Journal of Water and Climate Change (May 2023)

Quantifying the streamflow change and influencing factors with a spatio-temporal coupling analysis framework

  • Zehui Zhou,
  • Lei Yu,
  • Xiufeng Wu,
  • Luchen Zhang,
  • Shaoze Luo,
  • Yu Zhang,
  • Bin Yong,
  • Junqi Sheng

DOI
https://doi.org/10.2166/wcc.2023.391
Journal volume & issue
Vol. 14, no. 5
pp. 1482 – 1496

Abstract

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Streamflow change and its influencing factors are synchronous and correlated in temporal and spatial scales. The aim of this study is to develop a spatio-temporal coupling analysis framework for quantifying streamflow change and its influencing factors was established. Specifically, the Mann–Kendall test, Pettitt's test, hierarchical cluster analysis, and Ripley's L-function were jointly used to study the spatial heterogeneity of the temporal evolution of streamflow; and the Soil and Water Assessment Tool (SWAT) model was employed to quantify the impacts of climate and human activities on streamflow change. The preliminary application in the Dawen River Basin (China) case has shown that (1) the natural streamflow change in the basin during 1953–2013 is mainly affected by climate change–human activities, followed by climate change and human activities, accounting for a total area of 52.04, 24.90, and 23.06%, respectively; and (2) the vast majority of sub-basins with relatively large natural streamflow change are mainly driven by climate change (i.e., precipitation). In general, the proposed framework can effectively reflect the spatio-temporal patterns of streamflow change and its influencing factors, which can provide a theoretical basis for water resources management in the context of global change. HIGHLIGHTS Developing a spatio-temporal coupling analysis framework for quantifying streamflow and its influencing factors.; Quantifying the contribution of drivers to the streamflow change on the sub-basin scale.; Streamflow change and their spatial patterns in the DRB are mainly driven by climate change–human activities.; The vast majority of sub-basins with relatively large streamflow change are mainly driven by climate change.;

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