Water Balance Modelling Over Variable Time Scales
نویسنده
چکیده
Partitioning of rainfall into evapotranspiration and runoff is controlled by climate and catchment characteristics. The degree of control exerted by these factors varies with the spatial and temporal scales of processes being modelled. Understanding individual hydrological processes and their relationships with climatic and catchment characteristics is an important step in predicting catchment water balance. However, this does not mean that one should try to incorporate every known process into a model. The interaction and co-evolution of these processes may manifest themselves in such a way that the overall behaviour of the catchment can be described by simple relationships.
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