Articles | Volume 20, issue 9
https://doi.org/10.5194/cp-20-2055-2024
https://doi.org/10.5194/cp-20-2055-2024
Research article
 | 
20 Sep 2024
Research article |  | 20 Sep 2024

Glacial–interglacial Circumpolar Deep Water temperatures during the last 800 000 years: estimates from a synthesis of bottom water temperature reconstructions

David M. Chandler and Petra M. Langebroek

Viewed

Total article views: 1,676 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,145 332 199 1,676 39 41
  • HTML: 1,145
  • PDF: 332
  • XML: 199
  • Total: 1,676
  • BibTeX: 39
  • EndNote: 41
Views and downloads (calculated since 09 May 2023)
Cumulative views and downloads (calculated since 09 May 2023)

Viewed (geographical distribution)

Total article views: 1,676 (including HTML, PDF, and XML) Thereof 1,597 with geography defined and 79 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 13 Dec 2024
Download
Short summary
Sea level rise and global climate change caused by ice melt in Antarctica represent a puzzle of feedbacks between the climate, ocean, and ice sheets over tens to thousands of years. Antarctic Ice Sheet melting is caused mainly by warm deep water from the Southern Ocean. Here, we analyse close relationships between deep water temperatures and global climate over the last 800 000 years. This knowledge can help us to better understand how climate and sea level are likely to change in the future.