A large number of studies over the past four decades have demonstrated the ubiquity of
preferential flow in diverse soils. Because of its significant impacts on ecosystem services …

Although early studies of streamwater residence time included the use of stable isotopes
(deuterium, oxygen‐18) and tritium, work in the last decades has largely relied on stable …

The importance of lateral pipe flow on runoff generation in wet steep hillslopes has been
described in many case studies from around the world. However, most hillslope studies are …

The lag time between peak rainfall and peak discharge is an important index reflecting
hydrological properties in a catchment. To characterize lag times, we studied the effects of …

The effect of preferential flow on the stability of landslides is studied through numerical
simulation of two types of rainfall events on a hypothetical hillslope. A model is developed …

Intercomparisons of hillslopes and catchments in different hydrogeomorphic settings are
rare. Those comparison studies that have been completed have focused largely on bulk …

Hillslopes are fundamental landscape units that strongly control the processes whereby
precipitation or snowmelt is vertically and laterally transported to the streams. They are, in a …

Subsurface saturation near the bedrock surface is an important source of runoff generation
and deeper bedrock recharge. While many studies have reported the generation patterns of …

Until recently, there have been few attempts to link hillslope, headwater and meso-scale
hydrology. However, the paper by Shaman et al.(2004, Hydrological Processes18: 3195 …

The fast pore water pressure response to rain events is an important triggering factor for
slope instability. The fast pressure response may be caused by preferential flow that …