Articles | Volume 23, issue 12
https://doi.org/10.5194/acp-23-6743-2023
https://doi.org/10.5194/acp-23-6743-2023
Research article
 | 
20 Jun 2023
Research article |  | 20 Jun 2023

Change from aerosol-driven to cloud-feedback-driven trend in short-wave radiative flux over the North Atlantic

Daniel P. Grosvenor and Kenneth S. Carslaw

Viewed

Total article views: 2,489 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,943 496 50 2,489 37 35
  • HTML: 1,943
  • PDF: 496
  • XML: 50
  • Total: 2,489
  • BibTeX: 37
  • EndNote: 35
Views and downloads (calculated since 26 Aug 2022)
Cumulative views and downloads (calculated since 26 Aug 2022)

Viewed (geographical distribution)

Total article views: 2,489 (including HTML, PDF, and XML) Thereof 2,483 with geography defined and 6 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 23 Dec 2024
Download
Short summary
We determine what causes long-term trends in short-wave (SW) radiative fluxes in two climate models. A positive trend occurs between 1850 and 1970 (increasing SW reflection) and a negative trend between 1970 and 2014; the pre-1970 positive trend is mainly driven by an increase in cloud droplet number concentrations due to increases in aerosol, and the 1970–2014 trend is driven by a decrease in cloud fraction, which we attribute to changes in clouds caused by greenhouse gas-induced warming.
Altmetrics
Final-revised paper
Preprint