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Model described in:
G. Mariotti, and J. Carr, (2014), Dual role of salt marsh retreat: Long-term loss and short-term resilience, WRR, DOI: 10.1002/2013WR014676.
The source code reproduce figure 2 of this paper. +
No but possible +
No but possible +
No but possible +
Single Processor +
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16:14:40, 26 March 2014 +
Marsh vegetation and mudflat sediment characteristics
Backbarrier basin width
Reference wind speed
Tidal range
Reference sediment concentration +
length scale resolved 1-10 m +
Marsh depth, mudflat depth, mudflat width +
Marsh boundary erosion by waves
Marsh boun … Marsh boundary erosion by waves</br>Marsh boundary progradation by accumulating sediments</br>Mudflat sediment erosion/deposition by wind waves</br>Sediment exchange between mudflat and open ocean</br>Sediment exchange between mudflat and marsh platform</br>Organogenic sediment production on marsh platformenic sediment production on marsh platform +
time step ~ 1-100 days
do not resolve tides +
Only maintenance +
The model simplifies the geometry of a bac … The model simplifies the geometry of a backbarrier tidal basin with 3 variables: marsh depth, mudflat depth, mudflat width. These 3 variables are evolved by sediment redistribution driven by wave processes. Sediment are exchanged with the open ocean, which is an external reservoir. Organic sediments are produced on the marsh platform.iments are produced on the marsh platform. +
giulio +
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ASCII +
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0.08 +
Coastal +
Wetland 3 point +
As code +
Single +
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02:16:50, 17 September 2020 +
1 +
A 3-point dynamic model for the morphological evolution of a backbarrier basin composed by marshes and mudflats +
ASCII +
77 Massachusetts Ave +
02139 +
false +
false +
GPL v2 +
Matlab +
1 second +
Through CSDMS repository +
https://github.com/csdms-contrib/wetland3p +
Landscape-Scale +
2012 +
Model developer +
