Simulating ice thickness and velocity evolution of Upernavik Isstrøm 1849–2012 by forcing prescribed terminus positions in ISSM
Tidewater glacier velocity and mass balance are known to be highly responsive to terminus position change. Yet it remains challenging for ice flow models to reproduce observed ice margin changes. Here, using the Ice Sheet System Model (Larour et al., 2012), we simulate the ice velocity and thickness...
Published in: | The Cryosphere |
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Main Authors: | , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2018
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-12-1511-2018 https://noa.gwlb.de/receive/cop_mods_00006675 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00006632/tc-12-1511-2018.pdf https://tc.copernicus.org/articles/12/1511/2018/tc-12-1511-2018.pdf |