Evidence map›Paper›PMID 30854427›Full record

ArticleScience advances2019

Sea ice variability in the southern Norwegian Sea during glacial Dansgaard-Oeschger climate cycles.

Henrik Sadatzki, Trond M Dokken, Sarah M P Berben, Francesco Muschitiello, Ruediger Stein, Kirsten Fahl, Laurie Menviel, Axel Timmermann, Eystein Jansen

Abstract read
In one paragraph

Article in Science advances, 2019. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 10 papers.

0numbers the graph read from it
0cells of the map it votes in
10citing 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

10 citing papers in PubMed.

  1. Article
  2. Article
  3. Article
  4. Sea ice fluctuations in the Baffin Bay and the Labrador Sea during glacial abrupt climate changes.Proceedings of the National Academy of Sciences of the United States of America · 2022
    Article
  5. Article
  6. Article
  7. Rapid reductions and millennial-scale variability in Nordic Seas sea ice cover during abrupt glacial climate changes.Proceedings of the National Academy of Sciences of the United States of America · 2020
    Article
  8. Lagged atmospheric circulation response in the Black Sea region to Greenland Interstadial 10.Proceedings of the National Academy of Sciences of the United States of America · 2020
    Article
  9. Article
  10. 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

9 authors.

Henrik SadatzkiDepartment of Earth Science and Bjerknes Centre for Climate Research, University of Bergen, 5007 Bergen, Norway.ORCID 0000-0002-1270-6807
Trond M DokkenNORCE Norwegian Research Centre, Bjerknes Centre for Climate Research, 5007 Bergen, Norway.
Sarah M P BerbenDepartment of Earth Science and Bjerknes Centre for Climate Research, University of Bergen, 5007 Bergen, Norway.
Francesco MuschitielloDepartment of Geography, University of Cambridge, Cambridge CB2 3EQ, UK.
Ruediger SteinAlfred Wegener Institute Helmholtz Centre for Polar and Marine Research, 27568 Bremerhaven, Germany.ORCID 0000-0002-4453-9564
Kirsten FahlAlfred Wegener Institute Helmholtz Centre for Polar and Marine Research, 27568 Bremerhaven, Germany.ORCID 0000-0001-9317-4656
Laurie MenvielClimate Change Research Centre and PANGEA Research Centre, University of New South Wales, Sydney, New South Wales 2052, Australia.ORCID 0000-0002-5068-1591
Axel TimmermannCenter for Climate Physics, Institute for Basic Science (IBS), Busan, South Korea.
Eystein JansenDepartment of Earth Science and Bjerknes Centre for Climate Research, University of Bergen, 5007 Bergen, Norway.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The last glacial period was marked by pronounced millennial-scale variability in ocean circulation and global climate. Shifts in sea ice cover within the Nordic Seas are believed to have amplified the glacial climate variability in northern high latitudes and contributed to abrupt, high-amplitude temperature changes over Greenland. We present unprecedented empirical evidence that resolves the nature, timing, and role of sea ice fluctuations for abrupt ocean and climate change 32 to 40 thousand years ago, using biomarker sea ice reconstructions from the southern Norwegian Sea. Our results document that initial sea ice reductions at the core site preceded the major reinvigoration of convective deep-water formation in the Nordic Seas and abrupt Greenland warming; sea ice expansions preceded the buildup of a deep oceanic heat reservoir. Our findings suggest that the sea ice variability shaped regime shifts between surface stratification and deep convection in the Nordic Seas during abrupt climate changes.

Identifiers

PMID30854427
PMCPMC6402855

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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.