水稳定同位素示踪的冰川流域水文模拟及不确定性研究
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
), 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
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
Tianhao HE1(), Hongkai GAO1,2(), Xiangying LI3,4, Tianding HAN5, Zhihua HE6, Zhicai ZHANG7, Zheng DUAN8, Min LIU1,2(), Yongjian DING5,9
), Hongkai GAO1,2(), Xiangying LI3,4, Tianding HAN5, Zhihua HE6, Zhicai ZHANG7, Zheng DUAN8, Min LIU1,2(), Yongjian DING5,9
图3. 在检验期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
Fig.3. 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 evaluation period
