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, A, Rintoul, SR, Pena-Molino, B, Hobbs, WR, van Wijk, E, Aoki, S, Tamura, T, Williams, GD
Format: Article in Journal/Newspaper
Language:unknown
Published: American Association for the Advancement of Science 2018
Subjects:
Online Access:https://eprints.utas.edu.au/45115/