Articles | Volume 18, issue 1
Hydrol. Earth Syst. Sci., 18, 121–138, 2014
https://doi.org/10.5194/hess-18-121-2014
Hydrol. Earth Syst. Sci., 18, 121–138, 2014
https://doi.org/10.5194/hess-18-121-2014

Research article 13 Jan 2014

Research article | 13 Jan 2014

Predicting subsurface stormflow response of a forested hillslope – the role of connected flow paths

J. Wienhöfer and E. Zehe

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Cited articles

Abou Najm, M. R., Jabro, J. D., Iversen, W. M., Mohtar, R. H., and Evans, R. G.: New method for the characterization of three-dimensional preferential flow paths in the field, Water Resour. Res., 46, W02503, https://doi.org/10.1029/2009wr008594, 2010.
Allaire, S. E., Gupta, S. C., Nieber, J., and Moncrief, J. F.: Role of macropore continuity and tortuosity on solute transport in soils: 2. Interactions with model assumptions for macropore description, J. Contam. Hydrol., 58, 283–298, https://doi.org/10.1016/s0169-7722(02)00034-7, 2002a.
Allaire, S. E., Gupta, S. C., Nieber, J., and Moncrief, J. F.: Role of macropore continuity and tortuosity on solute transport in soils: 1. Effects of initial and boundary conditions, J. Contam. Hydrol., 58, 299–321, https://doi.org/10.1016/s0169-7722(02)00035-9, 2002b.
Anderson, A. E., Weiler, M., Alila, Y., and Hudson, R. O.: Subsurface flow velocities in a hillslope with lateral preferential flow, Water Resour. Res., 45, W11407, https://doi.org/10.1029/2008wr007121, 2009a.
Anderson, A. E., Weiler, M., Alila, Y., and Hudson, R. O.: Dye staining and excavation of a lateral preferential flow network, Hydrol. Earth Syst. Sci., 13, 935–944, https://doi.org/10.5194/hess-13-935-2009, 2009b.
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