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References (13)
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Willgoose Willgoose, Bras Bras, Rodriguez‐Iturbe Rodriguez‐Iturbe (1991a)
A physically based coupled network growth and hillslope evolution model: 1. TheoryWater Resources Research, 27
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The role of fluting in gully extensionJournal of the Soil Conservation Service of New South Wales, 36
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An experimental investigation of fluid flow resulting from the impact of a water drop with an unyielding dry surfaceProceedings of the Royal Society of London. A. Mathematical and Physical Sciences, 373
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G. Willgoose, R. Bras, I. Rodríguez‐Iturbe (1991)
A coupled channel network growth and hillslope evolution model: 2. Nondimensionalization and applicationsWater Resources Research, 27
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G. Willgoose (1989)
A physically based channel network and catchment evolution model -
Howard Howard (1971)
Simulation of stream networks by headward growth and branchingGeographical Analysis, 3
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Horton Horton (1945)
Erosional development of streams and their drainage basins: hydrophysical approach to quantitative morphologyBulletin of the Geological Society of America, 56
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G. Willgoose, R. Bras, I. Rodríguez‐Iturbe (1991)
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A physically based coupled network growth and hillslope evolution model: 2. ApplicationsWater Resources Research, 27
- Publisher
- Wiley
- Copyright
- Copyright © 2001 John Wiley & Sons, Ltd.
- ISSN
- 0885-6087
- eISSN
- 1099-1085
- DOI
- 10.1002/hyp.143
- Publisher site
- See Article on Publisher Site
Abstract
An experimental landscape simulator has been developed which uses a rainfall simulator to create overland flow and erosion. The simulator uses rainfall sprinklers that eliminate rainsplash and an artificial soil which has little cohesion. Experimental landscapes developed in the simulator evolved according to Howard's headward growth model. Elements of Glock's model could be identified during evolution (i.e. initiation and maximum extension), but other stages of this model were not observed (i.e. extension and integration). The Horton concept of cross‐grading and micropiracy and stream piracy was not observed despite the dominance of overland flow, nor the groundwater headward growth mechanism proposed by Dunne, the latter due to experimental design, which eliminated any perched groundwater table. The experimental apparatus produced model landscapes that are scaled‐down analogues of real world processes. Copyright © 2001 John Wiley & Sons, Ltd.
Journal
Hydrological Processes – Wiley
Published: Jan 1, 2001