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首页> 外文期刊>Irrigation and Drainage >ASSESSMENT OF CLIMATE CHANGE IMPACTS ON THE FUTURE HYDROLOGIC CYCLE OF THE HAN RIVER BASIN IN SOUTH KOREA USING A GRID-BASED DISTRIBUTED MODEL
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ASSESSMENT OF CLIMATE CHANGE IMPACTS ON THE FUTURE HYDROLOGIC CYCLE OF THE HAN RIVER BASIN IN SOUTH KOREA USING A GRID-BASED DISTRIBUTED MODEL

机译:基于网格的分布式模型对韩国汉江盆地未来水文循环的气候变化影响评估

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The purpose of this study is to assess the impacts of climate change on the hydrologic cycle of the Han River Basin in South Korea using the Projection of Hydrology via the Grid-based Assessment for Climate Change (PGA-CC) model. PGA-CC is a physically based continuous, long-term, distributed model. The model was calibrated and validated using 9 years (2001-2009) of inflow data from two sub-basins to reservoirs (the Chungju Reservoir and Soyang Reservoir) in the Han River Basin with a 4 km spatial resolution. The average Nash-Sutcliffe model efficiencies of the Chungju and Soyang reservoirs were 0.57 and 0.71, and the average coefficients of determination were 0.65 and 0.72, respectively. The applicability of the PGA-CC model was tested by assessing the future river basin hydrology with the HadGEM3-RA AR5 4.5 and 8.5 climate change scenarios. The annual total discharge from the RCP 4.5 scenario in the 2080s showed a change of up to +33.0% based on the 1070 mm yr(-1) value from the baseline period (1980-2009) due to a +28.1% increase in precipitation. The annual evapotranspiration from the RCP 8.5 scenario showed an increase of up to 46.2% compared to the baseline period of 357 mm yr(-1) due to a temperature increase of 5.4 degrees C. Copyright (C) 2016 John Wiley & Sons, Ltd.
机译:这项研究的目的是通过基于网格的气候变化评估(PGA-CC)模型,利用水文投影来评估气候变化对韩国汉江流域水文循环的影响。 PGA-CC是基于物理的连续,长期,分布式模型。该模型已使用汉江流域两个子流域至汉江流域水库(忠州水库和索阳水库)的9年(2001-2009年)入水数据进行了校准和验证,空间分辨率为4 km。忠州和索阳水库的平均Nash-Sutcliffe模型效率为0.57和0.71,平均确定系数分别为0.65和0.72。通过使用HadGEM3-RA AR5 4.5和8.5气候变化情景评估未来流域水文学,测试了PGA-CC模型的适用性。在2080年代,RCP 4.5情景的年度总排放量显示,与基准期(1980-2009年)的1070 mm yr(-1)值相比,变化高达+ 33.0%,这是由于降水增加了+ 28.1% 。由于温度升高5.4摄氏度,RCP 8.5情景下的年度蒸散量比基线期357毫米yr(-1)增长了高达46.2%。版权所有(C)2016 John Wiley&Sons,Ltd 。

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