ArticleNature communications2024
Atlantic Water warming increases melt below Northeast Greenland's last floating ice tongue.
Article in Nature communications, 2024. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 8 papers.
What it found
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The trial behind it
Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.
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Who cites it
8 citing papers in PubMed.
- Narwhals document atlantification of East Greenland.Science advances · 2026Article
- Petermann Glacier on the brink: Progress, challenges and insights.Science advances · 2026Review
- Article
- Ocean driven retreat of the Northeast Greenland Ice Stream following the Last Glacial Maximum.Nature communications · 2025Article
- Atlantic water recirculation in the northern Barents Sea affects winter sea ice extent.Nature communications · 2025Article
- Pervasive glacier retreats across Svalbard from 1985 to 2023.Nature communications · 2025Article
- Comparative Analysis of Prediction Models for Trawling Grounds of the Argentine Shortfin SquidBiology · 2025Article
- Atlantic Water warming increases melt below Northeast Greenland's last floating ice tongue.Nature communications · 2024Article
Corrections and comments
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Authors and funding
9 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
The 79 North Glacier (79NG) features Greenland's largest floating ice tongue. Even though its extent has not changed significantly in recent years, observations have indicated a major thinning of the ice tongue from below. Both ocean warming and an increase in subglacial discharge from the ice sheet induced by atmospheric warming could increase the basal melt; however, available observations alone cannot tell which of these is the main driver. Here, we employ a global simulation which explicitly resolves the ocean circulation in the cavity with 700 m resolution to disentangle the impact of the ocean and atmosphere. We find that the interannual variability of basal melt below 79NG over the past 50 years is mainly associated with changes in the temperature of the Atlantic Intermediate Water inflow, which can be traced back across the Northeast Greenland continental shelf to the eastern Fram Strait with a lag of 3 years.
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Registered trials
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