A subgrid parameterization of runoff based on the TOPMODEL hydrological framework is introduced within the ISBA surface scheme. Indeed, by the mean of a topographic index of hydrological similarity, the TOPMODEL framework suggests an explicit scaling equation linking; local scale and macro scale water deficit.. The idea is then to couple this scaling equation with ISBA to be able to associate the water con tent of each macro pixel (here 64km(2)) simulated hy ISBA to the corresponding subgrid spatial distribution of the local pixels (here 75x75m(2)) of the digital elevation model (DEM). The main advantage is that this subgrid runoff parameterization depends only on the topography, without any calibration parameters. The ISBA-TOPMODEL model is tested in the Ardeche basin (France), for the period 1981-1995. Soil, vegetation and atmospheric forcing are taken form the GEWEX-Rhone database.