This paper offers a synthesis of the disparate evidence on the importance of the magnitude
and duration of water level rise in both lacustrine and marine environments in relation to …

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 …

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 …

Preserved beach and foredune ridges may serve as proxies for coastal change, reflecting
alterations in sea level, wave energy, or past sediment fluxes. In particular, time‐varying …

Barrier coasts, including barrier islands, beach-ridge plains, and associated landforms, can
assume a broad spectrum of morphologies over decadal scales that reflect conditions of …

In this paper, a conceptual model is presented addressing the morphological evolution of a
headland-controlled inlet at Babitonga Bay, Southern Brazil. Multiple historic bathymetric …

Tidal-inlet systems are dynamic features that respond to short-term (eg, storms) and longer-
term processes (eg, sea-level rise, changes in tidal prism). The Chincoteague Inlet system …

Patterns of spit growth (elongation or re-orientation) can be sensitive to long-term changes
in wave climate, which can starve downdrift barriers of sediment. This study quantifies …

This paper addresses the range of processes (wind, waves, tides and currents) responsible
for transporting sediment past headlands by bypassing and overpassing. Field data was …