Coastal Management Report: Collaroy Beach
This report will also include the decision making processes considered by the management (both local and state), as well as the descriptions of their actions/ strategies, and thus the results of their polices. The Allocations site of interest, Collator beach is located in the suburbs of Northern Sydney, In the state of New South Wales, Australia. Collator Is part of the local government area of Warring Council and part of the Northern Beaches region. Collator is well known for its excellent surf beach which Joins with Narrate Beach in the north and Long Reef and Dee Why Beach in the south.
Also in close proximity is the Dee Why Lagoon as well as the Long Reef Head. Collator beach is the most highly capitalized shoreline in the Warring local government area, featuring beachfront houses and apartments built on the edge of the sand including the famous Flight Deck Apartments. Geographical Processional erosion is the loss of land along the shoreline due to the natural removal of beach and dune material In response to changing wave and water conditions.
Buildings and facilities located within the ‘active’ beach system, or areas subject to coastal erosion can be undermined and may even collapse. Approximately 60
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The extent of beach erosion during a particular storm event depends upon a variety of factors that wave conditions and elevated water levels generated by the stormed most prominent of these processes involves waves and the currents that they generate, along with tides Waves are generated by wind blowing over a odd of water and are ultimately responsible for the construction and erosion, as well as transportation of beach sediments. FIFO a wave is called a swash while the outgoing tide is called a backwash.
Swell waves are more powerful and cause erosion, whereas sea waves are less violent and encourage deposition. Large swell waves are usually accompanied by a storm, and the swell may become big enough to be classified as a ‘king tide’. A king tide’ arrives at Narrate-Collator Beach once or twice annual and has a devastating effect on the beach, eroding the beach until a near vertical erosion scarp is exposed. The sand than is deposited offshore to form a sand bar. Immediately following coastal erosion events on sand beaches, a near vertical erosion scarp of substantial height can be left.
If buildings are located close to the vertical erosion scarp, they may be at-risk of structural damage. Instability of the escarpment may pose a hazard to beach users following storms with recorded instances of children and beach users buried by the collapsing sand face. ;The presence of rip cells rip cell is a area with a strong surface flow of water returning seaward from near the shore). It is often called a “rip tide” However along with water returning seaward, much of the beach sediments are eroded as well helping to hasten the process of erosion. The condition of the beaches condition of the beach is also a factor in the severity of the erosion. The condition of the beach is determined by the amount of erosion that has occurred on the beach at that state of time. One indicator of condition is the identification of the beach profile. A beach which possesses a relatively large amounts of sand in the incipient dune, as well the stability of the fore dune, are in a re-storm form. A beach that has been recently eroded by a storm has a storm profile.
The features of a storm profile are the erosion of incipient dune and the exposure of the near vertical erosion scarp, near the fore dune of the beach, as well as a large offshore bar. This beach would therefore have a storm profile. A beach in which the sea waves have gradually restored the sand to the incipient dune from the sandbar, as well a stable fore-dune are the tell-tell signs of a post-osteoporosis. A beach which is in better conditions is more suited to fight sand erosion, while a second wind’ of a storm after the beach being in a storm profile could be devastating for the beach. The condition of dune vegetation which can influence the volume of sand in the dunes which help to buffer the effects of storm irresponsible sand dunes play an important part in protecting the coastline. They act as a buffer against wave damage during storms, protecting the land behind from salt-water intrusion. This sand barrier allows the development of more complex plant communities in areas protected from salt-water inundation, sea spray and strong winds. The dunes also act s a reservoir of sand, to replenish and maintain the beach at times of erosion.
When people build homes or resorts on beaches, the buildings interrupt this natural may build. In the diagram below the red line shows the extent of the danger zone. Key Interest Grouper’s key interest groups involved with the issue of the erosion of Collator include groups such as Sydney Coastal Councils Groups, which have criticize the non-actions of the Warring Council to set up a plan in the long term, instead focusing on short term relief such as sand replenishment, which CSCW deems as unsustainable in the long run. However, CSCW may be the only interest group targeting the issue.
However when it was announced that the sea wall was planned for construction two other peer groups, Surf rider Foundation Club, as well as the local Collator Surf Club Joined in action to stop the construction of the seawall. Decision Making Processes find a solution for the erosion of Collator Beach was a complicated process involving decision making and assistance in many levels. The NEWS and Commonwealth government provided assistance to Warring Council by roving material to help it construct an effective Management Strategy.
Material included in this state and commonwealth package Included 1990 the NEWS Government released its Coastline Management Manual, a guideline to help local council’s development, Coastal management plan by them. It also provided Commonwealth inquires such as reported on’ The Injured Coastline’ and’ The Coastal Zone Inquiry’. In 1993 the Warring Council set up the Warring Coastal Committee which has various stakeholders as members including: a WAC councilor, A NEWS Gobo Rep, a Surprised Rep, a SOLS Rep, Beachfront and other Local residents.
This diversity in the committee instead of Just containing members of the council helped to foster unbiased views on the opinions of the stakeholders as well increase the community involvement which helps to better serve the purpose of the community, making the ideas of the community in which is ultimately the council’s purpose anyway. The Committee meets once every two months to advice Council on the next action to stop the erosion. In August 1997 the Collator/Narrate Coastal Management Plan was adopted. Throughout this process and before any major strategies are implemented the public are invited to comment and provide community feedback.
However there have been criticisms of the committee as consensus-based Coastline Management Plan was pursued by Council but not achieved, with strong differences of opinion emerging within the community, and between the Warring Coastal Management Committee and Counterargument Actions and Strategies (and Consequences)There have been many different management strategies that could have been implemented to protect from or at least slow down the effects of erosion, enough to guarantee the safety of the dwelling.
Preliminary studies reviled that the existing rock seawalls are not strong enough to withstand a major storm. There are two long term solutions to this issue. They are voluntary purchase of high risk dwellings, and the protection of the beach through the building of a seawall or an erosion problem temporary solution involve minor to moderate sand nourishment, which are used in conjunction with either of these actions. The sand comes from the mouths of the Dee Why and Narrate Lagoons.
The management strategy of repurchasing high risk single homes has been a popular strategy amongst those whom want to protect and enhanced the recreational amenity of the beach. This method was successful back in 1945 when the council bought back 7 houses that were damaged by the storm. However in recent years, the price of backside property skyrocketed with high demand, and the strategy is currently not economically feasible at this point in time. With an average home in 2005 located on the fore dune of Collator Beach coasting a whopping 2. 7 million- the plan is estimated to cost more than 100 million dollars.
Even though the Tate government is willing to match the contributions the state government made, this strategy if implemented could take anywhere between 50 to 100 years to purchase every single home that is in the high risk zone. The alternative strategy is to develop a seawall on the beach to protect the property located on the fore dune. The sea wall would be approximately 1 km long and will be sufficient to protect the fore dune from collapsing. However the cost of the sea wall cheap in comparison to the ‘repurchase’ strategy costs approximately 11 million dollars to build.
In addition, the council expects at least 40% of the 11 million to be paid by the owners of the units, making it an unattractive deal for the residents. The seawall is also not environmentally friendly either. It is known for speeding up the process of erosion, as the energy of the storm waves is not absorbed but reflected, meaning the backwash will be stronger, and eventually the shore profile will retreat, removing what’s left of the beach. However this idea also seems to be out of reach, as after the successful “Line in the Sand” community protest in November 2002, the nuncio voted 4 months later not to proceed with the sea wall option.
So with the ‘repurchase’ strategy unlikely, and the seawall not likely to be built, how is the council going to solve the problem. Right now, the plan is to get by on minor beach nourishment from the mouth of Narrate and Dee Why Lagoons for now, while the council investigates new strategies, with the help of newly implemented coastal imaging cameras on top of Flight Deck. One of the new strategies being investigated includes an artificial surfing reef, which is basically a seawall underneath the water to amplify the surf.