Description in Journal Article
Process Type
Process
Sub-process
Sub-process
Type of Information
High infiltration rates well in excess of maximum precipitation intensities Surface Infiltration Magnitude
Uniform wetting front propagation with small and protracted events Sub-surface Soils Matrix flow Vertical Temporal
Two domains of lateral throughflow that include […] slow, more uniform matrix flow Sub-surface Soils Matrix flow Lateral Existence, response time (qualitative)
Vertical bypass flow to depth with large events Sub-surface Soils Macropore flow Temporal
Old water dominated throughflow (resident soil water as opposed to new rainfall) Sub-surface Soils Mixing Spatial
Transient water table development on hillslopes Sub-surface Groundwater GW Storage Perched water table Spatial
Topographic convergence of water flow into hollows Sub-surface Groundwater GW flow Topographic convergence Spatial
Rapid lateral throughflow response to precipitation following threshold water table development Sub-surface Groundwater GW flow Subsurface stormflow / Saturated Temporal, Response time (qualitative)
Two domains of lateral throughflow that include rapid (albeit disconnected) pipe flow at the soil bedrock interface Sub-surface Groundwater GW flow Subsurface stormflow / Saturated / soil-bedrock interface Spatial, Response time (qualitative)
High degree of throughflow variability across seemingly planar hillslopes Sub-surface Groundwater GW flow Subsurface stormflow Spatial
Bedrock topographical control on the spatial distribution of mobile subsurface saturated flow Sub-surface Groundwater GW flow Subsurface stormflow Spatial