Impact of projected climate change on the hydrology in the headwaters of the Yellow River basin |
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| Authors: | Yueguan Zhang Fengge Su Zhenchun Hao Chongyu Xu Zhongbo Yu Lu Wang Kai Tong |
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| Institution: | 1. Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China;2. State Key Laboratory of Hydrology‐Water Resources and Hydraulic Engineering, Hohai University, Nanjing, China;3. College of Water Resources and environment, Hohai University, Nanjing, China;4. State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, Wuhan, China;5. Department of Geosciences, University of Oslo, Oslo, Norway;6. Department of Geoscience, University of Nevada, Las Vegas, NV, USA;7. Faculty of Civil Engineering and Geosciences, Delft University of Technology, Delft, The Netherlands |
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| Abstract: | Located in the northeast of the Tibetan Plateau, the headwaters of the Yellow River basin (HYRB) are very vulnerable to climate change. In this study, we used the Soil and Water Assessment Tool (SWAT) model to assess the impact of future climate change on this region's hydrological components for the near future period of 2013–2042 under three emission scenarios A1B, A2 and B1. The uncertainty in this evaluation was considered by employing Bayesian model averaging approach on global climate model (GCM) multimodel ensemble projections. First, we evaluated the capability of the SWAT model for streamflow simulation in this basin. Second, the GCMs' monthly ensemble projections were downscaled to daily climate data using the bias‐correction and spatial‐disaggregation method and then were utilized as input into the SWAT model. The results indicate the following: (1) The SWAT model exhibits a good performance for both calibration and validation periods after adjusting parameters in snowmelt module and establishing elevation bands in sub‐basins. (2) The projected precipitation suggests a general increase under all three scenarios, with a larger extent in both A1B and B1 and a slight variation for A2. With regard to temperature, all scenarios show pronounced warming trends, of which A2 displays the largest amplitude. (3) In the terms of total runoff from the whole basin, there is an increasing trend in the future streamflow at Tangnaihai gauge under A1B and B1, while the A2 scenario is characterized by a declining trend. Spatially, A1B and B1 scenarios demonstrate increasing trends across most of the region. Groundwater and surface runoffs indicate similar trends with total runoff, whereas all three scenarios exhibit an increase in actual evapotranspiration. Generally, both A1B and B1 scenarios suggest a warmer and wetter tendency over the HYRB in the forthcoming decades, while the case for A2 indicates a warmer and drier trend. Findings from this study can provide beneficial reference to water resource and eco‐environment management strategies for governmental policymakers. Copyright © 2015 John Wiley & Sons, Ltd. |
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| Keywords: | climate change SWAT model Bayesian model averaging the headwaters of the Yellow River basin Tibetan Plateau |
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