SICOPOLIS by Ralf Greve. Each run was forced with the same temperature and sea level curves, but had different model parameter values. The variable model parameters included those that control ice flow, basal sliding, and surface melting. The results indicate a strong variability among model runs for future time slices, even after the runs that do not produce a reasonable modern ice volume are removed from the ensemble." /> SICOPOLIS by Ralf Greve. Each run was forced with the same temperature and sea level curves, but had different model parameter values. The variable model parameters included those that control ice flow, basal sliding, and surface melting. The results indicate a strong variability among model runs for future time slices, even after the runs that do not produce a reasonable modern ice volume are removed from the ensemble." />
+46 8 16 22 83
Patrick Applegate
Department of Physical Geography and Quaternary Geology
Stockholm University
SE-106 91 Stockholm
Sweden
Cryosphere > Glaciers/Ice Sheets > Glacier Thickness/Ice Sheet Thickness
Continent > North America > Greenland
Completed
English
Bolin Centre Database
1.0
None
Free
2013-03-27 17:21:01