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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 19, issue 7
Hydrol. Earth Syst. Sci., 19, 3253–3272, 2015
https://doi.org/10.5194/hess-19-3253-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
Hydrol. Earth Syst. Sci., 19, 3253–3272, 2015
https://doi.org/10.5194/hess-19-3253-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 28 Jul 2015

Research article | 28 Jul 2015

GRACE storage-runoff hystereses reveal the dynamics of regional watersheds

E. A. Sproles et al.

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Cited articles

Appleby, F. V.: Recession and the baseflow problem, Water Resour. Res., 6, 1398–1403, https://doi.org/10.1029/WR006i005p01398, 1970.
Aspinall, R.: A Century of physical geography research in the Annals, Ann. Assoc. Am. Geogr., 100, 1049–1059, 2010.
Ayala, A., McPhee, J., and Vargas, X.: Altitudinal gradients, midwinter melt, and wind effects on snow accumulation in semiarid midlatitude Andes under La Niña conditions, Water Resour. Res., 50, 3589–3594, 2014.
Bales, R. C., Molotch, N. P., Painter, T. H., Dettinger, M. D., Rice, R., and Dozier, J.: Mountain hydrology of the western United States, Water Resour. Res., 42, W08432, https://doi.org/10.1029/2005wr004387, 2006.
Barthel, R.: A call for more fundamental science in regional hydrogeology, Hydrogeol. J., 22, 507–510, 2014.
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The paper demonstrates how data from the Gravity Recovery and Climate Experiment (GRACE) can be used to describe the relationship between water stored at the regional scale and stream flow. Additionally, we employ GRACE as a regional-scale indicator to successfully predict stream flow later in the water year. Our work focuses on the Columbia River Basin (North America), but is widely applicable across the globe, and could prove to be particularly useful in regions with limited hydrological data.
The paper demonstrates how data from the Gravity Recovery and Climate Experiment (GRACE) can be...
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