多源再分析降水数据在拉萨河流域应用对比研究
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郭禹含, 王中根, 伍玉良
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Comparison of applications of different reanalyzed precipitation data in the Lhasa River Basin based on HIMS model
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Yuhan GUO, Zhonggen WANG, Yuliang WU
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表1 拉萨河流域分布式HIMS模型最终调参结果 |
Tab.1 Results of final parameters of the HIMS distributed model in the Lhasa River Basin |
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流域编号 | 土壤蓄水容量Wmm | 产流参数 | 壤中流 系数La | 地下水补给系数Rc | 实际蒸散发系数ε | 基流系数Kb | 汇流参数 | R | | r | C1 | C2 | 1 | 356.0 | 9.00 | 0.10 | 0.23 | 0.01 | 0.10 | 0.01 | 0.06 | 0.05 | 2 | 50.0 | 0.48 | 0.19 | 0.97 | 0.03 | 1.56 | 0.05 | 0.90 | 0.90 | 3 | 50.0 | 0.22 | 0.99 | 0.57 | 0.09 | 0.15 | 0.02 | 0.05 | 0.06 | 4 | 50.0 | 5.31 | 0.10 | 0.14 | 0.01 | 0.16 | 0.03 | 0.05 | 0.25 | 5 | 73.0 | 8.65 | 0.16 | 0.20 | 0.01 | 0.86 | 0.02 | 0.05 | 0.05 | 6 | 50.0 | 3.00 | 0.99 | 0.10 | 0.01 | 0.10 | 0.01 | 0.05 | 0.05 | 7 | 50.0 | 2.88 | 0.10 | 0.19 | 0.02 | 0.96 | 0.01 | 0.06 | 0.05 | 8 | 1000.0 | 3.60 | 0.63 | 0.15 | 0.09 | 0.10 | 0.02 | 0.09 | 0.28 | 9 | 50.0 | 2.62 | 0.36 | 0.51 | 0.01 | 0.15 | 0.01 | 0.07 | 0.16 | 10 | 96.0 | 11.25 | 0.10 | 0.10 | 0.13 | 0.10 | 0.01 | 0.05 | 0.05 | 11 | 93.5 | 0.30 | 0.10 | 0.33 | 0.02 | 0.38 | 0.01 | 0.07 | 0.17 | 12 | 50.0 | 0.22 | 0.10 | 0.10 | 0.01 | 0.14 | 0.01 | 0.13 | 0.07 | 13 | 50.0 | 4.83 | 0.70 | 0.10 | 0.03 | 0.35 | 0.06 | 0.06 | 0.05 | 14 | 50.0 | 0.68 | 0.10 | 0.10 | 0.14 | 0.10 | 0.01 | 0.09 | 0.09 | 15 | 50.0 | 4.34 | 0.99 | 0.15 | 1.00 | 0.13 | 0.01 | 0.05 | 0.05 | 16 | 113.0 | 0.37 | 0.19 | 0.42 | 0.01 | 0.10 | 0.01 | 0.05 | 0.90 |
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