Original source · versioned page text
Attachment C_R.B23636.001.02.SEMP_final_lowres
Very large file (26.6 MB): the original may take a few minutes to open or download. The page text below is quick to read.
Noosa Spit SEMP Final Report 12
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
September Continued expansion of the southern spit has forced the exit channel westward, Double Island Point: Wetter than Shore-parallel Short and Short and wide Southern – Limited to none Average
2018 scouring out the northern spit and facilitating a breach of the northern spit by the Less N to E winds than average but no west of narrow above above HWM, Hard up against
southern arm of a split northern channel, and by the central channel. The typical, SE dominant notable rainfall. coastline, then HWM, extensive Doggie Beach
northern arm of the northern channel is still narrowly blocked by the northern NE-SW extensive submerged
Tewantin:
spit, which is now significantly shortened but connected to Frying Pan Island submerged shoals to north-
Typical winds
below high-water mark. shoals to south west
The severed southern portion of the northern spit has migrated south, partially
infilling the central channel and consolidating with the sand shoal separating the
central and southern channels. The southern channel remains the dominant
channel, persisting hard up against Doggie Beach before heading northwards
towards Noosa North Shore where channel migration has undermined
established vegetation.
The northern spit has continued to expand to the northwest, and is now well
developed above the high-water mark, even though nearly 9,000 m3 was
intercepted by the sand shifter.
March TC Oma affected the area in February 2019, with increased wave action but no Double Island Point: 2018 Highest Shore-parallel Short above Short above Southern – Limited to none Limited
2019 rainfall. While erosion of Noosa Main Beach was observed, the complex wave Less N to E winds than October rainfall west of HWM, minimal HWM, average Hard up against
breaking processes over the ebb-tide delta would have limited the passage of typical, SE dominant on station coastline, then submerged submerged Doggie Beach,
large waves through the mouth. record, NE-SW shoals shoals to NW but multiple
Tewantin:
Significant channels
The northern channel has now completely broken through the northern spit close Typical winds
rainfall through shoals
to Noosa North Shore. The severed portion of the spit has migrated westward
November
to join onto Frying Pan Island.
2018.
The central and southern channels are both operational, with the southern
channel remaining dominant and largely unchanged, anchored firmly by the
scour points at the end of the training walls. The eastern end of the central
channel appears more well-defined than in previous imagery.
Growth of the southern spit stagnated but appeared to migrate slightly westward.
Nearly 19,000 m3 was recycled by the sand shifter, including pumping
undertaken immediately before and after TC Oma.
G:\Admin\B23636.g.mpb.NoosaSpit_SEMP\R.B23636.001.02.SEMP_final.docx
See the original
The page text is free to read. Viewing or downloading an original file needs an account.
Log in to see the originalLog in to download the original file
The download may take a few minutes. On mobile data, it is best to wait for Wi-Fi.