Low-lying reef islands are arguably the most exposed coastal formation to climate change due to the twin threats of rising sea levels and coral reef degradation. Reef islands are composed of sediment derived from the surrounding reef. To understand the future state of reef islands we need to know the amount of sediment produced by coral reefs, the rate of sediment transport across coral reef flats, and the mode in which islands respond to sea-level rise.

This project will:

  • Determine the quantity and characteristics of carbonate sediment produced by different calcifiers and bio-erosional processes on Heron Reef, using the SedBudget approach.
  • Determine the transport of sediment by monitoring and modelling hydrodynamic sediment transport processes.
  • Simulate the changes in sediment production and transport rates under climate change.
  • Model the future of Heron Island in these scenarios.