Model:RAFEM
RAFEM
Metadata
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Introduction
The River Avulsion and Floodplain Evolution Model (RAFEM) is a cellular model that simulates river and floodplain morphodynamics over large space and timescales. Cell size is larger than the channel belt width, and natural levees, which maintain a bankfull elevation above the channel bed, exist within a river cell. The river course is determined using a steepest-descent methodology, and erosion and deposition along the river profile are modeled as a linear diffusive process. An avulsion occurs when the riverbed becomes super-elevated relative to the surrounding floodplain, but only if the new steepest-descent path to sea level is shorter than the prior river course. If the new path to sea level is not shorter, then a crevasse splay is deposited in the adjacent river cells. The model has been designed to couple with the Coastline Evolution Model through the CSDMS Basic Model Interface.
History
References
| Nr. of publications: | 1 |
| Total citations: | 32 |
| h-index: | 1 |
| m-quotient: | 0.11 |
| Featured reference(s) | Open Access Status | Year | Type of Reference | Cited |
|---|---|---|---|---|
| Ratliff, Katherine M.; Hutton, Eric H. W.; Murray, A. Brad; 2018. Exploring Wave and Sea‐Level Rise Effects on Delta Morphodynamics With a Coupled River‐Ocean Model. Journal of Geophysical Research: Earth Surface, 1232887–2900. 10.1029/2018JF004757 | · publishedVersion |
2018 | a module overview describing a module | 32 |
