Feltham, DL;
Untersteiner, N;
Wettlaufer, JS;
Worster, MG;
(2006)
Sea ice is a mushy layer.
Geophysical Research Letters
, 33
(14)
, Article L14501. 10.1029/2006GL026290.
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Abstract
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.
| Type: | Article |
|---|---|
| Title: | Sea ice is a mushy layer |
| Open access status: | An open access version is available from UCL Discovery |
| DOI: | 10.1029/2006GL026290 |
| Publisher version: | http://dx.doi.org/10.1029/2006GL026290 |
| Language: | English |
| Additional information: | Copyright 2006 by the American Geophysical Union |
| Keywords: | Salinity profile, Model, Solidification, Evolution, Convection, Growth, Alloy, Flow, Melt |
| UCL classification: | UCL UCL > Provost and Vice Provost Offices > UCL BEAMS UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences |
| URI: | https://discovery.ucl.ac.uk/id/eprint/125986 |
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