Model:Sedflux: Difference between revisions
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{{Model identity | |||
|Model type=Modular | |||
}} | |||
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{{Model identity2 | |||
|ModelDomain=Coastal, Marine | |||
|Spatial dimensions=2D, 3D | |||
|One-line model description=Basin filling stratigraphic model | |||
|Extended model description=Sedflux-2.0 is the newest version of the Sedflux basin-filling model. Sedflux-2.0 provides a framework within which individual process-response models of disparate time and space resolutions communicate with one another to deliver multi grain sized sediment load across a continental margin. | |||
}} | |||
{{Start model keyword table}} | |||
{{Model keywords | |||
|Model keywords=sediment transport | |||
}} | |||
{{Model keywords | |||
|Model keywords=geodynamics | |||
}} | |||
{{Model keywords | |||
|Model keywords=stratigraphy | |||
}} | |||
{{End a table}} | |||
{{Modeler information | {{Modeler information | ||
|First name=Eric | |First name=Eric | ||
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|Town / City=Boulder | |Town / City=Boulder | ||
|Postal code=80305 | |Postal code=80305 | ||
|Country=United States | |||
|State=Colorado | |State=Colorado | ||
|Email address=huttone@colorado.edu | |Email address=huttone@colorado.edu | ||
}} | }} | ||
{{Model technical information | {{Model technical information | ||
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|Start year development=1997 | |Start year development=1997 | ||
|Does model development still take place?=Yes | |Does model development still take place?=Yes | ||
|DevelopmentCode=Only maintenance | |||
|DevelopmentCodeYearChecked=2020 | |||
|Model availability=As code | |Model availability=As code | ||
|Source code availability=Through | |Source code availability=Through web repository | ||
|Source web address=https://github.com/mcflugen/sedflux | |||
|Program license type=GPL v2 | |Program license type=GPL v2 | ||
|Memory requirements=2GB | |Memory requirements=2GB | ||
|Typical run time=minutes to days | |Typical run time=minutes to days | ||
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|Describe input parameters=River mouth characteristics (velocity, width, depth, concentration) averaged daily, or longer. | |Describe input parameters=River mouth characteristics (velocity, width, depth, concentration) averaged daily, or longer. | ||
Initial bathymetry. Input sediment distribution and properties of each grain type. Optionally, any of: tectonics, sea level, wave climate, and currents | Initial bathymetry. Input sediment distribution and properties of each grain type. Optionally, any of: tectonics, sea level, wave climate, and currents | ||
|Input format=ASCII | |Input format=ASCII | ||
|Describe output parameters=Sediment properties that include (but are not limited to) bulk density, grain size, porosity, and permeability. These are averaged over are user-specified vertical resolution (typically mm to cm). | |Describe output parameters=Sediment properties that include (but are not limited to) bulk density, grain size, porosity, and permeability. These are averaged over are user-specified vertical resolution (typically mm to cm). | ||
Sea-floor properties that include slope, water depth, and sand fraction. | Sea-floor properties that include slope, water depth, and sand fraction. | ||
|Output format=Binary | |Output format=Binary | ||
|Pre-processing software needed?=No | |Pre-processing software needed?=No | ||
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}} | }} | ||
{{Process description model | {{Process description model | ||
|Describe processes represented by the model=surface plumes, hyperpycnal plumes, sediment slope failure that results in turbidity currents or debris flows, subsidence, compaction, sediment remobilization due to waves and currents, river avulsion | |Describe processes represented by the model=surface plumes, hyperpycnal plumes, sediment slope failure that results in turbidity currents or debris flows, subsidence, compaction, sediment remobilization due to waves and currents, river avulsion | ||
|Describe key physical parameters and equations=Too numerous to list. | |Describe key physical parameters and equations=Too numerous to list. | ||
|Describe length scale and resolution constraints=Vertically: mm to cm; Horizontally: 10s of m to 1000 of m | |Describe length scale and resolution constraints=Vertically: mm to cm; Horizontally: 10s of m to 1000 of m | ||
|Describe time scale and resolution constraints=Days or greater. Component processes can have much higher resolutions for numerical stability. | |Describe time scale and resolution constraints=Days or greater. Component processes can have much higher resolutions for numerical stability. | ||
|Describe any numerical limitations and issues=-- | |Describe any numerical limitations and issues=-- | ||
}} | }} | ||
{{Model testing | {{Model testing}} | ||
}} | |||
{{Users groups model | {{Users groups model | ||
|Do you have current or future plans for collaborating with other researchers?=None | |Do you have current or future plans for collaborating with other researchers?=None | ||
}} | }} | ||
{{Documentation model | {{Documentation model | ||
|Manual model available=Yes | |Manual model available=Yes | ||
|Model website if any= | |Model website if any=https://github.com/mcflugen/sedflux | ||
}} | }} | ||
{{Additional comments model | {{Additional comments model | ||
|Comments=No | |Comments=No | ||
}} | }} | ||
{{CSDMS staff part | |||
|OpenMI compliant=No but possible | |||
|IRF interface=Yes | |||
|CMT component=Yes | |||
|PyMT component=Yes | |||
|CCA component=Yes | |||
}} | |||
{{DOI information | |||
|DOI model=10.1594/IEDA/100161 | |||
|DOI assigned to model version=2.1 | |||
|DOI-year assigned to model version=2011 | |||
|DOI-filelink=https://csdms.colorado.edu/pub/models/doi-source-code/sedflux-10.1594.IEDA.100161-2.1.tar.gz | |||
}} | |||
{{Start coupled table}} | |||
{{End a table}} | |||
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<!-- available source code can be: not, owner, source, commercial --> | <!-- available source code can be: not, owner, source, commercial --> | ||
== ''sedflux-2.0'' | |||
== ''sedflux-2.0'' == | |||
[[ image:Subsidence.jpg | 350 px | right ]] | [[ image:Subsidence.jpg | 350 px | right ]] | ||
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The spatial resolution of the architecture is typically 1-25 cm in the vertical, and 10-100 m in the horizontal when operating in 2D-mode. In 3D-mode, the .... | The spatial resolution of the architecture is typically 1-25 cm in the vertical, and 10-100 m in the horizontal when operating in 2D-mode. In 3D-mode, the .... | ||
[https://csdms.colorado.edu/ | <!-- This page is no longer viewable. Need to update link when a new page is created. | ||
[https://csdms.colorado.edu/trac/sedflux/ Read more....]. | |||
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== References == | |||
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Latest revision as of 20:18, 16 September 2020
Sedflux
Metadata
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sedflux-2.0
Sedflux-2.0 is the newest version of the Sedflux basin-filling model. Sedflux-2.0 provides a framework within which individual process-response models of disparate time and space resolutions communicate with one another to deliver multi grain sized sediment load across a continental margin. Version 2.0 introduces a series of new process models, and the ability to operate in one of two modes to track the evolution of stratigraphy in either two or three dimensions. Additions to the 2D-mode include the addition of models that simulate
- erosion and deposition of sediment along a riverbed,
- cross-shore transport due to ocean waves, and
- turbidity currents and hyperpycnal flows.
New processes in the 3D-mode include
- river channel avulsion,
- two-dimensional diffusion due to ocean storms, and
- two-dimensional flexure due to sediment loading.
The spatial resolution of the architecture is typically 1-25 cm in the vertical, and 10-100 m in the horizontal when operating in 2D-mode. In 3D-mode, the ....
References
Nr. of publications: | 25 |
Total citations: | 766 |
h-index: | 14 |
m-quotient: | 0.61 |
Featured publication(s) | Year | Model described | Type of Reference | Citations |
---|---|---|---|---|
Overeem, I.; Syvitski, J.P.M.; Hutton, E.W.H.; 2005. Three-dimensional numerical modeling of deltas.. River Deltas: concepts, models and examples. Volume 83. (View/edit entry) | 2005 | AquaTellUs Sedflux |
Model overview | 59 |
Hutton, Eric W.H.; Syvitski, James P.M.; 2008. Sedflux 2.0: An advanced process-response model that generates three-dimensional stratigraphy. Computers & Geosciences, 34, 1319–1337. 10.1016/j.cageo.2008.02.013 (View/edit entry) | 2008 | Avulsion Diffusion Plume Sedflux Subside |
Model overview | 67 |
Syvitski, James P.M; Hutton, Eric W.H; 2001. 2D SEDFLUX 1.0C:. Computers & Geosciences, 27, 731–753. 10.1016/S0098-3004(00)00139-4 (View/edit entry) | 2001 | Diffusion Sedflux |
Model overview | 97 |
See more publications of Sedflux |