Articles | Volume 13, issue 8
https://doi.org/10.5194/cp-13-1037-2017
https://doi.org/10.5194/cp-13-1037-2017
Research article
 | 
18 Aug 2017
Research article |  | 18 Aug 2017

Atmospheric circulation and hydroclimate impacts of alternative warming scenarios for the Eocene

Henrik Carlson and Rodrigo Caballero

Viewed

Total article views: 2,948 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,778 980 190 2,948 246 134 188
  • HTML: 1,778
  • PDF: 980
  • XML: 190
  • Total: 2,948
  • Supplement: 246
  • BibTeX: 134
  • EndNote: 188
Views and downloads (calculated since 21 Feb 2017)
Cumulative views and downloads (calculated since 21 Feb 2017)

Viewed (geographical distribution)

Total article views: 2,948 (including HTML, PDF, and XML) Thereof 2,843 with geography defined and 105 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (preprint)

Latest update: 08 Nov 2024
Download
Short summary
Climate models are able to simulate the surface temperature of the early Eocene as reconstructed from paleoclimatology data, but only by using extremely high CO2 concentrations or clouds that are more transparent to solar radiation. We explore the potential for distinguishing among these two forcing agents via their impact on regional climate. Better constraining the radiative forcing that led to Eocene warmth has important implications for understanding Earth's climate sensitivity.