Abstract:
Most of the existing distributed rainfall-runoff models simplify the interaction between the atmosphere and the groundwater processes. The objective of this research is to make an integrated hydrological model through the simulation of the hydrological interactions in the surface, ground and atmosphere. The methodology is based on the dynamic linking among the transient hydrological models at different time scales, which implies that the quantity and quality of the distributed runoff at every time step is affected by the impact of atmosphere and groundwater interactions.
