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Table 2: Climate change projections and their relevance for stormwater design

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Type of change Range of changes for 2030s Range of changes for 2080s Relevance for stormwater planning Possible additional expertise and in-depth studies
Increase in heavy rainfall Return frequency increases with temperature (up to twofold - specific figures in Table 2) Return frequency increases with temperature (up to fourfold - specific figures in Table 2) Increase in total rainfall depth for design storm events for durations of up to 72 hours More complex rainfall modelling (e.g. RAMS model) or dynamic time series modelling
Change in annual mean rainfall -19 to +22% (depending on region) -32 to +57% (depending on region) Change in antecedent soil moisture saturation Modelling of soil moisture saturation for pervious catchment areas
Increase in annual mean temperature 0.1 to 1.4°C (with some dependence on region) 0.2 to 4.0°C (with some dependence on region) Change in evaporation from soils and ponds, which changes antecedent soil moisture saturation Modelling of soil moisture saturation for pervious catchment areas
Increases in wind Not quantified: highly location specific but with a trend nationally to increased westerlies Not quantified: highly location specific but with a trend nationally to increased westerlies Changes in rainfall over complex topography – increases upwind of hills and ranges More complex airflow and rainfall modelling (e.g. RAMS model)
Sea level rise 0.2 m 0.5 m Changes to stormwater discharge, saltwater intrusion in coastal zones  

Note: Figures provided in this Table should only be used for a preliminary screening assessment; if based on this preliminary assessment the effects of climate change are potentially significant, a more in-depth assessment using additional expertise should be carried out. Table adopted from MfE (2004a) and MfE (2004b).