Meeting:Abstract 2011 CSDMS meeting-022: Difference between revisions
No edit summary |
No edit summary |
||
| Line 1: | Line 1: | ||
<!--{{CSDMS meeting program template | |||
|CSDMS meeting first hydrological choice=TopoFlow | |||
|CSDMS meeting second hydrological choice=WBM-WTM | |||
|CSDMS meeting first terrestrial choice=WRF | |||
|CSDMS meeting second terrestrial choice=CHILD | |||
|CSDMS meeting first coastal choice=I am not interested | |||
|CSDMS meeting second coastal choice=I am not interested | |||
|CSDMS meeting first marine choice=ROMS | |||
|CSDMS meeting second marine choice=TURBINS | |||
|CSDMS meeting first carbonate choice=Cyclopath | |||
|CSDMS meeting second carbonate choice=I am not interested | |||
|CSDMS meeting first tool choice=GRASS | |||
|CSDMS meeting second tool choice=TauDEM | |||
}}--> | |||
{{CSDMS meeting personal information template | {{CSDMS meeting personal information template | ||
|CSDMS meeting first name=Elchin | |CSDMS meeting first name=Elchin | ||
| Line 29: | Line 43: | ||
}} | }} | ||
{{blank line template}} | {{blank line template}} | ||
{{CSDMS meeting program template1 | |||
|CSDMS meeting first | |CSDMS meeting first day choice=TopoFlow | ||
|CSDMS meeting second | |CSDMS meeting second day choice=VisIt | ||
|CSDMS meeting | |CSDMS meeting third day choice=HPCC | ||
}} | |||
}} | |||
{{CSDMS meeting logistics template | {{CSDMS meeting logistics template | ||
|Attend all days=Yes | |Attend all days=Yes | ||
Revision as of 22:56, 4 October 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.
