- Abstract:
-
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 buoyancy fluxes for the polar oceans, and sea-ice biogeochemistry. We review work on the growth of mushy layers and convective flows driven by density gradients in the interstitial fluid. After intro...
Expand abstract - Publication status:
- Published
- Peer review status:
- Peer reviewed
- Version:
- Accepted Manuscript
- Files:
-
-
(pdf, 1.1MB)
-
- Publisher copy:
- 10.1098/rsta.2018.0165
-
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- Publisher:
- Royal Society Publisher's website
- Journal:
- Philosophical Transactions A: Mathematical, Physical and Engineering Sciences Journal website
- Volume:
- 377
- Issue:
- 2146
- Publication date:
- 2019-04-15
- Acceptance date:
- 2019-02-06
- DOI:
- EISSN:
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1471-2962
- ISSN:
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1364-503X
- Pubs id:
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pubs:969118
- URN:
-
uri:7569bfa6-e16d-4c5f-8d2a-bcde770feaa2
- UUID:
-
uuid:7569bfa6-e16d-4c5f-8d2a-bcde770feaa2
- Local pid:
- pubs:969118
- Copyright holder:
- Wells et al.
- Copyright date:
- 2019
- Notes:
- © 2019 The Author(s). This is the accepted manuscript version of the article. The final version is available online from Royal Society at: https://doi.org/10.1098/rsta.2018.0165
Journal article
Mushy layer growth and convection, with application to sea ice
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