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Understanding the Need for Resilience
At present, the foreshore benefits from an accessible We know our subtropical climate can be hot and this Riverbank Condition Flooding Legend
and scenic riverside location, where changes to its heat impacts liveability and community wellbeing.
Topographic High Point
condition have been happening for decades. These Our partnership with UniSC to monitor and model
changes have mostly occurred in small increments micro-climate on the foreshore is ongoing. Urban Urban Heat Island Area
and are not necessarily apparent day in and day out. Heat Island (UHI) is defined as ‘Urbanised areas that
Over time the foreshore has been and will continue to experience higher temperatures than the surrounding Rock Seawall
be impacted by extreme weather events. areas, largely caused by loss of vegetation, capacity to
Retaining Walls
infiltrate rainwater and an increase in heat absorption
Flooding is one of the biggest challenges, with tidal by built structures’.2 Indicative UHIs have been
inundation events historically impacting the foreshore. identified on the foreshore that are subject to the
Sea-level Rise Inundation Extent at
Highest Astronomical Tide (HAT)
The Queensland Government defines tidal inundation growing impacts of heat due to climate change.
as “abnormal elevation of the sea level (a storm surge) 2040
Figure 7. Historic image showing Figure 8. Erosion on the riverbank Figure 9. Pelican Boat Hire
over normal tide levels”. The foreshore is generally Existing tree canopy cover varies along the foreshore vegetation along the riverbank. caused by boat wash and wave impacted by flood waters. Credit:
flat and low-lying, therefore at present inundation with the highest identified in Pelican Beach Park Credit: Griffiths Studio action. Rob Maccoll 2070
impacts areas of the foreshore, particularly to the west. (35.3%) and the lowest in Gympie Terrace East (15.9%).
Predictive flood modelling for 2040 and 2070 indicate Lower canopy cover worsens the impacts UHIs and 2100
sea level rise and increased inundation due to climate reduces parkland amenity of unshaded footpaths, Tree Canopy Cover
change. The high points in the foreshore that are less seating and gathering spaces. Chaplin Park 23.8% Figure 10. Canopy Cover
prone to flooding include the tennis court, public boat Yacht & Rowing Club 25% (including Gympie Terrace) CE
Structures and vegetation can block cooling breezes, Note - The percentages shown E R RA E
OR
Lions & Apex Parks 26.5%
ramp and Ely Park. T
contributing to heat. South-easterly breezes are the Quota Park 30% are estimates only and do not
M P I E R ES H
Boat Ramp & Eli Park 26.3% represent an accurate survey of GY T FO
Beach nourishment activities are currently being main winds that affect Noosaville. The foreshore’s Pelican Beach Park 35.3% tree canopy. EAS
undertaken by Council, using dredged sand to top-up position on the southern river bank means it is
M
Gympie Terrace East 15.9%
areas impacted by erosion. Historically, retaining walls sheltered from the prevailing winds, but benefits from K
I A
20 40 60 80 100
PAR
I L S T
CH
and sea walls have been constructed to prevent sand cooling coastal breezes. BEA
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L
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ICA
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loss that is typically caused by high tides, wind and PE L
W T
Sea level rise and heat due to climate change is
A
wave action.
O S
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predicted to impact existing vegetation, with an
K
increase in inundation, salinity and temperatures.
Y PAR
& EL E
H
CHAPLIN PARK YACHT &
M P E P D
ROWING CLUB T RA T C S A
LIONS & A BOA E O
PEX PARK P I O
S M N
QUOTA PARK G Y
H
I L T C E
S T
P I E
S T
T
O Y M
S T
G
R D
S T
N
A R D
S T
E R T
T C
E
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THOMAS
E R T
1:5500 (A3)
B A
M A S
J A M
STREET
E D W
A L B
0 40 80 200
W E Y
R O B
T H O
10
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