Basal friction of Fleming Glacier, Antarctica – Part 1: Sensitivity of inversion to temperature and bedrock uncertainty

Many glaciers in the Antarctic Peninsula are now rapidly losing mass. Understanding of the dynamics of these fast-flowing glaciers, and their potential future behaviour, can be improved through ice sheet modelling studies. Inverse methods are commonly used in ice sheet models to infer the spatial di...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: Zhao, Chen, Gladstone, Rupert M., Warner, Roland C., King, Matt A., Zwinger, Thomas, Morlighem, Mathieu
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2018
Subjects:
Online Access:https://doi.org/10.5194/tc-12-2637-2018
https://noa.gwlb.de/receive/cop_mods_00005088
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00005045/tc-12-2637-2018.pdf
https://tc.copernicus.org/articles/12/2637/2018/tc-12-2637-2018.pdf