Sea ice is a mushy layer
Feltham, D.L.; Untersteiner, N.; Wettlaufer, J.S.; Worster, M.G.. 2006 Sea ice is a mushy layer. Geophysical Research Letters, 33 (14), L14501. 4, pp. https://doi.org/10.1029/2006GL026290
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Copyright 2006 by the American Geophysical Union Geophysical Research Letters - 2006 - Feltham - Sea ice is a mushy layer.pdf - Published Version Download (84kB) | Preview |
Abstract/Summary
Sea ice is a two-phase, two-component, reactive porous medium: an example of what is known in other contexts as a mushy layer. The fundamental conservation laws underlying the mathematical description of mushy layers provide a robust foundation for the prediction of sea-ice evolution. Here we show that the general equations describing mushy layers reduce to the model of Maykut and Untersteiner (1971) under the same approximations employed therein.
Item Type: | Publication - Article |
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Digital Object Identifier (DOI): | https://doi.org/10.1029/2006GL026290 |
Programmes: | BAS Programmes > Other Special Projects |
ISSN: | 0094-8276 |
Additional Keywords: | Sea ice |
NORA Subject Terms: | Marine Sciences Glaciology |
Date made live: | 04 Sep 2007 15:38 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/47 |
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