Articles | Volume 26, issue 3
https://doi.org/10.5194/hess-26-589-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-26-589-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
07 Feb 2022
Research article |
| 07 Feb 2022
| 07 Feb 2022
Drivers of drought-induced shifts in the water balance through a Budyko approach
Blue Forest Conservation, Sacramento, CA, USA
Department of Civil and Environmental Engineering, University of California, Berkeley, CA 94720, USA
Francesco Avanzi
CIMA Research Foundation, via Armando Magliotto 2, 17100, Savona, Italy
Steven D. Glaser
Department of Civil and Environmental Engineering, University of California, Berkeley, CA 94720, USA
Roger C. Bales
Department of Civil and Environmental Engineering, University of California, Berkeley, CA 94720, USA
Sierra Nevada Research Institute, University of California, Merced, CA, USA
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Cited
18 citations as recorded by crossref.
- Impacts of hydrometeorological regime shifts on drought Propagation: The meteorological to hydrological perspective J. Wu et al. 10.1016/j.jhydrol.2024.131476
- Stability of water yield in watersheds Y. Yan et al. 10.1007/s11430-023-1206-4
- Runoff response to the uncertainty from key water-budget variables in a seasonally snow-covered mountain basin G. Cui et al. 10.1016/j.ejrh.2023.101601
- 流域水文系统产水机制稳定性研究 宇. 颜 et al. 10.1360/SSTe-2023-0053
- Evaporation enhancement drives the European water-budget deficit during multi-year droughts C. Massari et al. 10.5194/hess-26-1527-2022
- MODIS-based modeling of evapotranspiration from woody vegetation supported by root-zone water storage G. Cui et al. 10.1016/j.rse.2024.114000
- Disentangling the role of subsurface storage in the propagation of drought through the hydrological cycle G. Bruno et al. 10.1016/j.advwatres.2022.104305
- Attribution of Extreme Drought Events and Associated Physical Drivers across Southwest China Using the Budyko Framework X. Sun et al. 10.3390/rs15112702
- The salmonid and the subsurface: Hillslope storage capacity determines the quality and distribution of fish habitat D. Dralle et al. 10.1002/ecs2.4436
- Decline in Seasonal Snow during a Projected 20-Year Dry Spell B. Hatchett et al. 10.3390/hydrology9090155
- Assessment of the shift in the precipitation–streamflow relationship influenced by multiyear drought, Yellow River basin, China Q. Liu et al. 10.1016/j.scitotenv.2023.166203
- Globally assessing how evapotranspiration feedbacks govern the impacts of multi-year droughts Q. Liu et al. 10.1016/j.jhydrol.2024.131852
- Alignment between water inputs and vegetation green‐up reduces next year's runoff efficiency S. Newcomb et al. 10.1002/hyp.15211
- Contribution of changes in vegetation composition and climate variability on streamflow across the global watersheds X. Tan et al. 10.1016/j.catena.2023.107394
- Examining the Water Scarcity Vulnerability in US River Basins Due To Changing Climate F. Wolkeba et al. 10.1029/2023GL106004
- Exploring drought‐to‐flood interactions and dynamics: A global case review M. Barendrecht et al. 10.1002/wat2.1726
- Water Balance Shifts Induced by Multiyear Drought Within the Budyko Framework Q. Liu et al. 10.1029/2022JD036758
- Fewer Basins Will Follow Their Budyko Curves Under Global Warming and Fossil‐Fueled Development F. Jaramillo et al. 10.1029/2021WR031825
16 citations as recorded by crossref.
- Impacts of hydrometeorological regime shifts on drought Propagation: The meteorological to hydrological perspective J. Wu et al. 10.1016/j.jhydrol.2024.131476
- Stability of water yield in watersheds Y. Yan et al. 10.1007/s11430-023-1206-4
- Runoff response to the uncertainty from key water-budget variables in a seasonally snow-covered mountain basin G. Cui et al. 10.1016/j.ejrh.2023.101601
- 流域水文系统产水机制稳定性研究 宇. 颜 et al. 10.1360/SSTe-2023-0053
- Evaporation enhancement drives the European water-budget deficit during multi-year droughts C. Massari et al. 10.5194/hess-26-1527-2022
- MODIS-based modeling of evapotranspiration from woody vegetation supported by root-zone water storage G. Cui et al. 10.1016/j.rse.2024.114000
- Disentangling the role of subsurface storage in the propagation of drought through the hydrological cycle G. Bruno et al. 10.1016/j.advwatres.2022.104305
- Attribution of Extreme Drought Events and Associated Physical Drivers across Southwest China Using the Budyko Framework X. Sun et al. 10.3390/rs15112702
- The salmonid and the subsurface: Hillslope storage capacity determines the quality and distribution of fish habitat D. Dralle et al. 10.1002/ecs2.4436
- Decline in Seasonal Snow during a Projected 20-Year Dry Spell B. Hatchett et al. 10.3390/hydrology9090155
- Assessment of the shift in the precipitation–streamflow relationship influenced by multiyear drought, Yellow River basin, China Q. Liu et al. 10.1016/j.scitotenv.2023.166203
- Globally assessing how evapotranspiration feedbacks govern the impacts of multi-year droughts Q. Liu et al. 10.1016/j.jhydrol.2024.131852
- Alignment between water inputs and vegetation green‐up reduces next year's runoff efficiency S. Newcomb et al. 10.1002/hyp.15211
- Contribution of changes in vegetation composition and climate variability on streamflow across the global watersheds X. Tan et al. 10.1016/j.catena.2023.107394
- Examining the Water Scarcity Vulnerability in US River Basins Due To Changing Climate F. Wolkeba et al. 10.1029/2023GL106004
- Exploring drought‐to‐flood interactions and dynamics: A global case review M. Barendrecht et al. 10.1002/wat2.1726
Latest update: 19 Nov 2024
Short summary
Predicting how much water will end up in rivers is more difficult during droughts because the relationship between precipitation and streamflow can change in unexpected ways. We differentiate between changes that are predictable based on the weather patterns and those harder to predict because they depend on the land and vegetation of a particular region. This work helps clarify why models are less accurate during droughts and helps predict how much water will be available for human use.
Predicting how much water will end up in rivers is more difficult during droughts because the...
