Similitude simulations of marine ice-sheet instability
Numerical simulations confirming theoretical results from scaling analysis of the shallow stress balance, i.e. the retreat time of a modeled 3D ice-sheet-shelf system with respect to variations in its characteristic properties matches the analytically derived time-scaling law Parameters a, b, c, d r...
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2019
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.908948 |
Summary: | Numerical simulations confirming theoretical results from scaling analysis of the shallow stress balance, i.e. the retreat time of a modeled 3D ice-sheet-shelf system with respect to variations in its characteristic properties matches the analytically derived time-scaling law Parameters a, b, c, d refer to the scaling parameters alpha (length scale), beta (vertical scale), gamma (friction scale), delta (accumulation scale), respectively. |
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