Introduction to Rainfall Runoff Modelling Flashcards
Mathematical representation of processes
Empirical models…
black box models, maths equations based on analysis of concurrent input and output time series, not from the physical processes in the catchment. e.g.:
* UH (Sherman, 1932; Nash, 1959)
Mathematical representation of processes
Conceptual models…
simplified equations with a physical basis. Model parameters need to be obtained through calibration.
Mathematical representation of processes
Physically-based models
rigorous numerical solution of partial differential equations governing flow through porous media, overland and channel flows.
Types – Spatial configuration
Lumped
Semi-lumped
Semi-disturbed
Distributed
Lumped (catchment or basin) - The spatial and temporal variation of meteorological, hydrological, geological and hydrogeological data across the model area is described as one aggregated value for input and output.
Semi-lumped (sub-catchment or sub-basin)
Semi-distributed (landuse classes, soil types, elevation, HRU)
Distributed (gridded) - Distributed models try to account for heterogeneity at finer scales, but due to the complexity of the land surface, sub-terrain layers, and the physics of infiltration, capillarity, etc. the so-called distributed models end up performing in a‘lumped’ manner.