Research news on barrier island migration

Barrier island migration refers to the landward, seaward, or alongshore translation of barrier island systems driven by sediment transport processes and relative sea-level change. It is governed by storm overwash, inlet formation and infilling, longshore sediment transport, and aeolian sand movement, which redistribute sediment across the shoreface, beach, dune, and back-barrier environments. Under rising sea level and high storm frequency, overwash and inlet breaching typically promote landward “rollover” of islands, while sediment surplus and progradation can drive seaward migration. Barrier island migration is a central topic in coastal morphodynamics, influencing shoreline resilience, habitat distribution, and coastal management strategies.

Discarded ancient 'trash' now protecting Georgia barrier islands

Penn State Assistant Professor of Anthropology Jacob Holland-Lulewicz is among a group of archaeologists who have spent years conducting research on the barrier islands off the coast of Georgia. The islands have changed shape ...

Flooding from below: The unseen risks of sea level rise

As climate change continues to drive global sea level rise, many people living in coastal areas are already seeing the effects. Coastal erosion is accelerating and shifting coastlines inland, and storm surges are getting ...