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BBNE01676-0001-REP-001-0-Noosa Calile Overland Flow_Optimized
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2.2.1.1 Topography Model topography has been based upon 2015 Light Detection and Ranging (LiDAR) along with the detailed site survey. Design DEM has been incorporated into the model to represent the proposed development. The catchment has been modelled using a 0.5m hydraulic model grid size. 2.2.1.2 Boundaries The inflow boundaries for the catchment have been read into the model using inflow polygons (2d_sa and 2d_bc) to represent inflow from the WBNM hydrology model. The outflow boundary for the model has been applied 70m downstream of the site, which is approximately 5m lower than the site outlet and is considered suitable for this assessment. A normal depth rating curve has been adopted for the downstream with a water surface slope of 0.02 m/m. 2.2.1.3 Roughness The model roughness is represented by the Manning’s roughness coefficient, n, in the TUFLOW materials file. Manning’s coefficients have been applied to reflect the land use within the catchment, assuming development conditions based on NSC zoning and aerial imagery. Roughness coefficients are outlined in Table 2.4, while the spatial distribution of material types in the TUFLOW model extent is included in FIGURE 2.3. TABLE 2.4: ADOPTED MANNING’S ‘N’ ROUGHNESS Land Use Manning’s ‘n’ Road 0.025 Buildings 0.3 Vegetated Channel 0.035 Vegetation 0.06 Gravel/Grass 0.065 Dense Vegetation 0.15 Residential 0.12 2.2.1.4 Structures The stormwater network represented in the hydraulic model aligns with the stormwater plan and long-section developed by Alta Projects and are presented in Appendix B. NOOSA CALILE I BBNE01676-0001-REP-001-0 7
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