Many overlapping mechanisms have been proposed to control horizontal seaward expansion of marshes and rates of elevation change that are associated with it. Key questions to resolve are: i) whether simple geomorphological conditions such as elevation are a reliable predictor of marsh expansion rates; ii) whether there are seasonal vegetation-induced effects on elevation change (both, increase and decrease of elevation); and iii) how steep the spatial gradient of elevation change is from the bare tidal flat into the vegetated marsh? These questions have been addressed with a two-scale study approach performed on two contrastingly wave-exposed marshes in the Scheldt Estuary (SW Netherlands and N Belgium) where <i>Scirpus maritimus</i> is the ...
A growing number of coastal eco-geomorphologic modeling studies have been conducted to understand co...
In the Wadden Sea, an increasing area of the man-made tidal marshes, which cover over 17,000 ha, are...
High-lying vegetated marshes and low-lying bare mudflats have been suggested to be two stable states...
Many overlapping mechanisms have been proposed to control horizontal seaward expansion of marshes an...
Tidal marshes often present cyclic dynamics, with alternating phases of expansion and lateral retrea...
Along coasts and estuaries, formerly embanked land is increasingly restored into tidal marshes in or...
Accelerating sea-level rise and human impacts to the coast (e.g., altered sediment supply and hydrol...
Tidal marshes maintain elevation relative to sea level through accumulation of mineral and organic m...
Tidal marshes maintain elevation relative to sea level through accumulation of mineral and organic m...
Salt marsh survival in the face of sea-level rise (SLR) depends largely on a marsh’s ability to comp...
The alternative stable states theory is increasingly applied to tidal marsh shorelines, where the tw...
Accretion rates and surface elevation changes were measured in three natural salt marshes in the Wad...
Accretion rates and surface elevation changes were measured in three natural salt marshes in the Wad...
A summer polder had developed a deficit in surface elevation of about 20 cm in respect to rising sea...
In the Wadden Sea, an increasing area of the man-made tidal marshes, which cover over 17,000 ha, are...
A growing number of coastal eco-geomorphologic modeling studies have been conducted to understand co...
In the Wadden Sea, an increasing area of the man-made tidal marshes, which cover over 17,000 ha, are...
High-lying vegetated marshes and low-lying bare mudflats have been suggested to be two stable states...
Many overlapping mechanisms have been proposed to control horizontal seaward expansion of marshes an...
Tidal marshes often present cyclic dynamics, with alternating phases of expansion and lateral retrea...
Along coasts and estuaries, formerly embanked land is increasingly restored into tidal marshes in or...
Accelerating sea-level rise and human impacts to the coast (e.g., altered sediment supply and hydrol...
Tidal marshes maintain elevation relative to sea level through accumulation of mineral and organic m...
Tidal marshes maintain elevation relative to sea level through accumulation of mineral and organic m...
Salt marsh survival in the face of sea-level rise (SLR) depends largely on a marsh’s ability to comp...
The alternative stable states theory is increasingly applied to tidal marsh shorelines, where the tw...
Accretion rates and surface elevation changes were measured in three natural salt marshes in the Wad...
Accretion rates and surface elevation changes were measured in three natural salt marshes in the Wad...
A summer polder had developed a deficit in surface elevation of about 20 cm in respect to rising sea...
In the Wadden Sea, an increasing area of the man-made tidal marshes, which cover over 17,000 ha, are...
A growing number of coastal eco-geomorphologic modeling studies have been conducted to understand co...
In the Wadden Sea, an increasing area of the man-made tidal marshes, which cover over 17,000 ha, are...
High-lying vegetated marshes and low-lying bare mudflats have been suggested to be two stable states...