Model:RAFEM: Difference between revisions
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| | |ModelDomain=Terrestrial | ||
|Spatial dimensions=2D | |Spatial dimensions=2D | ||
|Spatialscale=Continental, Regional-Scale | |Spatialscale=Continental, Regional-Scale | ||
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|Last name=Ratliff | |Last name=Ratliff | ||
|Type of contact=Model developer | |Type of contact=Model developer | ||
|Institute / Organization= | |Institute / Organization=Environmental Protection Agency (US EPA) | ||
|Town / City= | |Town / City=Research Triangle Park | ||
|Postal code=27707 | |Postal code=27707 | ||
|Country=United States | |Country=United States | ||
|Email address= | |State=North Carolina | ||
|Email address=ratliff.katherine@epa.gov | |||
}} | }} | ||
{{Model technical information | {{Model technical information | ||
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|Start year development=2014 | |Start year development=2014 | ||
|Does model development still take place?=Yes | |Does model development still take place?=Yes | ||
|DevelopmentCode=Active | |||
|DevelopmentCodeYearChecked=2020 | |||
|Source code availability=Through web repository | |Source code availability=Through web repository | ||
|Source web address=https://github.com/katmratliff/avulsion-bmi | |Source web address=https://github.com/katmratliff/avulsion-bmi | ||
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{{Additional comments model}} | {{Additional comments model}} | ||
{{CSDMS staff part | {{CSDMS staff part | ||
|OpenMI compliant= | |OpenMI compliant=No but possible | ||
|IRF interface= | |IRF interface=Yes | ||
|CMT component= | |CMT component=No but possible | ||
|PyMT component=Yes | |||
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== References == | == References == | ||
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== Issues == | == Issues == |
Latest revision as of 20:18, 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: | 24 |
h-index: | 1 |
m-quotient: | 0.17 |
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 | 24 |
See more publications of RAFEM |