Two-timescale response of a large Antarctic ice shelf to climate change

Abstract A potentially irreversible threshold in Antarctic ice shelf melting would be crossed if the ocean cavity beneath the large Filchner–Ronne Ice Shelf were to become flooded with warm water from the deep ocean. Previous studies have identified this possibility, but there is great uncertainty a...

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Bibliographic Details
Published in:Nature Communications
Main Authors: Naughten, Kaitlin A., De Rydt, Jan, Rosier, Sebastian H. R., Jenkins, Adrian, Holland, Paul R., Ridley, Jeff K.
Format: Article in Journal/Newspaper
Language:English
Published: Springer Science and Business Media LLC 2021
Subjects:
Online Access:http://dx.doi.org/10.1038/s41467-021-22259-0
http://www.nature.com/articles/s41467-021-22259-0.pdf
http://www.nature.com/articles/s41467-021-22259-0