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| {| class="wikitable collapsible collapsed" | | {| class="wikitable collapsible collapsed" |
| |- | | |- |
| ! class="model_header_col1"| sedflux | | ! class="fill_out_model_header_col1"| sedflux |
| ! class="model_header_col2"| Eric Hutton | | ! class="fill_out_model_header_col2"| Eric Hutton |
| ! class="model_header_col3"| Not yet | | ! class="fill_out_model_header_col3"| [[Sedflux|Learn more...]] |
| |- | | |- |
| ! class="model_section_header" colspan="3" | Contact information | | ! class="model_section_header" colspan="3" | Contact information |
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| |- | | |- |
| | class="model_col1"| Email: | | | class="model_col1"| Email: |
| | class="model_col2" colspan="2"| -- | | | class="model_col2" colspan="2"| eric.hutton@colorado.edu |
| |-
| |
| ! class="model_section_header" colspan="3" | Model description
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| |-
| |
| | class="model_col1"| Model type:
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| | class="model_col2" colspan="2"| Modular model
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| |-
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| | class="model_col1"| Description:
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| | class="model_col2" colspan="2"| 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.
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| |-
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| ! class="model_section_header" colspan="3" | Technical information
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| |-
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| | class="model_col1"| Supported platforms:
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| | class="model_col2" colspan="2"| Unix, Linux, Mac OSX
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| |-
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| | class="model_col1"| Programming language:
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| | class="model_col2" colspan="2"| C
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| |-
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| | class="model_col1"| Model was developed started from:
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| | class="model_col2" colspan="2"| 1997 and development still takes place
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| |-
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| | class="model_col1"| To what degree will the model become available:
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| | class="model_col2" colspan="2"| As code and as executable
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| |-
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| | class="model_col1"| Current license type:
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| | class="model_col2" colspan="2"| GPL_v2
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| |-
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| | class="model_col1"| Memory requirements:
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| | class="model_col2" colspan="2"| 2GB
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| |-
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| | class="model_col1"| Typical run time:
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| | class="model_col2" colspan="2"| minutes to days
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| |-
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| ! class="model_section_header" colspan="3" | Input / Output description
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| |-
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| | class="model_col1"| Input parameters:
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| | class="model_col2" colspan="2"| River mouth characteristics (velocity, width, depth, concentration) averaged daily, or longer.
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| Initial bathymetry.
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| Input sediment distribution and properties of each grain type.
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| Optionally, any of: tectonics, sea level, wave climate, and currents
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| |-
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| | class="model_col1"| Input format:
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| | class="model_col2" colspan="2"| ASCII
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| |-
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| | class="model_col1"| Output parameters:
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| | class="model_col2" colspan="2"| 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).
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| Sea-floor properties that include slope, water depth, and sand fraction.
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| |-
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| | class="model_col1"| Output format:
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| | class="model_col2" colspan="2"| Binary
| |
| |-
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| | class="model_col1"| Post-processing software (if needed):
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| | class="model_col2" colspan="2"| no
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| |-
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| | class="model_col1"| Visualization software (if needed):
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| | class="model_col2" colspan="2"| Yes, Matlab
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| |-
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| ! class="model_section_header" colspan="3" | Process description
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| |-
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| | class="model_col1"| Processes represented by model:
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| | class="model_col2" colspan="2"| 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
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| |-
| |
| | class="model_col1"| Key physical parameters & equations:
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| | class="model_col2" colspan="2"| Too numerous to list.
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| |-
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| | class="model_col1"| Length scale & resolution constraints:
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| | class="model_col2" colspan="2"| Vertically: mm to cm; Horizontally: 10s of m to 1000 of m
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| |-
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| | class="model_col1"| Time scale & resolution constraints:
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| | class="model_col2" colspan="2"| Days or greater. Component processes can have much higher resolutions for numerical stability.
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| |-
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| | class="model_col1"| Numerical limitations and issues :
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| | class="model_col2" colspan="2"| --
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| |-
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| ! class="model_section_header" colspan="3" | Testing
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| |-
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| | class="model_col1"| Available calibration data sets:
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| | class="model_col2" colspan="2"| --
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| |-
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| | class="model_col1"| Available test data sets:
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| | class="model_col2" colspan="2"| --
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| |-
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| | class="model_col1"| Ideal data for testing:
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| | class="model_col2" colspan="2"| --
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| |-
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| | class="model_section_header" colspan="3" | User groups
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| |-
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| | class="model_col1"| Currently or plans for collaborating with:
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| | class="model_col2" colspan="2"| None
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| |-
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| ! class="model_section_header" colspan="3" | Documentation
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| |-
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| | class="model_col1"| Key papers of the model:
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| | class="model_col2" colspan="2"| Sedflux-2.0: An advanced process-response model that generates three-dimensional stratigraphy.
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| |-
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| | class="model_col1"| Is there a manual available:
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| | class="model_col2" colspan="2"| Yes
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| |-
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| | class="model_col1"| Model website if any:
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| | class="model_col2" colspan="2"|(http://sedflux.googlecode.com)
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| |-
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| ! class="model_section_header" colspan="3" | Additional comments
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| |-
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| | class="model_col1"| Comments:
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| | class="model_col2" colspan="2"| No
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| |} | | |} |
