地表水地下水耦合模型在大型山丘平原交错区的研发与应用
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孙青言, 陆垂裕, 郭辉, 严聆嘉, 张博
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A coupled surface water-groundwater model and its application in a large-scale hill-plain region
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SUN Qingyan, LU Chuiyu, GUO Hui, YAN Lingjia, ZHANG Bo
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表1 代表性观测井和水文站的NSE和R2
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Tab.1 Nash-Sutcliffe efficiency (NSE) and R2 at representative observation wells and hydrological stations
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观测井地下水埋深拟合效果 | 编号 | 率定期R2 | 验证期R2 | 编号 | 率定期R2 | 验证期R2 | G1 | 0.55 | 0.63 | G12 | 0.65 | 0.76 | G2 | 0.58 | 0.60 | G13 | 0.54 | 0.70 | G3 | 0.56 | 0.64 | G14 | 0.83 | 0.76 | G4 | 0.67 | 0.61 | G15 | 0.75 | 0.66 | G5 | 0.72 | 0.66 | G16 | 0.43 | 0.47 | G6 | 0.45 | 0.63 | G17 | 0.49 | 0.67 | G7 | 0.50 | 0.57 | G18 | 0.75 | 0.80 | G8 | 0.68 | 0.75 | G19 | 0.73 | 0.58 | G9 | 0.49 | 0.62 | G20 | 0.84 | 0.90 | G10 | 0.36 | 0.55 | G21 | 0.55 | 0.69 | G11 | 0.82 | 0.58 | | | | 水文站地表径流拟合效果 | 编号 | 率定期NSE | 验证期NSE | 率定期R2 | 验证期R2 | S1 | 0.64 | 0.60 | 0.71 | 0.80 | S2 | 0.63 | 0.70 | 0.75 | 0.81 | S3 | 0.55 | 0.59 | 0.70 | 0.75 | S4 | 0.68 | 0.75 | 0.73 | 0.85 | S5 | 0.60 | 0.63 | 0.71 | 0.67 | S6 | 0.64 | 0.65 | 0.80 | 0.78 |
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