Articles | Volume 18, issue 9
https://doi.org/10.5194/hess-18-3681-2014
https://doi.org/10.5194/hess-18-3681-2014
Research article
 | 
24 Sep 2014
Research article |  | 24 Sep 2014

Hillslope-scale experiment demonstrates the role of convergence during two-step saturation

A. I. Gevaert, A. J. Teuling, R. Uijlenhoet, S. B. DeLong, T. E. Huxman, L. A. Pangle, D. D. Breshears, J. Chorover, J. D. Pelletier, S. R. Saleska, X. Zeng, and P. A. Troch

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Cited articles

Abdul, A. S. and Gillham, R. W.: Laboratory studies of the effects of the capillary fringe on streamflow generation, Water Resour. Res., 20, 691–698, 1984.
Abdul, A. S. and Gillham, R. W.: Field studies of the effects of the capillary fringe on streamflow generation, J. Hydrol., 112, 1–18, 1989.
Anderson, M. G. and Burt, T. P.: The role of topography in controlling throughflow generation, Earth Surf. Process., 3, 331–344, 1978.
Bernier, P. Y.: Variable source areas and storm-flow generation: An update of the concept and a simulation effort, J. Hydrol., 79, 195–213, 1985.
Beven, K.: Hillslope hydrographs by the finite element method, Earth Surf. Process., 2, 13–28, 1977.
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