Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics
ACP
Articles | Volume 24, issue 12
Articles | Volume 24, issue 12
https://doi.org/10.5194/acp-24-7203-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-24-7203-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 24, issue 12
Research article
 | 
24 Jun 2024
Research article |  | 24 Jun 2024

Why does stratospheric aerosol forcing strongly cool the warm pool?

Moritz Günther, Hauke Schmidt, Claudia Timmreck, and Matthew Toohey

Viewed

Total article views: 6,837 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
4,174 2,417 246 6,837 235 352
  • HTML: 4,174
  • PDF: 2,417
  • XML: 246
  • Total: 6,837
  • BibTeX: 235
  • EndNote: 352
Views and downloads (calculated since 20 Feb 2024)
Cumulative views and downloads (calculated since 20 Feb 2024)

Viewed (geographical distribution)

Total article views: 6,837 (including HTML, PDF, and XML) Thereof 6,730 with geography defined and 107 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 08 Aug 2026
Download
Short summary
Stratospheric aerosol has been shown to cause pronounced cooling in the tropical Indian and western Pacific oceans. Using a climate model, we show that this arises from enhanced meridional energy export via the stratosphere. The aerosol causes stratospheric heating and thus an acceleration of the Brewer–Dobson circulation that accomplishes this transport. Our findings highlight the importance of circulation adjustments and surface perspectives on forcing for understanding temperature responses.
Read more
Share
Altmetrics
Final-revised paper
Preprint