The lower shoreface provides the connection between the continental shelf and the
shoreline via its onshore transition called the upper shoreface. Lower shorefaces are …

Sediment budgets on wave-dominated coastlines are important in determining shoreline
behaviour and are primarily inherited from geological-scale coastal evolutionary history …

The response of coastal barrier islands to relative sea-level rise (SLR) is a long-debated
issue. Over centennial and longer periods, regional barrier retreat is generally proportional …

The response of barrier islands to sea‐level rise is modulated by combinations of coastal
processes, eco‐geomorphic feedbacks and structural controls, such as antecedent …

The development of coastal adaptation pathways along sandy barrier-island coasts requires
an understanding of multi-decadal barrier morphodynamics in response to forcings such as …

Natural and constructed dunes are increasingly being utilized to buffer flooding impacts from
storms and rising sea levels along sandy coastlines. However, a lack of data at the …

Quantitative predictions of marine and aeolian sediment transport in the nearshore–beach–
dune system are important for designing Nature-Based Solutions (NBS) in coastal …

The behavior of siliciclastic coastal systems is largely controlled by the interplay between
accommodation creation and infilling. Factors responsible for altering sediment fluxes to and …

Prograded barrier systems record shoreline behaviour and palaeoenvironmental
information. The Guichen Bay Holocene embayment fill succession in South Australia has …

The double tombolo of Orbetello, in Italy, has formed during the Holocene around an ancient
central tombolo. Earlier models consider that its sand barriers formed as sand spits that …