Abstract
The conceptual rainfall runoff model TAC (tracer aided catchment model) has been developed based on the experimental results of a tracer hydrological investigation for the mountainous Brugga basin (39.9 km2). The model contains an extensive physically realistic description of the runoff generation, which includes seven unit types each with characteristic dominating runoff generation processes. These processes are conceptualised by different linear and non-linear reservoir concepts. The model is applied to a period of 3.2 years with good success. In addition, the model is validated with additional information, e.g. tracer concentrations, beside to the simulated discharge.
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