Over the past decades coastal marshes around the world have declined dramatically. Their
deterioration is controlled by scarcity of sediments, erosion and accelerated rise of relative …

Much of the world's population lives close to coastlines and this proximity is becoming
increasingly impactful because of sea-level rise (SLR). Barrier islands and backbarrier …

Extensive loss of salt marshes in back‐barrier tidal embayments is ongoing worldwide as a
consequence of land‐use changes, wave‐driven lateral marsh erosion, and relative sea …

Worldwide, many tidal basins associated with barrier coasts have infilled over the past
millennia due to the combination of sediment supply, wave‐tidal sediment transport, and eco …

Storm surge has the potential to significantly increase suspended sediment flux to microtidal
marshes. However, the overall effects of storm surge on microtidal marsh deposition have …

During the last decades many salt marshes worldwide have suffered important losses in
their extent and associated ecosystem services. The salt marshes of San Vicente de la …

There has been a decline in fluvial sediment inputs to the world's deltas but it is still unclear
to which extent upstream changes in sediment supply directly relate to variations in wetlands …

The persistence of coastal marsh is dependent on its ability to maintain elevation relative to
sea level, particularly for marshes experiencing high rates of shoreline erosion due to wave …

Modeling long‐term marsh ecomorphodynamics often requires simplifying hydrodynamic
inputs. This is usually achieved by selecting the mean or spring astronomic tidal range …

Coastal marsh loss is commonly attributed to changes in external forcings, such as an
increase in sea-level rise rate or a reduction in sediment supply. Here we show that …