Model:CellularFanDelta: Difference between revisions

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{{Infobox Model
{{Model identity
|model name              = CellularFanDelta
|developer                = '''Wolinsky''', Matthew
|one-line-description    = Coarse-grained delta dynamics and stratigraphy 
|type                    = Model
|source                  = [[image:Red1.png]]
}}
}}
<!-- Edit the part above to update info on other papers -->
{{Model identity2
|ModelDomain=Coastal, Terrestrial
|Spatial dimensions=3D
|One-line model description=Coarse-grained delta dynamics and stratigraphy
|Extended model description=3D cellular model simulating delta evolution in coarse grained river dominated systems (e.g. a gravel fan delta).
}}
{{Start model keyword table}}
{{Model keywords
|Model keywords=delta evolution
}}
{{Model keywords
|Model keywords=stratigraphy
}}
{{Model keywords
|Model keywords=coarse grain
}}
{{End a table}}
{{Modeler information
|First name=Matthew
|Last name=Wolinsky
|Type of contact=Model developer
|Town / City=Matthew.Wolinsky@shell.com
|Postal code=77001
|State=Texas
|Country=United States
|Email address=Matthew.Wolinsky@shell.com
|Phone=713-245-8384
}}
{{Model technical information
|Supported platforms=Windows
|Programming language=C++, Matlab
|Other program language=(Programmed as C MEX files called from Matlab. Currently the two languages are intertwined, but could be modularized).
|Start year development=2006
|Does model development still take place?=Yes
|Model availability=As code
|Program license type=GPL v2
|Memory requirements=--
|Typical run time=hours to days
}}
{{Input - Output description
|Describe input parameters=Domain dimensions and cell size (regular 2D grid). Initial condition.


== CellularFanDelta ==
Locations and rates of sediment and water influxes. Subsidence pattern and rate. Sea level curve. (Presently all boundary conditions are constant, but could vary in space and time in future versions)
__TOC__
|Input format=ASCII
 
|Other input format=Runs from Matlab command line
===Introduction===
|Describe output parameters=Time series of 2D topography/bathymetry and water discharge. 3D stratigraphy grid
 
=== History ===


=== Papers ===
=== CellularFanDelta Questionnaire ===
==== Contact Information ====
{| class="wikitable"
| class="model_col1"| Model:
| class="model_col2"| CellularFanDelta
|-
| class="model_col1"| Contact person:
| class="model_col2"| Matthew Wolinsky (Model developer)
|-
| class="model_col1"| Institute:
| class="model_col2"| --
|-
| class="model_col1"| City:
| class="model_col2"| --
|-
| class="model_col1"| Country:
| class="model_col2"| --
|-
| class="model_col1"| Email:
| class="model_col2"| --
|-
| class="model_col1"| 2nd person involved:
| class="model_col2"| --
|-
| class="model_col1"| 3rd person involved:
| class="model_col2"| --
|-
|}
==== Model Description ====
{| class="wikitable" 
| class="model_col1"| Model type:
| class="model_col2"| Modular model for the terrestrial and coastal domain.
|-
| class="model_col1"| Description:
| class="model_col2"| 3D cellular model simulating delta evolution in coarse grained river dominated systems (e.g. a gravel fan delta).
|-
|}
==== Technical information ====
{| class="wikitable" 
| class="model_col1"| Supported platforms:
| class="model_col2"| Windows
|-
| class="model_col1"| Programming language:
| class="model_col2"| C++, Matlab (Programmed as C MEX files called from Matlab. Currently the two languages are intertwined, but could be modularized).
|-
| class="model_col1"| Model development started at:
| class="model_col2"| 2006 and development still takes place.
|-
| class="model_col1"| To what degree will the model become available:
| class="model_col2"| Source code will be available
|-
| class="model_col1"| Current license type:
| class="model_col2"| GPLv2
|-
| class="model_col1"| Memory requirements:
| class="model_col2"| --
|-
| class="model_col1"| Typical run time:
| class="model_col2"| hours to days
|}
==== Input / Output description ====
{| class="wikitable"
| class="model_col1"| Input parameters:
| class="model_col2"| Domain dimensions and cell size (regular 2D grid). Initial condition.
Locations and rates of sediment and water influxes. Subsidence pattern and rate. Sea level curve. (Presently all boundary conditions are constant, but could vary in space and time in future versions)
|-
| class="model_col1"| Input format:
| class="model_col2"| ASCII, Runs from Matlab command line
|-
| class="model_col1"| Output parameters:
| class="model_col2"| Time series of 2D topography/bathymetry and water discharge. 3D stratigraphy grid
(currently model is single grain-size, so stratigraphy only stores deposit age)
(currently model is single grain-size, so stratigraphy only stores deposit age)
|-
|Output format=ASCII
| class="model_col1"| Output format:
|Other output format=2D grids can be ASCII, but stratigraphy is custom-designed structure stored in Matlab format.
| class="model_col2"| ASCII, 2D grids can be ASCII, but stratigraphy is custom-designed structure stored in Matlab format.
|Pre-processing software needed?=Yes
|-
|Describe pre-processing software=Post-processing and (pre-processing) is through Matlab scripts.
| class="model_col1"| Post-processing software (if needed):
|Post-processing software needed?=Yes
| class="model_col2"| yes, Post-processing and (pre-processing) is through Matlab scripts.
|Describe post-processing software=Post-processing and (pre-processing) is through Matlab scripts.
|-
|Visualization software needed?=Yes
| class="model_col1"| Visualization software (if needed):
|If above answer is yes=Matlab
| class="model_col2"| Yes, Matlab
}}
|}
{{Process description model
 
|Describe processes represented by the model=The key processes are 1) topographically-driven overland flow and 2) bedload transport by this flow. Through these processes the model self-organizes channels which incise, back-fill, and avulse. Processes are similar to alluvial fans. There are no marine processes besides bedload dumping.
==== Process description ====
|Describe key physical parameters and equations=Topographic slope-weighted multiple flow direction water routing. Stream power transport.
 
|Describe length scale and resolution constraints=There are two primary constraints:
{| class="wikitable"
| class="model_col1"| Processes represented by model:
| class="model_col2"| The key processes are 1) topographically-driven overland flow and 2) bedload transport by this flow. Through these processes the model self-organizes channels which incise, back-fill, and avulse. Processes are similar to alluvial fans. There are no marine processes besides bedload dumping.
|-
| class="model_col1"| Key physical parameters & equations:
| class="model_col2"| Topographic slope-weighted multiple flow direction water routing. Stream power transport.
|-
| class="model_col1"| Length scale & resolution constraints:
| class="model_col2"| There are two primary constraints:
# Like most topographically-routed cellular river models, incised channels in the model will always be one cell wide. Hence it should not be applied at scales where the cell size is much less than main channel widths.
# Like most topographically-routed cellular river models, incised channels in the model will always be one cell wide. Hence it should not be applied at scales where the cell size is much less than main channel widths.
# The model does not really simulate low-Froude low-slope rivers such as most large coastal deltas. However processes are similar to many other codes (e.g. DIONISOS) commonly used for large-scale deltas. If primary questions are about large-scale basin filling on O(10 ka) or longer timescales the model should be fine. However when questions relate to details of sub-millenial geomorphic processes or reservoir-scale stratigraphic architecture, some care must be taken in interpreting model results.
# The model does not really simulate low-Froude low-slope rivers such as most large coastal deltas. However processes are similar to many other codes (e.g. DIONISOS) commonly used for large-scale deltas. If primary questions are about large-scale basin filling on O(10 ka) or longer timescales the model should be fine. However when questions relate to details of sub-millenial geomorphic processes or reservoir-scale stratigraphic architecture, some care must be taken in interpreting model results.
|-
|Describe time scale and resolution constraints=See above.
| class="model_col1"| Time scale & resolution constraints:
|Describe any numerical limitations and issues=Numerical limitations and issues:
| class="model_col2"| See above.
# Currently the model runs with a constant timestep, which is limited by the maximum inflow. Future versions may include adaptive time-stepping.
|-
| class="model_col1"| Numerical limitations and issues :
| class="model_col2"| # Currently the model runs with a constant timestep, which is limited by the maximum inflow. Future versions may include adaptive time-stepping.
# As mentioned above, the model channels tend to be one or two cells wide. Future versions may address this issue with some combination of diffusive regularization or multi-scale modeling.
# As mentioned above, the model channels tend to be one or two cells wide. Future versions may address this issue with some combination of diffusive regularization or multi-scale modeling.
|}
}}
{{Model testing
|Describe available calibration data sets=
|Describe available test data sets=
|Describe ideal data for testing=Coarse-grained delta experiments without too valley widening, e.g. many XES experiments conducted at the Saint Anthony Falls Laboratory by Paola et al.
}}
{{Users groups model
|Do you have current or future plans for collaborating with other researchers?=Possibly
}}
{{Documentation model
|Provide key papers on model if any=Will update when I get them written and published!
|Manual model available=No
}}
{{Additional comments model}}
{{CSDMS staff part
|OpenMI compliant=No but possible
|CCA component=No but possible
|IRF interface=No but possible
|CMT component=No but possible
}}
{{Start coupled table}}
{{End a table}}
{{End headertab}}
{{{{PAGENAME}}_autokeywords}}


==== Testing ====
{{NOINDEX}}
 
<!-- Edit the part above to update info on other papers -->
{| class="wikitable"
| class="model_col1"| Available calibration data sets:
| class="model_col2"| --
|-
| class="model_col1"| Available test data sets:
| class="model_col2"| --
|-
| class="model_col1"| Ideal data for testing:
| class="model_col2"| Coarse-grained delta experiments without too valley widening, e.g. many XES experiments conducted at the Saint Anthony Falls Laboratory by Paola et al.
|}
 
==== User groups ====
 
{| class="wikitable"
| class="model_col1"| Currently or plans for collaborating with:
| class="model_col2"| Possibly
|}
 
==== Documentation ====
 
{| class="wikitable"
| class="model_col1"| Key papers of the model:
| class="model_col2"| Will update when I get them written and published!
|-
| class="model_col1"| Is there a manual available:
| class="model_col2"| No
|-
| class="model_col1"| Model website if any:
| class="model_col2"| --
|}
 
==== Additional comments ====


{| class="wikitable"
==Introduction==
| class="model_col1"| Comments:
| class="model_col2"| --
|}


=== Issues ===
== History ==


=== Help ===
== References  ==
<br>{{AddReferenceUploadButtons}}<br><br>
{{#ifexist:Template:{{PAGENAME}}-citation-indices|{{{{PAGENAME}}-citation-indices}}|}}<br>
{{Include_featured_references_models_cargo}}<br>


=== Input Files ===
== Issues ==


=== Output Files ===
== Help ==
{{#ifexist:Model_help:{{PAGENAME}}|[[Model_help:{{PAGENAME}}]]|}}


=== Download ===
== Input Files ==


=== Source ===
== Output Files ==


[[Category:Terrestrial]]
[[Category:Source code not available]]
[[Category:Coastal]]

Latest revision as of 20:19, 16 September 2020



CellularFanDelta


Metadata

Also known as
Model type
Model part of larger framework
Note on status model
Date note status model
Spatial dimensions 3D
Spatial extent
Model domain Coastal, Terrestrial
One-line model description Coarse-grained delta dynamics and stratigraphy
Extended model description 3D cellular model simulating delta evolution in coarse grained river dominated systems (e.g. a gravel fan delta).
Keywords:

delta evolution, stratigraphy, coarse grain,

Name Matthew Wolinsky
Type of contact Model developer
Institute / Organization
Postal address 1
Postal address 2
Town / City Matthew.Wolinsky@shell.com
Postal code 77001
State Texas
Country United States
Email address Matthew.Wolinsky@shell.com
Phone 713-245-8384
Fax


Supported platforms
Windows
Other platform
Programming language

C++, Matlab

Other program language (Programmed as C MEX files called from Matlab. Currently the two languages are intertwined, but could be modularized).
Code optimized
Multiple processors implemented
Nr of distributed processors
Nr of shared processors
Start year development 2006
Does model development still take place? Yes
If above answer is no, provide end year model development
Code development status
When did you indicate the 'code development status'?
Model availability As code
Source code availability
(Or provide future intension)
Source web address
Source csdms web address
Program license type GPL v2
Program license type other
Memory requirements --
Typical run time hours to days


Describe input parameters Domain dimensions and cell size (regular 2D grid). Initial condition.

Locations and rates of sediment and water influxes. Subsidence pattern and rate. Sea level curve. (Presently all boundary conditions are constant, but could vary in space and time in future versions)

Input format ASCII
Other input format Runs from Matlab command line
Describe output parameters Time series of 2D topography/bathymetry and water discharge. 3D stratigraphy grid

(currently model is single grain-size, so stratigraphy only stores deposit age)

Output format ASCII
Other output format 2D grids can be ASCII, but stratigraphy is custom-designed structure stored in Matlab format.
Pre-processing software needed? Yes
Describe pre-processing software Post-processing and (pre-processing) is through Matlab scripts.
Post-processing software needed? Yes
Describe post-processing software Post-processing and (pre-processing) is through Matlab scripts.
Visualization software needed? Yes
If above answer is yes Matlab
Other visualization software


Describe processes represented by the model The key processes are 1) topographically-driven overland flow and 2) bedload transport by this flow. Through these processes the model self-organizes channels which incise, back-fill, and avulse. Processes are similar to alluvial fans. There are no marine processes besides bedload dumping.
Describe key physical parameters and equations Topographic slope-weighted multiple flow direction water routing. Stream power transport.
Describe length scale and resolution constraints There are two primary constraints:
  1. Like most topographically-routed cellular river models, incised channels in the model will always be one cell wide. Hence it should not be applied at scales where the cell size is much less than main channel widths.
  2. The model does not really simulate low-Froude low-slope rivers such as most large coastal deltas. However processes are similar to many other codes (e.g. DIONISOS) commonly used for large-scale deltas. If primary questions are about large-scale basin filling on O(10 ka) or longer timescales the model should be fine. However when questions relate to details of sub-millenial geomorphic processes or reservoir-scale stratigraphic architecture, some care must be taken in interpreting model results.
Describe time scale and resolution constraints See above.
Describe any numerical limitations and issues Numerical limitations and issues:
  1. Currently the model runs with a constant timestep, which is limited by the maximum inflow. Future versions may include adaptive time-stepping.
  2. As mentioned above, the model channels tend to be one or two cells wide. Future versions may address this issue with some combination of diffusive regularization or multi-scale modeling.


Describe available calibration data sets
Upload calibration data sets if available:
Describe available test data sets
Upload test data sets if available:
Describe ideal data for testing Coarse-grained delta experiments without too valley widening, e.g. many XES experiments conducted at the Saint Anthony Falls Laboratory by Paola et al.


Do you have current or future plans for collaborating with other researchers? Possibly
Is there a manual available? No
Upload manual if available:
Model website if any
Model forum / discussion board
Comments


This part will be filled out by CSDMS staff

OpenMI compliant No but possible
BMI compliant No but possible
WMT component No but possible
PyMT component
Is this a data component
Can be coupled with:
Model info
Authors
Matthew Wolinsky
Source code
Model citations
Nr. of publications: --
Total citations: 0
h-index: --"--" is not a number.
m-quotient: 0
QR-code
Qrcode CellularFanDelta.png
Link to this page
Other models by author

Template:CellularFanDelta autokeywords


Introduction

History

References



Nr. of publications: --
Total citations: 0
h-index: --"--" is not a number.
m-quotient: 0


See more publications of CellularFanDelta

Issues

Help

Input Files

Output Files

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