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24-01-2020 - Appeal No. 245 of 2019 - Final Order of Judge Rackemann · 51987.2951.01
Working Notes: M Design and Fourteen Enterprises Pty Ltd as trustee v Noosa Shire Council - 42 Seaview Terrace, Sunshine Beach A long-term erosion of 0 metres is considered more realistic given the effect of Noosa Headland which would act in a similar fashion to a groyne by trapping sand moving north along the coast with the prevailing south-easterly wave climate. 6.2. Short-term Erosion (C) The Department of Environment and Heritage Protection (2013) recommends the calculation of the short-term erosion based on a 100 year ARI storm event using the methodology developed by Vellinga (1983). Figure 5-1 shows a conceptual representation of the erosion and accretion zones associated with storm induced erosion predicted by Vellinga (1983). The Department provides the following recommendation in relation to defining a storm event: “For a tide-dominated coast where storm tide levels can be large, the parameters adopted for the minimum design storm are: (i) storm tide level corresponding to an average recurrence interval of 1-in-100 years (ii) wave height for a moderate storm using the 1-in-20-year significant wave height (Hs). However, for wave-dominated coastlines where extreme storm tide levels can be relatively minor, such as the Gold Coast, the significant wave height and duration of the storm event are major factors influencing short term erosion, rather than storm tide. Hence it may be necessary to consider a larger wave event (for example, a storm event with a 1-in-100 ARI) and a moderate storm tide level. Decisions on appropriate parameters to be used must be based on local conditions and the experience of the coastal engineer undertaking the assessment.” Figure 5-1 Sketch of pre-storm and predicted post-storm profiles based on Vellinga (1983) In relation to the probability of such an event occurring the Department of Environment and Heritage protection (2013) states: 30 127738:14917433_1 040 49
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