๐”– Bobbio Scriptorium
โœฆ   LIBER   โœฆ

Distributed dynamic modelling of interrill overland flow

โœ Scribed by Anthony J. Parsons; John Wainwright; Athol D. Abrahams; J. Roger Simanton


Publisher
John Wiley and Sons
Year
1997
Tongue
English
Weight
546 KB
Volume
11
Category
Article
ISSN
0885-6087

No coin nor oath required. For personal study only.

โœฆ Synopsis


A distributed, dynamic, process-based model for interrill overland ยฏow that has previously been shown to predict accurately both total runo and runo hydraulics for a site on semi-arid shrubland is assessed in terms of (i) its portability, (ii) its sensitivity to the quality of data inputs, and (iii) its sensitivity to the size of cell used in the model. It is found that the model can be used at another site, but only after modiยฎcations to take account of the local controls of runo routing. The model is portable, but not readily so. The model is sensitive to both the quality of data input and the size of cell. Data input cannot be reduced by use of stochastic distribution of model parameters without signiยฎcant loss of accuracy in model predictions, particularly of runo hydraulics. Larger cells produce poorer predictions of the runo hydrograph. It is concluded that process-based modelling of interrill runo may not be a realistic tool for predicting soil erosion, but is one that may be useful for identiยฎcation of our present poor understanding of erosion processes. Such models help to deยฎne the research agenda for soil erosion studies.


๐Ÿ“œ SIMILAR VOLUMES


Depth distribution of interrill overland
โœ Anthony J. Parsons; John Wainwright ๐Ÿ“‚ Article ๐Ÿ“… 2006 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 125 KB ๐Ÿ‘ 1 views

## Abstract A Gumbel distribution for maxima is proposed as a model for the depths of interrill overland flow. The model is tested against three sets of field measurements of interrill overland flow depths obtained on shrubland and grassland hillslopes at Walnut Gulch Experimental Watershed, southe

Sediment-transport competence of rain-im
โœ Parsons, Anthony J.; Stromberg, Simon G. L.; Greener, Mark ๐Ÿ“‚ Article ๐Ÿ“… 1998 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 459 KB ๐Ÿ‘ 1 views

Laboratory experiments to determine the maximum size of sediment transported in shallow, rain-impacted flow were conducted in a recirculating flume 4โ€ข80 m long and 0โ€ข50 m wide. Rainfall intensities were varied between 51 and 138 mm h -1 , flow was introduced from a header tank into the flume at rate

Incremental distributed modelling invest
โœ Antti Taskinen; Michael Bruen ๐Ÿ“‚ Article ๐Ÿ“… 2006 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 252 KB

## Abstract A distributed overland flow model is presented and the test results compared with those of the unit hydrograph (UH) model. Infiltration excess in the overland model was calculated using both a modified Green and Ampt (Gโ€“A) method and a more complicated method that keeps track of the soi

A simple model of hillslope response for
โœ Professor Carmelo Agnese; Giorgio Baiamonte; Cecilia Corrao ๐Ÿ“‚ Article ๐Ÿ“… 2001 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 345 KB

## Abstract This paper deals with the derivation of the hydrological response of a hillslope on the assumption of quick runoff by surface runoff generation. By using the simple nonโ€linear storage based model, first proposed by Horton, an analytical solution of the overland flow equations over a pla