Studies of runoff production mechanismsRunoff process on a steep forested slope
References (6)
Hillslope hydrology
- et al.
The behaviour of rainwater on a forested hillslope (I) The properties of vertical infiltration and the influence of bedrock on it
J. Jpn. For. Soc.
(1985) - et al.
The behaviour of rainwater on a forested hillslope(II) Lateral flow on a slope
J. Jpn. For. Soc.
(1985)
Cited by (68)
Subsurface and Surface Flow Leading to Channel Initiation
2022, Treatise on GeomorphologyHydrological responses in a natural forested headwater before and after subsurface displacement
2020, Journal of HydrologyCitation Excerpt :Hydrological behavior may differ among landforms or hillslope units (Kim et al., 2007; Fujimoto et al., 2011; Liang et al., 2017), with headwaters generally featuring active hydrological and erosional responses (Tsukamoto and Ohta, 1988).
Dynamics of pore water pressure at the soil–bedrock interface recorded during a rainfall-induced shallow landslide in a steep natural forested headwater catchment, Taiwan
2020, Journal of HydrologyCitation Excerpt :These two sources of subsurface saturation interconnected around the soil–bedrock interface at the unstable downslope, where perennially produced surface runoff had accumulated. Headwater catchments should be characterized by at least two sources of subsurface saturation, which cause a headwater to be most active hydrologically and erosionally among the various slope units (Tsukamoto and Ohta, 1988). To accurately predict the location and timing of shallow landslide occurrences in this type of headwater environment, future stability analysis models must separately consider the generation processes of different origins of subsurface saturation (e.g., Ebel et al., 2008).