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Assessment of Climate Change Impact on Snowmelt in Mountainous Watersheds of South Korea Using SLURP Hydrogical Model

机译:使用Slurp Hydricical Model评估韩国山区流域雪花雪地频道的影响

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The purpose of this paper is to evaluate climate impact on snow hydrology using SLURP (Semi-distributed Land Use-based Runoff Process) model for two mountainous watersheds ( 6661.5 km~2 and B; 2694.4 km~2) of South Korea. The climate change results ofCCCma CGCM2 based on SRES A2 and B2 were adopted. Four sets ofNOAAAVHRR images (1997-1998, 1999-2000, 2000-2001) were analyzed to prepare snow-related data of the model. Snow cover areas were extracted using channels 1, 3 and 4, and the snow depth was spatially interpolated using snowfall data of ground meteorological stations. For 4 years (1997-1998, 1999-2000, 2000-2001) discharge comparison, the average Nash-Sutcliffe efficiencies of watersheds during the snow period (December to May) were 0.64 and0.88, respectively In case ofA2 scenario, the 2100 runoff of A and B watersheds for 44.4 % and 85.9 % increase of snowfall increased 67.3 % and 19.6% comparing with the 2000 runoff. In case of B2 scenario, the 2100 runoff for 10.3 % and 41.3 % increase of snowfall increased 38.8 % and 9.8% for A and B watersheds, respectively. The results showed that the time ofsnowmelt runoff was advanced about one month.
机译:本文的目的是利用韩国两个山地流域(6661.5 km〜2)的斯波普(半分布式土地使用基础径流过程)模型来评估对雪水流程的气候影响(6661.5公里; 2694.4 km〜2)。采用了基于SRES A2和B2的CCCMA CGCM2的气候变化结果。分析了四组NoaaavHRR图像(1997-1998,1999-29-2000,2000-2001)以准备模型的雪相关数据。使用通道1,3和4提取雪覆盖区域,并且使用地面气象站的降雪数据在空间内插入雪坡。 4年(1997-1998,1999-2999-2000,2000-2001)放电比较,分别在雪期(12月至5月)期间流域的平均纳什 - Sutcriffe效率为0.64南部,分别为0.6岁,以便在A2场景,2100与2000次径流相比,A和B流域的径流增加了44.4%,增加了85.9%,增加了67.3%和19.6%。在B2场景的情况下,对于A和B流域分别增加了2100次径流10.3%和41.3%的降雪增加38.8%和9.8%。结果表明,径流的时间大约一个月。

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