自相关在相对较短的距离内急剧下降。然而,两个RCM模拟的降水的空间变异性与观测结果更好地吻合。对原始GCM和原始RCM输出进行偏差校正后,仅观察到空间变异性略有变化,而观察到降水强度有所改善。降水增加但偏向校正的GCM的原始产出具有相同的空间变异性,并不能改善非均质径流分布,反过来又调节了不切实际的高峰值下游水流。 GCM模拟的降水量具有较大的偏差校正,这是弥补目前气候模拟效果不佳所必需的,这似乎会使未来的预测中的水流模式发生扭曲,从而导致对气候变化对极端水文影响的预测具有误导性。

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