Evidence map›Paper›PMID 41313756›Full record

ArticleScience advances2025

Negligible contribution from aerosols to recent trends in Earth's energy imbalance.

Chanyoung Park, Brian J Soden

Abstract read
In one paragraph

Article in Science advances, 2025. 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

2 authors.

Chanyoung ParkRosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami, Miami, FL, USA.ORCID 0000-0001-8644-1031
Brian J SodenRosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami, Miami, FL, USA.ORCID 0000-0001-9693-8236

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

During the 21st century, Earth's energy imbalance (EEI) at the top of atmosphere has markedly increased because of greater absorbed shortwave (SW) rather than reduced outgoing longwave radiation. Previous studies using single-forcing (aerosol-only) experiments attributed approximately half of the positive SW trend to reductions in anthropogenic aerosols, particularly in the Northern Hemisphere (NH). In contrast, our analysis using observations and reanalysis indicates that both aerosol-radiation and aerosol-cloud interactions have made a negligible contribution to recent EEI trends. While NH anthropogenic aerosols have decreased, enhanced emissions from wildfires and volcanic activity in the Southern Hemisphere (SH) have produced comparable increases, yielding little net global impact. This hemispheric compensation also suggests that model-based estimates may overestimate aerosol influence by overlooking SH aerosol contributions. Despite uncertainties in aerosol proxies, the consistent results from two complementary proxies-satellite-derived aerosol index and reanalysis-based sulfate mass concentration-highlight the importance of accounting for natural source aerosols when assessing EEI trends.

Identifiers

PMID41313756
PMCPMC12662203

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Registered trials

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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.