Abstract
Climate models show that Antarctic surface melt will increase through the current century. Surface melting changes ice sheet albedo, the availability of liquid water for endemic and invasive species, and may even accelerate ice shelf collapse and global sea level rise. Here we show, using 1 km downscaled projections of potential Antarctic surface melt, that the total area experiencing surface melt will expand by more than 10% by 2100 under a Shared Socio-economic Pathway 3-7.0 scenario, with increased potential melt totals likely to threaten the viability of ice shelves mostly in the West Antarctic Peninsula and Amundsen Sea Embayment, through an elevated risk of hydrofracture. By calculating the latitudinal rate of melt migration we also find that Shared Socio-economic Pathway 1-2.6 is the only emissions scenario under which the rate of future Antarctic surface melt expansion will stabilize at present levels.
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Data availability
REMA surface elevation data are available at https://www.pgc.umn.edu/data/rema/. ERA5 reanalysis data are available at https://doi.org/10.24381/cds.adbb2d47. BedMachine Antarctica V3 data are available at https://doi.org/10.5067/FPSU0V1MWUB6. Satellite SSM/I and SMMR, AMSR-E surface melt day data are available at https://doi.org/10.18709/perscido.2022.09.ds376. RACMO2.3p2 surface melt rate data are available at https://doi.org/10.5281/zenodo.7845736. CMIP6 data are available at https://esgf-data.dkrz.de/search/cmip6-dkrz. CMIP6 and CORDEX-CMIP5 MMM temperature anomalies are available at https://interactive-atlas.ipcc.ch/. Information on these data can be found at https://wcrp-cmip.org/cmip-data-access/and https://cordex.org/data-access/. Ice surface elevation anomaly data are available at https://osf.io/aupnk/and https://doi.org/10.17605/OSF.IO/3EDXF, or from https://doi.org/10.1038/s41586-019-0889-9. The Zwally Antarctic drainage basin data are available at http://imbie.org/imbie-3/drainage-basins/and https://earth.gsfc.nasa.gov/cryo/data/polar-altimetry/antarctic-and-greenland-drainage-systems. Spatial maps of passive ice areas, vulnerable to hydrofracturing, and present-day fracture locations are available at https://doi.org/10.15784/601335. Data generated and analysed in this research are available at https://doi.org/10.17605/OSF.IO/CDKVT.
Code availability
Codes used in this research are available at https://doi.org/10.17605/OSF.IO/CDKVT.
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Acknowledgements
This work was funded by contract RDF-VUW1501 to N.R.G. from the Royal Society Te Apārangi, with support from the Antarctic Research Centre, Victoria University of Wellington (VUW). Y.Z. and S.S. are supported by the National Key Research and Development Program of China, (Grant No. 2024YFF0809404). N.R.G. and A.G. are supported by grant ANTA1801 ("New Zealand Antarctic Science Platform”) from the New Zealand Ministry of Business, Innovation, & Employment. N.R.G. is supported by grant RTVU2206 ("Our Changing Coast”) from the New Zealand Ministry of Business, Innovation, & Employment. We gratefully acknowledge technical assistance and access to compute resources provided through the Centre for Academic Development and the Rāpoi compute cluster at VUW. We are also grateful to the CMIP community for making their simulations freely available.
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Y.Z., N.R.G., and A.G. conceived the study. Y.Z. performed the simulations and analysis. Y.Z., N.R.G., and A.G. contributed to writing the paper. Y.Z., N.R.G., and A.G. contributed to revisions and editing. S.S. assisted Y.Z. whilst undertaking some of this work.
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Zheng, Y., Golledge, N.R., Gossart, A. et al. Expansion of Antarctic surface melt through the 21st century. Nat Commun (2026). https://doi.org/10.1038/s41467-026-71114-7
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DOI: https://doi.org/10.1038/s41467-026-71114-7


