Meeting:Abstract 2011 CSDMS meeting-022: Difference between revisions
No edit summary |
No edit summary |
||
| Line 29: | Line 29: | ||
}} | }} | ||
{{blank line template}} | {{blank line template}} | ||
{{CSDMS meeting program template | <!--{{CSDMS meeting program template | ||
|CSDMS meeting first hydrological choice=TopoFlow | |CSDMS meeting first hydrological choice=TopoFlow | ||
|CSDMS meeting second hydrological choice=WBM-WTM | |CSDMS meeting second hydrological choice=WBM-WTM | ||
| Line 42: | Line 42: | ||
|CSDMS meeting first tool choice=GRASS | |CSDMS meeting first tool choice=GRASS | ||
|CSDMS meeting second tool choice=TauDEM | |CSDMS meeting second tool choice=TauDEM | ||
}} | }}--> | ||
{{CSDMS meeting logistics template | {{CSDMS meeting logistics template | ||
|Attend all days=Yes | |Attend all days=Yes | ||
Revision as of 17:14, 26 September 2011
"USA" is not in the list (Afghanistan, Albania, Algeria, Andorra, Angola, Antigua and Barbuda, Argentina, Armenia, Australia, Austria, ...) of allowed values for the "Country member" property.
Browse abstracts
Elchin Jafarov choose to not submit an abstract for this conference.
[[Image:|300px|right|link=File:]]An increasing amount of ground temperature data from permafrost observation stations in Alaska provides a valuable dataset for calibration and simulation of permafrost thermal state dynamics. Snow is one of the major factors affecting ground temperature distribution. Recent permafrost observation stations include snow depth measuring devices. Snow depth and snow conductivity are two required parameters in order to model ground temperature distribution using GIPL transient model.
In this project we applied different calibration techniques to obtain optimal snow conductivity and reconstruct soil thermal properties. The modeling results represent calibrated soil properties for several permafrost observation stations along the Trans-Alaskan highway.
