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Deep glacial troughs and stabilizing ridges unveiled beneath the margins of the Antarctic ice sheet

Deep glacial troughs and stabilizing ridges unveiled beneath the margins of the Antarctic ice sheet

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_hal_primary_oai_HAL_hal_03025912v1

Deep glacial troughs and stabilizing ridges unveiled beneath the margins of the Antarctic ice sheet

Publication information

Publisher

London: Nature Publishing Group UK

More information

Scope and Contents

Contents

The Antarctic ice sheet has been losing mass over past decades through the accelerated flow of its glaciers, conditioned by ocean temperature and bed topography. Glaciers retreating along retrograde slopes (that is, the bed elevation drops in the inland direction) are potentially unstable, while subglacial ridges slow down the glacial retreat. Desp...

Alternative Titles

Full title

Deep glacial troughs and stabilizing ridges unveiled beneath the margins of the Antarctic ice sheet

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_hal_primary_oai_HAL_hal_03025912v1

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_hal_primary_oai_HAL_hal_03025912v1

Other Identifiers

ISSN

1752-0894

E-ISSN

1752-0908

DOI

10.1038/s41561-019-0510-8

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