Paul D. Bons | M@TE

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Marker lines prior to (a) and after 750 years of flow of (b) isotropic and (c) anisotropic ice. The axial plane of the resulting shear fold in isotropic ice mimics the bedrock topography, while it is controlled by shearing along a horizontal shear zone in the case of anisotropic ice. Green: bedrock, flow to the right.

Marker lines prior to (a) and after 750 years of flow of (b) isotropic and (c) anisotropic ice. The axial plane of the resulting shear fold in isotropic ice mimics the bedrock topography, while it is controlled by shearing along a horizontal shear zone in the case of anisotropic ice. Green: bedrock, flow to the right.

ISMIP-HOM benchmark experiments using Underworld

Uploaded by: Dan Sandiford

Uploaded: August 19, 2024

Software: Underworld2: Python Geodynamics Modelling for Desktop, HPC and Cloud

Tags:

Stokes anisotropy benchmark ice-sheet mechanical

Finite-Element Particle-in-cell Python

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