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Freshening by glacial meltwater enhances melting of ice shelves and reduces formation of Antarctic Bottom Water

Strong heat loss and brine release during sea ice formation in coastal polynyas act to cool and salinify waters on the Antarctic continental shelf. Polynya activity thus both limits the ocean heat flux to the Antarctic Ice Sheet and promotes formation of Dense Shelf Water (DSW), the precursor to Ant...

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Detalhes bibliográficos
Publicado no:Sci Adv
Main Authors: Silvano, Alessandro, Rintoul, Stephen Rich, Peña-Molino, Beatriz, Hobbs, William Richard, van Wijk, Esmee, Aoki, Shigeru, Tamura, Takeshi, Williams, Guy Darvall
Formato: Artigo
Idioma:Inglês
Publicado em: American Association for the Advancement of Science 2018
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC5906079/
https://ncbi.nlm.nih.gov/pubmed/29675467
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.aap9467
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