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Comparison of monthly rainfall generated from dynamical and statistical downscaling methods: a case study of the Heihe River Basin in China

机译:动态降尺度方法与统计降尺度方法产生的月降水量比较-以中国黑河流域为例

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摘要

Monthly rainfall in the Heihe River Basin (HRB) was simulated by the dynamical downscaling model (DDM) and statistical downscaling model (SDM). The rainy-season rainfall in the HRB obtained by SDM and DDM was compared with the observed datasets (OBS) over the period of 2003-2012. The results showed the following: (1) Both methods reasonably reproduced the spatial pattern of rainy-season rainfall in the HRB with a high-level skill. Rainfall simulated by DDM was better than that by SDM in the upstream, with biases of -12.09 and -13.59 %, respectively; rainfall simulated by SDM was better than that by DDM in the midstream, with biases of 3.91 and -23.22 %, respectively; there was little difference between the rainfall simulated by SDM and DDM in the downstream, with biases of -10.89 and -9.50 %, respectively. (2) Both methods reasonably reproduced monthly rainfall in rainy season in different subregions. Rainfall simulated by DDM was better than that by SDM in May and July in the upstream, whereas rainfall simulated by SDM was closer to OBS except August in the midstream and except August and September in the downstream. (3) For multi-year mean rainy-season rainfall in different stations, there was a little difference between the rainfall simulated by DDM and SDM in Tuole station in the upstream, with biases of -13.16 and -12.40 %, respectively; rainfall in Zhangye station simulated by SDM was overestimated with bias of 14.02 %, and rainfall simulated by DDM was underestimated with bias of -14.60 %; rainfall in Dingxin station simulated by DDM was reproduced better than that by SDM, with biases of -19.34 and -32.75 %, respectively.
机译:利用动态降尺度模型(DDM)和统计降尺度模型(SDM)模拟了黑河流域(HRB)的月降雨量。将SDM和DDM获得的HRB的雨季降雨量与2003-2012年期间的观测数据集(OBS)进行了比较。结果表明:(1)两种方法均能以较高的技巧合理再现HRB中雨季降雨的空间格局。 DDM模拟的上游降雨优于SDM模拟,分别为-12.09和-13.59%。 SDM模拟的降雨在中游要好于DDM,其偏差分别为3.91和-23.22%。 SDM和DDM在下游模拟的降雨之间几乎没有差异,偏差分别为-10.89和-9.50%。 (2)两种方法都合理地再现了不同分区在雨季的月降雨量。 DDM模拟的上游5月和7月的降雨好于SDM,而SDM模拟的降雨除了中游的8月和下游的8月和9月之外,更接近OBS。 (3)对于不同站点的多年平均雨季降水,DDM和SDM模拟的上游Tuole站点的降雨之间存在少许差异,偏差分别为-13.16%和-12.40%; SDM模拟的张ye站降水偏高了14.02%,DDM模拟的降水偏低了-14.60%。 DDM模拟的顶新站降水比SDM模拟的要好,其偏倚分别为-19.34和-32.75%。

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  • 来源
    《Theoretical and applied climatology》 |2017年第2期|437-444|共8页
  • 作者单位

    Chinese Acad Sci, Inst Atmospher Phys, Key Lab Reg Climate Environm Temperate East Asia, 40 HuaYanLi, Beijing 100029, Chaoyang Distri, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China;

    Chinese Acad Sci, Inst Atmospher Phys, Key Lab Reg Climate Environm Temperate East Asia, 40 HuaYanLi, Beijing 100029, Chaoyang Distri, Peoples R China;

    Beijing Normal Univ, State Key Lab Earth Surface Proc & Resource Ecol, Beijing 100087, Peoples R China;

    Chinese Acad Sci, Inst Atmospher Phys, Key Lab Reg Climate Environm Temperate East Asia, 40 HuaYanLi, Beijing 100029, Chaoyang Distri, Peoples R China;

    Chinese Acad Sci, Inst Atmospher Phys, Key Lab Reg Climate Environm Temperate East Asia, 40 HuaYanLi, Beijing 100029, Chaoyang Distri, Peoples R China|Univ Chinese Acad Sci, Beijing 100049, Peoples R China;

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