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Deep water inflow slowed offshore expansion of the West Antarctic Ice Sheet at the Eocene-Oligocene...

Deep water inflow slowed offshore expansion of the West Antarctic Ice Sheet at the Eocene-Oligocene...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_da1fdad3082b490395be2f920fb57794

Deep water inflow slowed offshore expansion of the West Antarctic Ice Sheet at the Eocene-Oligocene transition

About this item

Full title

Deep water inflow slowed offshore expansion of the West Antarctic Ice Sheet at the Eocene-Oligocene transition

Publisher

London: Nature Publishing Group

Journal title

Communications earth & environment, 2022-02, Vol.3 (1), p.1-10, Article 36

Language

English

Formats

Publication information

Publisher

London: Nature Publishing Group

More information

Scope and Contents

Contents

The stability of the West Antarctic Ice Sheet is threatened by the incursion of warm Circumpolar Deepwater which flows southwards via cross-shelf troughs towards the coast there melting ice shelves. However, the onset of this oceanic forcing on the development and evolution of the West Antarctic Ice Sheet remains poorly understood. Here, we use sin...

Alternative Titles

Full title

Deep water inflow slowed offshore expansion of the West Antarctic Ice Sheet at the Eocene-Oligocene transition

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_doaj_primary_oai_doaj_org_article_da1fdad3082b490395be2f920fb57794

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_da1fdad3082b490395be2f920fb57794

Other Identifiers

ISSN

2662-4435

E-ISSN

2662-4435

DOI

10.1038/s43247-022-00369-x

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