Articles | Volume 20, issue 9
https://doi.org/10.5194/cp-20-1989-2024
https://doi.org/10.5194/cp-20-1989-2024
Research article
 | Highlight paper
 | 
12 Sep 2024
Research article | Highlight paper |  | 12 Sep 2024

Can we reliably reconstruct the mid-Pliocene Warm Period with sparse data and uncertain models?

James D. Annan, Julia C. Hargreaves, Thorsten Mauritsen, Erin McClymont, and Sze Ling Ho

Viewed

Total article views: 810 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
592 167 51 810 37 40
  • HTML: 592
  • PDF: 167
  • XML: 51
  • Total: 810
  • BibTeX: 37
  • EndNote: 40
Views and downloads (calculated since 11 Sep 2023)
Cumulative views and downloads (calculated since 11 Sep 2023)

Viewed (geographical distribution)

Total article views: 810 (including HTML, PDF, and XML) Thereof 795 with geography defined and 15 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 12 Sep 2024
Download
Co-editor-in-chief
This study presents an interesting attempt to reconstruct global surface temperature by combining sparse SST proxy data and PlioMIP2 simulations using a state-of-the-art data assimilation framework. The work highlights the potential of this method for providing key insights into past warming patterns, and will serve as a good starting point for future investigations.
Short summary
We have created a new global surface temperature reconstruction of the climate of the mid-Pliocene Warm Period, representing the period roughly 3.2 million years before the present day. We estimate that the globally averaged mean temperature was around 3.9 °C warmer than it was in pre-industrial times, but there is significant uncertainty in this value.