Articles | Volume 20, issue 1
https://doi.org/10.5194/hess-20-393-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/hess-20-393-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
New interpretation of the role of water balance in an extended Budyko hypothesis in arid regions
C. Du
Key Laboratory of Water Cycle and Related Land Surface Processes,
Institute of Geographic Sciences and Natural Resources Research, Chinese
Academy of Sciences, Beijing 100101, China
University of Chinese Academy of Sciences, Beijing, 100049, China
F. Sun
CORRESPONDING AUTHOR
Key Laboratory of Water Cycle and Related Land Surface Processes,
Institute of Geographic Sciences and Natural Resources Research, Chinese
Academy of Sciences, Beijing 100101, China
J. Yu
CORRESPONDING AUTHOR
Key Laboratory of Water Cycle and Related Land Surface Processes,
Institute of Geographic Sciences and Natural Resources Research, Chinese
Academy of Sciences, Beijing 100101, China
X. Liu
Key Laboratory of Water Cycle and Related Land Surface Processes,
Institute of Geographic Sciences and Natural Resources Research, Chinese
Academy of Sciences, Beijing 100101, China
State Key Laboratory of Desert and Oasis Ecology, Xinjiang, Institute of
Ecology and Geography, Chinese Academy of Sciences, Urumqi, 830011, China
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- Unraveling the sensitivity and nonlinear response of water use efficiency to the water–energy balance and underlying surface condition in a semiarid basin Q. Fang et al. 10.1016/j.scitotenv.2019.134405
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- Controlling Factors of Evapotranspiration Predictability Under Diverse Climates With the Effects of Water Storage Change in the Budyko Framework C. Wu et al. 10.1029/2023WR034499
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- Modeling streamflow sensitivity to climate warming and surface water inputs in a montane catchment K. Hale et al. 10.1016/j.ejrh.2021.100976
- Drivers of drought-induced shifts in the water balance through a Budyko approach T. Maurer et al. 10.5194/hess-26-589-2022
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- Three-dimensional Budyko framework incorporating terrestrial water storage: Unraveling water-energy dynamics, vegetation, and ocean-atmosphere interactions Q. He et al. 10.1016/j.scitotenv.2023.166380
- Can we trust remote sensing evapotranspiration products over Africa? I. Weerasinghe et al. 10.5194/hess-24-1565-2020
- Application of Budyko framework to irrigation districts in China under various climatic conditions H. Chen et al. 10.1002/hyp.14542
- Climate vs. Human Impact: Quantitative and Qualitative Assessment of Streamflow Variation H. Kazemi et al. 10.3390/w13172404
- The importance of climate and anthropogenic influence in precipitation partitioning in the contiguous United States S. Alonso Vicario et al. 10.1016/j.jhydrol.2024.130984
- Impacts of climate and environmental changes on water resources: A multi-scale study based on Nakanbé nested watersheds in West African Sahel Y. Gbohoui et al. 10.1016/j.ejrh.2021.100828
- Understanding interactions among climate, water, and vegetation with the Budyko framework G. Gan et al. 10.1016/j.earscirev.2020.103451
- Quantifying the Relative Contribution of the Climate Change and Human Activity on Runoff in the Choshui River Alluvial Fan, Taiwan H. Chen et al. 10.3390/land10080825
- Development of a simple Budyko-based framework for the simulation and attribution of ET variability in dry regions X. Xu et al. 10.1016/j.jhydrol.2022.127955
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Latest update: 23 Nov 2024
Short summary
We define the equivalent precipitation to include local precipitation, inflow water and soil water storage change as the water supply in the Budyko framework. With the newly defined water supply, the Budyko curve can successfully describe the relationship between the evapotranspiration ratio and the aridity index at both annual and monthly timescales in unclosed basins. We develop a new Fu-type Budyko equation with two non-dimensional parameters (ω and λ) based on the deviation of Fu's equation.
We define the equivalent precipitation to include local precipitation, inflow water and soil...