Sea ice is a mushy layer
[1] 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 sh...
Published in: | Geophysical Research Letters |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Geophysical Union
2006
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Subjects: | |
Online Access: | https://centaur.reading.ac.uk/34911/ https://centaur.reading.ac.uk/34911/1/grl21578.pdf https://doi.org/10.1029/2006GL026290 |
Summary: | [1] 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. |
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