Parameterization for subgrid-scale motion of ice-shelf calving fronts

A parameterization for the motion of ice-shelf fronts on a Cartesian grid in finite-difference land-ice models is presented. The scheme prevents artificial thinning of the ice shelf at its edge, which occurs due to the finite resolution of the model. The intuitive numerical implementation dimini...

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Bibliographic Details
Main Authors: T. Albrecht, M. Martin, M. Haseloff, R. Winkelmann, A. Levermann
Format: Article
Language:English
Published: Copernicus Publications 2011-01-01
Series:The Cryosphere
Online Access:http://www.the-cryosphere.net/5/35/2011/tc-5-35-2011.pdf
Description
Summary:A parameterization for the motion of ice-shelf fronts on a Cartesian grid in finite-difference land-ice models is presented. The scheme prevents artificial thinning of the ice shelf at its edge, which occurs due to the finite resolution of the model. The intuitive numerical implementation diminishes numerical dispersion at the ice front and enables the application of physical boundary conditions to improve the calculation of stress and velocity fields throughout the ice-sheet-shelf system. Numerical properties of this subgrid modification are assessed in the Potsdam Parallel Ice Sheet Model (PISM-PIK) for different geometries in one and two horizontal dimensions and are verified against an analytical solution in a flow-line setup.
ISSN:1994-0416
1994-0424