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In addition, flows can be generated using expressionsfunctions.
Two techniques for processing input time series data are available:
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- Australian Water Balance Model (AWBM) - SRG
- GR4J - SRG
- IHACRES Classic -CMD - SRG
- Sacramento Model - SRG (the Sacramento model)
- SIMHYD - SRG and SIMHYD with routing - SRG
- SMARG - SRG
- PERFECT GWlag - SRG
The six rainfall-runoff models can be configured based on: (i) a delineation of the catchment into smaller lumped sub-catchments; or (ii) a lumped catchment scale. Inputs are spatially explicit for each sub-catchment, allowing representation of the heterogeneity in catchments at the sub-catchments for catchment scale. Variations in land use, rainfall, evapotranspiration, etc; the generated runoff is . are lumped at the sub-catchment scale. The models can be calibrated using observed climate and streamflow data in gauged catchments using a combination of objective functions and optimisation methods (the framework includes four optimisation methods and four pre-defined objective functions - more information is available via Enhanced Calibration analysis - SRG). The calibrated models Models can be used to simulate runoff from ungauged catchments using a suitable regionalisation method; alternatively, it may be possible to estimate parameter values from other studies or from the literature. Model inputs and outputs can be displayed as time series or spatial and temporal plots to assist with quality assurance. The framework also provides a number of test descriptive statistics that can be used to determine assess the quality of model calibration and simulation results. (Abridged from Welsh, et al, 2013.)
The general approach in these models is to use rainfall and evaporation data as inputs. Stream flow is produced as a model output, often as the sum of quick flow and slow flow components, as illustrated in Figure 1 (Note that slow quick flow includes may includs lateral subsurface throughflow - also known as interflow - as well as baseflow, but for the purposes of the SRG it is lumped together with baseflowsurface runoff). If evaporation data is not available, temperature may be used as an input in some models (e.g. IHACRES Classic). The complexity of the models varies considerably from four parameter models (e.g. GR4J) to models with a large number of conceptual stores and parameters (e.g. the Sacramento model).
Figure 1. Rainfall runoff model
Choosing the right model
Choosing which of the above models is the most appropriate to use for a given application may not necessarily be straightforward. Consider the following when choosing a rainfall runoff model:
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More information on model choice, and rainfall-runoff modelling as a whole, is available from a number of sources including eWater's Guidelines for water management modelling and the supporting Guidelines for Rainfall-Runoff Modelling (accessible via the link for Guidelines for water management modelling).
Reference
Welsh, W.D., Vaze, J., Dutta, D., Rassam, D., Rahman, J.M., Jolly, I.D., Wallbrink, P., Podger, GM., Bethune, M., Hardy, M.J., Teng, J., Lerat, J. (2013) An integrated modelling framework for regulated river systems. Environmental Modelling & Software, 39: 81-102.