The ability to map shorelines through time provides valuable insights into whether changes to Australia’s coastline are the result of specific events or actions, or processes of more gradual change over time. This information can enable scientists, managers and policy-makers to assess the effects of the drivers impacting our coastlines, and potentially aid planning and forecasting for future scenarios.
Digital Earth Australia (DEA) Coastlines (GA 2021) is a continental dataset that includes annual shorelines and rates of coastal change along the entire Australian coastline from 1988 to the present. DEA Coastlines combines satellite data from Geoscience Australia’s DEA program (Dhu et al. 2017, Lewis et al. 2017) with tidal modelling to map the dominant position of the shoreline at mean sea level tide each year. DEA Coastlines allows trends of coastal erosion and growth to be examined at both local and continental scales, and for patterns of coastal change to be mapped historically and updated regularly as data continues to be acquired. This allows current rates of coastal change to be compared with those observed in previous years or decades.
The 33-year DEA Coastlines record provides new insights into patterns and processes of coastal change across the entire Australian coastline. At a national scale, 22% of Australia’s nonrocky coastlines have retreated or grown significantly since 1988, with 78% remaining net stable over this time (Table 2) (Bishop-Taylor et al. 2021). Trends of retreat and growth were closely balanced across Australia over the past 3 decades, despite strong regional variability and extreme local hotspots of coastal change – for example, point 1 in Figure 7.
At a local scale, DEA Coastlines can be used to better understand the complex coastal processes occurring at these hotspots of coastal change. For example, on Australia’s wave-dominated coasts, coastal barriers and lagoons are threatened by the influence of relative sea level rise, altered storm systems and other climatic effects (Nanson et al. 2022). Barrier responses are likely to vary between regions, and detailed analyses of historical barrier dynamics can help to inform their management.
Figure 8 presents 2 examples of how DEA Coastlines can provide insights into historical erosion impacting coastal lagoon barriers. Figure 8a shows that that changes at Southport Lagoon are all negative, indicating sand loss, with losses of around 2 m being most common, apart from 0 m. Figure 8b shows the lagoon; the area in the white box is shown in more detail in Figure 8c. Figure 8d traces the barrier width over time, measured along the white dotted line in Figure 8c. Figures 8e–h give similar results for Bribie Island – again, the barrier is thinning.
These long-term insights can be used to aid management of these affected ecosystems and population centres, complementing coastal monitoring data from existing state and local government programs.