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The role of double-diffusive convection in basal melting of Antarctic ice shelves
The Antarctic Ice Sheet loses about half its mass through ocean-driven melting of its fringing ice shelves. However, the ocean processes governing ice shelf melting are not well understood, contributing to uncertainty in projections of Antarctica’s contribution to global sea level. We use high-resol...
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| Pubblicato in: | Proc Natl Acad Sci U S A |
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| Autori principali: | , , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
National Academy of Sciences
2021
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| Soggetti: | |
| Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC8017962/ https://ncbi.nlm.nih.gov/pubmed/33547235 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.2007541118 |
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