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2019-07-09 P&E Agenda - Item 10 - Attachment 1 - Coastal Hazards Risk, Vulnerability and Adaptation Assessment
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Noosa Shire Council Coastal Hazard Mapping 33
Permanent Inundation due to Sea Level Rise
4 Permanent Inundation due to Sea Level Rise
4.1 Hazard Assessment Approach
As discussed by BMT WBM (2017), the State EPA mapping defines permanent tidal inundation
due to SLR at 2100 as:
• Present-day Highest Astronomical Tide (HAT) plus 0.8 m SLR.
The hazard area is then obtained by extrapolating the water level across land. Areas adjacent to
tidal waters where the ground elevation falls below the threshold water level are deemed to be
within the hazard area.
The SLR hazard information provided by the State is useful for ‘first-pass risk screening’ only and
does not provide sufficient information regarding likelihood and consequence to undertake a more
detailed risk assessment. To address this issue, SLR hazard mapping including depth classification
has been developed for the Noosa CHAP planning horizons. The adopted approach generally
follows the State definition, whereby a threshold water level (mAHD) is defined by consideration of
HAT plus an appropriate SLR allowance. The water level mapping assumptions are summarised in
Table 4-1. These thresholds for different locations throughout the study area consider Maritime
Safety Queensland published tidal planes (MSQ 2017) along the open coast and within the lower
Noosa River. Linear interpolation of the water level between the sites has been adopted with the
Munna Point and Tewantin levels extending into Lake Cooroibah/Cootharaba and Lake Weyba
respectively.
Table 4-1 Permanent inundation due to Sea Level Rise mapping assumptions
Planning SLR Noosa Head HAT Munna Point HAT Tewantin HAT
Horizon allowance (m) (mAHD) (mAHD) (mAHD)
Present-day 0 1.16 0.68 0.55
2040 0.2 1.36 0.88 0.75
2070 0.5 1.66 1.18 1.05
2100 0.8 1.96 1.48 1.35
4.2 Assessment Results
The projected impact of inundation due to SLR is presented in Appendix E and is moderate across
the Noosa region, primarily impacting land adjacent to the lower Noosa River. Based on current
forecasts, and in the absence of an adaptation response, this impact would be realised between
2060 and 2080 and significantly escalate by 2100.
G:\Admin\B22613.g.mpb.Noosa_CHAS\R.B22613.002.04.NSC_CHAP_Mapping.docx
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