Olivia Cheriton Kurt J. Rosenberger Andrew Pomeroy Ryan J. Lowe Curt D. Storlazzi 2019 <p><span>Coral reefs generate significant volumes of carbonate sediment that becomes the primary source of beach material along many low-latitude shorelines that protect hundreds of millions of people globally. Despite this fact, there is little understanding of the specific processes that transport the carbonate sediment produced on the outer portions of coral reefs to the shoreline, let alone how those processes may be affected by projected sea-level rise. To better constrain the influence of sea-level rise on waves and sediment transport over a fringing coral reef flat, an experiment was conducted across the large fringing reef off the south shore of Moloka’i, Hawai’i, in the summer of 2018. Here we describe the influence of water levels on waves, currents, and the resulting sediment resuspension and fluxes observed during this field effort</span></p> application/pdf 10.1142/9789811204487_0087 en World Scientific The influence of sea level on incident and infragravity wave-driven sediment dynamics across a fringing coral reef text