Modeling rain-driven overland flow: Empirical versus analytical friction terms in the shallow water approximation
- Others:
- Institut Jean le Rond d'Alembert (DALEMBERT) ; Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS)
- Université de Nice Sophia-Antipolis (UNSA)
- Unité de Science du Sol (Orléans) (URSols) ; Institut National de la Recherche Agronomique (INRA)
- ANR project METHODE #ANR-07-BLAN-0232
Description
Modeling and simulating overland flow fed by rainfall is a common issue in watershed surface hydrology. Modelers have to choose among various friction models when defining their simulation framework. The purpose of this work is to compare the simulation quality for the Manning, Darcy–Weisbach, and Poiseuille friction models on the simple case of a constant rain on a thin experimental flume. Results show that the usual friction law of Manning is not suitable for this type of flow. The Poiseuille friction model gave the best results both on the flux at the outlet and the velocity and depth profile along the flume. The Darcy–Weisbach model shows good results for laminar flow. Additional testing should be carried out for turbulent cases.
Abstract
International audience
Additional details
- URL
- https://hal.inrae.fr/hal-02637839
- URN
- urn:oai:HAL:hal-02637839v1
- Origin repository
- UNICA