27 citations as recorded by crossref.

1. Hillslope-storage and rainfall-amount thresholds as controls of preferential stormflow J. Dusek & T. Vogel 10.1016/j.jhydrol.2016.01.047
2. Simulating surface and subsurface initiation of macropore flow M. Weiler & F. Naef 10.1016/S0022-1694(02)00361-X
3. An infiltration model based on flow variability in macropores: development, sensitivity analysis and applications M. Weiler 10.1016/j.jhydrol.2005.01.010
4. Subsurface flow velocities in a hillslope with lateral preferential flow A. Anderson et al. 10.1029/2008WR007121
5. A decision scheme to indicate dominant hydrological flow processes on temperate grassland S. Scherrer & F. Naef 10.1002/hyp.1131
6. Combining dual-continuum approach with diffusion wave model to include a preferential flow component in hillslope scale modeling of shallow subsurface runoff J. Dusek et al. 10.1016/j.advwatres.2012.05.006
7. Micro-scale dry bulk density variation around earthworm (Lumbricus terrestris L.) burrows based on X-ray computed tomography H. Rogasik et al. 10.1016/j.geoderma.2013.08.034
8. Role of upslope soil pore pressure on lateral subsurface storm flow dynamics T. Uchida et al. 10.1029/2003WR002139
9. Fully-coupled hydrologic processes for modeling landscape evolution Y. Zhang et al. 10.1016/j.envsoft.2016.04.014
10. Seasonal dynamics of surface runoff in mountain grassland ecosystems differing in land use G. Leitinger et al. 10.1016/j.jhydrol.2010.02.006
11. Field Investigation and Modeling of Rapid Subsurface Stormflow through Preferential Pathways in a Vegetated Hillslope of Northeast India R. Sarkar & S. Dutta 10.1061/(ASCE)HE.1943-5584.0000431
12. Macropores and water flow in soils revisited K. Beven & P. Germann 10.1002/wrcr.20156
13. An experimental tracer study of the role of macropores in infiltration in grassland soils M. Weiler & F. Naef 10.1002/hyp.1136
14. Model-based quantification of runoff generation processes at high spatial and temporal resolution A. Steinbrich et al. 10.1007/s12665-016-6234-9
15. Modeling Subsurface Hillslope Runoff Dominated by Preferential Flow: One- vs. Two-Dimensional Approximation J. Dusek & T. Vogel 10.2136/vzj2013.05.0082
16. Rain simulation in patchy landscapes: Insights from a case study in the Central Alps C. Newesely et al. 10.1016/j.catena.2014.11.013
17. Evaluation and application of a portable rainfall simulator on subalpine grassland Y. Schindler Wildhaber et al. 10.1016/j.catena.2011.03.004
18. Process-based hydrological modelling: The potential of a bottom-up approach for runoff predictions in ungauged catchments M. Antonetti et al. 10.1002/hyp.11232
19. Parametric study of a physically-based, plot-scale hillslope hydrological model through virtual experiments R. Sarkar & S. Dutta 10.1080/02626667.2014.897407
20. Virtual experiments: a new approach for improving process conceptualization in hillslope hydrology M. Weiler & J. McDonnell 10.1016/S0022-1694(03)00271-3
21. Conceptualizing lateral preferential flow and flow networks and simulating the effects on gauged and ungauged hillslopes M. Weiler & J. McDonnell 10.1029/2006WR004867
22. Towards an alternative blueprint for a physically based digitally simulated hydrologic response modelling system K. Beven 10.1002/hyp.343
23. Field study of macropore flow processes using tension infiltration of a dye tracer in partially saturated soils E. Cey & D. Rudolph 10.1002/hyp.7302
24. Model-based exploration of hydrological connectivity and solute transport in a forested hillslope H. Laine-Kaulio & H. Koivusalo 10.1002/ldr.2823
25. Hillslope dynamics modeled with increasing complexity I. Meerveld & M. Weiler 10.1016/j.jhydrol.2008.07.019
26. Plant‐compositional effects on surface runoff and sediment yield in subalpine grassland A. Merz et al. 10.1002/jpln.200800231
27. Inferring flow types from dye patterns in macroporous soils M. Weiler & H. Flühler 10.1016/j.geoderma.2003.08.014