Articles | Volume 17, issue 2
https://doi.org/10.5194/cp-17-843-2021
https://doi.org/10.5194/cp-17-843-2021
Research article
 | Highlight paper
 | 
14 Apr 2021
Research article | Highlight paper |  | 14 Apr 2021

Snapshots of mean ocean temperature over the last 700 000 years using noble gases in the EPICA Dome C ice core

Marcel Haeberli, Daniel Baggenstos, Jochen Schmitt, Markus Grimmer, Adrien Michel, Thomas Kellerhals, and Hubertus Fischer

Viewed

Total article views: 6,467 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
5,223 1,157 87 6,467 81 102
  • HTML: 5,223
  • PDF: 1,157
  • XML: 87
  • Total: 6,467
  • BibTeX: 81
  • EndNote: 102
Views and downloads (calculated since 08 Oct 2020)
Cumulative views and downloads (calculated since 08 Oct 2020)

Viewed (geographical distribution)

Total article views: 6,467 (including HTML, PDF, and XML) Thereof 5,945 with geography defined and 522 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 23 Nov 2024
Download
Short summary
Using the temperature-dependent solubility of noble gases in ocean water, we reconstruct global mean ocean temperature (MOT) over the last 700 kyr using noble gas ratios in air enclosed in polar ice cores. Our record shows that glacial MOT was about 3 °C cooler compared to the Holocene. Interglacials before 450 kyr ago were characterized by about 1.5 °C lower MOT than the Holocene. In addition, some interglacials show transient maxima in ocean temperature related to changes in ocean circulation.