Evidence map›Paper›PMID 36028494›Full record

ArticleNature communications2022

Tropical volcanoes synchronize eastern Canada with Northern Hemisphere millennial temperature variability.

Feng Wang, Dominique Arseneault, Étienne Boucher, Fabio Gennaretti, Shulong Yu, Tongwen Zhang

Open access · goldAbstract 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 2 papers.

0numbers the graph read from it
0cells of the map it votes in
2citing papers in PubMed
4.9field-weighted citation impact, top 4% 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

2 citing papers in PubMed, 37 citations in OpenAlex.

  1. Article
  2. 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

6 authors at 4 institutions in 2 countries.

Feng WangDépartement de Biologie, Chimie et Géographie, Centre d'Études Nordiques, Université du Québec à Rimouski, Rimouski, QC, G5L 3A1, Canada. feng.wang@uqar.ca.ORCID 0000-0002-9562-4849
Dominique ArseneaultDépartement de Biologie, Chimie et Géographie, Centre d'Études Nordiques, Université du Québec à Rimouski, Rimouski, QC, G5L 3A1, Canada.ORCID 0000-0002-3419-2480
Étienne BoucherDépartement de Géographie, GEOTOP, and Centre d'Études Nordiques, Université du Québec à Montréal, Montréal, QC, H2X 3R9, Canada.
Fabio GennarettiInstitut de Recherche sur les Forêts, Groupe de Recherche en Écologie de la MRC-Abitibi, Centre d'Étude de la Forêt, Université du Québec en Abitibi-Témiscamingue, Amos, QC, J9T 2L8, Canada.ORCID 0000-0002-8232-023X
Shulong YuXinjiang Key Laboratory of Tree-Ring Ecology, Key Laboratory of Tree-Ring Physical and Chemical Research, Institute of Desert Meteorology, China Meteorological Administration, 830002, Urumqi, China.
Tongwen ZhangXinjiang Key Laboratory of Tree-Ring Ecology, Key Laboratory of Tree-Ring Physical and Chemical Research, Institute of Desert Meteorology, China Meteorological Administration, 830002, Urumqi, China.
China Meteorological Administration · CNUniversité du Québec à Rimouski · CAUniversité du Québec à Montréal · CAUniversité du Québec en Abitibi-Témiscamingue · CA

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Although global and Northern Hemisphere temperature reconstructions are coherent with climate model simulations over the last millennium, reconstructed temperatures tend to diverge from simulations at smaller spatial scales. Yet, it remains unclear to what extent these regional peculiarities reflect region-specific internal climate variability or inadequate proxy coverage and quality. Here, we present a high-quality, millennial-long summer temperature reconstruction for northeastern North America, based on maximum latewood density, the most temperature-sensitive tree-ring proxy. Our reconstruction shows that a large majority (31 out of 44) of the coldest extremes can be attributed to explosive volcanic eruptions, with more persistent cooling following large tropical than extratropical events. These forced climate variations synchronize regional summer temperatures with hemispheric reconstructions and simulations at the multidecadal time scale. Our study highlights that tropical volcanism is the major driver of multidecadal temperature variations across spatial scales.

Indexed as

ClimateTreesCanadaSeasonsTemperature

Identifiers

PMID36028494
PMCPMC9418434
OpenAlexW4293116290

What OpenQuestion holds

Textmetadata
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.