## Abstract Water is a major limiting factor in arid and semiβarid agriculture. In the Sahelian zone of Africa, it is not always the limited amount of annual rainfall that constrains crop production, but rather the proportion of rainfall that enters the root zone and becomes plantβavailable soil mo
Application of an optimization technique to a physically based erosion model
β Scribed by Celso A. G. Santos; Vajapeyam S. Srinivasan; Koichi Suzuki; Masahiro Watanabe
- Publisher
- John Wiley and Sons
- Year
- 2003
- Tongue
- English
- Weight
- 248 KB
- Volume
- 17
- Category
- Article
- ISSN
- 0885-6087
- DOI
- 10.1002/hyp.1176
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β¦ Synopsis
Abstract
The difficulties involved in calibration of physically based erosion models have been partly attributable to the lack of robust optimization tools. This paper presents the essential concepts and application to optimize channel and plane parameters in an erosion model, with a global optimization method known as the SCEβUA (Duan et al., 1992. Water Resources Research 28(4): 1015β1031), which has recently shown promise as an effective and efficient optimization method for calibrating watershed models. It is based on the simplex method, and in order to improve its efficiency by making the simplex expand in a direction of more favourable conditions, or contract if a move was taken in a direction of less favourable conditions, new evolution steps have been introduced. The physically based erosion model that was chosen is called WESP (watershed erosion simulation program), developed by Lopes and Lane (1988. In Sediment Budgets, Bordas MP, Walling DE (eds). IAHS Publication no. 174. IAHS: Wallingford). The optimization technique was tested with the field data collected in an experimental watershed located in a semiβarid region of Brazil. On the basis of these results, the recommended erosion parameter values for a semiβarid region are given, which could serve as an initial estimate for other similar areas. Copyright Β© 2003 John Wiley & Sons, Ltd.
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A new hydrological and soil erosion model has been developed and tested: LISEM, the Limburg soil erosion model. The model uses physically based equations to describe interception, infiltration and soil water transport, storage in surface depressions, splash and flow detachment, transport capacity an
## Abstract Watershed scale hydrological and biogeochemical models rely on the correct spatialβtemporal prediction of processes governing water and contaminant movement. The Soil and Water Assessment Tool (SWAT) model, one of the most commonly used watershed scale models, uses the popular curve num