Articles | Volume 18, issue 4
https://doi.org/10.5194/cp-18-759-2022
https://doi.org/10.5194/cp-18-759-2022
Research article
 | 
12 Apr 2022
Research article |  | 12 Apr 2022

Climate and ocean circulation in the aftermath of a Marinoan snowball Earth

Lennart Ramme and Jochem Marotzke

Viewed

Total article views: 2,456 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,763 624 69 2,456 53 54
  • HTML: 1,763
  • PDF: 624
  • XML: 69
  • Total: 2,456
  • BibTeX: 53
  • EndNote: 54
Views and downloads (calculated since 20 Dec 2021)
Cumulative views and downloads (calculated since 20 Dec 2021)

Viewed (geographical distribution)

Total article views: 2,456 (including HTML, PDF, and XML) Thereof 2,303 with geography defined and 153 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 04 Nov 2024
Download
Short summary
After the Marinoan snowball Earth, the climate warmed rapidly due to enhanced greenhouse conditions, and the freshwater inflow of melting glaciers caused a strong stratification of the ocean. Our climate simulations reveal a potentially only moderate global temperature increase and a break-up of the stratification within just a few thousand years. The findings give insights into the environmental conditions relevant for the geological and biological evolution during that time.