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...

Deskribapen osoa

Gorde:
Xehetasun bibliografikoak
Argitaratua izan da:Sci Adv
Egile Nagusiak: Silvano, Alessandro, Rintoul, Stephen Rich, Peña-Molino, Beatriz, Hobbs, William Richard, van Wijk, Esmee, Aoki, Shigeru, Tamura, Takeshi, Williams, Guy Darvall
Formatua: Artigo
Hizkuntza:Inglês
Argitaratua: American Association for the Advancement of Science 2018
Gaiak:
Research Articles
Sarrera elektronikoa: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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