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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Bibliographic Details
Main Author: Feldmann, Johannes
Format: Dataset
Language:English
Published: PANGAEA 2019
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.908948
Description
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.