Sea ice rheology

The polar oceans of Earth are covered by sea ice. On timescales much greater than a day, the motion and deformation of the sea ice cover (i.e., its dynamics) are primarily determined by atmospheric and oceanic tractions on its upper and lower surfaces and by internal ice forces that arise within the...

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Published in:Annual Review of Fluid Mechanics
Main Author: Feltham, Daniel F.
Format: Article in Journal/Newspaper
Language:unknown
Published: Annual reviews 2008
Subjects:
Online Access:https://centaur.reading.ac.uk/30575/
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spelling ftunivreading:oai:centaur.reading.ac.uk:30575 2024-06-23T07:56:38+00:00 Sea ice rheology Feltham, Daniel F. 2008 https://centaur.reading.ac.uk/30575/ unknown Annual reviews Feltham, D. F. <https://centaur.reading.ac.uk/view/creators/90004991.html> orcid:0000-0003-2289-014X (2008) Sea ice rheology. Annual Review of Fluid Mechanics, 40 (1). pp. 91-112. ISSN 1545-4479 doi: https://doi.org/10.1146/annurev.fluid.40.111406.102151 <https://doi.org/10.1146/annurev.fluid.40.111406.102151> Article PeerReviewed 2008 ftunivreading https://doi.org/10.1146/annurev.fluid.40.111406.102151 2024-06-11T14:59:15Z The polar oceans of Earth are covered by sea ice. On timescales much greater than a day, the motion and deformation of the sea ice cover (i.e., its dynamics) are primarily determined by atmospheric and oceanic tractions on its upper and lower surfaces and by internal ice forces that arise within the ice cover owing to its deformation. This review discusses the relationship between the internal ice forces and the deformation of the ice cover, focusing on representations suitable for inclusion within global climate models. I first draw attention to theories that treat the sea ice cover as an isotropic continuum and then to the recent development of anisotropic models that deal with the presence of oriented weaknesses in the ice cover, known as leads. Article in Journal/Newspaper Sea ice CentAUR: Central Archive at the University of Reading Annual Review of Fluid Mechanics 40 1 91 112
institution Open Polar
collection CentAUR: Central Archive at the University of Reading
op_collection_id ftunivreading
language unknown
description The polar oceans of Earth are covered by sea ice. On timescales much greater than a day, the motion and deformation of the sea ice cover (i.e., its dynamics) are primarily determined by atmospheric and oceanic tractions on its upper and lower surfaces and by internal ice forces that arise within the ice cover owing to its deformation. This review discusses the relationship between the internal ice forces and the deformation of the ice cover, focusing on representations suitable for inclusion within global climate models. I first draw attention to theories that treat the sea ice cover as an isotropic continuum and then to the recent development of anisotropic models that deal with the presence of oriented weaknesses in the ice cover, known as leads.
format Article in Journal/Newspaper
author Feltham, Daniel F.
spellingShingle Feltham, Daniel F.
Sea ice rheology
author_facet Feltham, Daniel F.
author_sort Feltham, Daniel F.
title Sea ice rheology
title_short Sea ice rheology
title_full Sea ice rheology
title_fullStr Sea ice rheology
title_full_unstemmed Sea ice rheology
title_sort sea ice rheology
publisher Annual reviews
publishDate 2008
url https://centaur.reading.ac.uk/30575/
genre Sea ice
genre_facet Sea ice
op_relation Feltham, D. F. <https://centaur.reading.ac.uk/view/creators/90004991.html> orcid:0000-0003-2289-014X (2008) Sea ice rheology. Annual Review of Fluid Mechanics, 40 (1). pp. 91-112. ISSN 1545-4479 doi: https://doi.org/10.1146/annurev.fluid.40.111406.102151 <https://doi.org/10.1146/annurev.fluid.40.111406.102151>
op_doi https://doi.org/10.1146/annurev.fluid.40.111406.102151
container_title Annual Review of Fluid Mechanics
container_volume 40
container_issue 1
container_start_page 91
op_container_end_page 112
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