Articles | Volume 20, issue 6
https://doi.org/10.5194/cp-20-1269-2024
https://doi.org/10.5194/cp-20-1269-2024
Research article
 | 
11 Jun 2024
Research article |  | 11 Jun 2024

Local summer temperature changes over the past 440 ka revealed by the total air content in the Antarctic EPICA Dome C ice core

Dominique Raynaud, Qiuzhen Yin, Emilie Capron, Zhipeng Wu, Frédéric Parrenin, André Berger, and Vladimir Lipenkov

Viewed

Total article views: 1,203 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
868 285 50 1,203 36 31 40
  • HTML: 868
  • PDF: 285
  • XML: 50
  • Total: 1,203
  • Supplement: 36
  • BibTeX: 31
  • EndNote: 40
Views and downloads (calculated since 17 Oct 2023)
Cumulative views and downloads (calculated since 17 Oct 2023)

Viewed (geographical distribution)

Total article views: 1,203 (including HTML, PDF, and XML) Thereof 1,173 with geography defined and 30 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 13 Dec 2024
Download
Short summary
There is a lack of reconstructions from Antarctic ice cores of the temperature during the summer, a critical season in terms of solar energy received, preventing a good understanding of the link between Antarctic past climate and astronomically induced insolation changes. Here, the variations in total air content in an Antarctic ice core are found to be correlated to local summer temperatures simulated with a climate model. This tracer can be used to reconstruct past local summer temperatures.