The rainfall-runoff process consists of an excess rainfall process and a runoff concentration process. A transient one-dimensional finite difference model describing the partitioning of precipitation between surface runoff, soil moisture storage and deep percolation, through the coupling of saturate
Study of the rainfall-runoff process in the Andes region using a continuous distributed model
✍ Scribed by I.; P. Fernandez; F. Bouraoui
- Book ID
- 117139787
- Publisher
- Elsevier Science
- Year
- 1999
- Tongue
- English
- Weight
- 585 KB
- Volume
- 216
- Category
- Article
- ISSN
- 0022-1694
No coin nor oath required. For personal study only.
📜 SIMILAR VOLUMES
## Abstract In this study a simple modelling approach was applied to identify the need for spatial complexity in representing hydrological processes and their variability over different scales. A data set of 18 basins was used, ranging between 8 and 4011 km^2^ in area, located in the Nahe basin (Ge
## Abstract The delicate balance between human utilization and sustaining its pristine biodiversity in the Mara River basin (MRB) is being threatened because of the expansion of agriculture, deforestation, human settlement, erosion and sedimentation and extreme flow events. This study assessed the
## Abstract Rainfall–runoff processes appear to be highly nonlinear in Bayinbluk watersheds of the northwestern China. In this study, the time‐scale wavelet transform has been used for the analysis of this nonstationary system. The Haar and Morlet wavelet transform were used to analyse the rainfall
## Abstract This paper investigates the effect of introducing spatially varying rainfall fields to a hydrological model simulating runoff and erosion. Pairs of model simulations were run using either spatially uniform (i.e. spatially averaged) or spatially varying rainfall fields on a 500‐m grid. T