Effect partition of climate and catchment changes on runoff variation at the headwater region of the Yellow River based on the Budyko complementary relationship
- 1. State Key Laboratory of Hydroscience and Engineering, Tsinghua University, Beijing 100084 (China)
- 2. State Key Laboratory of Plateau Ecology and Agriculture, Qinghai University, Xining, Qinghai 810016 (China)
- 3. Department of Earth and Environmental Engineering, Columbia University, NY, New York 10027 (United States)
Description
Highlights: • The effect of climate and catchment changes on runoff variation can be partitioned precisely using the Complementary method. • The change of precipitation has a positive impacts on the runoff variation, while the catchment change has a negative impacts on the runoff variation. • Climate changes are the main reason for runoff reduction at the headwater region of the Yellow River. The headwater region of the Yellow River (HRYR) is one of the most important water supply areas of the whole river basin, which has suffered a serious water shortage problem for recent years. A better understanding of impacts of climate and catchment changes on runoff variation will help to determine efficient measures to deal with the runoff reduction in the Yellow River. The Budyko complementary relationship between the partial elasticity of runoff (R) with respect to precipitation (P) and that with potential evapotranspiration (E0) was used in this study to partition the effects of climate and catchment changes on runoff variation at the HRYR. The upper and lower bounds of the contributions of climate and catchment changes to runoff variation were determined for every five years during 1961–2010. Results show that the complementary relation method based on the Budyko hypothesis can partition the contributions of climate and catchment changes to runoff variation effectively. And the climate changes are the main reasons (account for 60%–70% of the runoff variation) for runoff reduction at the HRYR. The sensitivity coefficient of R with respect to P has a significant decreasing trend at the 0.05 level with arid ratio (E0/P) and that with respect to E0 has a significant increasing trend at the 0.05 level with E0/P, indicating that with drying climate, R becomes more insensitive to climate changes. More precipitation is consumed by evapotranspiration returning to the atmosphere, leading to the runoff reduction at the HRYR.
Availability note (English)
Available from http://dx.doi.org/10.1016/j.scitotenv.2018.06.195Additional details
Identifiers
- DOI
- 10.1016/j.scitotenv.2018.06.195;
- PII
- S004896971832271X;
Publishing Information
- Journal Title
- Science of the Total Environment
- Journal Volume
- 643
- Journal Page Range
- p. 1166-1177
- ISSN
- 0048-9697
- CODEN
- STENDL
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 53054072
- Subject category
- S54: ENVIRONMENTAL SCIENCES;
- Descriptors DEI
- ATMOSPHERIC PRECIPITATIONS; CLIMATIC CHANGE; RUNOFF; WATER REQUIREMENTS; WATER SUPPLY; YELLOW RIVER
- Descriptors DEC
- DEMAND; ENVIRONMENTAL TRANSPORT; MASS TRANSFER; RIVERS; SURFACE WATERS
Optional Information
- Copyright
- Copyright (c) 2018 Elsevier B.V. All rights reserved.