Model:Lake-Permafrost with Subsidence: Difference between revisions

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{{Infobox Model
{{Model identity
|model name              = Lake-Permafrost with Subsidence
|Model type=Single
|developer                = '''Matell''', Nora
|one-line-description    = 1-D lake-permafrost thermal model with subsidence.
|type                     = Model
|source                  = [[image=Red1.png]]
}}
}}
{{Model identity2
|ModelDomain=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.
}}
{{Start model keyword table}}
{{Model keywords
|Model keywords=thermal model
}}
{{Model keywords
|Model keywords=permafrost
}}
{{Model keywords}}
{{End a table}}
{{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=United States
|Email address=nlmatell@gmail.com
}}
{{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
|Program license type=GPL v2
|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=Key Papers:
* '''Matell, N., 2009. Shoreline erosion and thermal impact of thaw lakes in a warming landscape, Arctic Coastal Plain, Alaska. M.Sc. thesis project, Department of Geology, University of Colorado, Boulder.'''
|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}}
{{NOINDEX}}
<!-- Edit the part above to update info on other papers -->
<!-- Edit the part above to update info on other papers -->


== Lake-Permafrost with Subsidence  ==
==Introduction==
__TOC__
===Introduction===
 
=== History ===
 
=== Papers ===
 
=== Lake-Permafrost with Subsidence  Questionnaire ===
 
==== Contact Information ====
 
{| class="wikitable"
| class="model_col1"| Model:
| class="model_col2"| Lake-Permafrost with Subsidence 
|-
| class="model_col1"| Contact person:
| class="model_col2"| Nora Matell
|-
| class="model_col1"| Institute:
| class="model_col2"| CU Boulder - INSTAAR
|-
| class="model_col1"| City:
| class="model_col2"| Boulder
|-
| class="model_col1"| Country:
| class="model_col2"| USA
|-
| class="model_col1"| Email:
| class="model_col2"| nlmatell@gmail.com
|-
| 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"| Single model for the terrestrial domain.
|-
| class="model_col1"| Description:
| class="model_col2"| 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 ====
 
{| class="wikitable"
| class="model_col1"| Supported platforms:
| class="model_col2"| Windows
|-
| class="model_col1"| Programming language:
| class="model_col2"| Matlab
|-
| class="model_col1"| Model development started at:
| class="model_col2"| 2008 and ended in 2009
|-
| 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"| --
|}
 
==== Input / Output description ====
 
{| class="wikitable"
| class="model_col1"| Input parameters:
| class="model_col2"| Daily average solar radiation for location (at surface).
 
|-
| class="model_col1"| Input format:
| class="model_col2"| matlab .mat file
|-
| class="model_col1"| Output parameters:
| class="model_col2"| Matlab variables, Matlab graphs   
|-
| class="model_col1"| Output format:
| class="model_col2"| Matlab variables, Matlab graphs
|-
| class="model_col1"| Post-processing software (if needed):
| class="model_col2"| --
|-
| class="model_col1"| Visualization software (if needed):
| class="model_col2"| --
|}
 
==== Process description ====
 
{| class="wikitable"
| class="model_col1"| Processes represented by model:
| class="model_col2"| Heat conduction in permafrost, lake ice growth-decay, permafrost subsidence due to excess ice
|-
| class="model_col1"| Key physical parameters & equations:
| class="model_col2"| Heat conduction equations, lake ice growth-decay equations
|-
| class="model_col1"| Length scale & resolution constraints:
| class="model_col2"| Near surface, length scale should be 5-10 cm if subsidence occurring.  Deeper in permafrost, 1+ m okay.
|-
| class="model_col1"| Time scale & resolution constraints:
| class="model_col2"| Model needs daily (or smaller) timesteps.
|-
| class="model_col1"| Numerical limitations and issues :
| class="model_col2"| Runs slowly - iterates implicit scheme.  Some sort of matrix algebra might improve speed.
|}
 
==== Testing ====
 
{| class="wikitable"
| class="model_col1"| Available calibration data sets:
| class="model_col2"| --
|-
| class="model_col1"| Available test data sets:
| class="model_col2"| 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).
|-
| class="model_col1"| Ideal data for testing:
| class="model_col2"| Lake temperature time series, known lake depth, underlying permafrost time series.  Surface temperature time series as input (not air temperature).
|}
 
==== User groups ====
 
{| class="wikitable"
| class="model_col1"| Currently or plans for collaborating with:
| class="model_col2"| --
|}
 
==== Documentation ====
 
{| class="wikitable"
| class="model_col1"| Key papers of the model:
| class="model_col2"| 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).
|-
| 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"
| 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]]

Latest revision as of 20:14, 16 September 2020



Lake-Permafrost with Subsidence


Metadata

Also known as
Model type Single
Model part of larger framework
Note on status model
Date note status model
Spatial dimensions 1D
Spatial extent
Model domain Terrestrial
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.
Keywords:

thermal model, permafrost, ,

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 United States
Email address nlmatell@gmail.com
Phone
Fax


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)
Source web address
Source csdms web address
Program license type GPL v2
Program license type other
Memory requirements --
Typical run time --


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


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.


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).


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


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
Nora Matell
Source code
Model citations
Nr. of publications: --
Total citations: 0
h-index: --"--" is not a number.
m-quotient: 0
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Link to this page
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Introduction

History

References



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


See more publications of Lake-Permafrost with Subsidence

Issues

Help

Input Files

Output Files

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