Evidence map›Paper›PMID 41932884›Full record

ArticleNature communications2026

Subglacial water flow and ice dynamics during glacial lake outburst floods observed from space.

Eyjólfur Magnússon, Vincent Drouin, Finnur Pálsson, Tómas Jóhannesson, Joaquín M C Belart, Jan Wuite, Valentyn Tolpekin, Krista Hannesdóttir, Etienne Berthier, Gunnar Sigurðsson and 5 more

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

15 authors.

Eyjólfur MagnússonInstitute of Earth Sciences, University of Iceland, Reykjavík, Iceland. eyjolfm@hi.is.ORCID http://orcid.org/0000-0002-9816-0787
Vincent DrouinIcelandic Meteorological Office, Reykjavík, Iceland.ORCID http://orcid.org/0000-0002-5340-0484
Finnur PálssonInstitute of Earth Sciences, University of Iceland, Reykjavík, Iceland.ORCID http://orcid.org/0000-0002-0874-6443
Tómas JóhannessonIcelandic Meteorological Office, Reykjavík, Iceland.ORCID http://orcid.org/0000-0001-7274-8593
Joaquín M C BelartNatural Science Institute of Iceland, Garðabær, Iceland.ORCID http://orcid.org/0000-0002-0853-8935
Jan WuiteENVEO IT GmbH, Innsbruck, Austria.ORCID http://orcid.org/0000-0001-9333-1586
Valentyn TolpekinICEYE Oy, Espoo, Finland.ORCID http://orcid.org/0000-0003-4517-113X
Krista HannesdóttirInstitute of Earth Sciences, University of Iceland, Reykjavík, Iceland.
Etienne BerthierLEGOS, Université de Toulouse, CNES, CNRS, IRD, UPS, Toulouse, France.ORCID http://orcid.org/0000-0001-5978-9155
Gunnar SigurðssonIcelandic Meteorological Office, Reykjavík, Iceland.
Bergur EinarssonIcelandic Meteorological Office, Reykjavík, Iceland.ORCID http://orcid.org/0000-0002-1984-9982
Benedikt G ÓfeigssonIcelandic Meteorological Office, Reykjavík, Iceland.
Thomas NaglerENVEO IT GmbH, Innsbruck, Austria.ORCID http://orcid.org/0000-0003-1298-8469
Magnús T GudmundssonInstitute of Earth Sciences, University of Iceland, Reykjavík, Iceland.ORCID http://orcid.org/0000-0001-5325-3368
Thórdís HögnadóttirInstitute of Earth Sciences, University of Iceland, Reykjavík, Iceland.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Glacial lake outburst floods (jökulhlaups) are challenging to study because they often take place below hundreds of meters of ice, and the complex interplay between lifting of the glacier and melting of the flood path is not well understood. Here, we provide unique insights into the mechanics of jökulhlaups and how they affect three-dimensional glacier motion using satellite synthetic aperture radar (SAR) and field observations, acquired before, during and after two recent jökulhlaups (in 2021 and 2022) from the subglacial lake Grímsvötn in Iceland. The results indicate that the same event may alternate between channel flow and sheet flow and that ponding of water along the subglacial flood path can play a major role in jökulhlaup dynamics. This has important implications for physical jökulhlaup modeling and for better understanding the role of subglacial hydraulics on glacier dynamics, required for improved predictions of the future evolution of glaciers and ice sheets.

Identifiers

PMID41932884
PMCPMC13076879

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LicenceCC BY-NC-ND
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Registered trials

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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.