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Massive subsurface ice formed by refreezing of ice-shelf melt ponds
Surface melt ponds form intermittently on several Antarctic ice shelves. Although implicated in ice-shelf break up, the consequences of such ponding for ice formation and ice-shelf structure have not been evaluated. Here we report the discovery of a massive subsurface ice layer, at least 16 km acros...
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| Vydáno v: | Nat Commun |
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| Hlavní autoři: | , , , , , , , , , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Publishing Group
2016
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4906384/ https://ncbi.nlm.nih.gov/pubmed/27283778 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms11897 |
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