Meeting:Abstract 2011 CSDMS meeting-065: Difference between revisions
m (WikiSysop moved page Temp:Abstract 2011 CSDMS meeting-065 to Meeting:Abstract 2011 CSDMS meeting-065 without leaving a redirect) |
No edit summary |
||
| Line 5: | Line 5: | ||
|CSDMS meeting city=Cambridge | |CSDMS meeting city=Cambridge | ||
|CSDMS meeting state=NO STATE | |CSDMS meeting state=NO STATE | ||
|CSDMS meeting country= | |CSDMS meeting country=United Kingdom | ||
|CSDMS meeting email address=rm423@cam.ac.uk | |CSDMS meeting email address=rm423@cam.ac.uk | ||
|CSDMS meeting phone=0044 7870 585881 | |CSDMS meeting phone=0044 7870 585881 | ||
| Line 20: | Line 20: | ||
|CSDMS meeting coauthor institute / Organization=University of Cambridge | |CSDMS meeting coauthor institute / Organization=University of Cambridge | ||
|CSDMS meeting coauthor town-city=Cambridge | |CSDMS meeting coauthor town-city=Cambridge | ||
|CSDMS meeting coauthor country= | |CSDMS meeting coauthor country=United Kingdom | ||
|CSDMS meeting coauthor email address=pc350@cam.ac.uk | |CSDMS meeting coauthor email address=pc350@cam.ac.uk | ||
}} | }} | ||
| Line 28: | Line 28: | ||
|CSDMS meeting coauthor institute / Organization=University of Cambridge | |CSDMS meeting coauthor institute / Organization=University of Cambridge | ||
|CSDMS meeting coauthor town-city=Cambridge | |CSDMS meeting coauthor town-city=Cambridge | ||
|CSDMS meeting coauthor country= | |CSDMS meeting coauthor country=United Kingdom | ||
|CSDMS meeting coauthor email address=jd16@cam.ac.uk | |CSDMS meeting coauthor email address=jd16@cam.ac.uk | ||
}} | }} | ||
Latest revision as of 15:17, 10 June 2017
Browse abstracts
Modeling a Continuous Permafrost Basin on the North Slope of Alaska
[[Image:|300px|right|link=File:]]GEOtop 1.145 is used to model the thermal and hydrological state of the subsurface in the Kuparuk basin, Alaska. GEOtop is a distributed hydrological model with coupled water and energy budgets. The surface energy balance scheme includes sensible, latent and radiative heat fluxes at the air-soil or air-snow interface. The subsurface represents heat fluxes in the vertical and water fluxes in the vertical and horizontal directions. The ERA-Interim atmospheric reanalysis product, which is used to force the model, is compared to meteorological and radiation data from the Kuparuk Basin and other stations on the North Slope of Alaska. The use of ERA-Interim reanalysis to force GEOtop enables large-scale simulations to be performed over areas where in situ meteorological data is sparse, such as the North Slope of Alaska. Model simulations forced by ERA-Interim reanalysis data are validated using borehole observations of soil temperature. Model results will be presented demonstrating the interactions between soil properties, snow cover, vegetation and climate.
