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A model for polythermal ice incorporating gravity-driven moisture transport

Abstract:

The flow of ice sheets and glaciers dissipates significant amounts of heat, which can result in the formation of ‘temperate ice’, a binary mixture of ice and small amounts of melt water that exists at the melting point. Many ice masses are polythermal, in the sense that they contain cold ice, below the melting point, as well as temperate ice. Temperature and melt water (or moisture) content conversely affect the flow of these ice masses through their effect on ice viscosity and sliding behavi...

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Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1017/jfm.2016.251

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Institution:
University of Oxford
Division:
MPLS
Department:
Mathematical Institute
Role:
Author
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Funding agency for:
Hewitt, I
Grant:
Marie Curie FP7 Career Integration Grant
Publisher:
Cambridge University Press Publisher's website
Journal:
Journal of Fluid Mechanics Journal website
Volume:
797
Issue:
June
Pages:
504-535
Publication date:
2016-05-23
Acceptance date:
2016-04-04
DOI:
EISSN:
1469-7645
ISSN:
1469-7645 and 0022-1120
Source identifiers:
614695
Keywords:
Pubs id:
pubs:614695
UUID:
uuid:c6e2cb86-0f50-47b1-b77c-c30630e90e2f
Local pid:
pubs:614695
Deposit date:
2016-04-09

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