The numerical surface water modelling in a has a very specific objective: to probabilistically evaluate potential hydrological change in the (CRDP) relative to the at specified locations in the subregion to inform the and analysis reported in product 3-4. Outputs from the surface water modelling are also used as inputs to product 2.7 (receptor impact modelling) to facilitate evaluation of the of mining on water-dependent ecological and economic assets.
The probabilistic aspect of the analysis implies that modelling does not provide a single best estimate of the change, but rather an ensemble of estimates. This ensemble enables statements such as: ‘In 95% of the simulations, the change at location x,y does not exceed z.’
To generate these ensembles of predictions, a large number of model parameter sets are evaluated for the and models. The range of parameters reflects both the natural variability of the system and the in the understanding of the system. During the uncertainty analysis, these parameter combinations are filtered in such a way that only those that are consistent with the available observations and the understanding of the system are used to generate the ensemble of predictions. The details are documented in companion submethodology M09 (as listed in Table 1) for propagating uncertainty through models ().
It is not possible to capture all uncertainty of the understanding of the system in the parameterisation of the numerical models, so it is inevitable that there will be a number of assumptions and model choices necessary to create the models. These assumptions are introduced and briefly discussed in Section 22.214.171.124 on model development. The uncertainty analysis in Section 126.96.36.199 further provides a systematic and comprehensive discussion of these assumptions. This discussion focuses on the rationale behind the assumptions and the effect on the predictions.
The latter is crucial in justifying assumptions. In the numerical modelling the precautionary principle is adopted: impacts are over estimated rather than under estimated. As long as it can be shown that an assumption over estimates – not under estimates – impacts, the assumption is considered valid for the specific purpose of this modelling.
However, an overly conservative estimate of impact is not desirable either. If there are sound reasons to believe that predicted impacts are deemed unrealistically high (e.g. in comparison to earlier modelling efforts in the bioregion or subregion), the assumptions may need to be revisited.
Another advantage of this probabilistic modelling approach is that it enables a comprehensive analysis to identify the model parameters or aspects of the system that are most influential on the predictions – and others that have little or no effect on the predictions. This information can guide future data collection and model development or inform the regulatory process.
This product starts with an overview of the methods as applied to the (Section 188.8.131.52.2), focusing on the interaction between the and model, followed with a review of the existing surface water models (Section 184.108.40.206). Section 220.127.116.11 and Section 18.104.22.168 describe the development of the model and its calibration. Next is the uncertainty analysis (Section 22.214.171.124), which contains the justification of assumptions and the resulting ensembles of predicted impacts. The product concludes by describing the predictions arising from the surface water model (Section 126.96.36.199).
Product Finalisation date
- 188.8.131.52 Methods
- 184.108.40.206 Review of existing models
- 220.127.116.11 Model development
- 18.104.22.168.1 Spatial and temporal dimensions
- 22.214.171.124.2 Location of model nodes
- 126.96.36.199.3 Choice of seasonal scaling factors for climate trend
- 188.8.131.52.4 Representing the hydrological changes from mining
- 184.108.40.206.5 Modelling river management
- 220.127.116.11.6 Rules to simulate industry water discharge
- 18.104.22.168 Calibration
- 22.214.171.124 Uncertainty
- 126.96.36.199 Prediction
- Currency of scientific results
- Contributors to the Technical Programme
- About this technical product