Abstract
The impact of climate change on streamflow in the Xitiaoxi catchment is assessed by using VIC (variable infiltration capacity) model coupled with PRECIS (providing regional climate for impacts studies). Results show that the VIC model is adaptable for the study area. Both deterministic coefficient and Nash-Suttcliffe efficiency coefficient are greater than 0.75, with a good agreement between observed and simulated discharge. The runoff will increase in the future, especially during flood seasons. The magnitude of floods in the future (2021–2050) under A2 and B2 scenarios will be greater than that during the baseline period (1961–1990), but it may not exceed that during the 1990s.
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Foundation item: Supported by China/UK Scientific Cooperation Project from the Ministry of Science and Technology of China (2006DFA71390) and Open Research Foundation of China Institute of Water Resources and Hydropower Research
Biography: LIU Liu (1986–), male, Ph.D. candidate, research direction: flood risk, response of hydrology and water resources to climate change.
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Liu, L., Xu, Z. & Huang, J. Impact of climate change on streamflow in the Xitiaoxi catchment, Taihu Basin. Wuhan Univ. J. Nat. Sci. 14, 525–531 (2009). https://doi.org/10.1007/s11859-009-0612-z
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DOI: https://doi.org/10.1007/s11859-009-0612-z
Key words
- VIC (variable infiltration capacity) Model
- climate change
- PRECIS (providing regional climate for impacts studies)
- streamflow
- Xitiaoxi catchment