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Noosa Spit SEMP Final Report 9
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
Beach. This progressively evolved into a lagoon as the continued sand supply
to the southern spit forced the channel westward away from the training wall.
July 2010 During the period from 2004 to 2010 there is a lack of regular imagery available Double Island Point: Significantly N-S up to open Average, wide, Minimal above Multiple Average Limited to none
for review, so it is not possible to describe the evolution of the channels with 2009 more N than higher than coast submerged HWM, average channels
confidence. average average (and alignment, then shoals to west submerged through shoals
highest monthly NE-SW shoals to north-
It is presumed that following the 2003 nourishment, the southern channel Tewantin:
totals on west
resumed southward migration. In August 2007, a new central channel was most More NE consistently
record):
likely formed in response to the heavy rainfall associated with the East Coast from 2005 to 2009 than
January 2006,
Low. average
August &
The continued supply of sand to the northern spit has infilled and eventually September
blocked the northern channel, which has split into two. The central and southern 2007,
channels have shared dominance. Notable recession of Noosa Woods at the November 2008
upstream end of the training wall is evident. and April 2009.
Known East
Coast Low in
August 2007.
November Gradual consolidation of the northern spit continued, with patchy dune grass Double Island Point: Significantly Multiple Average, wide, Minimal above Central, but Limited to none Average
2011 colonisation evident. Overall less N than higher than disconnected N- submerged HWM, minimal multiple (pre-groyne)
average, but Spring average: S and NE-SW shoals to west submerged channels
The central channel appears to be slightly more defined and the southern spit
2011 more N than October & channels shoals to north- through shoals
has mostly disappeared. This is possibly in response to significant rainfall
average December west
inflows reinforcing the existing channel and carving a more direct exit channel
2010, April 2011
close to the training wall. The scour pocket at the upstream end of the Noosa Tewantin:
Woods training wall has persisted, encouraging the retention of the southern 2011 less NE than
channel. average
Localised beach nourishment equipment and small sand bulges are visible
along the eastern end of Doggie Beach. Notable beach narrowing and loss of
established vegetation continues to occur at the western end of Doggie Beach.
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