水稳定同位素示踪的冰川流域水文模拟及不确定性研究
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何天豪 1( ), 高红凯 1,2( ), 李向应 3,4, 韩添丁 5, 贺志华 6, 张志才 7, 段峥 8, 刘敏 1,2( ), 丁永建 5,9
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Hydrological simulation traced by water stable isotope and uncertainty analysis in a glacier catchment: taking Glacier No. 1 in headwater of Urumqi River as an example
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Tianhao HE 1( ), Hongkai GAO 1,2( ), Xiangying LI 3,4, Tianding HAN 5, Zhihua HE 6, Zhicai ZHANG 7, Zheng DUAN 8, Min LIU 1,2( ), Yongjian DING 5,9
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图2. 在率定期4种方案有效参数集模拟的日径流深、径流δ18O、各海拔高度带冰川年物质平衡的不确定性范围
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Fig.2. Uncertainty envelopes of daily runoff depth, runoff δ18O, and annual glacier mass balance in different elevation bands, produced by the valid parameter sets of the four schemes in calibration period
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