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M. Kirkby, R. Chorley (1967)
THROUGHFLOW, OVERLAND FLOW AND EROSIONHydrological Sciences Journal-journal Des Sciences Hydrologiques, 12
H. Ingram (1967)
Problems of Hydrology and Plant Distribution in MiresJournal of Ecology, 55
D. Pilgrim, D. Huff, T. Steele (1978)
A field evaluation of subsurface and surface runoff: II. Runoff processes☆Journal of Hydrology, 38
Jones Jones (1979)
Extending the Hewlett model of stream runoff generationArea, 11
N. Crawford, R. Linsley (1966)
DIGITAL SIMULATION IN HYDROLOGY' STANFORD WATERSHED MODEL 4
D. Day (1978)
Drainage density changes during rainfall, 3
T. Dunne, R. Black (1970)
An Experimental Investigation of Runoff Production in Permeable SoilsWater Resources Research, 6
M. Kirkby, K. Beven (1979)
A physically based, variable contributing area model of basin hydrology, 24
Bello Bello, Day Day, Douglas Douglas, Kin‐Che Kin‐Che, Soh Soh (1978)
Field experiments to analyse runoff, sediment and solute production in the New England region of AustraliaZeitschrift für Geomorphologie N. F. Supple. Bd., 29
Kirkby Kirkby, Chorley Chorley (1967)
Throughflow, overland flow and erosionBulletin of International Association for Scientific Hydrology, 12
Dunne Dunne, Moore Moore, Taylor Taylor (1975)
Recognition and prediction of runoff‐producing zones in humid regionsHydrological Sciences Bulletin, XX
Newson Newson, Harrison Harrison (1978)
Channel studies in the Plynlimon experimental catchmentsInstitute of Hydrology Report, 47
Analysis of hydrographs from a 4·3 hectare stream head catchment indicates that storm runoff is generated from dynamic source areas. The volume and timing of contributions from different parts of the catchment show, when compared with the extent of surface saturation, that pipeflow generated from areas not saturated at the soil surface is a significant component of the quickflow hydrograph. A simple model of pipeflow generation and contribution is discussed in the light of field results.
Earth Surface Processes and Landforms – Wiley
Published: May 1, 1983
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