The use of distributed hydrological models for the Gard 2002 Flash-Flood event: Analysis of associated hydrological processes

Isabelle Braud (1) , Hélène Roux (2) , S. Anquetin (3) , Marie-Madeleine Maubourguet (2) , C. Manus (4) , P. Viallet (5) , Denis Dartus (2)

1 UR HHLY - Hydrologie-Hydraulique
2 IMFT - Institut de mécanique des fluides de Toulouse
3 HMCI
4 LTHE - Laboratoire d'étude des transferts en hydrologie et environnement
5 Hydrowide

This paper presents a detailed analysis of the September 8-9 2002 flash flood event in the Gard region (southern France) using two distributed hydrological models: CVN built within the LIQUID® hydrological platform and MARINE. The models differ in terms of spatial discretization, infiltration and water redistribution representation, and river flow transfer. MARINE can also account for sub-surface lateral flow. Both models are set up using the same available information, namely a DEM and a pedology map. They are forced with high resolution radar rainfall data over a set of 18 sub-catchments ranging from 2.5 to 99 km2 and are run without calibration. To begin with, models simulations are assessed against post field estimates of the time of peak and the maximum peak discharge showing a fair agreement for both models. The results are then discussed in terms of flow dynamics, runoff coefficients and soil saturation dynamics. The contribution of the sub-surface lateral flow is also quantified using the MARINE model. This analysis highlights that rainfall remains the first controlling factor of flash flood dynamics. High rainfall peak intensities are very influential of the maximum peak discharge for both models, but especially for the CVN model which has a simplified overland flow transfer. The river bed roughness also influences the peak intensity and time. Soil spatial representation is shown to have a significant role on runoff coefficients and on the spatial variability of saturation dynamics. Simulated soil saturation is found to be strongly related with soil depth and initial storage deficit maps, due to a full saturation of most of the area at the end of the event. When activated, the signature of sub-surface lateral flow is also visible in the spatial patterns of soil saturation with higher values concentrating along the river network. However, the data currently available do not allow the assessment of both patterns. The paper concludes with a set of recommendations for enhancing field observations in order to progress in process understanding and gather a larger set of data to improve the realism of distributed models.

Mots clés: CRUE SOUDAINE; MODELE HYDROLOGIQUE; MODELE DISTRIBUE; SOL; INFILTRATION; GARD; FLASH FLOODS; DISTRIBUTED MODELLING; SOIL VARIABILITY; HYDROLOGICAL PROCESSES; SATURATION EXCESS; INFILTRATION EXCESS; MODEL INTER-COMPARISON

Domaines: Sciences de l'environnement

Isabelle Braud, Hélène Roux, S. Anquetin, Marie-Madeleine Maubourguet, C. Manus, et al.. The use of distributed hydrological models for the Gard 2002 Flash-Flood event: Analysis of associated hydrological processes. Journal of Hydrology, 2010, 394 (1-2), p. 162 - 181. ⟨10.1016/j.jhydrol.2010.03.033⟩. ⟨hal-00546711⟩