Half a century of dynamic instability following the ocean-driven break-up of Wordie Ice Shelf

Ice shelves restrain grounded ice discharge into the ocean, and their break-up contributes significantly to Antarctica's sea level rise. Using aerial imagery from the 1960s and modern satellite data, we construct a long-term record of Wordie Ice Shelf's disintegration and its effects on tributary glaciers. Early changes in pinning points and ocean warming in Marguerite Bay since the 1960s strongly suggest increasing basal melt as the primary driver of the ice shelf disintegration. Some glaciers responded immediately to the ice shelf break-up, with surface velocities tripling, thinning up to 160 m, and grounding line retreat of 7.5 km, while others reacted decades later due to buttressing from remnant parts of the ice shelf. Our findings emphasize the importance of long-term observations to understand ice shelf disintegration and its impacts, offering crucial insights for assessments of future ice loss from the Antarctic Ice Sheet.

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Publication Details

Journal
Nature Communications
Published
2025-04-29
DOI
https://doi.org/10.1038/s41467-025-59293-1
Citations
4
Primary Topic
Cryospheric studies and observations
Type
article
Field-Weighted Citation Impact
5.20

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article

Half a century of dynamic instability following the ocean-driven break-up of Wordie Ice Shelf

Romain Millan, Mads Dømgaard, B. Scheuchl, Eric J. Rignot et al.
4 citations
Nature Communications
Cryospheric studies and observations
5.20
article

Half a century of dynamic instability following the ocean-driven break-up of Wordie Ice Shelf

Romain Millan, Mads Dømgaard, B. Scheuchl, Eric J. Rignot, Maaike Izeboud, Anders Anker Bjørk, Jonas Kvist Andersen, Maud Bernat
article en
4 citations

Abstract

Ice shelves restrain grounded ice discharge into the ocean, and their break-up contributes significantly to Antarctica's sea level rise. Using aerial imagery from the 1960s and modern satellite data, we construct a long-term record of Wordie Ice Shelf's disintegration and its effects on tributary glaciers. Early changes in pinning points and ocean warming in Marguerite Bay since the 1960s strongly suggest increasing basal melt as the primary driver of the ice shelf disintegration. Some glaciers responded immediately to the ice shelf break-up, with surface velocities tripling, thinning up to 160 m, and grounding line retreat of 7.5 km, while others reacted decades later due to buttressing from remnant parts of the ice shelf. Our findings emphasize the importance of long-term observations to understand ice shelf disintegration and its impacts, offering crucial insights for assessments of future ice loss from the Antarctic Ice Sheet.

Nature CommunicationsVol. 16(1)
Institut polytechnique de Grenoble (FR), University of Copenhagen (DK), Centre National de la Recherche Scientifique (FR), Jet Propulsion Laboratory (US), Université Fédérale de Toulouse Midi-Pyrénées (FR), University of California, Irvine (US), Institut National de Recherche pour l'Agriculture, l'Alimentation et l'Environnement (FR), Laboratoire d’Études en Géophysique et Océanographie Spatiales (FR), Institut des Géosciences de l'Environnement (FR), Irvine University (US), Institut de Recherche pour le Développement (FR), Université Grenoble Alpes (FR), Delft University of Technology (NL)
Villum Fonden, European Commission
Life below water
Openalex Percentile: Top 5%
Cryospheric studies and observations
5.20
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