Evidence map›Paper›PMID 36241652›Full record

ArticleNature communications2022

Tidewater-glacier response to supraglacial lake drainage.

Laura A Stevens, Meredith Nettles, James L Davis, Timothy T Creyts, Jonathan Kingslake, Ian J Hewitt, Aaron Stubblefield

Abstract read
In one paragraph

Article in Nature communications, 2022. 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
–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

3 citing papers in PubMed.

  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

7 authors.

Laura A StevensDepartment of Earth Sciences, University of Oxford, Oxford, UK. laura.stevens@earth.ox.ac.uk.ORCID http://orcid.org/0000-0003-0480-8018
Meredith NettlesLamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA.ORCID http://orcid.org/0000-0003-4613-4162
James L DavisLamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA.
Timothy T CreytsLamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA.
Jonathan KingslakeLamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA.ORCID http://orcid.org/0000-0002-2065-9473
Ian J HewittMathematical Institute, University of Oxford, Oxford, UK.ORCID http://orcid.org/0000-0002-9167-6481
Aaron StubblefieldThayer School of Engineering, Dartmouth College, Hanover, NH, USA.ORCID http://orcid.org/0000-0003-3949-934X

Funding

National Science Foundation (NSF) 1643970National Science Foundation (NSF) 2003464
6 · The paper itself

Abstract

The flow speed of the Greenland Ice Sheet changes dramatically in inland regions when surface meltwater drains to the bed. But ice-sheet discharge to the ocean is dominated by fast-flowing outlet glaciers, where the effect of increasing surface melt on annual discharge is unknown. Observations of a supraglacial lake drainage at Helheim Glacier, and a consequent velocity pulse propagating down-glacier, provide a natural experiment for assessing the impact of changes in injected meltwater, and allow us to interrogate the subglacial hydrological system. We find a highly efficient subglacial drainage system, such that summertime lake drainage has little net effect on ice discharge. Our results question the validity of common remote-sensing approaches for inferring subglacial conditions, knowledge of which is needed for improved projections of sea-level rise.

Identifiers

PMID36241652
PMCPMC9568665

What OpenQuestion holds

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LicenceCC BY
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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.