${session.getAttribute("locale")} 5 A conceptual model of preferential flow systems in forested hillslopes: Evidence of self-organization Mon 25 Nov 2019 15:22:42 AEST ]]> Spatially distributed morphological characteristics of macropores in forest soils of Hitachi Ohta Experimental Watershed, Japan Fri 14 Jun 2019 13:49:23 AEST ]]> Shallow lateral flow from a forested hillslope: Influence of antecedent wetness 170 m2) and the effective contributing slope length (>36 m) were substantially greater for the "wet" antecedent storm compared to the "dry" storm events. Shallow lateral flow over unsaturated soil is therefore unlikely to be a significant contributor to storm runoff at such forested sites. Flow at the organic horizon-mineral soil interface may contribute to interconnected preferential flow pathways during wetter antecedent conditions. © 2005 Elsevier B.V. All rights reserved.]]> Fri 14 Jun 2019 13:49:04 AEST ]]> Subsurface runoff characteristics from a forest hillslope soil profile including macropores, Hitachi Ohta, Japan Fri 14 Jun 2019 13:48:21 AEST ]]> Throughflow variability during snowmelt in a forested mountain catchment, coastal British Columbia, Canada Fri 14 Jun 2019 13:48:10 AEST ]]> Unraveling the dynamics of a creeping slope in Northwestern Colombia: Hydrological variables, and geoelectrical and seismic signatures Fri 14 Jun 2019 13:47:22 AEST ]]>