Model:Cyclopath: Difference between revisions

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{{Modeler information
|First name=Peter
|Last name=Burgess
|Type of contact=Model developer
|Institute / Organization=Royal Holloway University of London
|Town / City=Egham
|Postal code=TW20 0EX
|State=NO STATE
|Country=United Kingdom
|Email address=p.burgess@es.rhul.ac.uk
}}
{{Model identity
|Model type=Single
|Categories=Carbonate
|Spatial dimensions=2D, 3D
|One-line model description=A 2D/3D model of carbonate cyclicity
|Extended model description=A 2D or 3D model of carbonate sediment production and transport that generates high-frequency platform top auto and allocycles as well as various aspects of large scale platform geomtry
}}
{{Model technical information
|Supported platforms=Unix, Linux
|Programming language=C
|Start year development=1998
|Does model development still take place?=No
|End year development=2005
|Model availability=As code
|Source code availability=Through owner
|Program license type=Other
|Program license type other=--
|OpenMI compliant=No but possible
|CCA component=No but possible
|IRF interface=No but possible
|Memory requirements=Variable
|Typical run time=Minutes to hours
}}
{{Input - Output description
|Describe input parameters=Various text files defining initial conditions and parameter values
|Input format=ASCII
|Describe output parameters=A 3D cube of model strata coded by water depth of deposition and thickness transported versus thickness deposited in-situ per time step
|Output format=ASCII
|Pre-processing software needed?=No
|Post-processing software needed?=Yes
|Describe post-processing software=GMT routines or Matlab
|Visualization software needed?=Yes
|If above answer is yes=Matlab
|Other visualization software=GMT
}}
{{Process description model
|Describe processes represented by the model=Subsidence and uplift
Eustatic oscillations
Water depth dependent in-situ carbonate production
Spatial variations in sediment production rate
Depth dependent sediment transport
Diffusional sediment transport
|Describe key physical parameters and equations=See Burgess et al. (2001), Basin Research
|Describe length scale and resolution constraints=10s to 100s km length scale
|Describe time scale and resolution constraints=Internal time step years to decades
Model chron resolution 1000 years
Total run time 1-10 My
|Describe any numerical limitations and issues=Diffusion and other sediment transport routines require short time steps
}}
{{Model testing
|Describe available calibration data sets=Any outcrop data showing (or purporting to show) cyclical platform interior strata
|Describe available test data sets=--
|Describe ideal data for testing=--
}}
{{Users groups model
|Do you have current or future plans for collaborating with other researchers?=No, but open to suggestions
}}
{{Documentation model
|Provide key papers on model if any=Papers:
* Burgess, P.M., Wright, V.P. & Emery, D. (2001) Numerical forward modelling of a peritidal carbonate parasequence development: implications for outcrop interpretation. Basin Research, 13, p.1-16.
* Burgess, P.M. (2001) Modelling Carbonate Sequence Development without Relative Sea Level Oscillations, Geology, vol. 29, p. 1127-1130.
* Barnett, A.J., Burgess, P.M., and Wright, V.P. (2002), Icehouse world sea-level behaviour and resulting stratal patterns in late Visean (Mississippian) carbonate platforms: integration of numerical forward modelling and outcrop studies, Basin Research, v.14, p.417-438.
* Burgess, P.M., and Wright, V.P, (2003) Numerical forward modelling of carbonate platform dynamics: An evaluation of complexity and completeness, Journal of Sedimentary research, v.73, p.637-652.
* Burgess, P.M., and Emery, D. (2005), Sensitive dependence, divergence and unpredictable behaviour in a stratigraphic forward model of a carbonate system, in Curtis, A., and Wood, R. (eds.) Geological prior information: informing science and engineering, Geological Society, London, Special Publication 239, p.77-94.
* Burgess, P.M., 2006, The signal and the noise: forward modeling of allocyclic and autocyclic processes influencing peritidal carbonate stacking patterns, Journal of Sedimentary Research; v. 76; no. 7; p. 962-977.
|Manual model available=No
}}
{{Additional comments model}}
{{Infobox Model
{{Infobox Model
|model name              = Cyclopath
|model name              = Cyclopath

Revision as of 11:25, 14 September 2009

Contact

Name Peter Burgess
Type of contact Model developer
Institute / Organization Royal Holloway University of London
Postal address 1
Postal address 2
Town / City Egham
Postal code TW20 0EX
State NO STATE
Country United Kingdom
Email address p.burgess@es.rhul.ac.uk
Phone
Fax



Cyclopath


Metadata

Summary

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

Technical specs

Supported platforms
Unix, Linux
Other platform
Programming language

C

Other program language
Code optimized
Multiple processors implemented
Nr of distributed processors
Nr of shared processors
Start year development 1998
Does model development still take place? No
If above answer is no, provide end year model development 2005
Code development status
When did you indicate the 'code development status'?
Model availability As code
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 --
Memory requirements Variable
Typical run time Minutes to hours


In/Output

Describe input parameters Various text files defining initial conditions and parameter values
Input format ASCII
Other input format
Describe output parameters A 3D cube of model strata coded by water depth of deposition and thickness transported versus thickness deposited in-situ per time step
Output format ASCII
Other output format
Pre-processing software needed? No
Describe pre-processing software
Post-processing software needed? Yes
Describe post-processing software GMT routines or Matlab
Visualization software needed? Yes
If above answer is yes Matlab
Other visualization software GMT


Process

Describe processes represented by the model Subsidence and uplift

Eustatic oscillations Water depth dependent in-situ carbonate production Spatial variations in sediment production rate Depth dependent sediment transport Diffusional sediment transport

Describe key physical parameters and equations See Burgess et al. (2001), Basin Research
Describe length scale and resolution constraints 10s to 100s km length scale
Describe time scale and resolution constraints Internal time step years to decades

Model chron resolution 1000 years Total run time 1-10 My

Describe any numerical limitations and issues Diffusion and other sediment transport routines require short time steps


Testing

Describe available calibration data sets Any outcrop data showing (or purporting to show) cyclical platform interior strata
Upload calibration data sets if available:
Describe available test data sets --
Upload test data sets if available:
Describe ideal data for testing --


Other

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


Cyclopath

Introduction

History

Papers

Cyclopath Questionnaire

Contact Information

Model: Cyclopath
Contact person: Peter Burgess (Model developer)
Institute: Royal Holloway University of London
City:
Country:
Email: p.burgess@es.rhul.ac.uk
2nd person involved: --
3rd person involved: --

Model description

Model type: Single model for the carbonate domain.
Description: A 2D or 3D model of carbonate sediment production and transport that generates high-frequency platform top auto and allocycles as well as various aspects of large scale platform geomtry

Technical information

Supported platforms: Unix, Linux
Programming language: C
Model was developed started from: 1998 and ended in 2005
To what degree will the model become available: As code
Current license type: --
Memory requirements: variable
Typical run time: minutes to hours

Input / Output description

Input parameters: Various text files defining initial conditions and parameter values
Input format: ASCII
Output parameters: A 3D cube of model strata coded by water depth of deposition and thickness transported versus thickness deposited in-situ per time step
Output format: ASCII
Post-processing software (if needed): Yes, GMT routines or Matlab
Visualization software (if needed): Yes, Matlab, GMT.

Process description

Processes represented by model: Subsidence and uplift

Eustatic oscillations
Water depth dependent in-situ carbonate production
Spatial variations in sediment production rate
Depth dependent sediment transport
Diffusional sediment transport

Key physical parameters & equations: See Burgess et al. (2001), Basin Research
Length scale & resolution constraints: 10s to 100s km length scale
Time scale & resolution constraints: Internal time step years to decades

Model chron resolution 1000 years
Total run time 1-10 My

Numerical limitations and issues : Diffusion and other sediment transport routines require short time steps

Testing

Available calibration data sets: Any outcrop data showing (or purporting to show) cyclical platform interior strata
Available test data sets: --
Ideal data for testing: --

User groups

Currently or plans for collaborating with: No, but open to suggestions

Documentation

Key papers of the model:
  • Burgess, P.M., Wright, V.P. & Emery, D. (2001) Numerical forward modelling of a peritidal carbonate parasequence development: implications for outcrop interpretation. Basin Research, 13, p.1-16.

Burgess, P.M. (2001) Modelling Carbonate Sequence Development without Relative Sea Level Oscillations, Geology, vol. 29, p. 1127-1130.

  • Barnett, A.J., Burgess, P.M., and Wright, V.P. (2002), Icehouse world sea-level behaviour and resulting stratal patterns in late Visean (Mississippian) carbonate platforms: integration of numerical forward modelling and outcrop studies, Basin Research, v.14, p.417-438.
  • Burgess, P.M., and Wright, V.P, (2003) Numerical forward modelling of carbonate platform dynamics: An evaluation of complexity and completeness, Journal of Sedimentary research, v.73, p.637-652.
  • Burgess, P.M., and Emery, D. (2005), Sensitive dependence, divergence and unpredictable behaviour in a stratigraphic forward model of a carbonate system, in Curtis, A., and Wood, R. (eds.) Geological prior information: informing science and engineering, Geological Society, London, Special Publication 239, p.77-94.
  • Burgess, P.M., 2006, The signal and the noise: forward modeling of allocyclic and autocyclic processes influencing peritidal carbonate stacking patterns, Journal of Sedimentary Research; v. 76; no. 7; p. 962-977.
Is there a manual available: No
Model website if any: --

Additional comments

Comments: --

Issues

Help

Input Files

Output Files

Download

Source