Articles | Volume 18, issue 9
Hydrol. Earth Syst. Sci., 18, 3681–3692, 2014
https://doi.org/10.5194/hess-18-3681-2014
Hydrol. Earth Syst. Sci., 18, 3681–3692, 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 et al.

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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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