ArticleNature communications2023
Atlantic water intrusion triggers rapid retreat and regime change at previously stable Greenland glacier.
Article in Nature communications, 2023. 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 abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
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Who cites it
8 citing papers in PubMed.
- Narwhals document atlantification of East Greenland.Science advances · 2026Article
- Unraveling daily dynamics of supraglacial lakes in response to hydrological pulses and anomalous climate signals.Nature communications · 2026Article
- Multi-phase retreat of the Laurentide Ice Sheet and associated freshwater release from Hudson Bay during the last deglaciation.Scientific reports · 2026Article
- Seasonal changes of mélange thickness coincide with Greenland calving dynamics.Nature communications · 2025Article
- Increased crevassing across accelerating Greenland Ice Sheet margins.Nature geoscience · 2025Article
- Heterogeneous impacts of ocean thermal forcing on ice discharge from Greenland's peripheral tidewater glaciers over 2000-2021.Scientific reports · 2024Article
- Ocean warming drives rapid dynamic activation of marine-terminating glacier on the west Antarctic Peninsula.Nature communications · 2023Article
- Atlantic water intrusion triggers rapid retreat and regime change at previously stable Greenland glacier.Nature communications · 2023Article
Corrections and comments
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Authors and funding
4 authors.
Funding
Abstract
Ice discharge from Greenland's marine-terminating glaciers contributes to half of all mass loss from the ice sheet, with numerous mechanisms proposed to explain their retreat. Here, we examine K.I.V Steenstrups Nordre Bræ ('Steenstrup') in Southeast Greenland, which, between 2018 and 2021, retreated ~7 km, thinned ~20%, doubled in discharge, and accelerated ~300%. This rate of change is unprecedented amongst Greenland's glaciers and now places Steenstrup in the top 10% of glaciers by contribution to ice-sheet-wide discharge. In contrast to expected behaviour from a shallow, grounded tidewater glacier, Steenstrup was insensitive to high surface temperatures that destabilised many regional glaciers in 2016, appearing instead to respond to a >2 °C anomaly in deeper Atlantic water (AW) in 2018. By 2021, a rigid proglacial mélange had developed alongside notable seasonal variability. Steenstrup's behaviour highlights that even long-term stable glaciers with high sills are vulnerable to sudden and rapid retreat from warm AW intrusion.
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Registered trials
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