Articles | Volume 17, issue 5
https://doi.org/10.5194/cp-17-2223-2021
https://doi.org/10.5194/cp-17-2223-2021
Research article
 | 
21 Oct 2021
Research article |  | 21 Oct 2021

Data-constrained assessment of ocean circulation changes since the middle Miocene in an Earth system model

Katherine A. Crichton, Andy Ridgwell, Daniel J. Lunt, Alex Farnsworth, and Paul N. Pearson

Viewed

Total article views: 4,978 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,108 1,720 150 4,978 501 168 187
  • HTML: 3,108
  • PDF: 1,720
  • XML: 150
  • Total: 4,978
  • Supplement: 501
  • BibTeX: 168
  • EndNote: 187
Views and downloads (calculated since 14 Jan 2020)
Cumulative views and downloads (calculated since 14 Jan 2020)

Viewed (geographical distribution)

Total article views: 4,978 (including HTML, PDF, and XML) Thereof 4,736 with geography defined and 242 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 06 May 2026
Download
Short summary
The middle Miocene (15 Ma) was a period of global warmth up to 8 °C warmer than present. We investigate changes in ocean circulation and heat distribution since the middle Miocene and the cooling to the present using the cGENIE Earth system model. We create seven time slices at ~2.5 Myr intervals, constrained with paleo-proxy data, showing a progressive reduction in atmospheric CO2 and a strengthening of the Atlantic Meridional Overturning Circulation.
Share