Evidence map›Paper›PMID 41912508›Full record

ArticleNature communications2026

Expansion of Antarctic surface melt through the 21st century.

Yaowen Zheng, Nicholas R Golledge, Alexandra Gossart, Shoujuan Shu

Abstract read
In one paragraph

Article in Nature communications, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

0numbers the graph read from it
0cells of the map it votes in
0citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

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.

2 · The registry

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.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

0 citing papers in PubMed.

No citing paper in PubMed yet.

4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

4 authors.

Yaowen ZhengAntarctic Research Centre, Victoria University of Wellington, Wellington, New Zealand.
Nicholas R GolledgeAntarctic Research Centre, Victoria University of Wellington, Wellington, New Zealand. nicholas.golledge@vuw.ac.nz.ORCID http://orcid.org/0000-0001-7676-8970
Alexandra GossartAntarctic Research Centre, Victoria University of Wellington, Wellington, New Zealand.ORCID http://orcid.org/0000-0002-1927-2685
Shoujuan ShuDepartment of Atmospheric Sciences, School of Earth Sciences, Zhejiang University, Hangzhou, China.

Funding

Ministry for Business Innovation and Employment (MBIE) ANTA1801Ministry for Business Innovation and Employment (MBIE) RTVU2206
6 · The paper itself

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.

Identifiers

PMID41912508
PMCPMC13250155

What OpenQuestion holds

Textmetadata
LicenceCC BY-NC-ND
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Registered trials

None linked

Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.