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2019-12-16 GC Agenda - Item 5 - Attachment 1 - Noosa Spit Shoreline Erosion Management Plan-Part 1
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Log in to see the plans as drawnNoosa Spit SEMP Final Report 10
Noosa Spit Shoreline Erosion
Imagery Observed Changes Wind Climate Notable Orientation Northern Spit Southern Spit Dominant Flow High Tide High Tide
Date (since previous image) Compared to Average Rainfall and Condition Length and Length and Channel Recreational Recreational
(since previous (since of Mouth Condition Condition Beach Beach
image) previous Availability at Availability at
image) central Doggie eastern
Beach Doggie Beach
August Major manual interference in the southern channel and along Doggie Beach Double Island Point: Significantly Multiple Average, wide, Non-existent Central, but Wide (post- Wide (post-
2013 occurred in the lead up to this image. A training wall was constructed at the Typical winds higher than disconnected patchy multiple groyne, groyne,
western end of Noosa Spit to control channel migration and limit further erosion average: NE-SW overwash, channels nourished) nourished)
Tewantin:
of Doggie Beach, accompanied by nourishment along the length of the beach. December channels submerged through shoals
Typical winds
Manual infilling of the channel near the submerged geobag groyne at the eastern 2011, January shoals to west
end of Doggie Beach is visible. Nourishment material was sourced from the 2012, March
shoals near the new training wall. The dredge holes created in this process 2012, June
appear to have naturally re-filled. 2012, January
2013 (ex-TC
Very little change was observed in the central channel, which is dominant now
Oswald),
that the southern channel has been partially infilled. The exit channel has
February 2013,
remained close to the Noosa Woods training wall, assisted by the training wall
July 2013
scour pocket, and reduced sediment supply from Noosa Main Beach due to
sand shifter activities between February and May 2013 (approx. 30,000 m3).
Sediment supply to the northern spit appears to have reduced, and localised
breaching of the northern spit at higher water levels is evident.
June 2014 Very gradual increase in length and height of northern spit sand mass, with the Double Island Point: Nil. Dryer than Multiple Average, wide, Non-existent Central, but Average Average
spit blocking flow of the northern channel. Visible increase in dune grass Typical winds average. 2014 disconnected N- submerged multiple
colonisation. close to lowest S channels shoals to west channels
Tewantin:
rainfall on through shoals
The central channel remains dominant, although some shoaling is occurring just Typical winds
station record.
upstream of its intersection with the southern channel, forcing development of a
currently short section of new channel aligned to N-S. The channel exit remains
close to the Noosa Woods training wall, although minor development of the
southern spit has occurred.
The southern channel has remained largely stable, although redistribution of the
nourishment material placed in the southern channel has exposed the upper
layer of the submerged geobag groyne. The scour pocket at the end of the
Noosa Spit training wall has become well developed.
September Consolidation of the northern spit continued, with easterly winds expanding the Double Island Point: Nil. Dryer than Poorly defined Average, wide, Minimal above Multiple Average Average
2015 spit to the west, almost connecting with Frying Pan Island above the high-water Spring 2014 more E average. Ex-TC N-S channels submerged HWM, minimal channels
mark. This spit growth was assisted by further dune grass stabilisation. The than average Marcia in area shoals to west submerged through shoals
northern channel largely remains a backwater. Shoaling of the eastern end of February 2015, shoals to north-
Tewantin:
the central channel has progressed to a stage where the channel, although heavy rainfall west
Typical winds
dominant, is no longer continuous through the flood-tide delta. recorded for
one day only.
Further exposure of the submerged geobag groyne has occurred, with the entire
length of the structure now visible. The scour pockets at the ends of both training
walls (i.e. at each end of the southern channel) are well developed.
Gradual narrowing of Doggie Beach above the high-water mark has occurred,
although no further loss of vegetation is evident.
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