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Scale relationships in hillslope runoff and erosion Reply

โœ Scribed by Anthony J. Parsons; Richard E. Brazier; John Wainwright; D. Mark Powell


Publisher
John Wiley and Sons
Year
2008
Tongue
English
Weight
54 KB
Volume
33
Category
Article
ISSN
0360-1269

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๐Ÿ“œ SIMILAR VOLUMES


Scale relationships in hillslope runoff
โœ Anthony J. Parsons; Richard E. Brazier; John Wainwright; D. Mark Powell ๐Ÿ“‚ Article ๐Ÿ“… 2006 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 312 KB
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The results are presented of an intensive monitoring programme to determine eroded volumes due to observed rainfall events on a hillslope surface. The surface investigated has been reproduced through a digital elevation model and analysed in terms of drainage network, contributing area and slope by

Hillslope runoff and erosion as affected
โœ Ross A. Sutherland; Alan D. Ziegler ๐Ÿ“‚ Article ๐Ÿ“… 2006 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 249 KB

## Abstract A replicated field study using rainfall simulation and overland flow application was conducted in central Oahu, Hawaii, on a clayโ€dominated Oxisol with a 9% slope. Three main treatment groups were examined: a bare treatment, a group of four rolled erosion control systems (RECSs) with op

Runoff formation in a small catchment at
โœ Miroslav Hrnฤรญล™; Martin ล anda; Alena Kulasovรก; Milena Cรญslerovรก ๐Ÿ“‚ Article ๐Ÿ“… 2010 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 304 KB

## Abstract The study is focused on runoff formation processes at two scales: the scale of a small mountainous catchment at its outlet and the scale of an experimental plot located in a typical hillslope subregion. The heterogeneous soil profile of the catchments is formed by Cambisols developed on

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## Abstract It is common for runoff and erosion models to be run at coarse time steps (e.g. daily) owing to limited data availability. However, such models are unable to capture adequately the smallโ€scale surface runoff and erosion processes that are dominated by, for example, precipitation charact