Acta Geographica Sinica ›› 2017, Vol. 72 ›› Issue (3): 457-470.doi: 10.11821/dlxb201703008
Special Issue: 黑土侵蚀格局及机理
• Climate Change and Surface Processes • Previous Articles Next Articles
Zhiyuan YANG1(), Chao GAO2, Shuying ZANG1(
), Xiuchun YANG3
Received:
2016-11-13
Revised:
2017-02-13
Online:
2017-03-15
Published:
2017-03-15
Supported by:
Zhiyuan YANG, Chao GAO, Shuying ZANG, Xiuchun YANG. Assessing SWIM model applicability in the black soil region of Northeast China: A case study in the middle and upper reaches of the Wuyuer River Basin[J].Acta Geographica Sinica, 2017, 72(3): 457-470.
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Tab.1
Character parameter of subbasins and accuracy of simulated runoff under different drainage area thresholds
集水区面积(km2) | 子流域个数(个) | 水文单元数量(个) | 年均径流量(m3/s) | R值 | 效率系数E |
---|---|---|---|---|---|
90 | 93 | 1206 | 29.88 | 0.834 | 0.39 |
100 | 37 | 653 | 29.27 | 0.896 | 0.43 |
140 | 29 | 577 | 27.69 | 0.898 | 0.47 |
150 | 27 | 556 | 27.73 | 0.899 | 0.48 |
160 | 27 | 556 | 27.67 | 0.898 | 0.48 |
170 | 25 | 525 | 29.30 | 0.898 | 0.46 |
Tab.2
Calibrated value of main parameter in SWIM model
参数代码 | 参数含义 | 取值范围 | 参数值 | 泾河上游流域参数取值 |
---|---|---|---|---|
thc | 土壤蒸发修正系数 | 0.5~1.5 | 0.7 | 1.6 |
CN | SCS曲线形参数 | 10~100 | 70 | - |
bff | 流域基流修正系数 | 0.2~1.0 | 0.7 | 0.01 |
gwq0 | 土壤初始含水量贡献率 | 0.01~1.0 | 0.03 | 0.5 |
abf0 | 地下水回流速率 | 0.001~1.0 | 0.001 | 0.001 |
roc2 | 汇流系数 | 1~100 | 1.5 | 0.5 |
roc4 | 汇流系数 | 1~100 | 3 | 2 |
sccor | 土壤饱和传导率校正因子 | 0.01~10 | 1.8 | 5 |
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