Evidence map›Paper›PMID 38748800›Full record

ArticleScience advances2024

Amplified seasonality in western Europe in a warmer world.

Niels J de Winter, Julia Tindall, Andrew L A Johnson, Barbara Goudsmit-Harzevoort, Nina Wichern, Pim Kaskes, Philippe Claeys, Fynn Huygen, Sonja van Leeuwen, Brett Metcalfe and 4 more

Abstract read
In one paragraph

Article in Science advances, 2024. 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

14 authors.

Niels J de WinterDepartment of Earth Sciences, Vrije Universiteit Amsterdam, Amsterdam, Netherlands.ORCID 0000-0002-1453-5407
Julia TindallSchool of Earth and Environment, University of Leeds, Leeds, UK.ORCID 0000-0002-2360-5761
Andrew L A JohnsonSchool of Science, University of Derby, Derby, UK.ORCID 0000-0001-5727-1889
Barbara Goudsmit-HarzevoortDepartment of Estuarine and Delta Systems, Royal Netherlands Institute for Sea Research, Texel, Netherlands.ORCID 0000-0002-5038-9697
Nina WichernInstitut für Geologie und Paläontologie, Universität Münster, Münster, Germany.ORCID 0000-0001-5872-8086
Pim KaskesArchaeology, Environmental Changes and Geochemistry group, Vrije Universiteit Brussel, Brussels, Belgium.ORCID 0000-0002-2605-6366
Philippe ClaeysArchaeology, Environmental Changes and Geochemistry group, Vrije Universiteit Brussel, Brussels, Belgium.ORCID 0000-0002-4585-7687
Fynn HuygenInstitut für Geowissenschaften, Universität Kiel, Kiel, Germany.
Sonja van LeeuwenDepartment of Estuarine and Delta Systems, Royal Netherlands Institute for Sea Research, Texel, Netherlands.ORCID 0000-0003-2180-1969
Brett MetcalfeDepartment of Earth Sciences, Vrije Universiteit Amsterdam, Amsterdam, Netherlands.ORCID 0000-0002-5873-9815
Pepijn BakkerDepartment of Earth Sciences, Vrije Universiteit Amsterdam, Amsterdam, Netherlands.ORCID 0000-0001-6249-0162
Stijn GoolaertsDirectorate Earth and History of Life, Royal Belgian Institute for Natural Sciences, Brussels, Belgium.ORCID 0000-0002-7082-9012
Frank WesselinghDepartment of Earth Sciences, Utrecht University, Utrecht, Netherlands.ORCID 0000-0003-3655-0701
Martin ZieglerDepartment of Earth Sciences, Utrecht University, Utrecht, Netherlands.ORCID 0000-0003-3198-6434

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Documenting the seasonal temperature cycle constitutes an essential step toward mitigating risks associated with extreme weather events in a future warmer world. The mid-Piacenzian Warm Period (mPWP), 3.3 to 3.0 million years ago, featured global temperatures approximately 3°C above preindustrial levels. It represents an ideal period for directed paleoclimate reconstructions equivalent to model projections for 2100 under moderate Shared Socioeconomic Pathway SSP2-4.5. Here, seasonal clumped isotope analyses of fossil mollusk shells from the North Sea are presented to test Pliocene Model Intercomparison Project 2 outcomes. Joint data and model evidence reveals enhanced summer warming (+4.3° ± 1.0°C) compared to winter (+2.5° ± 1.5°C) during the mPWP, equivalent to SSP2-4.5 outcomes for future climate. We show that Arctic amplification of global warming weakens mid-latitude summer circulation while intensifying seasonal contrast in temperature and precipitation, leading to an increased risk of summer heat waves and other extreme weather events in Europe's future.

Indexed as

Global WarmingSeasonsAnimalsClimate ChangeClimate ModelsEuropeFossilsTemperature

Identifiers

PMID38748800
PMCPMC11095466

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.