Evidence map›Paper›PMID 39881125›Full record

ArticleNature communications2025

Precession modulates the poleward expansion of atmospheric circulation to the Arctic Ocean.

Yi Zhong, Zhengyao Lu, Stefanie Kaboth-Bahr, Jimin Yu, Keiji Horikawa, Mark J Dekkers, Juan C Larrasoaña, Peter D Clift, Michael E Weber, Flor Vermassen and 16 more

Abstract read
In one paragraph

Article in Nature communications, 2025. 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

26 authors.

Yi ZhongCentre for Marine Magnetism (CM2, Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen, 518055, China. zhongy@sustech.edu.cn.ORCID http://orcid.org/0000-0002-4298-8737
Zhengyao LuDepartment of Physical Geography and Ecosystem Science, Lund University, Lund, Sweden. zhengyao.lu@nateko.lu.se.ORCID http://orcid.org/0000-0002-5911-7110
Stefanie Kaboth-BahrInstitute of Geological Sciences, Frei Universität Berlin, 12249, Berlin, Germany.
Jimin YuLaoshan Laboratory, Qingdao, China.
Keiji HorikawaFaculty of Science, Academic Assembly, University of Toyama, Toyama, Japan.ORCID http://orcid.org/0000-0003-0337-0413
Mark J DekkersPaleomagnetic Laboratory 'Fort Hoofddijk', Department of Earth Sciences, Faculty of Geosciences, Utrecht University, Utrecht, The Netherlands.ORCID http://orcid.org/0000-0002-4156-3841
Juan C LarrasoañaDepartamento de Ciencias, Universidad Pública de Navarra, Campus de Arrosadia, 31006, Pamplona, Spain.ORCID http://orcid.org/0000-0003-4568-631X
Peter D CliftDepartment of Earth Sciences, University College London, London, WC1E 6BS, UK.
Michael E WeberInstitute for Geosciences, Department of Geochemistry and Petrology, University of Bonn, Bonn, Germany.ORCID http://orcid.org/0000-0003-2175-8980
Flor VermassenDepartment of Geological Sciences, Stockholm University, Stockholm, Sweden.ORCID http://orcid.org/0000-0003-0276-1973
Sev KenderCamborne School of Mines, Department of Earth and Environment Sciences, University of Exeter, Cornwall, UK.ORCID http://orcid.org/0000-0003-4216-3214
Chijun SunDepartment of Earth and Planetary Sciences, University of California Davis, Davis, CA, 95616, USA.ORCID http://orcid.org/0000-0002-3668-346X
Hu YangSouthern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, China.ORCID http://orcid.org/0000-0003-2054-2256
Xianfeng WangEarth Observatory of Singapore and Asian School of the Environment, Nanyang Technological University, Singapore, 639798, Singapore.ORCID http://orcid.org/0000-0002-8614-5627
Camilla S AndresenGeological Survey of Denmark and Greenland, Department of Glaciology and Climate, Øster Voldgade10, 1350, Copenhagen K, Denmark.ORCID http://orcid.org/0000-0002-5249-1812
Yanguang LiuKey Laboratory of Marine Geology and Metallogeny, First Institute of Oceanography, Ministry of Natural Resources (MNR), Qingdao, 266061, China.ORCID http://orcid.org/0000-0002-4524-2930
Haiwei ZhangInstitute of Global Environmental Change, Xi'an Jiaotong University, Xi'an, 710054, China.ORCID http://orcid.org/0000-0002-0855-1283
Zhengyang DaiCentre for Marine Magnetism (CM2, Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen, 518055, China.
Lu NiuAlfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany.ORCID http://orcid.org/0000-0002-8314-7416
Jingyu ZhangCentre for Marine Magnetism (CM2, Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen, 518055, China.ORCID http://orcid.org/0000-0002-9507-3223
Xuguang FengKey Laboratory of Marine Geology and Metallogeny, First Institute of Oceanography, Ministry of Natural Resources (MNR), Qingdao, 266061, China.
Debo ZhaoKey Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, 266071, China.ORCID http://orcid.org/0000-0002-4406-8985
Wenyue XiaCentre for Marine Magnetism (CM2, Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen, 518055, China.
Sheng YangCentre for Marine Magnetism (CM2, Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen, 518055, China.
Hai LiSouthern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou, 511458, China.
Qingsong LiuCentre for Marine Magnetism (CM2, Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen, 518055, China. qsliu@sustech.edu.cn.

Funding

National Natural Science Foundation of China (National Science Foundation of China) 42274094
6 · The paper itself

Abstract

Under sustained global warming, Arctic climate is projected to become more responsive to changes in North Pacific meridional heat transport as a result of teleconnections between low and high latitudes, but the underlying mechanisms remain poorly understood. Here, we reconstruct subarctic humidity changes over the past 400 kyr to investigate the role of low-to-high latitude interactions in regulating Arctic hydroclimate. Our reconstruction is based on precipitation-driven sediment input variations in the Subarctic North Pacific (SANP), which reveal a strong precessional cycle in subarctic humidity under the relatively low eccentricity variations that dominated the past four glacial-interglacial cycles. Combined with climate model simulations, we highlight that precession drives meridional shifts in the northern rim of the North Pacific Subtropical Gyre (NPSG) and modulates the efficiency of heat and water vapor transfer to the SANP and Arctic regions. Our findings suggest that projections of a northward shift of the NPSG in response to future global warming will lead to wetter conditions in the Arctic Ocean and enhanced sea-ice loss.

Identifiers

PMID39881125
PMCPMC11779882

What OpenQuestion holds

Textmetadata
LicenceCC BY-NC-ND
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.