Abstract
Many studies have focused on analyzing variation characteristics of the watershed resilience based on different indicators, while few efforts have been made to quantificationally evaluate contributions of climatic and anthropogenic factors to the varied resilience. In this study, we investigate changes in the seasonal runoff resilience of the entire Yangtze River basin during 1961–2014 by using a convex model and a resilience indicator (Pi). The MIKE 11HD model and the regression method were adopted to further differentiate effects of climate variations and human activities. Results show that climate variation (especially droughts and floods) and human activities exert negative and positive effects, respectively, and become primary reasons for falling and increasing trends in entire watershed resilience. These impacts grow with time under the gradually intensified climate variability and human activity.
| Original language | English |
|---|---|
| Pages (from-to) | 1817-1833 |
| Number of pages | 17 |
| Journal | Water Science & Technology: Water Supply |
| Volume | 21 |
| Issue number | 4 |
| Early online date | 2 Feb 2021 |
| DOIs | |
| Publication status | Published - 1 Jun 2021 |
Bibliographical note
© 2021 The Authors.Funding
This work was supported by the CRSRI Open Research Program (Nos. CKWV2018463/KY, CKWV2019727/KY and CKWV2017502/KY) and the Research Program of the Education Department of Hunan Province (No. 20B021). We also highly appreciate the valuable insights from the reviewers.
| Funders | Funder number |
|---|---|
| Education Department of Hunan Province | 20B021 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 13 Climate Action
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