Articles | Volume 26, issue 10
https://doi.org/10.5194/acp-26-7677-2026
https://doi.org/10.5194/acp-26-7677-2026
Research article
 | 
01 Jun 2026
Research article |  | 01 Jun 2026

Multi-model analysis of the impact of water vapor on the radiative forcing of volcanic aerosols after the 2022 Hunga Eruption

Ilaria Quaglia, Daniele Visioni, Ewa M. Bednarz, Yunqian Zhu, Georgiy Stenchikov, Valentina Aquila, Cheng-Cheng Liu, Graham W. Mann, Yifeng Peng, Takashi Sekiya, Simone Tilmes, Xinyue Wang, Shingo Watanabe, Pengfei Yu, Jun Zhang, Wandi Yu, and Zhihong Zhuo

Viewed

Total article views: 20,290 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
16,232 3,778 280 20,290 257 228
  • HTML: 16,232
  • PDF: 3,778
  • XML: 280
  • Total: 20,290
  • BibTeX: 257
  • EndNote: 228
Views and downloads (calculated since 05 Sep 2025)
Cumulative views and downloads (calculated since 05 Sep 2025)

Viewed (geographical distribution)

Total article views: 20,290 (including HTML, PDF, and XML) Thereof 20,268 with geography defined and 22 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 01 Jun 2026
Download
Short summary
On January 15, 2022, the Hunga volcano eruption released unprecedented amounts of water vapor into the atmosphere alongside a modest amount of SO2. In this work we analyse results from multiple Earth system models. The models agree that the eruption led to small negative radiative forcing from sulfate aerosols and that the contribution from water vapor was minimal. Therefore, the Hunga eruption cannot explain the exceptional surface warming observed in 2023.
Share
Altmetrics
Final-revised paper
Preprint