Identifying how future climate and land use/cover changes impact streamflow in Xinanjiang Basin, East China

Identifying how future climate and land use/cover changes impact streamflow in Xinanjiang Basin, East China

Guo, Yuxue (Zhejiang University)
Fang, Guohua (Hohai University)
Xu, Yue Ping (Zhejiang University)
Tian, X. (TU Delft Water Resources)
Xie, Jingkai (Zhejiang University)

2020

Climate and land use/cover changes are the main factors altering hydrological regimes. To understand the impacts of climate and land use/cover changes on streamflow within a specific catchment, it is essential to accurately quantify their changes given many possibilities. We propose an integrated framework to assess how individual and combined climate and land use/cover changes impact the streamflow of Xinanjiang Basin, in East China, in the future. Five bias-corrected and downscaled General Circulation Model (GCM) projections are used to indicate the inter-model uncertainties under three Representative Concentration Pathways (RCPs). Additionally, three land use/cover change scenarios representing a range of tradeoffs between ecological protection (EP) and urban development (UD) are projected by Cellular Automata - Markov (CA-Markov). The streamflow in 2021–2050 is then assessed using the calibrated Soil and Water Assessment Tool (SWAT) with 15 scenarios and 75 possibilities. Finally, the uncertainty and attribution of streamflow changes to climate and land use/cover changes at monthly and annual scale are analyzed. Results show that while both land use/cover change alone and combined changes project an increase in streamflow, there is a disagreement on the direction of streamflow change under climate change alone. Future streamflow may undergo a more blurred boundary between the flood and non-flood seasons, potentially easing the operation stress of Xinanjiang Reservoir for water supply or hydropower generation. We find that the impacts of climate and land use/cover changes on monthly mean streamflow are sensitive to the impermeable area (IA). The impacts of climate change are stronger than those induced by land use/cover change under EP (i.e., lower IA); and land use/cover change has a greater impact in case of UD (i.e., higher IA). However, changes in annual mean streamflow are mainly driven by land use/cover change, and climate change may decrease the influence attributed to land use/cover change.

Attribution
Climate change
Land use/cover change
Multiple scenarios
Streamflow response
Uncertainty

http://resolver.tudelft.nl/uuid:dce4748c-e881-4512-b224-ec934795f250

https://doi.org/10.1016/j.scitotenv.2019.136275

2022-01-07

0048-9697

Science of the Total Environment, 710

Accepted Author Manuscript

Institutional Repository

journal article

© 2020 Yuxue Guo, Guohua Fang, Yue Ping Xu, X. Tian, Jingkai Xie