Thermal structure and basal sliding parametrisation at Pine Island Glacier – a 3-D full-Stokes model study
Pine Island Glacier is one of the fastest changing glaciers of the Antarctic Ice Sheet and therefore of scientific interest. The glacier holds enough ice to raise the global sea level significantly (~ 0.5 m) when fully melted. The question addressed by numerous modelling studies of the glacier focus...
Published in: | The Cryosphere |
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Main Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2015
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-9-675-2015 https://noa.gwlb.de/receive/cop_mods_00016996 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00016951/tc-9-675-2015.pdf https://tc.copernicus.org/articles/9/675/2015/tc-9-675-2015.pdf |