YuZhang16101/Underworld_large-scale-folds-in-ice-sheets: Underworld_large-scale-folds-in-ice-sheets
Code for the revising manuscript, Zhang et al., Ice Modeling Indicates Formation Mechanisms of Large-scale Folding in Greenland's Ice Sheet Large-scale stratigraphic folds have been universally observed in the ice-penetrating radargrams of Greenland's ice sheet. Here we use the full-Stokes...
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| Format: | Software |
| Language: | unknown |
| Published: |
2023
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| Online Access: | https://zenodo.org/record/8309765 https://doi.org/10.5281/zenodo.8309765 |
| Summary: | Code for the revising manuscript, Zhang et al., Ice Modeling Indicates Formation Mechanisms of Large-scale Folding in Greenland's Ice Sheet Large-scale stratigraphic folds have been universally observed in the ice-penetrating radargrams of Greenland's ice sheet. Here we use the full-Stokes code Underworld to simulate ice movements in three-dimensional convergent flow, mainly concerning ice anisotropy due to crystallographic preferred orientation (CPO), vertical viscosity and density contrasts in ice layers, and bedrock conditions. Model 1: isotropic ice, free-slip basal boundary Model 2: anisotropic ice, free slip Model 3: anisotropy, flat bedrock surface Model 4: anisotropy, bumpy bedrock surface (200m) Model 5: anisotropy, bumpy bedrock surface (400m) Model 6: isotropy, bumpy bedrock surface (400m) Model 7: larger anisotropy based on Model 5 Model 8: larger bumps based on Model 5 Model 9: larger ice thickness based on Model 5 |
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