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2020-10-21 Final Order - Approval Conditions and Approved Plans - P&E Appeal No 61 of 2018 - RAL17-0504
Plans and drawings: the text below has words only, no drawings.
TABLE A-2 KEY LEVELS
Event Notes Source Peak Water
Level (mAHD)
Practical minimum level of first floor 4.9
PMF Probable Maximum Flood based on Current Climate Model 3.43
Minimum finished floor level of ground floor 2.8
Building pad level 2.6
Flood
1% AEP 2100 climate change conditions Information 2.30
Certificate
20% increase rainfall intensity, 0.8m sea level rise and
1% AEP Model 2.23
0.8m increase in bathymetry
1% AEP 20% increase rainfall intensity and 0.8m sea level rise Model 2.24
1% AEP Current Climate Model 1.61
1% AEP Typical road level of Lake Weyba Drive Survey 1.61
Nominated level to cease evacuation and shelter in place Survey 1.5
Nominated level to commence site evacuation Survey 1.3
10% AEP Nominated level to prepare for site evacuation Survey 1.1
Historic Flooding
The historical annual peak heights which have been recorded at the Tewantin gauge are illustrated in Figure
A-3. The records indicate that the highest flood level recorded at the Tewantin gauge to date was in 1968,
which peaked at 2.0m. Please note that based on other historic events, the within Lake Weyba will have been
lower than at the Tewantin Gauge. This event pre-dated the installation of the initial flood warning network
which occurred in 1987. The largest event which has occurred since the installation of the flood warning
network occurred in February 1992. Events post-1987 have been utilised in the calibration of Noosa Shire
Council’s regional hydrological/hydraulic model of the Noosa River system.
As discussed previously, there is no flood alert station within Lake Weyba. Therefore, the Noosa Shire
Council’s calibrated hydrological/hydraulic model has been used to represent the response of Lake Weyba to
regional flooding. Time-series water surface plots of the available alert gauge levels, water levels at the site
and modelled rainfall have been provided in Figure . This chart indicates that water levels in Lake Weyba may
peak prior to flood peaks occurring at the Tewantin Gauge. The chart also indicates that the February 1992
event was characterised with a lengthy period of relatively low intensity rainfall (~10mm/hr) in the lower
catchment, however areas of the upper catchment experienced 1 to 2 hours of high intensity (~40mm/hr)
rainfall approximately half way through the rainfall event.
5865_R02_V06_Final_FEMP.docx
Andres Gabarrin | 27 February 2020
135 Lake Weyba Drive, Noosaville
41
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