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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 21, issue 2
Hydrol. Earth Syst. Sci., 21, 1117–1135, 2017
https://doi.org/10.5194/hess-21-1117-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Observations and modeling of land surface water and energy...

Hydrol. Earth Syst. Sci., 21, 1117–1135, 2017
https://doi.org/10.5194/hess-21-1117-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 22 Feb 2017

Research article | 22 Feb 2017

Systematic shifts in Budyko relationships caused by groundwater storage changes

Laura E. Condon and Reed M. Maxwell

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Cited articles

Barnes, M. L., Welty, C., and Miller, A. J.: Global Topographic Slope Enforcement to Ensure Connectivity and Drainage in an Urban Terrain, J. Hydrol. Eng., 21, 06015017, https://doi.org/10.1061/(ASCE)HE.1943-5584.0001306, 2016.
Budyko, M. I.: The Heat Balance of the Earth's Surface Rep., US Department of Commerce, Weather Bureau, Washington, D.C., 140–161, 1958.
Budyko, M. I.: Climate and LIfe, Academic Press, New York, 1974.
Choudhury, B.: Evaluation of an empirical equation for annual evaporation using field observations and results from a biophysical model, J. Hydrol., 216, 99–110, https://doi.org/10.1016/S0022-1694(98)00293-5, 1999.
Condon, L. E., Hering, A. S., and Maxwell, R. M.: Quantitative assessment of groundwater controls across major US river basins using a multi-model regression algorithm, Adv. Water Resour., 82, 106–123, https://doi.org/10.1016/j.advwatres.2015.04.008, 2015.
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We evaluate the impact of groundwater–surface water exchanges on the fraction of precipitation that leaves a watershed as either surface runoff or evapotranspiration. Results show that groundwater storage can systematically influence watershed behavior at the land surface. This is an important finding because most studies of tradeoffs between runoff and evapotranspiration assume that watersheds are in a steady-state condition where there are no net exchanges between the surface and subsurface.
We evaluate the impact of groundwater–surface water exchanges on the fraction of precipitation...
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