Model:RAFEM: Difference between revisions
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Latest revision as of 19:18, 16 September 2020
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: | 26 |
| h-index: | 1 |
| m-quotient: | 0.12 |
| Featured publication(s) | Year | Model described | Type of Reference | Citations |
|---|---|---|---|---|
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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, 123, 2887–2900. 10.1029/2018JF004757 (View/edit entry) | 2018 | RAFEM |
Model overview | 26 |
| See more publications of RAFEM |
