Modelling the three-dimensional, diagnostic anisotropy field of an ice rise ...
Polar ice develops anisotropic crystal orientation fabrics under deformation, yet ice is most often modelled as an isotropic fluid. We present three-dimensional simulations of the crystal orientation fabric of Derwael Ice Rise including the surrounding ice shelf using a crystal orientation tensor ev...
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Online Access: | https://dx.doi.org/10.48550/arxiv.2408.01069 https://arxiv.org/abs/2408.01069 |
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ftdatacite:10.48550/arxiv.2408.01069 2024-09-15T18:12:39+00:00 Modelling the three-dimensional, diagnostic anisotropy field of an ice rise ... Henry, A. Clara J. Martín, Carlos Drews, Reinhard 2024 https://dx.doi.org/10.48550/arxiv.2408.01069 https://arxiv.org/abs/2408.01069 unknown arXiv Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Fluid Dynamics physics.flu-dyn Geophysics physics.geo-ph FOS: Physical sciences CreativeWork Preprint Article article 2024 ftdatacite https://doi.org/10.48550/arxiv.2408.01069 2024-09-02T07:58:21Z Polar ice develops anisotropic crystal orientation fabrics under deformation, yet ice is most often modelled as an isotropic fluid. We present three-dimensional simulations of the crystal orientation fabric of Derwael Ice Rise including the surrounding ice shelf using a crystal orientation tensor evolution equation corresponding to a fixed velocity field. We use a semi-Lagrangian numerical method that constrains the degree of crystal orientation evolution to solve the equations in complex flow areas. We perform four simulations based on previous studies, altering the rate of evolution of the crystal anisotropy and its dependence on a combination of the strain rate and deviatoric stress tensors. We provide a framework for comparison with radar observations of the anisotropy field, outlining areas where the assumption of one vertical eigenvector may not hold and provide resulting errors in measured eigenvalues. We recognise the areas of high horizontal divergence at the ends of the flow divide as important ... Article in Journal/Newspaper Ice Shelf DataCite |
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Open Polar |
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DataCite |
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ftdatacite |
language |
unknown |
topic |
Fluid Dynamics physics.flu-dyn Geophysics physics.geo-ph FOS: Physical sciences |
spellingShingle |
Fluid Dynamics physics.flu-dyn Geophysics physics.geo-ph FOS: Physical sciences Henry, A. Clara J. Martín, Carlos Drews, Reinhard Modelling the three-dimensional, diagnostic anisotropy field of an ice rise ... |
topic_facet |
Fluid Dynamics physics.flu-dyn Geophysics physics.geo-ph FOS: Physical sciences |
description |
Polar ice develops anisotropic crystal orientation fabrics under deformation, yet ice is most often modelled as an isotropic fluid. We present three-dimensional simulations of the crystal orientation fabric of Derwael Ice Rise including the surrounding ice shelf using a crystal orientation tensor evolution equation corresponding to a fixed velocity field. We use a semi-Lagrangian numerical method that constrains the degree of crystal orientation evolution to solve the equations in complex flow areas. We perform four simulations based on previous studies, altering the rate of evolution of the crystal anisotropy and its dependence on a combination of the strain rate and deviatoric stress tensors. We provide a framework for comparison with radar observations of the anisotropy field, outlining areas where the assumption of one vertical eigenvector may not hold and provide resulting errors in measured eigenvalues. We recognise the areas of high horizontal divergence at the ends of the flow divide as important ... |
format |
Article in Journal/Newspaper |
author |
Henry, A. Clara J. Martín, Carlos Drews, Reinhard |
author_facet |
Henry, A. Clara J. Martín, Carlos Drews, Reinhard |
author_sort |
Henry, A. Clara J. |
title |
Modelling the three-dimensional, diagnostic anisotropy field of an ice rise ... |
title_short |
Modelling the three-dimensional, diagnostic anisotropy field of an ice rise ... |
title_full |
Modelling the three-dimensional, diagnostic anisotropy field of an ice rise ... |
title_fullStr |
Modelling the three-dimensional, diagnostic anisotropy field of an ice rise ... |
title_full_unstemmed |
Modelling the three-dimensional, diagnostic anisotropy field of an ice rise ... |
title_sort |
modelling the three-dimensional, diagnostic anisotropy field of an ice rise ... |
publisher |
arXiv |
publishDate |
2024 |
url |
https://dx.doi.org/10.48550/arxiv.2408.01069 https://arxiv.org/abs/2408.01069 |
genre |
Ice Shelf |
genre_facet |
Ice Shelf |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.48550/arxiv.2408.01069 |
_version_ |
1810450235351105536 |