Model:Lake-Permafrost with Subsidence: Difference between revisions

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{{Modeler information
|First name=Nora
|Last name=Matell
|Type of contact=Model developer
|Institute / Organization=INSTAAR, University of Colorado
|Postal address 1=450 UCB
|Town / City=Boulder
|Postal code=80305
|State=Colorado
|Country=USA
|Email address=nlmatell@gmail.com
}}
{{Model identity
|Model type=Single
|Categories=Terrestrial
|Spatial dimensions=1D
|One-line model description=1-D lake-permafrost thermal model with subsidence.
|Extended model description=Models temperature of 1-D lake-permafrost system through time, given input surface temperature and solar radiation. Model is fully implicit control volume scheme, and cell size can vary with depth. Thermal conductivity and specific heat capacity are dependent on cell substrate (% soil and % ice) and temperature using the apparent heat capacity scheme where freezing/thawing occurs over a finite temperature range and constants are modified to account for latent heat. Lake freezes and thaws depending on temperature; when no ice is present lake is fully mixed and can absorb solar radiation. Upper 10 m substrate contains excess ice and, if thawed, can subside by this amount (lake then deepens by amount of subsidence). "Cell type" controls whether cell has excess ice, only pore space ice, or is lake water.
}}
{{Model technical information
|Supported platforms=Windows
|Programming language=Matlab
|Code optimized=Single Processor
|Start year development=2008
|Does model development still take place?=No
|End year development=2009
|Model availability=As code
|Source code availability=Through owner
|Program license type=GPL v2
|OpenMI compliant=No but possible
|CCA component=No but possible
|IRF interface=No but possible
|Memory requirements=--
|Typical run time=--
}}
{{Input - Output description
|Describe input parameters=Daily average solar radiation for location (at surface).
|Other input format=Matlab .mat file
|Describe output parameters=Matlab variables, Matlab graphs
|Other output format=Matlab variables, Matlab graphs
|Pre-processing software needed?=No
|Post-processing software needed?=No
|Visualization software needed?=No
}}
{{Process description model
|Describe processes represented by the model=Heat conduction in permafrost, lake ice growth-decay, permafrost subsidence due to excess ice
|Describe key physical parameters and equations=Heat conduction equations, lake ice growth-decay equations
|Describe length scale and resolution constraints=Near surface, length scale should be 5-10 cm if subsidence occurring. Deeper in permafrost, 1+ m okay.
|Describe time scale and resolution constraints=Model needs daily (or smaller) timesteps.
|Describe any numerical limitations and issues=Runs slowly - iterates implicit scheme. Some sort of matrix algebra might improve speed.
}}
{{Model testing
|Describe available calibration data sets=--
|Describe available test data sets=Permafrost model can be tested with ground temperature time series at several depths. Lake model can be tested with known ice depths (though snow, not accounted for in model, can affect depth by several 10s of cm).
|Describe ideal data for testing=Lake temperature time series, known lake depth, underlying permafrost time series. Surface temperature time series as input (not air temperature).
}}
{{Users groups model
|Do you have current or future plans for collaborating with other researchers?=--
}}
{{Documentation model
|Provide key papers on model if any=Model based on previous models by Ling and Zhang (2004), Plug and West (2008), Liston and Hall (1995). Model described in Matell et al. (in preparation) and Matell (2009, masters thesis).
|Manual model available=No
}}
{{Additional comments model}}
{{Infobox Model
{{Infobox Model
|model name              = Lake-Permafrost with Subsidence  
|model name              = Lake-Permafrost with Subsidence  

Revision as of 08:26, 29 September 2009

Contact

Name Nora Matell
Type of contact Model developer
Institute / Organization INSTAAR, University of Colorado
Postal address 1 450 UCB
Postal address 2
Town / City Boulder
Postal code 80305
State Colorado
Country USA"USA" is not in the list (Afghanistan, Albania, Algeria, Andorra, Angola, Antigua and Barbuda, Argentina, Armenia, Australia, Austria, ...) of allowed values for the "Country" property.
Email address nlmatell@gmail.com
Phone
Fax



Lake-Permafrost with Subsidence


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
Windows
Other platform
Programming language

Matlab

Other program language
Code optimized Single Processor
Multiple processors implemented
Nr of distributed processors
Nr of shared processors
Start year development 2008
Does model development still take place? No
If above answer is no, provide end year model development 2009
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 GPL v2
Program license type other
Memory requirements --
Typical run time --


In/Output

Describe input parameters Daily average solar radiation for location (at surface).
Input format
Other input format Matlab .mat file
Describe output parameters Matlab variables, Matlab graphs
Output format
Other output format Matlab variables, Matlab graphs
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
Other visualization software


Process

Describe processes represented by the model Heat conduction in permafrost, lake ice growth-decay, permafrost subsidence due to excess ice
Describe key physical parameters and equations Heat conduction equations, lake ice growth-decay equations
Describe length scale and resolution constraints Near surface, length scale should be 5-10 cm if subsidence occurring. Deeper in permafrost, 1+ m okay.
Describe time scale and resolution constraints Model needs daily (or smaller) timesteps.
Describe any numerical limitations and issues Runs slowly - iterates implicit scheme. Some sort of matrix algebra might improve speed.


Testing

Describe available calibration data sets --
Upload calibration data sets if available:
Describe available test data sets Permafrost model can be tested with ground temperature time series at several depths. Lake model can be tested with known ice depths (though snow, not accounted for in model, can affect depth by several 10s of cm).
Upload test data sets if available:
Describe ideal data for testing Lake temperature time series, known lake depth, underlying permafrost time series. Surface temperature time series as input (not air temperature).


Other

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


Lake-Permafrost with Subsidence

Introduction

History

Papers

Lake-Permafrost with Subsidence Questionnaire

Contact Information

Model: Lake-Permafrost with Subsidence
Contact person: Nora Matell
Institute: CU Boulder - INSTAAR
City: Boulder
Country: USA
Email: nlmatell@gmail.com
2nd person involved: --
3rd person involved: --

Model description

Model type: Single model for the terrestrial domain.
Description: Models temperature of 1-D lake-permafrost system through time, given input surface temperature and solar radiation. Model is fully implicit control volume scheme, and cell size can vary with depth. Thermal conductivity and specific heat capacity are dependent on cell substrate (% soil and % ice) and temperature using the apparent heat capacity scheme where freezing/thawing occurs over a finite temperature range and constants are modified to account for latent heat. Lake freezes and thaws depending on temperature; when no ice is present lake is fully mixed and can absorb solar radiation. Upper 10 m substrate contains excess ice and, if thawed, can subside by this amount (lake then deepens by amount of subsidence). "Cell type" controls whether cell has excess ice, only pore space ice, or is lake water.

Technical information

Supported platforms: Windows
Programming language: Matlab
Model development started at: 2008 and ended in 2009
To what degree will the model become available: Source code will be available
Current license type: GPLv2
Memory requirements: --
Typical run time: --

Input / Output description

Input parameters: Daily average solar radiation for location (at surface).
Input format: matlab .mat file
Output parameters: Matlab variables, Matlab graphs
Output format: Matlab variables, Matlab graphs
Post-processing software (if needed): --
Visualization software (if needed): --

Process description

Processes represented by model: Heat conduction in permafrost, lake ice growth-decay, permafrost subsidence due to excess ice
Key physical parameters & equations: Heat conduction equations, lake ice growth-decay equations
Length scale & resolution constraints: Near surface, length scale should be 5-10 cm if subsidence occurring. Deeper in permafrost, 1+ m okay.
Time scale & resolution constraints: Model needs daily (or smaller) timesteps.
Numerical limitations and issues : Runs slowly - iterates implicit scheme. Some sort of matrix algebra might improve speed.

Testing

Available calibration data sets: --
Available test data sets: Permafrost model can be tested with ground temperature time series at several depths. Lake model can be tested with known ice depths (though snow, not accounted for in model, can affect depth by several 10s of cm).
Ideal data for testing: Lake temperature time series, known lake depth, underlying permafrost time series. Surface temperature time series as input (not air temperature).

User groups

Currently or plans for collaborating with: --

Documentation

Key papers of the model: Model based on previous models by Ling and Zhang (2004), Plug and West (2008), Liston and Hall (1995). Model described in Matell et al. (in preparation) and Matell (2009, masters thesis).
Is there a manual available: no
Model website if any: --

Additional comments

Comments: --

Issues

Help

Input Files

Output Files

Download

Source