ArticleScientific data2025
Bedmap3 updated ice bed, surface and thickness gridded datasets for Antarctica.
Article in Scientific data, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 6 papers.
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Who cites it
6 citing papers in PubMed.
- Modelling Future Evolution of the Antarctic Ice Sheet With Explainable Machine Learning.Journal of the Royal Society of New Zealand · 2026Article
- Islands of Biodiversity: Characterization of Lichen Flora in Antarctic Nunataks.Journal of fungi (Basel, Switzerland) · 2026Article
- Hard rocks and deep wetlands beneath Thwaites Glacier in Antarctica.Communications earth & environment · 2026Article
- Entrained debris records regrowth of the Greenland Ice Sheet after the last interglacial.Nature geoscience · 2026Article
- Bedmap3 updated ice bed, surface and thickness gridded datasets for Antarctica.Scientific data · 2025Article
- Extensive fluvial surfaces at the East Antarctic margin have modulated ice-sheet evolution.Nature geoscience · 2025Article
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Authors and funding
82 authors.
Funding
Abstract
We present Bedmap3, the latest suite of gridded products describing surface elevation, ice-thickness and the seafloor and subglacial bed elevation of the Antarctic south of 60 °S. Bedmap3 incorporates and adds to all post-1950s datasets previously used for Bedmap2, including 84 new aero-geophysical surveys by 15 data providers, an additional 52 million data points and 1.9 million line-kilometres of measurement. These efforts have filled notable gaps including in major mountain ranges and the deep interior of East Antarctica, along West Antarctic coastlines and on the Antarctic Peninsula. Our new Bedmap3/RINGS grounding line similarly consolidates multiple recent mappings into a single, spatially coherent feature. Combined with updated maps of surface topography, ice shelf thickness, rock outcrops and bathymetry, Bedmap3 reveals in much greater detail the subglacial landscape and distribution of Antarctica's ice, providing new opportunities to interpret continental-scale landscape evolution and to model the past and future evolution of the Antarctic ice sheets.
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Registered trials
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