Estimation of stream water components and residence time in a permafrost catchment in the central Tibetan Plateau using long-term water stable isotopic data
Shaoyong Wang,Xiaobo He,Shichang Kang,Hui Fu,and Xiaofeng Hong
Shaoyong Wang
State Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000,
China
College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
State Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000,
China
Shichang Kang
State Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000,
China
College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
Hui Fu
State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, China
Xiaofeng Hong
Water Resources Department, Changjiang River Scientific Research
Institute, Wuhan 430010, China
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Total article views: 3,070 (including HTML, PDF, and XML)
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Total article views: 2,048 (including HTML, PDF, and XML)
Thereof 1,988 with geography defined
and 60 with unknown origin.
Total article views: 1,022 (including HTML, PDF, and XML)
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This study used the sine-wave exponential model and long-term water stable isotopic data to estimate water mean residence time (MRT) and its influencing factors in a high-altitude permafrost catchment (5300 m a.s.l.) in the central Tibetan Plateau (TP). MRT for stream and supra-permafrost water was estimated at 100 and 255 d, respectively. Climate and vegetation factors affected the MRT of stream and supra-permafrost water mainly by changing the thickness of the permafrost active layer.
This study used the sine-wave exponential model and long-term water stable isotopic data to...
