Evidence map›Paper›PMID 37935697›Full record

ArticleNature communications2023

Rapid disintegration and weakening of ice shelves in North Greenland.

R Millan, E Jager, J Mouginot, M H Wood, S H Larsen, P Mathiot, N C Jourdain, A Bjørk

Open access · goldAbstract read
In one paragraph

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 3 papers.

0numbers the graph read from it
0cells of the map it votes in
3citing papers in PubMed
6.4field-weighted citation impact, top 2% of its field
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

3 citing papers in PubMed, 30 citations in OpenAlex.

  1. Article
  2. Article
  3. Article
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

8 authors at 5 institutions in 3 countries.

R MillanUniversité Grenoble Alpes, CNRS, IRD, INP, 38400, Grenoble, Isère, France. romain.millan@univ-grenoble-alpes.fr.ORCID http://orcid.org/0000-0002-7987-1305
E JagerUniversité Grenoble Alpes, CNRS, IRD, INP, 38400, Grenoble, Isère, France.
J MouginotUniversité Grenoble Alpes, CNRS, IRD, INP, 38400, Grenoble, Isère, France.ORCID http://orcid.org/0000-0001-9155-5455
M H WoodMoss Landing Marine Laboratories, San José State University, San Jose, CA, 95192, USA.ORCID http://orcid.org/0000-0003-3074-7845
S H LarsenDepartment of Glaciology and Climate, Geological Survey of Denmark and Greenland (GEUS), Copenhagen, Denmark.ORCID http://orcid.org/0000-0002-3656-3521
P MathiotUniversité Grenoble Alpes, CNRS, IRD, INP, 38400, Grenoble, Isère, France.ORCID http://orcid.org/0000-0002-2001-0762
N C JourdainUniversité Grenoble Alpes, CNRS, IRD, INP, 38400, Grenoble, Isère, France.ORCID http://orcid.org/0000-0002-1372-2235
A BjørkDepartment of Geosciences and Natural Resources Management, University of Copenhagen, 1350, Copenhagen, Denmark.ORCID http://orcid.org/0000-0002-4919-792X
Centre National de la Recherche Scientifique · FRGeological Survey of Denmark and Greenland · DKInstitut polytechnique de Grenoble · FRSan Jose State University · USUniversity of Copenhagen · DK

Funding

Agence Nationale de la Recherche (French National Research Agency) ANR-19-CE01-0011-01Agence Nationale de la Recherche (French National Research Agency) ANR-19-CE01-0015EC | Horizon 2020 Framework Programme (EU Framework Programme for Research and Innovation H2020) 101003536NASA | Jet Propulsion Laboratory (JPL) NNH20ZDA001N-CRYONASA | Jet Propulsion Laboratory (JPL) NNH22ZDA001N-POVillum Fonden (Villum Foundation) 29456
6 · The paper itself

Abstract

The glaciers of North Greenland are hosting enough ice to raise sea level by 2.1 m, and have long considered to be stable. This part of Greenland is buttressed by the last remaining ice shelves of the ice sheet. Here, we show that since 1978, ice shelves in North Greenland have lost more than 35% of their total volume, three of them collapsing completely. For the floating ice shelves that remain we observe a widespread increase in ice shelf mass losses, that are dominated by enhanced basal melting rates. Between 2000 and 2020, there was a widespread increase in basal melt rates that closely follows a rise in the ocean temperature. These glaciers are showing a direct dynamical response to ice shelf changes with retreating grounding lines and increased ice discharge. These results suggest that, under future projections of ocean thermal forcing, basal melting rates will continue to rise or remain at high level, which may have dramatic consequences for the stability of Greenlandic glaciers.

Identifiers

PMID37935697
PMCPMC10630314
OpenAlexW4388446536

What OpenQuestion holds

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LicenceCC BY
Read underepoch 390

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.