Results 11 to 20 of about 1,927 (195)

Evapotranspiration Estimation with the Budyko Framework for Canadian Watersheds

open access: yesHydrology
Actual evapotranspiration (AET) estimation plays a crucial role in watershed management. Hydrological models are commonly used to simulate watershed responses and estimate AET.
Zehao Yan, Zhong Li, Brian Baetz
doaj   +3 more sources

Systematic shifts in Budyko relationships caused by groundwater storage changes [PDF]

open access: yesHydrology and Earth System Sciences, 2017
Traditional Budyko analysis is predicated on the assumption that the watershed of interest is in dynamic equilibrium over the period of study, and thus surface water partitioning will not be influenced by changes in storage.
L. E. Condon, R. M. Maxwell
doaj   +4 more sources

Shift of annual water balance in the Budyko space for catchments with groundwater-dependent evapotranspiration [PDF]

open access: yesHydrology and Earth System Sciences, 2016
The Budyko framework represents the general relationship between the evapotranspiration ratio (F) and the aridity index (φ) for the mean annual steady-state water balance at the catchment scale.
X.-S. Wang, Y. Zhou
doaj   +3 more sources

Does the Budyko curve reflect a maximum-power state of hydrological systems? A backward analysis [PDF]

open access: yesHydrology and Earth System Sciences, 2016
Almost all catchments plot within a small envelope around the Budyko curve. This apparent behaviour suggests that organizing principles may play a role in the evolution of catchments.
M. Westhoff   +3 more
doaj   +4 more sources

Is There a Baseflow Budyko Curve? [PDF]

open access: yesWater Resources Research, 2019
AbstractThere is no general theory to explain differences in baseflow between catchments, despite evidence that it is mainly controlled by climate and landscape. One hypothesis is that baseflow fraction (the ratio between baseflow and precipitation) can be primarily attributed to the aridity index (the ratio between potential evapotranspiration and ...
Sebastian J. Gnann   +2 more
openaire   +5 more sources

Incorporating the Vadose Zone into the Budyko Framework [PDF]

open access: yesWater, 2017
The Budyko framework provides a quantitative description of long-term average annual evapotranspiration at catchment scales in terms of macro-climatic variables. This framework, however, makes no reference to the vadose zone because it neglects changes in ubsurface storage in the catchment water balance.
Garrison Sposito
openaire   +2 more sources

Assessing future availability of water resources in Taiwan based on the Budyko framework

open access: yesEcological Indicators, 2023
Assessing water resources availability in a changing climate is a determinant of promoting sustainable development in a region. Such assessment should better be inter-basin in order to unveil a region’s overall risk, so a time-varying Budyko framework is
Tsung-Yu Lee   +4 more
doaj   +2 more sources

Water scarcity, data scarcity and the Budyko curve—An application in the Lower Jordan River Basin

open access: yesJournal of Hydrology: Regional Studies, 2017
Study region: Lower Jordan River Basin, Eastern Mediterranean Study focus: Water scarcity and data scarcity are two of the main challenges for water management in the study region, therefore, all possible information should be extracted from existing ...
Anne Gunkel, Jens Lange
doaj   +2 more sources

A two-parameter Budyko function to represent conditions under which evapotranspiration exceeds precipitation [PDF]

open access: yesHydrology and Earth System Sciences, 2016
A comprehensive assessment of the partitioning of precipitation (P) into evapotranspiration (E) and runoff (Q) is of major importance for a wide range of socio-economic sectors.
P. Greve   +3 more
doaj   +3 more sources

New interpretation of the role of water balance in an extended Budyko hypothesis in arid regions [PDF]

open access: yesHydrology and Earth System Sciences, 2016
The Budyko hypothesis (BH) is an effective approach to investigating long-term water balance at large basin scale under steady state. The assumption of steady state prevents applications of the BH to basins, which is unclosed, or with significant ...
C. Du, F. Sun, J. Yu, X. Liu, Y. Chen
doaj   +3 more sources

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