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The Unit operates a twin-engined Piper PA 44 Seminole, registered VH-UNG, which is fully approved for commercial aerial survey operations and for flight under the Instrument Flight Rules, and which meets current requirements for scientific flight instrumentation. With one seat removed for instrumentation, the Seminole is a 3-seat aircraft with a cruise speed of around 250 km/h and a range of 1200 km, and an airborne endurance of over 210 minutes, depending on fuel and payload.

Modifications to the aircraft to facilitate scientific surveys are fully approved and include an observation port in the floor of the rear luggage compartment which allows a direct and unimpeded view of data acquisition equipment of the earths surface below the aircraft. Scientific power is available from either or both of the engines alternators, and an instrument rack is fitted to enable attachment of various types of scientific equipment.

The primary equipment is a Riegl VQ480i airborne scanning laser which transmits and receives lidar return data from the earth’s surface. The VQ480i acquires multiple returns, has a cross-track field of view of 60^o, uses scan rates from 50 – 550 KHz, and is effective up to a height of 700 m above the earth’s surface. To facilitate positioning, the lidar also uses a Novatel OEMV precision dual-frequency carrier-phase receiver, and a Novatel SPAN HG1700/H62 tactical grade inertial sensor. The Novatel Waypoint GPS/IMU software Riegl RiProcess is used to post-process the data. Survey flight lines can be created and followed using the navigational GPS, or the scientific GPS. A 50 megapixel Canon camera allows acquisition of visual images for descriptive or stereoscopic analyses. At 1000 ft altitude, the swath width is over 300 m, and with a groundspeed of about 70 ms^-1 we can capture a beach such as Wamberal in less than a minute of flight time, but with over 10 topographic data points per m². Accuracy is better than 10 cm vertically, and 15 cm horizontally. At 1500 ft altitude the data density is lower, but the swath width wider.

New scientific equipment purchased for aerial survey use include a Picarro 2401-m Gas analyser, which will be housed in the cabin, and that will be used to assess ambient air gas concentrations, and an Aventech AIMS-30 meteorology probe which will acquire outside air temperature, humidity, temperature and wind velocity.

Early work at �����Ʊ using airborne lidar was conducted at Lady Elliot Island in 2008 (Melville et. al., 2012). Observations of beach erosion from the northern Sydney beaches began in 2011, and with an early paper by Middleton et. al. (2013) defining the resolution an accuracy of airborne lidar. A well-cited study by Harley et al. (2017) used �����Ʊ airborne lidar to describe and analyse erosion at beaches from Coffs Harbour to Sydney that occurred during a major storm from 5th to 7th June, 2016.

The processes of erosion and deposition of sand along Australia’s beaches are complex, and depend on a large number of factors including tide height, wave height and incident direction, and wind. Broadly speaking erosion occurs during intense storm events of large waves and high winds, for example in North Narrabeen in 2016, over 180 m³ of sands were removed from a linear metre segment of beach over 3 days. Deposition happens very slowly over a number of months of milder conditions as wind waves gradually replenish the sand. Replenishment happens in the swash zone where waves are active, and the process of beach replenishment is finished off by winds that drive dry sands in to the dune areas. The balance between erosion and deposition depends primarily on the frequency and strength of storms. With a groundspeed of about 70 ms^{-1 ,} and a swath width of 300 m, we can capture topography for a beach such as Wamberal in less than a minute of flight time, but with over 10 topographic data points per m². Accuracy is better than 10 cm vertically, and 15 cm horizontally. Here we present data from surveys undertaken since 2016, to allow readers to understand some of the complexities.

A plan view of sands lost between 5^th April 2016 and 22^nd July 2020 in the Wamberal beach area is shown in Figure A. The dark blue colour indicates no changes, and is evident for the fixed topography of building and roads. The red shading on some roofs is false and should be ignored, and arises from a data density difference from the two surveys. On the beach itself the colour shades represent changes in topographic beach heights, as indicated by the colour bar scale. Blue indicates no change while red indicates changes in excess of 3m. The red shading in the area of beach near the Profiles line directly abuts the blue of residential infrastructure, indicating major losses at the edge of and within private properties. At Wamberal a significant width of beach has shown over 3m loss of sand height over the 5-year period, and this loss is not just in a small area of beach but extends for hundreds of metres alongshore. The scale of sand loss is clearly huge.

Comparing profiles obtained at different times gives us some idea of the complexity of changes. Figure B shows cross sectional beach profiles taken at the section indicated in Figure A on five different dates. The red profile was obtained before the East Coast Low event of 5^th June 2016, and shows a gradually sloping beach all the way from the ocean up toward the houses, with a small coastal dune at the top of the beach. Much of this was swept away during that storm event as indicated by the green profile obtained on 7^th June 2016. The blue profile of 11^th June 2018 shows that a significant amount of sand has returned to the beach, but mostly on the lower beach by wave action, and sand has yet to build up near the steep areas abutting the housing. By 18^th June 2016 after a small storm, the outer beach had lost a metre or two of sand, while the main slope near the housing was unaffected. The last profile taken recently on 22^nd July shows that all of the gains since July 2016 were lost and the beach is almost non existent, with sand cliffs next to housing of slope approximately 0.8 (40^o), steeper than the angle of repose for dry sand slopes to remain stable.

So the descriptive story is straightforward, and with Dr Kathleen McInnes of CSIRO forecasting that storms will potentially become more numerous and stronger as sea level rises and climate warming drives more water vapour into our atmosphere, coastal erosion is likely to become more severe, not less.

Experts in coastal erosion and coastal engineering in local Universities, the NSW State Government, and local councils are looking into solutions for sensitive “hotspots” of erosion in NSW, but as Dr Mitchell Harley, a beach erosion expert from �����Ʊ indicates “There is no easy solution”. Climate change and its impacts will remain one of our biggest challenges.

Ongoing beach topographic studies have continued with funding from the NSW Department of Planning and Environment, and data is archived with public access at��.

In February, 2019, the aircraft was in southern Queensland, and the opportunity arose to undertake a lidar and aerial photographic survey of Lady Elliot Island, the most southern cay of the Great Barrier Reef. This was a follow up to research that was undertaken in 2008. The first sub-section below describes the lidar data, while the second concerns the aerial photography.

Lidar Data

Accuracy of the lidar is better than 30 cm horizontally and 10 cm vertically (Middleton et al, 2013). Lidar pulses are emitted via a scanning mechanism that provides returns from a swath approximately 250 m wide at 1000 ft altitude. The aircraft flies at approximately 50m s-1, so the lidar will survey approximately 12500 m2. s-1��. Each square metre will have up to 10 points of return, and creating an overlap of all survey swaths gives 20 points m-2, taken from different angles. This provides penetration through the canopy to lower levels of vegetation and to the ground, allowing estimation of mid level vegetation heights as well as the canopy and ground surface. Flights are conducted along parallel tracks so the surveys cover the island with overlapping swaths to ensure that data density is adequate. The basic ground topography can be deduced from the last lidar return data set, and this is shown in Figure 1.

A false-colour image of the canopy of Lady Elliot as obtained from the first returns is shown in Figure 2. The resort buildings are located on the south-eastern quadrant of the island, and the grass covered runway which is 800 m long and 70 m wide runs approximately north-south from beach to beach across the entire island. There is a pedestrian pathway with low grass running from the resort to the south-western side of the island where there are two light-houses, 3 housing structures, and 2 sheds.

The colour bar indicates heights in metres above sea level. To gain an idea of the nature of the lidar images, a brief description of the vegetation is useful. The tall trees just to the southwest of the swimming pool are old naturally-occurring Pisonia trees and these have a relatively dense top canopy.Other Pisonia trees line the southern edges of the walkway to the west, and these were planted by the Resort owners in the last decade. The northern beaches either side of the runway end are fringed by Casuarina trees, but have extensive Octopus bushes beneath.

The highest point of the island is only about 5 m above low water, or 3 m above high tide, and is at the northwest corner of the island. Sandy beaches with relatively smooth contours run from low water to the vegetated area. Changes in beach topography can easily be detected by repeat surveys as have been done a number of times in other places (see for example, Harley et al, 2017). Deducting the ground topography from the canopy heights gives a direct measure of the vegetation heights. This is shown in Figure 2(B).

One way of depicting the vegetation density as a function of height is to plot vertical cross-sections of the canopy, and these are shown in Figure 3. The dot point depictions show the heights at which the lidar signals are reflected, and so are a direct measure of the height and density of the vegetation. One east-west cross section runs from the runway east at northern end of the Island, and the other from the lighthouse to the resort.