Articles | Volume 20, issue 6
https://doi.org/10.5194/hess-20-2195-2016
© 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-20-2195-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
A two-parameter Budyko function to represent conditions under which evapotranspiration exceeds precipitation
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
Center for Climate Systems Modeling (C2SM), ETH Zurich, Zurich, Switzerland
Lukas Gudmundsson
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
Boris Orlowsky
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
Sonia I. Seneviratne
Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
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71 citations as recorded by crossref.
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66 citations as recorded by crossref.
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- The Budyko functions under non-steady-state conditions R. Moussa & J. Lhomme 10.5194/hess-20-4867-2016
- Assessing Hydrological Response and Resilience of Watersheds as Strategy for Climatic Change Adaptation in Neotropical Region M. Ogasawara et al. 10.3390/su16208910
- Assessing the impact of future climate scenarios on crop water requirements and agricultural water supply across different climatic zones of Pakistan M. Shafeeque & A. Bibi 10.3389/feart.2023.1283171
- Long‐Term Water Imbalances of Watersheds Resulting From Biases in Hydroclimatic Data Sets for Water Budget Analyses X. Tan et al. 10.1029/2021WR031209
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- Global analysis of the hydrologic sensitivity to climate variability M. Domínguez-Tuda & H. Gutiérrez-Jurado 10.1016/j.jhydrol.2021.126720
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- The Shrinkage of Lake Lop Nur in the Twentieth Century: A Comprehensive Ecohydrological Analysis D. Cai et al. 10.1175/JHM-D-21-0217.1
- Quantifying uncertainty sources in runoff change attribution based on the Budyko framework C. Mo et al. 10.1016/j.jhydrol.2024.130790
- Modeling streamflow variability at the regional scale: (1) perceptual model development through signature analysis F. Fenicia & J. McDonnell 10.1016/j.jhydrol.2021.127287
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- Multi-model climatic water balance prediction in the Zala River Basin (Hungary) based on a modified Budyko framework P. Csáki et al. 10.2478/johh-2020-0016
- Estimation and attribution of water storage changes in regulated lakes based on Budyko’s supply–demand framework M. Zhou et al. 10.1016/j.ejrh.2023.101505
- Explanation of climate and human impacts on sediment discharge change in Darwinian hydrology: Derivation of a differential equation J. Zhang et al. 10.1016/j.jhydrol.2018.02.084
- Sensitivity of aridity diagnoses to land-atmosphere coupling in South America J. Eugenio Russmann et al. 10.1007/s00382-024-07413-w
- Effect of watershed disturbance on seasonal hydrological drought: An improved double mass curve (IDMC) technique Y. Aryal & J. Zhu 10.1016/j.jhydrol.2020.124746
5 citations as recorded by crossref.
- A scaling approach to Budyko's framework and the complementary relationship of evapotranspiration in humid environments: case study of the Amazon River basin A. Carmona et al. 10.5194/hess-20-589-2016
- Hydroclimatic and ecohydrological resistance/resilience conditions across tropical biomes of Costa Rica G. Esquivel‐Hernández et al. 10.1002/eco.1860
- Vegetation regulation on streamflow intra‐annual variability through adaption to climate variations S. Ye et al. 10.1002/2015GL066396
- Uncertainty of runoff sensitivity to climate change in the Amazon River basin A. Carmona et al. 10.1111/nyas.14515
- Urbanization and climate change: Insights from eco-hydrological diagnostics D. Cai et al. 10.1016/j.scitotenv.2018.07.319
Saved (preprint)
Latest update: 21 Nov 2024
Short summary
The widely used Budyko framework is by definition limited to steady-state conditions. In this study we analytically derive a new, two-parameter formulation of the Budyko framework that represents conditions under which evapotranspiration exceeds precipitation. This is technically achieved by rotating the water supply limit within the Budyko space. The new formulation is shown to be capable to represent first-order seasonal dynamics within the hydroclimatological system.
The widely used Budyko framework is by definition limited to steady-state conditions. In this...