Model:Caesar: Difference between revisions

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{{Modeler information
|First name=Tom
|Last name=Coulthard
|Type of contact=Model developer
|Institute / Organization=University of Hull
|Postal address 1=Cottingham Road
|Town / City=Hull
|Postal code=HU6 7RX
|State=NO STATE
|Country=United Kingdom
|Email address=T.Coulthard@hull.ac.uk
}}
{{Model identity
|Model type=Modular
|Categories=Terrestrial
|One-line model description=Cellular landscape evolution model
|Extended model description=CAESAR is a cellular landscape evolution model, with an emphasis on fluvial processes, including flow routing, multi grainsize sediment transport. It models morphological change in river catchments.
}}
{{Model technical information
|Supported platforms=Linux, Windows
|Programming language=C
|Other program language=C#
|Start year development=1996
|Does model development still take place?=Yes
|Model availability=As code, As teaching tool, As executable
|Source code availability=Through owner
|Program license type=Other
|Program license type other=GNU
|OpenMI compliant=No not possible
|CCA component=No not possible
|IRF interface=No not possible
|Memory requirements=>512MB
|Typical run time=5 min to 50 days
}}
{{Input - Output description
|Describe input parameters=DEM as ascii grid (output from arcGIS),
Rainfall data as a space separated ascii file (straightforward list), Inputs of water/sediment in an ascii file. Other single value parameter inputs for grainsize, flow parameters, slope processes etc..
|Input format=ASCII
|Describe output parameters=ascii grids (readable into arcGIS) and google earth images of: DEM, flow depth, surface grainsize, shear stress, vegetation cover, velocity.
Also time series of water discharge and sediment discharge (across 9 grainsizes) at user chosen interval.
Also visual output to AVI file.
|Output format=ASCII
|Pre-processing software needed?=No
|Post-processing software needed?=No
|Visualization software needed?=No
|If above answer is yes=ESRI
|Other visualization software=but you can use ESRI (ArcGIS)
}}
{{Process description model
|Describe processes represented by the model=2d multiple flow direction steady state flow model
Erosion and deposition over 9 separate grainsizes
Bedload and suspended load sediment transport
Slope processes (creep, enhanced creep and mass movement)
Vegetation growth
Aeolian transport (under development - slab dune model)
|Describe key physical parameters and equations=Flow depths calculated using version of mannings implemented across a cellular grid using a scanning algorithm.
Sediment tranport using either Einstein or Wilcock and Crowe functions
Slope model using simple slab failure and psuedo USLE implementation
Dune model adaption of DECAL and Werner slab model
|Describe length scale and resolution constraints=Has been applied to catchments ranging from 1km^2 to 500km^2, at grid resolutions ranging from 1m to 50m.
|Describe time scale and resolution constraints=The model has simulated periods from 1 day to 9000 years.
The length of run is largely contingent on the number of grid cells, thus a balance between resoltion and area of study. A small catchment with a coarse resolution will run very fast. Increase the area or make grid cells smaller and run times will increase.
|Describe any numerical limitations and issues=Run times can be long (60 +days for large areas over many 100's of years).
Flow model is steady state
}}
{{Model testing
|Describe available calibration data sets=Tested on several catchments in UK over long and short time scales.
|Describe available test data sets=none yet; in development
|Describe ideal data for testing=Flow and sediment discharge data, images of topographic change
}}
{{Users groups model
|Do you have current or future plans for collaborating with other researchers?=Yes, I am happy to collaborate with any potential users. There is a long history of CAESAR being take up by others including researchers in Italy, France, Spain, NZ, Australia, USA.
}}
{{Documentation model
|Provide key papers on model if any=Van De Wiel, M.J., Coulthard, T.J., Macklin, M.G., Lewin, J. (2007) Embedding reach-scale fluvial dynamics within the CAESAR cellular automaton landscape evolution model. Geomorphology, 90 (3-4), pp. 283-301.
Coulthard, T. J. Macklin, M. G. & Kirkby, M. J. (2002) Simulating upland river catchment and alluvial fan evolution. Earth Surface Processes and Landforms. 27, 269-288.
|Manual model available=Yes
|Model website if any=http://www.coulthard.org.uk
}}
{{Additional comments model}}
{{Infobox Model
{{Infobox Model
|model name              = Caesar
|model name              = Caesar

Revision as of 14:05, 19 September 2009

Contact

Name Tom Coulthard
Type of contact Model developer
Institute / Organization University of Hull
Postal address 1 Cottingham Road
Postal address 2
Town / City Hull
Postal code HU6 7RX
State NO STATE
Country United Kingdom
Email address T.Coulthard@hull.ac.uk
Phone
Fax



Caesar


Metadata

Summary

Also known as
Model type Modular
Model part of larger framework
Note on status model
Date note status model

Technical specs

Supported platforms
Linux, Windows
Other platform
Programming language

C

Other program language C#
Code optimized
Multiple processors implemented
Nr of distributed processors
Nr of shared processors
Start year development 1996
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, As teaching tool, As executable"As executable" is not in the list (As code, As teaching tool) of allowed values for the "Model availability" property.
Source code availability
(Or provide future intension)
Through owner"Through owner" is not in the list (Through web repository, Through CSDMS repository) of allowed values for the "Source code availability" property.
Source web address
Source csdms web address
Program license type Other
Program license type other GNU
Memory requirements >512MB
Typical run time 5 min to 50 days


In/Output

Describe input parameters DEM as ascii grid (output from arcGIS),

Rainfall data as a space separated ascii file (straightforward list), Inputs of water/sediment in an ascii file. Other single value parameter inputs for grainsize, flow parameters, slope processes etc..

Input format ASCII
Other input format
Describe output parameters ascii grids (readable into arcGIS) and google earth images of: DEM, flow depth, surface grainsize, shear stress, vegetation cover, velocity.

Also time series of water discharge and sediment discharge (across 9 grainsizes) at user chosen interval. Also visual output to AVI file.

Output format ASCII
Other output format
Pre-processing software needed? No
Describe pre-processing software
Post-processing software needed? No
Describe post-processing software
Visualization software needed? No
If above answer is yes ESRI
Other visualization software but you can use ESRI (ArcGIS)


Process

Describe processes represented by the model 2d multiple flow direction steady state flow model

Erosion and deposition over 9 separate grainsizes Bedload and suspended load sediment transport Slope processes (creep, enhanced creep and mass movement) Vegetation growth Aeolian transport (under development - slab dune model)

Describe key physical parameters and equations Flow depths calculated using version of mannings implemented across a cellular grid using a scanning algorithm.

Sediment tranport using either Einstein or Wilcock and Crowe functions Slope model using simple slab failure and psuedo USLE implementation Dune model adaption of DECAL and Werner slab model

Describe length scale and resolution constraints Has been applied to catchments ranging from 1km^2 to 500km^2, at grid resolutions ranging from 1m to 50m.
Describe time scale and resolution constraints The model has simulated periods from 1 day to 9000 years.

The length of run is largely contingent on the number of grid cells, thus a balance between resoltion and area of study. A small catchment with a coarse resolution will run very fast. Increase the area or make grid cells smaller and run times will increase.

Describe any numerical limitations and issues Run times can be long (60 +days for large areas over many 100's of years).

Flow model is steady state


Testing

Describe available calibration data sets Tested on several catchments in UK over long and short time scales.
Upload calibration data sets if available:
Describe available test data sets none yet; in development
Upload test data sets if available:
Describe ideal data for testing Flow and sediment discharge data, images of topographic change


Other

Do you have current or future plans for collaborating with other researchers? Yes, I am happy to collaborate with any potential users. There is a long history of CAESAR being take up by others including researchers in Italy, France, Spain, NZ, Australia, USA.
Is there a manual available? Yes
Upload manual if available:
Model website if any http://www.coulthard.org.uk
Model forum / discussion board
Comments


Caesar

Introduction

History

Papers

Caesar Questionnaire

Contact Information

Model: CAESAR
Contact person: Tom Coulthard
Institute: University of Hull
City: Hull
Country: United Kingdom
Email: T.Coulthard@hull.ac.uk
2nd person involved: --
3rd person involved: --

Model description

Model type: Modular model for the terrestrial domain.
Description: CAESAR is a cellular landscape evolution model, with an emphasis on fluvial processes, including flow routing, multi grainsize sediment transport. It models morphological change in river catchments.

Technical information

Supported platforms: Linux, Windows
Programming language: C, C#
Model development started at: 1996 and is still going on
To what degree will the model become available: Source code will be available, and model can be used as well as a teaching tool and executable will be available.
Current license type: GNU
Memory requirements: >512MB
Typical run time: 5 min to 50 days

Input / Output description

Input parameters: DEM as ascii grid (output from arcGIS),

Rainfall data as a space separated ascii file (straightforward list), Inputs of water/sediment in an ascii file. Other single value parameter inputs for grainsize, flow parameters, slope processes etc..

Input format: ASCII
Output parameters: ascii grids (readable into arcGIS) and google earth images of: DEM, flow depth, surface grainsize, shear stress, vegetation cover, velocity.
Also time series of water discharge and sediment discharge (across 9 grainsizes) at user chosen interval.
Also visual output to AVI file.
Output format: ASCII
Post-processing software (if needed): no
Visualization software (if needed): no: but you can use ESRI (ArcGIS)

Process description

Processes represented by model: 2d multiple flow direction steady state flow model
Erosion and deposition over 9 separate grainsizes
Bedload and suspended load sediment transport
Slope processes (creep, enhanced creep and mass movement)
Vegetation growth
Aeolian transport (under development - slab dune model)
Key physical parameters & equations: Flow depths calculated using version of mannings implemented across a cellular grid using a scanning algorithm.
Sediment tranport using either Einstein or Wilcock and Crowe functions
Slope model using simple slab failure and psuedo USLE implementation
Dune model adaption of DECAL and Werner slab model
Length scale & resolution constraints: Has been applied to catchments ranging from 1km^2 to 500km^2, at grid resolutions ranging from 1m to 50m.
Time scale & resolution constraints: The model has simulated periods from 1 day to 9000 years.
The length of run is largely contingent on the number of grid cells, thus a balance between resoltion and area of study. A small catchment with a coarse resolution will run very fast. Increase the area or make grid cells smaller and run times will increase.
Numerical limitations and issues : Run times can be long (60 +days for large areas over many 100's of years).
Flow model is steady state

Testing

Available calibration data sets: Tested on several catchments in UK over long and short time scales.
Available test data sets: none yet; in development
Ideal data for testing: Flow and sediment discharge data, images of topographic change

User groups

Currently or plans for collaborating with: Yes, I am happy to collaborate with any potential users. There is a long history of CAESAR being take up by others including researchers in Italy, France, Spain, NZ, Australia, USA.

Documentation

Key papers of the model: Van De Wiel, M.J., Coulthard, T.J., Macklin, M.G., Lewin, J. (2007) Embedding reach-scale fluvial dynamics within the CAESAR cellular automaton landscape evolution model. Geomorphology, 90 (3-4), pp. 283-301.

Coulthard, T. J. Macklin, M. G. & Kirkby, M. J. (2002) Simulating upland river catchment and alluvial fan evolution. Earth Surface Processes and Landforms. 27, 269-288.

Is there a manual available: yes
Model website if any: http://www.coulthard.org.uk

Additional comments

Comments: --


Issues

Help

Input Files

Output Files

Download

Source

Command-Line Access

GUI and IDE Access

Subversion Help