Articles | Volume 14, issue 2
https://doi.org/10.5194/esd-14-345-2023
https://doi.org/10.5194/esd-14-345-2023
Research article
 | 
21 Mar 2023
Research article |  | 21 Mar 2023

The implications of maintaining Earth's hemispheric albedo symmetry for shortwave radiative feedbacks

Aiden R. Jönsson and Frida A.-M. Bender

Viewed

Total article views: 2,827 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,353 424 50 2,827 88 45 31
  • HTML: 2,353
  • PDF: 424
  • XML: 50
  • Total: 2,827
  • Supplement: 88
  • BibTeX: 45
  • EndNote: 31
Views and downloads (calculated since 29 Aug 2022)
Cumulative views and downloads (calculated since 29 Aug 2022)

Viewed (geographical distribution)

Total article views: 2,827 (including HTML, PDF, and XML) Thereof 2,756 with geography defined and 71 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 25 Apr 2024
Download
Short summary
The Earth has nearly the same mean albedo in both hemispheres, a feature not well replicated by climate models. Global warming causes changes in surface and cloud properties that affect albedo and that feed back into the warming. We show that models predict more darkening due to ice loss in the Northern than in the Southern Hemisphere in response to increasing CO2 concentrations. This is, to varying degrees, counteracted by changes in cloud cover, with implications for cloud feedback on climate.
Altmetrics
Final-revised paper
Preprint