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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Detalles Bibliográficos
Autores principales: Silvano, Alessandro, Rintoul, Stephen Rich, Peña-Molino, Beatriz, Hobbs, William Richard, van Wijk, Esmee, Aoki, Shigeru, Tamura, Takeshi, Williams, Guy Darvall
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2018
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5906079/
https://www.ncbi.nlm.nih.gov/pubmed/29675467
http://dx.doi.org/10.1126/sciadv.aap9467

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5906079/
https://www.ncbi.nlm.nih.gov/pubmed/29675467
http://dx.doi.org/10.1126/sciadv.aap9467

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