Mushy layer growth and convection, with application to sea ice
Sea ice is a reactive porous medium of ice crystals and liquid brine, which is an example of a mushy layer. The phase behaviour of sea ice controls the evolving material properties and fluid transport through the porous ice, with consequences for ice growth, brine drainage from the ice to provide bu...
| Main Authors: | , , |
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| Format: | Journal article |
| Published: |
Royal Society
2019
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