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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Bibliographic Details
Published in:Science Advances
Main Authors: Silvano, Alessandro, Rintoul, Stephen Rich, Peña-Molino, Beatriz, Hobbs, William Richard, Wijk, Esmee van, Aoki, Shigeru, Tamura, Takeshi, Williams, Guy Darvall
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Online Access:https://eprints.soton.ac.uk/469726/